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<title>GeoScience e-Journals</title>
<description>Online publications grouped under the aegis &quot;Geoscience e-Journals&quot; incorporate those peer-reviewed electronic journals dedicated to open access publishing in the field of Earth Sciences (geochemistry, geophysics, paleontology, regional geology, stratigraphy, geography, etc.), that is those e-journals that permit free online access to all or at least a major part of their current issue and/or archives.</description>
<link>http://paleopolis.rediris.es/geosciences/</link>
<pubDate>Mon, 20 Mar 2017 10:22:51 GMT</pubDate>
<image>
<url>http://paleopolis.rediris.es/geosciences/geosciences.gif</url>
<title>GeoScience e-Journals</title>
<link>http://paleopolis.rediris.es/geosciences/</link>
<width>132</width>
<height>196</height>
<description>RSS Feed provided by GeoScience e-Journals. Click to visit.</description>
</image>
<language>en</language>
<webMaster>carnets@univ-brest.fr</webMaster>

<item>
<title>Oceanologia No. 59(2)/2017</title>
<link>http://iopan.gda.pl/oceanologia/59_2.html</link>
<description>
* Epibenthic diversity and productivity on a heavily trawled Barents Sea bank (Troms&#248;flaket).- K&#281;dra Monika,  
Renaud Paul E., Andrade Hector &#060;br /&#062;
* Wave-induced bottom shear stress estimation in shallow water exemplified by using deep water wind statistics.- Myrhaug Dag &#060;br /&#062;
* Possible means of overcoming sedimentation by motile sea-picoplankton cells.-  Pundyak Oleh&#060;br /&#062;
* On the buoyant sub-surface salinity maxima in the Gulf of Riga.- Liblik Taavi, Skudra Maris, Lips Urmas &#060;br /&#062;
* Morphometric variations in white seabream Diplodus sargus (Linneus, 1758) populations along the Tunisian coast.-  
Kaou&#232;che Myriam, Bahri-Sfar Lilia, Hammami Ibtissem, Hassine Oum Kalthoum Ben &#060;br /&#062;
* Current observations from a looking down vertical V-ADCP: interaction with winds and tide? The case of Giglio Island (Tyrrhenian Sea, Italy).-  Cutroneoa Laura, Ferrettia Gabriele,  Scafidia Davide, Ardizzoneb Gian Domenico, Vaggea Greta,  Capello Marco&#060;br /&#062;
* Spatio-temporal variability of the phytoplankton biomass in the Levantine basin between 2002 and 2015 using MODIS products.- El Hourany Roy, Fadel Ali, Gemayel Elissar, Abboud-Abi Saab Marie, Faour Ghaleb &#060;br /&#062;
* Toward downscaling oceanic hydrodynamics &#8211; suitability of a high-resolution OGCM for describing regional ocean variability in the South China Sea.- Zhang Meng, von Storch Hans &#060;br /&#062;
* Microorganisms associated with charophytes under different salinity conditions.- Katar&#382;yt&#279;  Marija, Vai&#269;i&#363;t&#279; Diana, Bu&#269;as Martynas, Gyrait&#279; Greta, Petkuvien&#279; Jolita &#060;br /&#062;
* Oceanographic observations in the Nordic Sea and Fram Strait in 2016 under the IO PAN long-term monitoring program AREX.- Walczowski Waldemar,  Beszczy&#324;ska-M&#246;ller Agnieszka, Wieczorek Piotr, Merchel Ma&#322;gorzata, Grynczel Agata </description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Mon, 20 Mar 2017 10:22:51 GMT</pubDate>
</item>
<item>
<title>Oceanologia No. 59(1)/2017</title>
<link>http://iopan.gda.pl/oceanologia/59_1.html</link>
<description>
* Tracking trends in eutrophication based on pigments in recent coastal sediments.-  Szymczak-&#379;y&#322;a Ma&#322;gorzata, Krajewska Magdalena,  Winogradow Aleksandra, Agata Zaborska,  Breedveld Gijs D.,  Kowalewska Gra&#380;yna&#060;br /&#062;
* Application of Dean's curve to investigation of a long-term evolution of the southern Baltic multi-bar shore profile.- Cerkowniak Grzegorz R., Ostrowski Rafa&#322;,  
Pruszak Zbigniew&#060;br /&#062;
* The impact of tides and waves on near-surface suspended sediment concentrations in the English Channel.-  Guillou  
Nicolas, Rivier Aur&#233;lie, Chapalain  Georges,  Gohin Francis&#060;br /&#062;
* Characteristics and inter-annual changes in temperature, salinity and density distribution in the Gulf of Riga: .-  
Skudra Maris, Lips  Urmas &#060;br /&#062;
* Effect of physicochemical parameters on zooplankton in the brackish, coastal Vistula Lagoon:.- Ewa Paturej, Agnieszka Gutkowska, Jacek Kosza&#322;ka, Magdalena Bowszys&#060;br /&#062;
* Testing the performance of empirical remote sensing algorithms in the Baltic Sea waters with modelled and in situ reflectance data.- Ligi Martin, Kutser Tiit,  Kallio Kari,  Attila Jenni,  Koponen Sampsa,  Paavel Birgot,  
Soomets Tuuli, Reinart Anu &#060;br /&#062;
*  Processes and factors influencing the through-flow of new deepwater in the Bornholm Basin.-  Stigebrandt Anders&#060;br /&#062;
* New data on benthic Naididae (Annelida, Clitellata) in Polish brackish waters.- Marszewska Lena, Dumnicka El&#380;bieta,  Normant-Saremba Monika&#060;br /&#062;
* The killer shrimp <i>Dikerogammarus villosus</i> (Crustacea, Amphipoda) invades Lithuanian waters, South-Eastern Baltic Sea.- &#352;idagyt&#279; Egl&#279;,  
Solovjova Sabina, &#352;niauk&#353;tait&#279; Vikt&#279;, &#352;iaulys Andrius,  Olenin Sergej,  Arba&#269;iauskas K&#281;stutis</description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Thu, 12 Jan 2017 13:42:04 GMT</pubDate>
</item>


<item>
  <title>Oceanologia No. 58(4)/2016</title>
  <link>http://iopan.gda.pl/oceanologia/58_4.html</link>
  <description>
* Satellite observations of seasonal and regional variability of particulate organic carbon concentration in the Barents Sea.- Stramska Ma&#322;gorzata, Bia&#322;ogrodzka Jagoda &#060;br /&#062;
* Detecting imprints of atmospheric waves in the Bering Sea with MODIS data.- Evdoshenko Marina &#060;br /&#062;
* The effect of temperature and nitrogen deprivation on cell morphology and physiology of Symbiodinium.- Buntora Pasaribu, Yu-Si Li, I-Ping Lin, Kwee Siong Tew, Jason T.C. Tzen, Yue Ken Liao, Chii-Shiarng Chen, Pei-Luen Jiang&#060;br /&#062;
* Narrowband shortwave minima in spectra of backscattered light from the sea obtained from ocean color scanners as a remote indication of algal blooms.-  Karabashev G.S., Evdoshenko M.A. &#060;br /&#062;
* Size-selective microzooplankton grazing on the phytoplankton in the Curonian Lagoon (SE Baltic Sea).- Grinien&#279; Evelina, &#352;ul&#269;ius Sigitas, Kuosa Harri &#060;br /&#062;
* Eutrophication influence on phytoplankton community composition in three bays on the eastern Adriatic coast.- Bu&#382;an&#269;i&#263; Mia, Nin&#269;evi&#263; Gladan &#381;ivana,  Marasovi&#263; Ivona, Ku&#353;pili&#263; Grozdan, Grbec Branka &#060;br /&#062;
* Performance of operational satellite bio-optical algorithms in different water types in southeastern Arabian Sea.- Minu P.,Lotliker  Aneesh A., Shaju  S.S., Muhamed Ashraf P.,  Srinivasa Kumar T.,  Meenakumari B.&#060;br /&#062;
*  UV filters are an environmental threat in the Gulf of Mexico: a case study of Texas coastal zones.- Sharifan Hamidreza, Klein David,  Morse Audra N.&#060;br /&#062;
*  Colonies of Gyrosigma eximium: a new phenomenon in Arctic tidal flats.- Wiktor J&#243;zef, Tatarek Agnieszka,  W&#281;s&#322;awski Jan M., Kotwicki Lech, Poulin Michel &#060;br /&#062;
* How do differences in the nutritional and hydrological background influence phytoplankton in the Vistula Lagoon during a hot summer day?.-  Kruk Marek, Jaworska Bo&#380;ena,  Jab&#322;o&#324;ska-Barna  Izabela,  Rychter  Agata</description>
  <category>Journal</category>
  <author>sabina@iopan.gda.pl</author>
  <pubDate>Tue, 18 Oct 2016 12:33:37 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 58(3)/2016</title>
<link>http://iopan.gda.pl/oceanologia/58_3.html</link>
<description>
* New simple statistical formulas for estimating surface concentrations of suspended particulate matter (SPM) and particulate organic carbon (POC) from remote-sensing reflectance in the southern Baltic Sea.- Wo&#378;niak S&#322;awomir B.,  Darecki Miros&#322;aw, Zab&#322;ocka Monika, Burska Dorota, Dera Jerzy &#060;br /&#062;
* The impact of surface currents and sea level on the wave field evolution during St. Jude storm in the eastern Baltic Sea.-  Viitak Marili, Maljutenko Ilja , Alari Victor , Suursaar &#220;lo,  Rikka  Sander,  Lagema Priidika&#060;br /&#062;
* Fisher&#8211;Shannon analysis of the time variability of remotely sensed sea surface temperature at the Brazil&#8211;Malvinas Confluence.- Pierini Jorge O.,  Lovallo Michele, G&#243;mez Eduardo A., Telesca Luciano &#060;br /&#062;
* First occurrence of thinlip grey mullet, Liza ramada (Risso, 1827) in the Odra River estuary (NW Poland): genetic identification.-  Panicz Remigiusz, Keszka S&#322;awomir &#060;br /&#062;
* Phytoplankton pigments and functional community structure in relation to environmental factors in the Pearl River Estuary.-  Chao Chai, Tao Jiang, Jingyi Cen, Wei Ge, Songhui Lu&#060;br /&#062;
* Distribution and invasiveness of a colonial ascidian, Didemnum psammathodes, along the southern Indian coastal water.- Jaffar H. Abdul, Akram  A. Soban, Arshan M.L. Kaleem, Sivakumar  V., Tamilselvi M. &#060;br /&#062;
* Determination of antibiotic residues in southern Baltic Sea sediments using tandem solid-phase extraction and liquid chromatography coupled with tandem mass spectrometry.- Siedlewicz Grzegorz, Borecka Marta, Bia&#322;k-Bieli&#324;ska Anna, Sikora Kinga, Stepnowski Piotr, Pazdro Ksenia &#060;br /&#062;
*  Position, swimming direction and group size of fin whales (Balaenoptera physalus) in the presence of a fast-ferry in the Bay of Biscay.-  Aniceto Ana S.,  Carroll JoLynn,  Tetley Michael J., van Oosterhout Cock &#060;br /&#062;
*  The inflow in the Baltic Proper as recorded in January&#8211;February 2015.- Daniel Rak</description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Tue, 05 Jul 2016 09:16:33 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 58(2)/2016</title>
<link>http://iopan.gda.pl/oceanologia/58_2.html</link>
<description>
* On the nonlinear internal waves propagating in an inhomogeneous shallow sea.
- Massel Stanis&#322;aw R. &#060;br /&#062;
* An integrated wave modelling framework for extreme and rare events for climate change in coastal areas &#8211; the case of Rethymno, Crete.
- Tsoukala Vasiliki K.,  Chondros Michalis, Kapelonis Zacharias G., Martzikos Nikolaos, Lykou Archodia, Belibassakis Kostas,  Makropoulos Christos&#060;br /&#062;
* Curonian Lagoon drainage basin modelling and assessment of climate change impact.
- &#268;erkasova Natalja, Ert&#252;rk Ali,  Zemlys Petras,
Denisov Vitalij, Umgiesser Georg &#060;br /&#062;
* Modeling the buoyancy-driven Black Sea Water outflow into the North Aegean Sea.-  Kokkos Nikolaos, Sylaios Georgios &#060;br /&#062;
* Spatial distribution and diet of larval snailfishes (Liparis fabricii, Liparis gibbus, Liparis tunicatus) in the Canadian Beaufort Sea.
-  Walkusz Wojciech,  Paulic Joclyn E., Wong Sally,
Kwasniewski Slawomir, Papst Michael H., Reist James D.&#060;br /&#062;
* Scale-dependent environmental control of mesozooplankton community structure in three aquaculture subtropical bays of China.
- Dong Sun, Zhensheng Liu, Chunsheng Wang&#060;br /&#062;
* Assessment of recent and chalcolithic period environmental pollution using Mytilus galloprovincialis Lamarck, 1819 from Yarimburgaz Cave, the northern Marmara Sea and Bosphorus coasts.
- Barut Ipek F., Meri&#231; Engin, Yoke&#351; M. Baki &#060;br /&#062;
* Addendum to &#8220;Sea spray aerosol flux estimation based on long-term variation of wave statistics&#8221;: estimation based on long-term variation of wind statistics.
-  Myrhaug Dag, Hong Wang,  Holmedal Lars Erik&#060;br /&#062;
* The quagga mussel (Dreissena rostriformis bugensis Andrusov, 1897) &#8211; another Ponto-Caspian dreissenid bivalve in the southern Baltic catchment: the first record from the Szczecin Lagoon.
-  Wo&#378;niczka Adam, Wawrzyniak-Wydrowska Brygida,
Radziejewska Teresa,  Skrzypacz Anna</description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Mon, 18 Apr 2016 12:33:05 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 58(1)/2016</title>
<link>http://iopan.gda.pl/oceanologia/58_1.html</link>
<description>
* Significant increase of aerosol number concentrations in air masses crossing a densely trafficked sea area .- Kecorius Simonas, Kivek&#228;s Niku,  Kristensson Adam, Tuch Thomas, Covert David S., Birmili Wolfram,  Lihavainen Heikki,  Antti-Pekka Hyv&#228;rinen, Martinsson Johan, Sporre Moa K., Swietlicki Erik,  Wiedensohler Alfred, Ulevicius Vidmantas&#060;br /&#062;
* Impact of wild forest fires in Eastern Europe on aerosol composition and particle optical properties.- Zielinski Tymon, Petelski Tomasz, Strzalkowska Agata, Pakszys Paulina,  Makuch Przemyslaw&#060;br /&#062;
* Thermoelastic surface properties of seawater in coastal areas of the Baltic Sea.- Boniewicz-Szmyt Katarzyna, Pogorzelski Stanis&#322;aw J. &#060;br /&#062;
* Influence of dissolved organic nitrogen on surface waters.- Czerwionka Krzysztof &#060;br /&#062;
* Baltic herring prey selectively on older copepodites of Eurytemora affinis and Limnocalanus macrurus in the Gulf of Riga.- Livd&#257;ne L&#299;na, Putnis Ivars, Rubene Gunta, Elferts Didzis,  Ikauniece Anda&#060;br /&#062;
The first report on the establishment and spread of the alien clam Rangia cuneata (Mactridae) in the Polish part of the Vistula Lagoon (southern Baltic).- Warzocha Jan, Szymanek  Lena,  Witalis Bartos, Wodzinowski Tycjan </description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Tue, 12 Jan 2016 10:11:33 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 57(4)/2015</title>
<link>http://iopan.gda.pl/oceanologia/57_4.html</link>
<description>
* Sea-level change and projected future flooding along the Egyptian Mediterranean coast.- Shaltout Mohamed, Tonbol Kareem, Omstedt Anders &#060;br /&#062;
* Numerical study of wave transmission over double submerged breakwaters using non-hydrostatic wave model.- Liang Bingchen, Wu Guoxiang, Liu Fushun, Fan Hairong,  Li Huajun&#060;br /&#062;
* Tidal currents in the western Svalbard Fjords.- Kowalik Zygmunt, Marchenko Aleksey, Brazhnikov Dmitry,  Marchenko Nataly&#060;br /&#062;
* Response patterns of phytoplankton growth to variations in resuspension in the German Bight revealed by daily MERIS data in 2003 and 2004.- Su  Jian, Tian Tian, Krasemann Hajo, Schartau Markus, Wirtz  Kai&#060;br /&#062;
* Context-dependent consequences of&#060;i/&#062; Marenzelleria&#060;/i/&#062; spp. (Spionidae: Polychaeta) invasion for nutrient cycling in the Northern Baltic Sea.- Maximov Alexey,  Bonsdorff Erik, Eremina Tatjana,  Kauppi Laura, Norkko Alf,  Norkko Joanna&#060;br /&#062;
* Ocean acidification and marine microorganisms: responses and consequences.- Das Surajit, Mangwani Neelam &#060;br /&#062;
*  Seasonal assessment of biological indices, bioaccumulation and bioavailability of heavy metals in mussels &#060;i/&#062;Mytilus galloprovincialis&#060;/i/&#062; from Algerian west coast, applied to environmental monitoring.- Rouane-Hacene Omar, Boutiba Zitouni, Belhaouari Benkhedda, Guibbolini-Sabatier Marielle E.,  Francour Patrice, Risso-de Faverney  Christine &#060;br /&#062;
* Characteristics of the spring/summer production in the Mecklenburg Bight (Baltic Sea) as revealed by long-term pCO&#060;sub&#062;2&#060;/sub&#062; data.- Schneider B., Buecker S., Kaitala S., Maunula P., Wasmund N.
</description>
<category>Journal</category>
<author>editor@iopan.gda.pl</author>
<pubDate>Tue, 20 Oct 2015 01:00:00 GMT</pubDate>
</item>

<item>
<title>Bulletin of Geosciences, Volume 90, Issue 3 (2015)</title>
<link>http://www.geology.cz/bulletin/contents/2015/vol90no3</link>
<description>* The morphology and affinities of Skania fragilis (Arthropoda) from the middle Cambrian Burgess Shale.- Legg DA&#060;br /&#062;
* Earliest Silurian graptolites from Kalpin, western Tarim, Xinjiang, China.- Wang W, Muir LA, Chen X &#038; Tang P&#060;br /&#062;
* The oldest brachymetopid trilobite record from the European peri-Gondwana.- Pereira S, Marques da Silva C, Pires M &#038; Sa AA&#060;br /&#062;
* Micromammal faunas from the Mio-Pliocene boundary in the Alcoy Basin (SE Spain): biostratigraphical and palaeoecological inferences.- Mansino S, Fierro I, Montoya P &#038; Ruiz -Sanchez FJ&#060;br /&#062;
* Brachiopods and crinoids from the Middle-Upper Devonian boundary beds in the Darende-G&#252;r&#252;n and Van-Zincirkiran areas (Eastern Taurus, Turkey).- Gourvennec R &#038; Hosgor I&#060;br /&#062;
* Mesozoic-Cenozoic crustaceans preserved within echinoid tests and bivalve shells.- Gasparic R, Fraaije RHB,  Van Bakel BWM, Jagt JWM &#038; Skupien P&#060;br /&#062;
* Palaeoecology of Valletia antiqua Favre in Joukowsky &amp; Favre, 1913 (Bivalvia, Hippuritida, Diceratidae); with comments on the taxonomy and distribution of the genus Valletia.- Schneider S &#038; Skupien P&#060;br /&#062;
* Taxonomy and palaeoecology of a decapod crustacean assemblage from the Oxfordian of Stranska skala (Southern Moravia, Czech Republic).- Hyzny M, Starzyk N, Robins CM &#038; Kocova Veselska M 2015&#060;br /&#062;
* Sponge growth on the Cenomanian carbonate shelves of the Carpathian Basin: a record from spicule-rich turbidites.- B&#261;, k M, Gorny Z, B&#261; &#038; k K&#060;br /&#062;
* Petrophysical and geochemical signature of the Hangenberg Events: an integrated stratigraphy of the Devonian-Carboniferous boundary interval in the Northern Rhenish Massif (Avalonia, Germany).- Kumpan T, Babek O, Kalvoda J, Matys Grygar T, Fryda J, Becker  RT &#038; Hartenfels S&#060;br /&#062;
* Palaeoenvironmental evaluation of Cainozoic plant assemblages from the Bohemian Massif (Czech Republic) and adjacent Germany.- Teodoridis V &#038; Kvacek Z&#060;br /&#062;
* Pennsylvanian fossil flora from the Velebit Mountains and Lika region (SW Croatia).- Cleal CJ, Tenchov YG, Sremac J, Derek T &#038; Japundzic J</description>
<category>Journal</category>
<author>admin.bulletin@geology.cz</author>
<pubDate>Wed, 30 Sep 2015 01:00:00 GMT</pubDate>
</item>


<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 13</title>
 <link>http://paleopolis.rediris.es/cg/1513/</link>
 <description>Josep A. Moreno-Bedmar &#038; Keith P. Minor.- Review of some Aptian ammonites collected by Gaston Astre in Lleida Province, Catalonia, Spain.- We study the three best preserved ammonites collected by Astre in 1924-1925 in Lleida Province, Catalonia, Spain, in order to assess their taxonomic assignment. We also include images of these ammonoids since they were not illustrated in Astre's original 1934 work. This taxonomic review allows us to identify these lower Aptian ammonites as Pseudohaploceras liptoviense, Deshayesites sp. and Dufrenoyia sp.- Handle-ID: http://hdl.handle.net/2042/56911</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Thu, 06 Aug 2015 17:01:03 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 12</title>
 <link>http://paleopolis.rediris.es/cg/1512/</link>
 <description>Badre Essafraoui, Serge Ferry, Dani&#232;le Grosh&#233;ny, Nourrisaid I&#231;ame, Hassan El Aouli, Moussa Masrour, Luc G. Bulot, Yves G&#233;raud &#038; Mohamed Aoutem.- Sequence stratigraphic architecture of marine to fluvial deposits across a passive margin (Cenomanian, Atlantic margin, Morocco, Agadir transect).- Seven sections, covering the upper Albian to lowermost Turonian, have been correlated from full-marine to continental-dominated deposits across a passive margin, along a transect 425 km long, from the present-day Atlantic coast to the &quot;Pre-African Trough&quot; between the Anti-Atlas and the High-Atlas. The thickness of the Cenomanian succession changes from around 500 metres in the fully marine sections to 250 metres in mostly continental facies in the western High-Atlas, about 150 km updip, to a few tens of metres in the Bou Tazoult area. The strata thicken again eastwards into the Pre-African Trough where they can be traced without major facies changes to the Kem Kem embayment and to the Bechar area in Algeria. Over all this eastern area, continental facies are overlain by the fully-marine shallow-water deposits of the Cenomanian-Turonian boundary interval. A first major conclusion is that fluvial aggradation in high-frequency transgressive-regressive sequences is coeval with the seaward-shift of the shoreline, in accordance with the genetic sequence stratigraphic model of Galloway (1989). Both the flatness of the depositional profile and the corresponding very low energy of the marine environment during the transgressions account for the blanket of red continental clays on top of marine facies in updip depositional sequences, which is then preserved under the marine transgressive surface of the next sequence. A second major conclusion is that the high-frequency transgressive-regressive (T-R) sequences do not look like classical parasequences bounded by transgression surfaces. They usually exhibit a surface created by a sea-level fall within the regressive half-cycle. This is interpreted in the following way: regressions did not operate through a regular seaward-shift of the shoreline, but through stepped sea-level falls. The very low slope of the depositional ramp is thought to have enhanced the sequence stratigraphic record of such stepped regressions. Short-term, high-frequency sequences are organized into medium-frequency T-R sequences (seven in the Cenomanian) which show an overall aggrading and slowly retrograding pattern along the whole transect. Comparisons with other basins show that medium-frequency sequences do not fit the third-order depositional sequences described elsewhere, casting doubts about a eustatic mechanism for their deposition.- Handle-ID: http://hdl.handle.net/2042/56909</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Thu, 06 Aug 2015 16:58:05 GMT</pubDate>
</item>



<item>
  <title>Oceanologia No. 57(3)/2015</title>
  <link>http://iopan.gda.pl/oceanologia/57_3.html</link>
  <description>* Spatial and temporal variability of sea surface temperature in the Baltic Sea based on 32-years (1982&#8211;2013) of satellite data.- Stramska Malgorzata, Bia&#322;ogrodzka Jagoda &#060;br /&#062;* Heavy metals contamination and distribution of benthic foraminifera from the Red Sea coastal area, Jeddah, Saudi Arabia.- Youssef Mohamed &#060;br /&#062;* Seasonal changes in phytoplankton on the north-eastern shelf of Kangaroo Island (South Australia) in 2012 and 2013.- Balzano Sergio,  Ellis Amanda V.,  Le Lan Charlotte, Leterme Sophie C. &#060;br /&#062;* Impact of Chinese mitten crab &#060;i&#062;Eriocheir sinensis&#060;/i/&#062; on blue mussel &#060;i&#062;Mytilus edulis trossulus&#060;/i&#062;  &#8211; laboratory studies of claw strength, handling behavior, consumption rate, and size selective predation.-  W&#243;jcik Dagmara,  Normant Monika,  Dmochowska Barbara, Fowler Amy &#060;br /&#062;* Engineering effect of &#060;i/&#062;Pinna nobilis&#060;/i/&#062; shells on benthic communities.- Rabaoui Lotfi,  Belgacem Walid,  Ben Ismail Dorsaf, Mansour Lamjed, Tlig-Zouari Sabiha &#060;br /&#062;*  Changes in the parasite communities as one of the potential causes of decline in abundance of the three-spined sticklebacks in the Puck Bay.- Morozi&#324;ska-Gogol Jolanta &#060;br /&#062;*  Sea spray aerosol flux estimation based on long-term variation of wave statistics.- Myrhaug Dag,  Wang Hong, Holmedal Lars Erik </description>
  <category>Journal</category>
  <author>editor@iopan.gda.pl</author>
  <pubDate>Tue, 04 Aug 2015 12:36:11 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 11</title>
 <link>http://paleopolis.rediris.es/cg/1511/</link>
 <description>Bruno Granier &#038; Dimas Dias-Brito.- End of a modern geological myth: there are no rudists in Brazil! Paleobiogeographic implications.- Out of the few records of rudists from the Cretaceous strata of the South Atlantic coastal basins only two refer to Brazilian localities. However, petrographic analyses demonstrate that these shells should be assigned to Ostreids or to Pycnodontids rather than to Rudistids. More specifically, the domain considered herein, north of the R&#237;o Grande Rise - Walvis Ridge barrier, was part of the warm-water &quot;tropical&quot; realm, but it was not part of the Mesogean domain because both Rudistids and Orbitolinas are missing. In addition, the scarcity of corals leads us to ascribe the taphonomic assemblage to the Chloralgal facies. Neither generalized hypersalinity or extreme sea-water temperatures seem to account for these biotic peculiarities. Instead, our alternative hypothesis favors the driving role played by oceanic circulation in the dispersal of the benthic organisms.- Handle-ID: http://hdl.handle.net/2042/56880</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Tue, 14 Jul 2015 16:49:00 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 10</title>
 <link>http://paleopolis.rediris.es/cg/1510/</link>
 <description>Jayagopal Madhavaraju, Robert W. Scott, Yong Il Lee, Kunjukrishnan Sathy Bincy, Carlos M. Gonz&#225;lez-Le&#243;n &#038; Sooriamuthu Ramasamy.- Facies, biostratigraphy, diagenesis, and depositional environments of Lower Cretaceous strata, Sierra San Jos&#233; section, Sonora (Mexico).- We used petrofacies analysis, carbon, oxygen and strontium isotope data to interpret the isotopic variations in the carbonate rocks of the Mural Formation of Sonora (Sierra San Jos&#233; section), Mexico. The petrographic study reveals a range of lithofacies from wackestone to packstone. The analyzed limestones show significant negative &#948;18O values (-18.6 to -10.9 VPDB) and &#948;13C values ranging from negative to positive (-2.6 to +2.5&#8240; VPDB). The absence of correlation between &#948;13C and &#948;18O values suggests a primary marine origin for the &#948;13C values of limestones from the Sierra San Jos&#233; section. The limestones have large variations in 87Sr/86Sr values (0.707479 to 0.708790). Higher 87Sr/86Sr ratios in various levels of the studied section suggest that most of the sediments were derived from the Proterozoic basement of the Caborca block during Early Cretaceous time. A decrease in 87Sr/86Sr ratios at certain levels indicates an influx of lesser amounts of radiogenic Sr that could have been caused by contribution of sediments from the Triassic and Jurassic volcanic rocks.- Handle-ID: http://hdl.handle.net/2042/56879</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Tue, 14 Jul 2015 16:46:15 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 09</title>
 <link>http://paleopolis.rediris.es/cg/1509/</link>
 <description>Old&#345;ich Fatka, Petr Budil, Catherine Cr&#244;nier, Jessie Cuvelier, Luk&#225;&#353; Laibl, Thierry Oudoire, Marika Polechov&#225; &#038; Lucie Fatkov&#225;.- Cambrian fossils from the Barrandian area (Czech Republic) stored in the Mus&#233;e d'Histoire Naturelle de Lille.- A complete list of fossils originating from the Cambrian of the Barrandian area and housed in the Mus&#233;e d'Histoire Naturelle de Lille is compiled. The collection includes two agnostids, ten trilobites, one brachiopod and one echinoderm species, all collected at ten outcrops in the Buchava Formation of the Skryje-T&#253;&#345;ovice Basin and most probably also at two outcrops in the Jince Formation of the P&#345;&#237;bram-Jince Basin. A large part of the material was collected by Prof. Charles Barrois and Dr. Louis Doll&#233; (both University of Lille) during the excursion organised before the Ninth International Geological Congress in Vienna in 1903. Other, poorly documented specimens were purchased from the enterprise Krantz towards the end of the 19th century and in the first years of 20th century. The geographic position and stratigraphy of outcrops, from which the material originates, are briefly discussed.- Handle-ID: http://hdl.handle.net/2042/56878</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Tue, 14 Jul 2015 16:24:47 GMT</pubDate>
</item>


<item>
  <title>Oceanologia No. 57(2)/2015</title>
  <link>http://iopan.gda.pl/oceanologia/57_2.html</link>
  <description>
*Barycenter reflected equatorial Pacific sea level structure evolution and its indication of ENSO events.- Wen Luo, Lin Yi, Zhaoyuan Yu, Hui Sun, Linwang Yuan&#060;br /&#062;
*Modelling the water and heat balances of the Mediterranean Sea using a two-basin model and available meteorological, hydrological, and ocean data.- Shaltout Mohamed, Omstedt Anders &#060;br /&#062;
*Variability of currents over the southern slope of the Gulf of Finland.- Suhhova Irina,  Pavelson Juss, Lagemaa Priidik&#060;br /&#062;
*Morpholithodynamical changes of the beach and the nearshore zone under the impact of submerged breakwaters &#8211; a case study (Or&#322;owo Cliff, the Southern Baltic).- Kubowicz-Grajewska Agnieszka&#060;br /&#062;
*Spectrophotometric studies of marine surfactants in the southern Baltic Sea: Violetta Drozdowska, Marek J&#243;zefowicz.- &#060;br /&#062;
*DOC and POC in the southern Baltic Sea. Part II &#8211; Evaluation of factors affecting organic matter concentrations using multivariate statistical methods.- Maciejewska Anna, Pempkowiak Janusz &#060;br /&#062;
*Water type quantification in the Skagerrak, the Kattegat and off the Jutland west coast.- Kristiansen Trond, Aas Eyvind &#060;br /&#062;
*Comparison of PCBs and PAHs levels in European coastal waters using mussels from the Mytilus edulis complex as biomonitors: Production and mortality rates.- Olenycz Micha&#322;, Soko&#322;owski Adam,  Niewi&#324;ska Agnieszka, Wo&#322;owicz Maciej,  Namie&#347;nik Jacek,  Hummel Herman, Jansen Jeroen &#060;br /&#062;
*Deep water masses in the Iceland Basin during the Last Interglacial (MIS 5e): Evidence from benthic foraminiferal data.- Lukashina Nadezhda P.,  Bashirova Leyla D.</description>
  <category>Journal</category>
  <author>sabina@iopan.gda.pl</author>
  <pubDate>Tue, 16 Jun 2015 09:28:33 GMT</pubDate>
</item>


<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 08</title>
 <link>http://paleopolis.rediris.es/cg/1508/</link>
 <description>Miguel Company &#038; Jos&#233; M. Tavera.- Lower Valanginian ammonite biostratigraphy in the Subbetic Domain (Betic Cordillera, southeastern Spain).- A new zonation for the lower Valanginian in the Betic Cordillera is presented. It is based on the study of 16 sections located near Caravaca and Ceheg&#237;n (Region of Murcia). From bottom to top, the following interval zones, defined by the first appearance of the index-species, are distinguished: * &quot;Thurmanniceras&quot; pertransiens Zone, which can be subdivided into two subzones, a lower &quot;Th.&quot; pertransiens Subzone and an upper Vergoliceras salinarium Subzone. The latter is characterized by the disappearance of Olcostephanus drumensis and the appearance of Luppovella superba. * Neocomites neocomiensiformis Zone, also with two subzones, the Baronnites hirsutus Subzone below (characterized by the appearance of &quot;Busnardoites&quot; subcampylotoxus and Olcostephanus guebhardi) and the Valanginites dolioliformis Subzone above (&quot;Busnardoites&quot; campylotoxus is restricted to this subzone). * Karakaschiceras inostranzewi Zone, subdivided as well into two subzones, a lower Karakaschiceras inostranzewi Subzone and an upper Saynoceras contestanum Subzone. The assemblages characterizing each of these biozones can be recognized throughout the Mediterranean region.- Handle-ID: http://hdl.handle.net/2042/56745</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Thu, 11 Jun 2015 12:53:12 GMT</pubDate>
</item>


<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 07</title>
 <link>http://paleopolis.rediris.es/cg/1507/</link>
 <description>Olev Vinn &#038; Ursula Toom.- Some encrusted hardgrounds from the Ordovician of Estonia (Baltica).- The Ordovician hardground faunas of Estonia are not diverse. They include echinoderm holdfasts (i.e., eocrinoids and crinoids), edrioasteroids, bryozoans (both hemispherical trepostomes and stalked ptilodictyids) and cornulitids. The earliest hardground faunas appeared in the Dapingian (i.e., bryozoans and echinoderms). The Estonian hardground faunas are less diverse than the North American ones. North American hardgrounds seem to be more heavily encrusted than the Estonian ones. These differences may be due to the paleogeographic distances, different climates and different sedimentation environments of the paleocontinents.- Handle-ID: http://hdl.handle.net/2042/56744</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Thu, 11 Jun 2015 12:49:16 GMT</pubDate>
</item>

<item>
  <title>Oceanologia No. 57(1)/2015</title>
  <link>http://iopan.gda.pl/oceanologia/57_1.html</link>
  <description>
* Making coastal research useful &#8211; cases from practice. - von Storch Hans, Emeis Kay,  Meinke Insa, Kannen Andreas, Volker Matthias, Ratter Beate M.W., Stanev Emil,  Weisse Ralf, Wirtz Kai &#060;br /&#062;
* Assimilation of the satellite SST data in the 3D CEMBS model. - Nowicki Artur, Dzierzbicka-G&#322;owacka Lidia, Janecki Maciej, Ka&#322;as Maciej&#060;br /&#062;
* Comparison of in situ and satellite ocean color determinations of particulate organic carbon concentration in the global ocean. - &#346;wirgo&#324; Marek, Stramska Malgorzata &#060;br /&#062;
* Temporal changes in Hg, Pb, Cd and Zn environmental concentrations in the southern Baltic Sea sediments dated with 210Pb method. - Zalewska Tamara, Woro&#324; Jerzy, Danowska Beata, Supli&#324;ska Maria &#060;br /&#062; 
* A comparison between the suspended sediment concentrations derived from DELFT3D model and collected using transmissometer &#8211; a case study in tidally dominated area of Dithmarschen Bight.- Rahbani Maryam &#060;br /&#062;
* Influence of the winter phytoplankton bloom on the settled material in a temperate shallow estuary. - Guinder Valeria A., L&#243;pez-Abbate M. Celeste, Berasategui Anabela A., Negrin Vanesa L., Zapperi Georgina,  Pratolongo Paula D., Fern&#225;ndez Severini Melisa D., Popovich Cecilia A. &#060;br /&#062;
* Potential effects of abiotic factors on the abundance and distribution of the plankton in the Western Harbour, south-eastern Mediterranean Sea, Egypt. -  Heneash Ahmed M.M., Tadrose Hermine R.Z., Maged M.A. Hussein, Samia K. Hamdona, Abdel-Aziz Nagwa, Gharib Samiha M. &#060;br /&#062;
* The short-term effects of crude oil on the survival of different size-classes of cladoceran Daphnia magna (Straus, 1820). - Lennuk Lennart,  Kotta Jonne, Taits Kristiina, Teeveer Karolin &#060;br /&#062;
* Seasonal variability in the population dynamics of the main mesozooplankton species in the Gulf of Gda&#324;sk (southern Baltic Sea): Production and mortality rates. - Dzierzbicka-G&#322;owacka Lidia, Kalarus Marcin, Musialik-Koszarowska Maja, Lemieszek Anna, &#379;mijewska Maria Iwona &#060;br /&#062;
* Lipid content and fatty acid composition of Mediterranean macro-algae as dynamic factors for biodiesel production.- El Maghraby Dahlia M., Fakhry Eman M. &#060;br /&#062; 
* Bioaccumulation of microcystins in invasive bivalves: A case study from the boreal lagoon ecosystem. - Paldavi&#269;ien&#279; Aist&#279;,  Zaiko Anastasija, Mazur-Marzec Hanna, Razinkovas-Baziukas Art&#363;ras &#060;br /&#062;
* First report on intersex in invasive round goby Neogobius melanostomus from the Baltic Sea (Gulf of Gda&#324;sk, Poland). - Guellard Tatiana, Soko&#322;owska Ewa, Arciszewski Bart&#322;omiej </description>
  <category>Journal</category>
  <author>sabina@iopan.gda.pl</author>
  <pubDate>Wed, 11 Mar 2015 14:20:22 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 06</title>
 <link>http://paleopolis.rediris.es/cg/1506/</link>
 <description>Andreas May.- MayLib - a textfile-based bibliographic database for geosciences and a list of references on Devonian matters.- Scientists need to manage their own collections of bibliographic data as well as exchange these data easily with colleagues. One solution for this need is MayLib, a bibliographic database that runs on many different operating systems and does not require pre-installation of any software. MayLib is a very small, efficient and comprehensive JAVA program that handles references to publications in any Unicode-compatible language. It is user-friendly and not only contains the basic functions of a bibliographic database, but also has some advanced features. Using MayLib the author has been able to create a list of references, which contains 500 periodicals and 4206 literature references. Of these 4206 references 3191 deal with Devonian matters and 1594 references deal with corals.- Handle-ID: http://hdl.handle.net/2042/56481</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Mon, 09 Mar 2015 11:58:25 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 05</title>
 <link>http://paleopolis.rediris.es/cg/1505/</link>
 <description>Francesco Sciuto, Antonietta Rosso, Rossana Sanfilippo &#038; Rosanna Maniscalco.- New faunistic data on the Pleistocene environmental evolution of the south-western edge of the Hyblean Plateau (SE Sicily).- Faunistic associations of the Lower Pleistocene sediments, out-cropping at Cartiera Molino along the true right bank of the Ippari River (Vittoria, SE Sicily), have been investigated. This study integrates data obtained from the analysis of ostracods, foraminifers, bryozoans and serpulids found within a six metre thick sedimentary section. This multiproxy approach allowed us to reconstruct the palaeoenvironmental evolution of this south-western sector of the Hyblean Plateau (Comiso-Vittoria area) from fluvially-influenced shallow marine settings, recorded in the lower portion of the succession, to progressively shallower, transitional and brackish environments, testified in mid levels, up to freshwater environments at the top of the section.- Handle-ID: http://hdl.handle.net/2042/56401</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Sat, 28 Feb 2015 11:20:57 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 04</title>
 <link>http://paleopolis.rediris.es/cg/1504/</link>
 <description>Simon F. Mitchell.- A reassessment of the validity and affinities of Belemnites sulcatus Miller, 1826, Belemnopsis Edwards in Gray, 1849, and Belemnopsis Bayle, 1878.- A reinvestigation of the validity of the belemnite genus Belemnopsis Bayle is undertaken, together with a survey of the early history of the usage of the names Belemnites sulcatus, Belemnopsis Bayle and Belemnopsis Edwards. Belemnites sulcatus Miller has been variously equated with either Belemnites apiciconus Blainville or with the group of belemnites including Belemnites Altdorfensis Blainville and B. Beaumontianus Orbigny. Riegraf (and not Phillips) subsequently designated a lectotype which may be valid and, in case it is not, is validated here. The species concept for Belemnites sulcatus, as based on this lectotype, places it in the genus Holcobeloides Gustomesov. Belemnopsis Edwards has date priority over Belemnopsis Bayle, but must be interpreted as an &quot;incorrect original spelling&quot; and, therefore, does not enter into homonymy according to the ICZN; Belemnopsis Bayle is thus a valid genus. Douvill&#233; subsequently nominated Belemnites sulcatus, which was figured as Belemnopsis sulcata by Bayle, and therefore is a valid designation because this species is amongst the original species included in Belemnopsis by Bayle. One of Bayle's figures of Belemnopsis sulcata agrees with Belemnites apiciconus Blainville, but does not agree with Belemnites sulcatus as defined by its lectotype; as such this is a case of misidentified type species. Belemnites apiciconus Blainville, the species involved in the misidentification, is therefore designated type species of Belemnopsis Bayle here and validated by citing the ICZN. The actions taken here maintain nomenclature at the genus, family and suborder level in respect to the names Belemnopsis and Belemnosis and serve to stabilize the complicated nomenclature issues related to these taxa.- Handle-ID: http://hdl.handle.net/2042/56399</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Sun, 15 Feb 2015 10:06:17 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 03</title>
 <link>http://paleopolis.rediris.es/cg/1503/</link>
 <description>Jean-Pierre Masse, Sibelle Maksoud, Mukerrem Fenerci-Masse, Bruno Granier &#038; Dany Azar.- Earliest Aptian Caprinidae (Bivalvia, Hippuritida) from Lebanon.- The presence in Lebanon of Offneria murgensis and Offneria nicolinae, two characteristic components of the Early Aptian Arabo-African rudist faunas, fills a distributional gap of the corresponding assemblage between the Arabic and African occurrences, on the one hand, and the Apulian occurrences, on the other hand. This fauna bears out the palaeogeographic placement of Lebanon on the southern Mediterranean Tethys margin established by palaeostructural reconstructions. The associated micropaleontological elements suggest an earliest Aptian age (early Bedoulian) for the Offneria murgensis - O. nicolinae assemblage found in the &quot;Falaise de Blanche&quot; stratigraphic interval, instead of a late Early Aptian age as proposed for most of the peri-Adriatic and Middle East occurrences recognized so far. These caprinid specimens are characterized by relatively modest sizes, moreover other rudists commonly part of the assemblage are lacking. The dominance of caprinids in the study area suggests a distal platform setting, i.e., close proximity to the platform edge.- Handle-ID: http://hdl.handle.net/2042/56397</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Sun, 15 Feb 2015 10:01:52 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 02</title>
  <link>http://paleopolis.rediris.es/cg/1502/</link>
  <description>Katarzyna Zalecka, Tomasz Wrzo&#322;ek &#038; Bruno Granier.- Simple and practical techniques to manage small databases, illustrated by a case study: bibliographic data from the &quot;Fossil Cnidaria &#038; Porifera&quot; newsletter.- Small databases, i.e., with less than 15,000 entries, are sometimes handled using inappropriate, complex, and often expensive data management systems. We present and briefly discuss a few types of proprietary and open-source, relational and non-relational, server-based versus portable databases and specific tools to handle the latter. With a collection of nearly 7,000 bibliographic notes during its 40-year history &quot;Fossil Cnidaria &#038; Porifera (FC&#038;P)&quot;, the newsletter of the &quot;International Association for Study of Fossil Cnidaria and Porifera&quot;, was chosen as a case study. The analysis of the temporal trends in the FC&#038;P bibliographic database shows a decrease over the years in the number of publications effectively reported in FC&#038;P. Almost all relevant papers for the decade 1981-1990 are reported, but this good coverage ratio falls down to less than 50% after 2000; accordingly, the concern about the data representativeness is addressed in our interpretation. Besides the classical database management systems and spreadsheet software, which were originally used with the FC&#038;P case study, we present two discrete, open-source, flat and portable options where data can be displayed using any widely available Internet browser, and that are suitable to handle most small databases (XML or JS files) as documented herein.- Handle-ID: http://hdl.handle.net/2042/56249</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 14 Jan 2015 16:33:14 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 15, n&#186; 01</title>
  <link>http://paleopolis.rediris.es/cg/1501/</link>
  <description>Jos&#233; R. Ovando-Figueroa, Josep A. Moreno-Bedmar, Gabriel  Ch&#225;vez-Cabello &#038; Keith P. Minor.- Lower Aptian ammonites of the Sierra de Parras, Coahuila State, northern Mexico.- We report an interesting Aptian ammonite record from the La Pe&#241;a Formation in the Sierra de Parras, Coahuila State. This assemblage is analyzed from a paleoecological perspective. It contains the first reported occurrence of a macroconch of Dufrenoyia from Mexico, and the largest known specimen of &#039;Gargasiceras&#039; adkinsi. Such an assemblage yielding large ammonites is unusual in deposits of this age in Mexico. To properly document this ammonite record, we review &#039;Gargasiceras&#039; adkinsi, formerly misidentified as Rhytidoplites robertsi, and allied taxa. From our analysis, we conclude that &#039;Gargasiceras&#039; adkinsi exhibits strong intraspecific variability. We also analyze in detail the differences that exist between &#039;Gargasiceras&#039; adkinsi and Rhytidoplites robertsi, and emend the concept of the genus Rhytidoplites. These revisions are important from a biostratigraphic point of view since &#039;Gargasiceras&#039; adkinsi is an index species for the lower Aptian ammonite zonation of Mexico.- Handle-ID: http://hdl.handle.net/2042/56250</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 14 Jan 2015 12:02:12 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, Obituary notice</title>
  <link>http://paleopolis.rediris.es/cg/Guy_Tronchetti/</link>
  <description>Michel  Moullade.- In memoriam of my colleague and friend Guy Tronchetti (1938-2014).- The chief editor of a prestigious scientific journal, who is about to publish a major article of which Guy is one of the lead authors, replied to the news of his passing: &quot;I am very sorry to hear about that. I have known Guy Tronchetti from publications, for a long time. It is really sad.&quot; This quote and Googling his name show that, according to his publications, some of them very recent, Guy was still both at the cutting edges of research and a scientist at an international level. His great modesty did not allow people to necessarily acknowledge this, especially those who did not attempt to overcome such an obstacle. - Handle-ID: http://hdl.handle.net/2042/56047</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 24 Dec 2014 15:06:35 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 22</title>
  <link>http://paleopolis.rediris.es/cg/1422/</link>
  <description>Bruno Granier, Vincent Barbin &#038; Jean Charollais.- Significance of partial leaching in calcareous ooids: The case study of Hauterivian oolites in Switzerland.- In the Canton of Vaud (Switzerland), two Hauterivian oolitic units were penetrated by a borehole. In both units, the ooids are partly leached. More specifically, the ooid cortices were partly leached and some ooid nuclei appear suspended in the middle of cortical moldic cavities created by leaching, rather than having fallen to the bottom of these cavities before the final cementation take place. We demonstrate that these ooids were originally calcitic, not aragonitic, not &quot;two-phase&quot; nor &quot;bimineral&quot;. This leaching is not an early diagenetic feature related to subaerial exposure, but a late diagenetic feature, possibly related to the migration of acidic pore waters, brought about by Alpine tectonics and/or karstification.- Handle-ID: http://hdl.handle.net/2042/56045</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 24 Dec 2014 15:01:57 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 21</title>
  <link>http://paleopolis.rediris.es/cg/1421/</link>
  <description>Bruno Granier.- Borings and etchings in the Upper Bathonian-Lower Callovian oolite of the Paris Basin (France).- The oolite of the &quot;Dalle Nacr&#233;e&quot; Formation in the Paris Basin is made of marine calcareous ooids with, from base to top, radial (and therefore likely to have been calcite), concentric and micritic fabrics, each corresponding to a discrete stratigraphic unit. Several hardgrounds and oolitic pebble-cobble layers in the succession are encrusted and bored. Three main types of boring have been identified ranging in sizes from some tens of &#181;m (sponge borings) to centimeters (bivalve borings), with an intermediate category (worm borings). Some worm borings have rough walls, where early marine fibrous cement is less corroded than the cortices of cemented ooids. The key to understanding this differential dissolution could be related to organic matter, present within the ooid cortices but lacking in the fibrous cement. Polychaete worms that use chemical means (enzymes or acids) to bore are probably responsible for these peculiar borings. A secondary conclusion is that partly or fully leached ooid cortices do not necessarily indicate an original aragonitic mineralogy of the dissolved parts.- Handle-ID: http://hdl.handle.net/2042/56043</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 24 Dec 2014 14:58:26 GMT</pubDate>
</item>

<item>
  <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 20</title>
  <link>http://paleopolis.rediris.es/cg/1420/</link>
  <description>Tomasz Wrzo&#322;ek.- Devonian Phillipsastreid tetracorals of the genus Rozkowskaella from the Holy Cross Mountains, Poland.- Solitary or weakly colonial Phillipsastreid tetracorals of the Upper Frasnian of Holy Cross Mountains, Poland, with triangular to oval shape of transverse-section and tendency towards reduction of the horseshoe dissepiments, are included here in the genus Rozkowskaella, with Rozkowskaella sandaliformis, R. cf. sandaliformis and Rozkowskaella sp.- Handle-ID: http://hdl.handle.net/2042/56041</description>
  <category>Publication</category>
  <author>carnetsgeol@rediris.es</author>
  <pubDate>Wed, 24 Dec 2014 14:55:40 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 19</title>
 <link>http://paleopolis.rediris.es/cg/1419/</link>
 <description>Francesco Sciuto.- Two new species of Early Pleistocene marine ostracods
from Southeast Sicily.- Two fossil species of Ostracoda belonging to the genera Urocythereis Ruggieri, 1950, and Semicytherura Wagner, 1957, discovered in the Lower Pleistocene shallow marine sandy-silty sediments outcropping at &quot;Cartiera Molino&quot; (F. 276, IV NO, Vittoria, Southeast Sicily) are described and figured.- Handle-ID: http://hdl.handle.net/2042/56039</description>
 <category>Publication</category>
 <author>carnetsgeol@rediris.es</author>
 <pubDate>Wed, 24 Dec 2014 14:35:09 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 18</title>
 <link>http://paleopolis.rediris.es/cg/1418/</link>
 <description>Sibelle Maksoud, Bruno Granier, Dany Azar, Raymond G&#232;ze, Jean-Claude Paicheler &#038; Josep A. Moreno-Bedmar.- Revision of &quot;Falaise de Blanche&quot; (Lower Cretaceous) in Lebanon, with the definition of a Jezzinian Regional Stage.- The &quot;Falaise de Blanche&quot; is a prominent cliff, consisting mostly of Lower Cretaceous limestones that extends as linear outcrops over most of the Lebanese territory and provides geologists a remarkable reference for stratigraphic studies. However, until now, this unit was lacking a clear definition. We introduce herein the Jezzinian Regional Stage, the type-locality of which is at Jezzine. It equates as an unconformity-bounded unit and, per definition, it is framed by two discontinuities. Because we identified an additional, median sequence-boundary, poorly-expressed in the type-section but better at Aazour, only 4.5 km westward of Jezzine, the new regional stage implicitly spans two sequences. The lithostratigraphic framework being properly redefined, we were able to investigate time-constrained micropaleontological assemblages, consisting mostly of benthic foraminifers and calcareous algae. Typically Southern Tethysian, these assemblages contribute to high-resolution, holostratigraphic correlations with the Persian Gulf area, on the eastern part of the Arabian Plate. The Jezzinian interval correlates with the upper part of the Kharaibian Regional Stage (also known as &quot;Thamama II&quot; reservoir unit in the oil industry). In turn, the Jezzinian is indirectly correlated with the Northern Tethysian Urgonian stratigraphic units where it corresponds to a rather short interval encompassing the standard Barremian - Bedoulian stage boundary. Locally the upper discontinuity is associated to a significant intra-Bedoulian hiatus. The macrofossil assemblages found in the Jezzinian (echinids) and above it (ammonites) support, or at least do not contradict, our micropaleontological dating.- Handle-ID: http://hdl.handle.net/2042/54359</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Fri, 14 Nov 2014 17:55:40 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 17</title>
 <link>http://paleopolis.rediris.es/cg/1417/</link>
 <description>Alain Bonnot, Pierre-Yves Boursicot &#038; Patrice Ferchaud.- Les genres Subgrossouvria Spath et Orionoides Spath (Ammonitina, Perisphinctidae) de l'Horizon &#224; Leckenbyi (Callovien sup&#233;rieur, Zone &#224; Athleta) de Montreuil-Bellay (Maine-et-Loire, France) [The genera Subgrossouvria Spath and Orionoides Spath (Ammonitina, Perisphinctidae) from the Leckenbyi Horizon (Upper Callovian, Athleta Zone) of Montreuil-Bellay (Maine-et-Loire, France)].- &#192; Montreuil-Bellay (Maine-et-Loire, France), le premier banc d'&#226;ge Callovien sup&#233;rieur (Horizon &#224; Leckenbyi) a fourni une tr&#232;s abondante faune ammonitique (N=3275). Dans la famille des Perisphinctidae, &#224; c&#244;t&#233; de Choffatia isabellae Bonnot et al. et du genre Pseudopeltoceras Spath, on trouve deux autres genres : le genre Subgrossouvria Spath est repr&#233;sent&#233; par S. famula (Bean in Spath) et S. crassa G&#233;rard &#038; Contaut, le genre Orionoides Spath par O. indicus Spath. L'abondance et la qualit&#233; du mat&#233;riel ont permis la description de l'ontogen&#232;se et la figuration de macroconques et de microconques de ces trois esp&#232;ces, parmi lesquels des adultes complets &#224; p&#233;ristome conserv&#233;. La diagnose du genre Orionoides, souvent mal interpr&#233;t&#233;, a &#233;t&#233; amend&#233;e. L'extension stratigraphique de ces esp&#232;ces est &#233;galement pr&#233;cis&#233;e et leur devenir potentiel est envisag&#233;. Nous avan&#231;ons l'hypoth&#232;se que ces esp&#232;ces ont colonis&#233; la plate-forme nord-ouest europ&#233;enne via la marge sud de la T&#233;thys, comme Peltoceras marysae Bonnot et al. et Choffatia isabellae Bonnot et al. [In the Montreuil-Bellay area (Maine-et-Loire, France), the lowermost bed of the Upper Callovian (Leckenbyi Horizon) contains a very abundant ammonite fauna (N=3275). The Family Perisphinctidae is represented by Choffatia isabellae Bonnot et al., the genus Pseudopeltoceras Spath, the genus Subgrossouvria Spath, which includes S. famula (Bean in Spath) and S. crassa G&#233;rard &#038; Contaut, and the genus Orionoides Spath, which comprises O. indicus Spath. Thanks to the abundance and quality of the material, it was possible to describe and figure macroconchs and microconchs of these three species, including adult specimens with preserved peristome. The stratigraphical ranges of these taxa are also specified and their potential descendants can be considered. These species are unknown in the uppermost Middle Callovian, and we assume that they colonized the northwestern part of the European platform via the southern margin of the Tethys, as did Peltoceras marysae Bonnot et al. and Choffatia isabellae Bonnot et al.]- Handle-ID: http://hdl.handle.net/2042/54363</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Fri, 14 Nov 2014 18:01:21 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 16</title>
 <link>http://paleopolis.rediris.es/cg/1416/</link>
 <description>Margarita Simeoni.- Nannofossils and foraminifera from the Salamanca Formation (Paleocene) in Punta Peligro Norte (Chubut, Argentina).- An assemblage of nannofossils from the Salamanca Formation is reported for the first time from the Punta Peligro Norte locality in the San Jorge Gulf Basin, Argentina. Several recognized nannofossils have a stratigraphic distribution within the lower Danian. The assemblage of nannofossils and associated foraminifera is here discussed taking into account biostratigraphic and paleoecological aspects.- Handle-ID: http://hdl.handle.net/2042/54361</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Fri, 14 Nov 2014 18:05:56 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 15</title>
 <link>http://paleopolis.rediris.es/cg/1415/</link>
 <description>Enelise Katia Piovesan, Maria Cristina Cabral, Jean-Paul Colin, Gerson Fauth &#038; Cristianini Trescastro Bergue.- Ostracodes from the Upper Cretaceous deposits of the Potiguar Basin, northeastern Brazil: taxonomy, paleoecology and paleobiogeography. Part 2: Santonian-Campanian.- Sixty-four Ostracoda taxa were recorded from the Santonian&#8211;Campanian of Potiguar Basin, northeastern Brazil. The following new species were described: Triebelina anterotuberculata, Triebelina obliquocostata, Cophinia ovalis, Fossocytheridea potiguarensis, Ovocytheridea anterocompressa, Ovocytheridea triangularis, Perissocytheridea jandairensis, Semicytherura musacchioi and Protocosta babinoti. The faunal association indicates predominantly shallow marine environments, intercalated with typically mixohaline levels. These species are mostly endemic, although the presence of six species common to West and North Africa shows that migration was still possible by the end of the Cretaceous.- Handle-ID: http://hdl.handle.net/2042/54151</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Tue, 14 Oct 2014 13:23:13 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 14</title>
 <link>http://paleopolis.rediris.es/cg/1414/</link>
 <description>Pierre Lozouet.- Temporal and latitudinal trends in the biodiversity of European Atlantic Cenozoic gastropod (Mollusca) faunas. A base for the history of biogeographic provinces.- A general overview of the biodiversity of the marine fauna during the Tertiary period is developed in the context of the biogeographical evolution of the European realm. This study combines a reappraisal of the literature with a unique first-hand source of data on the richest marine group (the gastropods) from over a 25 million year period (Early Oligocene to Late Miocene). In total the French deposits have yielded more than 10,000 species from the Eocene to the Upper Miocene. Evidence of significant bias in the fossil record is pointed out for the Palaeocene (Danian) and Upper Eocene (Priabonian). For the period considered (Palaeocene to Late Miocene, ca 50 million years) the second highest diversity is reported in the Late Oligocene. This study reveals also the importance of pre-Miocene extinctions of genera. The Oligocene was when the latitudinal differentiation of the faunas was greatest. The local generic gastropod richness ranges from 59 (Rupelian of Belgium) to 494 (Chattian of Aquitaine). A clear trend towards homogenization appears in the Late Oligocene which leads to the development of a vast biogeographical region named Euro-West Africa. This faunal evolutionary pattern has never been demonstrated before and is a novel feature of the biogeography of the Eastern-Atlantic region.- Handle-ID: http://hdl.handle.net/2042/54150</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Tue, 14 Oct 2014 13:18:13 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 13</title>
 <link>http://paleopolis.rediris.es/cg/1413/</link>
 <description>Didier Bert &#038; St&#233;phane Bersac.- Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an immigration event?.- The Late Barremian Hemihoplitidae (Ancyloceratina, Ammonoidea) are widely known in the northern Tethyan Margin and the Essaouira-Agadir Basin (Morocco). Their rapid evolution and diversification make them one of the key groups for that period, but their origin remains poorly known and several competing hypotheses have been published. These hypotheses are tested here with cladistic analysis in order to reject those receiving the least support and discuss those well supported. The analysis discards the Crioceratitidae, Emericiceratidae (Emericiceras and Honnoratia) and Toxancyloceras as stem-groups of the Hemihoplitidae (Gassendiceras). The Toxancyloceras appear instead to be a sister-taxon of the Moutoniceras, so we propose the latter to be classified with the Ancyloceratidae rather than with the Heteroceratidae. The best supported hypothesis assumes that the Hemihoplitidae first appeared suddenly in the Essaouira-Agadir Basin at the end of the Early Barremian from small populations of Boreal Paracrioceras. These latter could have migrated southward episodically before invading the northern Tethyan margin at the beginning of the Late Barremian. As a consequence, the Paracrioceratidae fam. nov. is proposed to include the Boreal groups Fissicostaticeras / Paracrioceras / Parancyloceras, and Gassendiceras essaouirae sp. nov. is proposed as a new name for the Moroccan endemic &quot;Barrancyloceras&quot; maghrebiense sensu Company et al., 2008, non Immel, 1978.- Handle-ID: http://hdl.handle.net/2042/54149</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Tue, 14 Oct 2014 13:14:08 GMT</pubDate>
</item>

<item>
<title>Bulletin of Geosciences, Volume 89, Issue 4 (2014)</title>
<link>http://www.geology.cz/bulletin/contents/2014/vol89no4</link>
<description>* Dapingian-lower Darriwilian (Ordovician) stratigraphic gap in the Faraghan Mountains, Zagros Ranges, south-eastern Iran.- Ghavidel-Syooki M, Popov LE, Alvaro JJ, Ghobadi Pour M, Tolmacheva TY &#038; Ehsani M-H&#060;br /&#062;
* Crangopsis Salter, 1863 from the Lower Carboniferous (Mississippian) of the Ostrava Formation - the first record of Aeschronectida (Malacostraca: Hoplocarida) from continental Europe.- Hyzny M, Hoch I, Schram FR &#038; Rybar S&#060;br /&#062;
* Carbon isotope stratigraphy and ammonite biochronostratigraphy across the Sinemurian-Pliensbachian boundary in the western Iberian margin.- Duarte LV, Comas-Rengifo MJ, Silva RL, Paredes R &#038; Goy A&#060;br /&#062;
* Visean Lithostrotionidae (Rugosa) from Zonguldak and Bart&amp;#305;n (NW Turkey).- Denayer J&#060;br /&#062;
* T0 peat-forming plant assemblage preserved in growth position by volcanic ash-fall: A case study from the Middle Pennsylvanian of the Czech Republic.- Oplustil S, Psenicka J, Bek J, Wang J, Feng Z, Libertin M, Simunek Z, Bures J &#038; Drabkova J&#060;br /&#062;
* The Early Miocene (Burdigalian) mollusc fauna of the North Bohemian Lake (Most Basin).- Harzhauser M, Neubauer TA, Georgopoulou E &#038; Harl J</description>
<category>Journal</category>
<author>admin.bulletin@geology.cz</author>
<pubDate>Tue, 30 Sep 2014 01:00:00 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 56(4)/2014</title>
<link>http://iopan.gda.pl/oceanologia/56_4.html</link>
<description>
  Formation and species composition of stormcast beach wrack in the Gulf of Riga, Baltic Sea.
  - Suursaar Ulo, Torn Kaire, Martin Georg, Herk&#252;l Kristjan, Kullas Tiit
&#060; br /&#062;
  Studies of vertical coarse aerosol fluxes in the boundary layer over the Baltic Sea.
  - Petelski Tomasz, Markuszewski Piotr, Makuch Przemys&#322;aw, Jankowski Andrzej, Rozwadowska Anna
&#060; br /&#062;
   Nutrient turnover at the hypoxic boundary: flux measurements and model representation for the bottom water environment of the Gulf of Riga, Baltic Sea.
   - Egl&#299;te Elvita,  Lavrinovi&#269;s Aigars,  M&#252;ller-Karulis B&#227;rbel, Aigars Juris, Poik&#257;ne Rita
&#060; br /&#062;
   Regional algorithms for the estimation of chlorophyll and suspended matter concentration in the Gulf of Finland from MODIS-Aqua satellite data.
   - Vazyulya Svetlana, Khrapko Alexander, Kopelevich Oleg, Vladimir Burenkov, Tatyana Eremina, Isaev Alexey
&#060; br /&#062;
   Annual phytoplankton dynamics in the Gulf Saint Vincent, South Australia, in 2011.
   - Leterme Sophie C., Jendyk Jan-Georg, Ellis Amanda V., Brown Melissa H., Kildea Tim
&#060; br /&#062;
   Gonad maturity in female Chinese mitten crab Eriocheir sinensis from the southern Baltic Sea &#8211; the first description of ovigerous females and the embryo developmental stage.
   - W&#243;jcik Dagmara, Normant Monika
&#060; br /&#062;
   Baltic herring (Clupea harengus membras) spawning grounds on the Lithuanian coast: current status and shaping factors.
   - &#352;a&#353;kov Aleksej, &#352;iaulys Andrius,  Bu&#269;as Martynas, Daunys Darius &#060; br /&#062;
   Population structure, morphometry and individual condition of the non-native crab <i>Rhithropanopeus harrisii</i> (Gould, 1841),
   a recent coloniser of the Gulf of Gda&#324;sk (southern Baltic Sea).
   - Hegele-Drywa Joanna, Normant Monika, Szwarc Barbara, Pod&#322;uska Anna
&#060; br /&#062;
   Bacterial community structure influenced by Coscinodiscus sp. in the Vistula river plume.
   - Ameryk Anetta, Hahnke Richard L., Gromisz S&#322;awomira, Kownacka Janina, Zalewski Mariusz, Szymanek Lena, Ca&#322;kiewicz Joanna,  Dunalska Julita,  Harder Jens&#060; br /&#062;
   Impact of sand extraction from the bottom of the southern Baltic Sea on the relief and sediments of the seabed.
   - U&#347;cinowicz Szymon, Jegli&#324;ski Wojciech,  Miotk-Szpiganowicz Gra&#380;yna, Nowak Jaros&#322;aw, Urszula P&#261;czek, Przezdziecki Piotr, Szefler Kazimierz, Por&#281;ba Grzegorz
&#060; br /&#062;
    Seasonal changes in the biochemical components of Pseudonereis anomala (Polychaeta, Nereididae) from the Alexandria coast, Egypt.
    - Dorgham Mohamed Moussa, Hamdy Rasha, Al-Rassheedy Hoda Hassan, Atta Manal Mohamed
</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Wed, 27 Aug 2014 11:15:07 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 12</title>
 <link>http://paleopolis.rediris.es/cg/1412/</link>
 <description>Enelise Katia Piovesan, Maria Cristina Cabral, Jean-Paul Colin, Gerson Fauth &#038; Cristianini Trescastro Bergue.- Ostracodes from the Upper Cretaceous deposits of the Potiguar Basin, northeastern Brazil: taxonomy, paleoecology and paleobiogeography. Part 1: Turonian.- This paper describes thirteen new species and two new genera of marine and brackish water ostracodes from the Turonian deposits of Potiguar Basin, NE Brazil, among a total of 53 taxa. The new species include Cophinia grekoffi, Fossocytheridea tiberti, Haughtonileberis dinglei, Hemicytherura viviersae, Jandairella obesa (new genus and species), Loxocorniculum? narendrai, Ovocytheridea posteroprojecta, O. reymenti, Perissocytheridea caudata, P. mossoroensis, Potiguarella grosdidieri (new genus and species), P. coimbrai and Procytherura ballentae. The diversity and dominance indexes vary according to the paleoenvironment. Three assemblages were identified: a predominantly mixohaline fauna in the basal part of the section, followed by a diversified shallow marine fauna and, in the upper part, a marine and brackish water ostracode fauna. Most of the recorded species are endemic. Eight species are common to Northwest and North Africa, indicating a faunal link during the Turonian. The study of the Turonian faunas of the Potiguar Basin represents a significant improvement to understand the dynamic evolution of the Brazilian basins and the paleobiogeographical relationship with other regions.- Handle-ID: http://hdl.handle.net/2042/54003</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 03 Jul 2014 18:55:29 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 11</title>
 <link>http://paleopolis.rediris.es/cg/1411/</link>
 <description>Ioan I. Bucur, Adriana P&#259;curariu, Emanoil S&#259;s&#259;ran, Sorin Filipescu &#038; Rodica Filipescu.- First record of lowermost Cretaceous shallow-water limestones in the basement of the Transylvanian Depression (Romania).- Triassic, Upper Jurassic and upper Lower Cretaceous sedimentary formations were previously studied from the Transylvanian Depression basement, but the presence of lowermost Cretaceous (Berriasian-Valanginian) has not been confirmed paleontologically. The carbonate sequence cored from a borehole drilled in the central part of the Transylvanian Depression yields microfossil assemblages dominated by benthic foraminifera. These new data unequivocally document the presence of characteristic Berriasian-Valanginian taxa in these deposits.- Handle-ID: http://hdl.handle.net/2042/54001</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 03 Jul 2014 18:50:35 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 10</title>
 <link>http://paleopolis.rediris.es/cg/1410/</link>
 <description>Old&#345;ich Fatka &#038; Vladislav Koz&#225;k.- A new type of entombment of Peronopsis (Agnostida) in a hyolithid conch.- An enrolled exoskeleton of the holaspid specimen of a tiny agnostid Peronopsis integra (Beyrich, 1845) entombed inside a conch of the hyolithid ?Buchavalites sp. is described from the middle Cambrian (Drumian) Jince Formation of the P&#345;&#237;bram-Jince Basin (Czech Republic). The agnostid is associated with an ichnofossil of the feeding trace classified as Arachnostega-type behaviour. The enrolled attitude of the agnostid exoskeleton suggests that the specimen is a carcass rather than moult. Either the storm disturbance and/or well-protected source of food hypotheses could explain the entombed agnostid. This additional example supports a benthic mode of life in the agnostid P. integra. The studied association of feeding tunnels of an unknown Arachnostega-strategist and Peronopsis preserved inside a hyolithid conch is a case of &#034;frozen&#034; behaviour.- Handle-ID: http://hdl.handle.net/2042/54000</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 03 Jul 2014 18:44:20 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 9</title>
 <link>http://paleopolis.rediris.es/cg/1409/</link>
 <description>Michel Hennebert.- The Cretaceous-Paleogene boundary and its 405-kyr eccentricity cycle phase: a new constraint on radiometric dating and astrochronology.- Radiometric dating and astrochronologic dating still suffer discrepancies without knowing which one gives the most reliable results. A new tool is proposed to constrain both the approaches. The phase of the 405-kyr signal with respect to the Cretaceous - Paleogene boundary event has been determined in the A&#239;n Settara section (Kalaat Senan, central Tunisia). We use this phase value (Option 2), as well as an average of phase values obtained from the literature (Option 1), to examine the relationship linking both the radiometric (absolute) age assigned to the K-Pg boundary and the Cenozoic average-value of the ~405-kyr eccentricity period. A new useful constraint emerges: to any absolute age assumed for the K-Pg boundary corresponds a value of the mean Cenozoic 405-kyr period, and vice versa. Supposing a K-Pg boundary radiometric age in the vicinity of 66.0 Ma, then the number of entire cycles (comprised between two minima of the 405-kyr eccentricity signal) within the Cenozoic Period could only be equal to 163. When adding to this figure the parts of the cycles preceding and following these 163 entire cycles the total duration of the Cenozoic Era becomes equal to 163.168 cycles (Option 1) or 163.081 cycles (Option 2). We propose to grant a special interest to the determination of the 405-kyr cycle phase at stratigraphically well documented levels, particularly those that correspond to world-wide, sudden and catastrophic events, that are well located in time by reliable radiometric dates.- Handle-ID: http://hdl.handle.net/2042/53981</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 19 Jun 2014 01:05:04 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 8</title>
 <link>http://paleopolis.rediris.es/cg/1408/</link>
 <description>Christian C. Emig.- Novocrania turbinata synonyme de N. anomala.- Anomia turbinata, ou Anomie conique, (= Novocrania turbinata) a &#233;t&#233; d&#233;crite par Poli (1795) dans le Bathyal des c&#244;tes du Royaume des Deux-Siciles, avec comme synonyme Patella anomala M&#252;ller, 1776 (= N. anomala). Longtemps consid&#233;r&#233;e comme la forme m&#233;diterran&#233;enne de N. anomala, son histoire est bri&#232;vement d&#233;crite. R&#233;cemment, N. turbinata a &#233;t&#233; consid&#233;r&#233;e par plusieurs auteurs, comme une esp&#232;ce valide, mais sur quelques caract&#232;res ne correspondant pas &#224; ceux de la description originelle ; ils apparaissent comme des variations des caract&#232;res de N. anomala. La pr&#233;sence conjointe des deux "esp&#232;ces" dans plusieurs localit&#233;s surtout sur le plateau continental tend &#224; accr&#233;diter leur synonymie. Celle-ci a &#233;t&#233; r&#233;cemment corrobor&#233;e par des analyses mol&#233;culaires et est discut&#233;e en prenant aussi en compte les caract&#233;ristiques des bassins m&#233;diterran&#233;ens et leur histoire depuis le Mioc&#232;ne. Novocrania turbinata synonym of N. anomala.- Anomia turbinata, or conical Anomia (= Novocrania turbinata), was described by Poli (1795) in the bathyal environment off the coast of the Kingdom of the Two Sicilies, Patella anomala M&#252;ller, 1776 (= N. anomala) being considered a synonym. The history of this species, commonly considered as the Mediterranean form of N. anomala, will be described. Recently, several authors have described N. turbinata as a valid species on the basis of shell variations, as compared to N. anomala. After analysis of the taxonomic validity of these characters, both species are considered as synonymous. That is supported by their occurrence in various localities, mainly in the continental shelf. Their synonymy has been corroborated by molecular analyses and is discussed with reference to the characteristics of the Mediterranean basins and their history since the Miocene.- Handle-ID: http://hdl.handle.net/2042/53979</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 19 Jun 2014 01:01:18 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 56(3)/2014</title>
<link>http://iopan.gda.pl/oceanologia/56_3.html</link>
<description>
* Recent sea surface temperature trends and future scenarios for the Mediterranean Sea.- Shaltout Mohamed, Anders Omstedt<br /> * Pronounced anomalies of air, water, ice conditions in the Barents and Kara Seas, and the Sea of Azov.- Matishov Gennady G., Dzhenyuk Sergei L., Moiseev Denis V., Zhichkin Aleksandr P. <br /> * Field study of film spreading on a sea surface.- Korinenko Aleksandr E., Malinovsky Vladimir V. <br /> * Groundwater flow due to a nonlinear wave set-up on a permeable beach .- Anna Przyborska<br /> * Relative infaunal bivalve density assessed from split beam echosounder angular information.- S&#225;nchez-Carnero Noela, Rodr&#237;guez-Prez Daniel, Zaragoz&#225; Nuria, Espinosa Victor, Freire Juan<br /> * DOC and POC in the water column of the southern Baltic. Part I. Evaluation of factors influencing sources, distribution and concentration dynamics of organic matter.- Maciejewska Anna, Pempkowiak Janusz<br /> * Genetic characteristics of three Baltic <i>Zostera marina</i>populations.- Gonciarz Magdalena, Wiktor J&#243;zef, Tatarek Agnieszka, Weglenski Piotr, Stankovic Anna<br /> * Importance of bacteria and protozooplankton for faecal pellet degradation.- Morata Nathalie, Seuthe Lena <br /> * Short-term variation in zooplankton community from Daya Bay with outbreaks of <i>Penilia avirostris</i>.- Kaizhi Li, Jianqiang Yin, Yehui Tan, Liangmin Huang, Xingyu Song<br /> * Benthic non-indigenous species among indigenous species and their habitat preferences in Puck Bay (southern Baltic Sea).- Janas Urszula, Kendzierska Halina<br /> * Epibionts and parasites on crustaceans (Copepoda, Cladocera, Cirripedia larvae) inhabiting the Gulf of Gdansk (Baltic Sea) in very large numbers.- Bielecka Luiza, Boehnke Rafal</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Tue, 10 Jun 2014 06:37:43 GMT</pubDate>
</item>

<item>
<title>Bulletin of Geosciences, Volume 89, Issue 3 (2014)</title>
<link>http://www.geology.cz/bulletin/contents/2014/vol89no3</link>
<description>* A probable case of heterochrony in the solutan Dendrocystites Barrande, 1887 (Echinodermata: Blastozoa) from the Upper Ordovician of the Prague Basin (Czech Republic) and a revision of the family Dendrocystitidae Bassler, 1938.- Noailles F, Lefebvre B &#038; Kasicka L<br /> * The classification of the Pterobranchia (Cephalodiscida and Graptolithina).- Maletz J <br /> * Arthropod cuticles from the upper Visean (Mississippian) of eastern Germany.- Haug JT, H?bers M, Haug C, Maas A, Waloszek D, Schneider JW &#038; Kerp H<br /> * Diverse scelionid wasps in Early Cretaceous amber from Spain (Hymenoptera: Platygastroidea).- Ortega-Blanco J, McKellar RC &#038; Engel MS<br /> * New Cricetodontini from the middle Miocene of Europe: an example of mosaic evolution.- Lopez-Guerrero P, Alvarez-Sierra MA, Garcia-Paredes I &#038; Pelaez-Campomanes P<br /> * Middle Devonian invertebrate trace fossils from the marginal marine carbonates of the Zachelmie tetrapod tracksite, Holy Cross Mountains, Poland.- Niedzwiedzski G, Narkiewicz M &#038; Szrek P<br /> * Jacoburbirostrum, a new middle Famennian rhynchonellid (brachiopod) genus from southwestern New York State.- Sartenaer P<br /> * First evidence for the Homerian (late Wenlock, Silurian) positive carbon isotope excursion from peri-Gondwana: new data from the Barrandian (Perunica).- Fryda J &#038; Frydova B<br /> * The largest Lower Devonian placoderm - Antineosteus rufus sp. nov. from the Barrandian area (Czech Republic).- Vaskaninova V &#038; Kraft P <br /> * Early Devonian polygnathids of Northeast Asia and correlation of Pragian/Emsian strata of the marginal seas of Angarida.- Baranov VV, Slavik L &#038; Blodgett RB</description>
<category>Journal</category>
<author>admin.bulletin@geology.cz</author>
<pubDate>Mon, 9 Jun 2014 01:00:00 GMT</pubDate>
</item>

<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 7</title>
 <link>http://paleopolis.rediris.es/cg/1407/</link>
 <description>William J. Woelkerling, Bruno Granier &#038; Dimas Dias-Brito.- Heydrichia (?) poignantii, sp. nov. (Sporolithaceae, Sporolithales, Rhodophyta), a 100 million year old fossil coralline red alga from north-eastern Brazil, and a new Hauterivian record of Sporolithon from Switzerland.- Fossil specimens of Heydrichia (?) poignantii, sp. nov. (Sporolithaceae, Sporolithales, Rhodophyta), representing the first confirmation of the genus in the fossil record, were discovered in thin sections of Albian limestones from the Riachuelo Formation, Sergipe Basin, and in thin sections of Albian - Cenomanian limestones from the Ponta do Mel Formation, Potiguar Basin in north-eastern Brazil. A detailed morphological-anatomical account of the species is provided, and its placement in Heydrichia is discussed in relation to current classification proposals. Comparisons with the four other known species of the genus, all non-fossil, show that H. poignantii is the only known species of Heydrichia in which thalli are encrusting to sparsely warty to horizontally layered with overlapping lamellate branches that commonly appear variously curved or arched, and in which thalli have sporangial complexes that become buried in the thallus. The evolutionary history of Heydrichia remains uncertain, but available data suggest that the genus may have diverged from the sporolithacean genus Sporolithon, known as early as Hauterivian times (c. 129.4-132.9 &#177; 1 Ma) from Spain (and newly reported here from Switzerland), or it may have arisen from a graticulacean alga such as Graticula, dating from mid-Silurian times (c. 427-435 Ma). Current data also suggest that Heydrichia is more likely to have arrived in Brazil from Central Atlantic waters than from higher latitude South Atlantic waters. This implies that currently living species in southern Africa probably arose later from ancestors further equatorward in the South Atlantic, although confirming studies are needed. All non-fossil species of Heydrichia are known only from the southern hemisphere.- Handle-ID: http://hdl.handle.net/2042/53736</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 08 May 2014 00:56:32 GMT</pubDate>
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<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 6</title>
 <link>http://paleopolis.rediris.es/cg/1406/</link>
 <description>Fernando Nu&#241;ez-Useche, Josep Anton Moreno-Bedmar, Miguel Company &#038; Ricardo Barrag&#225;n.- A negative carbon isotope excursion within the Dufrenoyia furcata Zone: proposal for a new episode for chemo-stratigraphic correlation in the Aptian.- In this work we discuss a proposed updated division of the C7 isotope segment of Menegatti et al. (1998). The new standard division of the segment C7 is based on a revision of published Barremian-Aptian carbon isotope curves from stratigraphic sections of the Prebetic Domain in Spain. It includes four distinct isotopic subunits labeled C7a to C7d, with a characteristic negative carbon isotope excursion at the base of the segment and which correlates with the Dufrenoyia furcata ammonite Zone. The negative excursion is recognized on a regional extent, and the term Intra-Furcata Negative Excursion (IFNE) is proposed to identify it. We provide possible sites correlatable with the IFNE in both the Old and New worlds, which suggest its potential use as an even global chemostratigraphic marker for the Aptian record.- Handle-ID: http://hdl.handle.net/2042/53734</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 08 May 2014 00:51:52 GMT</pubDate>
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<item>
 <title>Carnets de Geologie [Notebooks on Geology], Publication, vol. 14, n&#186; 5</title>
 <link>http://paleopolis.rediris.es/cg/1405/</link>
 <description>Francis Am&#233;dro &#038; Bertrand Matrion.- L'&#233;tage Albien dans sa r&#233;gion-type, l'Aube (France) : une synth&#232;se dans un contexte s&#233;dimentaire global.- Le d&#233;partement de l'Aube est la r&#233;gion-type de l'&#233;tage Albien cr&#233;&#233; par d'Orbigny (1842). Deux formations sont reconnues dans les faci&#232;s argileux ou &#034;Gault&#034; auct. du stratotype : les Argiles t&#233;gulines de Courcelles (82 m) surmont&#233;es des Marnes de Brienne (43 m). La limite entre les deux formations est d&#233;finie au sommet d'un niveau indur&#233; (hardground L'&#201;tape) ais&#233;ment identifiable &#224; la fois sur le terrain et en sondages. La r&#233;gion-type de l'&#233;tage Albien est particuli&#232;rement int&#233;ressante en raison de l'&#233;paisseur exceptionnelle des faci&#232;s argileux (plus de 120 m), une situation unique dans le bassin anglo-parisien. Aujourd'hui, 82 % de la succession lithologique sont connus pr&#233;cis&#233;ment gr&#226;ce &#224; 16 affleurements. Dans deux intervalles &#233;pais respectivement de 33 m et 28,50 m, une suite lithologique composite continue est construite &#224; l'aide de coupes qui se suivent et se relaient, corr&#233;l&#233;es l'une &#224; l'autre sur le terrain &#224; l'aide de niveaux rep&#232;res. Six faci&#232;s successifs sont d&#233;crits : dans les Argiles t&#233;gulines de Courcelles et du bas vers le haut : 1 - lit de nodules gr&#233;so-phosphat&#233;s ; 2 - argiles silteuses ; 3 - argiles et bancs calcaires ; dans les Marnes de Brienne : 4 - marnes argileuses ; 5 - gaize ; 6 - marnes argileuses. &#192; une &#233;chelle plus fine, une rythmicit&#233; est d&#233;montr&#233;e dans la s&#233;dimentation. Elle se traduit dans les Argiles t&#233;gulines de Courcelles par des cycles pluri-d&#233;cim&#233;triques d&#233;butant par des niveaux silteux et limit&#233;s au sommet par des surfaces perfor&#233;es. Dans les Marnes de Brienne, les cycles, m&#233;triques (sauf dans la gaize o&#249; ils sont d&#233;cim&#233;triques), montrent des alternances de marne argileuse gris fonc&#233; et de marne gris p&#226;le annon&#231;ant les craies rythm&#233;es du C&#233;nomanien. Ces couplets correspondent probablement &#224; des cycles de pr&#233;cession des &#233;quinoxes (20 ka). Treize &#233;v&#233;nements &#224; caract&#232;re lithologique (lits de nodules phosphat&#233;s, fonds durcis, niveaux riches en sable quartzeux et glauconie) et &#233;cologiques (horizons caract&#233;ris&#233;s par l'abondance momentan&#233;e d'un certain nombre de fossiles) sont identifi&#233;s dans la suite stratigraphique. Ces niveaux rep&#232;res sont tr&#232;s utiles pour des corr&#233;lations pr&#233;cises &#224; travers le bassin. Une comparaison est propos&#233;e entre les faci&#232;s sableux de l'Yonne et les faci&#232;s argileux de l'Aube. La continuit&#233; de plusieurs lits de nodules phosphat&#233;s est d&#233;montr&#233;e depuis l'Yonne au sud-ouest jusqu'&#224; l'Aube et le Perthois au nord-est, sur une distance sup&#233;rieure &#224; 130 km. Ces niveaux rep&#232;res sont interpr&#233;t&#233;s comme des surfaces d'inondation de cycles eustatiques de 3e ordre. Enfin, une &#233;tude d&#233;taill&#233;e de la lithologie, compl&#233;t&#233;e par une analyse des faunes d'ammonites et d'inoc&#233;rames, est utilis&#233;e pour une interpr&#233;tation s&#233;quentielle. Le r&#233;sultat est l'identification de huit s&#233;quences eustatiques de 3e ordre dans la moiti&#233; sup&#233;rieure des Argiles de Courcelles et les Marnes de Brienne, dont deux nouvelles s&#233;quences index&#233;es AL 5a et AL 6a. The Albian Stage in its type area, the Aube (France): a synthesis in a global sedimentary context.- The Aube department is the type locality of the Albian stage created by d'Orbigny (1842). Two formations are recognised in the clay facies (the &#034;Gault&#034; auct.) of the stratotype, the Argiles t&#233;gulines de Courcelles (82 m), which is overlain by the Marnes de Brienne (43 m). The boundary between the two formations is defined at the top of an indurated bed (hardground L'&#201;tape) that is readily identifiable, both in the field, and from boreholes. The type area of the Albian stage is of great interest because of the size of the clay facies (more than 120 m) unique in the Anglo-Paris basin. Today, 82 % of the lithological succession is documented accurately from 16 outcrops. In two intervals of respectively 33 m and 28.50 m thick, composite sections are made of overlapping sections which are correlated in the field with the help of lithological marker beds. Six successive facies are described: in the Argiles t&#233;gulines de Courcelles and from bottom to top: 1 - phosphatic nodules bed; 2 - silty clays; 3 - clays and limestone beds; in the Marnes de Brienne: 4 - clay marls; 5 - gaize; 6 - clay marls. On a smaller scale, a decimetre to metre-scale rhythmicity can be identified in the sedimentation. This is reflected in the Argiles t&#233;gulines de Courcelles by pluri-decimetric cycles that start with a silty level and are bounded at the top by a bored surface. In the Marnes de Brienne, the metric cycles (except for the gaize where they are decimetric) exhibit alternating dark grey clay marl and a pale grey marl that herald the rhythmic chalks of the Cenomanian. Individual couplets probably represent the precession cycles (20 kyr). On the other hand, 13 lithoevents as phosphatic nodules beds, hardgrounds, glauconitic and sandy beds and ecoevents characterised by the brief abundance of some fossils. These marker beds are very useful for fine correlations across the basin. A comparison is proposed between sandy units of Yonne and clay facies of Aube. The continuity of several phosphatic nodules beds is shown from Yonne in the South West to Aube and Perthois in the North East, that is a distance exceeding 130 km. These marker beds are interpreted as Flooding Surfaces of 3rd-order cycles. Finally, a detailed study of the lithology, complemented with the analysis of the ammonite and inoceramid faunas, is used for a depositional sequence interpretation. As a result, eight sequences are identified in the upper half of the Argiles t&#233;gulines de Courcelles and in the Marnes de Brienne in the type area of the Albian stage, including two new sequences indexed AL 5a and AL 6a.- Handle-ID: http://hdl.handle.net/2042/53732</description>
 <category>Publication</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Thu, 08 May 2014 00:42:26 GMT</pubDate>
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<item>
 <title>Carnets de Geologie [Notebooks on Geology], Article, vol. 14, n&#186; 4</title>
 <link>http://paleopolis.rediris.es/cg/1404/</link>
 <description>Vicent Vicedo, Jos&#233; Antonio Berlanga &#038; Josep Serra-Kiel.- Paleocene larger foraminifera from the Yucat&#225;n Peninsula (SE Mexico).- The larger foraminifera found in the material from the Chichen Itz&#225; Formation of Campeche (SE Mexico) were studied in detail. The architectural analyses allow the description of four new species and a new genus, namely, two agglutinated conical foraminifera, Coskinolina yucatanensis n.sp. and Pseudofallotella drobneae n.gen. n.sp., one new alveolinid, Borelis hottingeri n.sp., and one new rotaliid, Dictyoconoides boneti n.sp. The larger foraminifera of the Chichen Itz&#225; Formation are distributed across two different associations: one includes Pseudofallotella drobneae, Neotaberina sp., Rhabdorites sp., Borelis hottingeri, Dictyoconoides boneti, Kathina sp., Miscellaneidae, Ranikothalia soldadensis and Hexagonocyclina cristensis, while the other assemblage is composed of Coskinolina yucatensis, Fallotella causae, Rhabdorites sp., Borelis floridanus and Cincoriola cf. ovoidea. Some of these genera, including Neotaberina and Dictyoconoides, are cited in the Caribbean paleobioprovince for the first time in this paper. The first association is dated as Thanetian (SBZ 3? to SBZ 4) by the presence of Ranikothalia soldadensis. Though the age of the second association remains uncertain, a similar age has been inferred.- Handle-ID: http://hdl.handle.net/2042/53527</description>
 <category>Article</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Mon, 17 Mar 2014 18:16:47 GMT</pubDate>
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<item>
 <title>Journal of GEOsciences, Volume 59, Issue 1 (2014)</title>
 <link>http://www.jgeosci.org/issue-59-1</link>
 <description>* Foreword to the thematic set on 'Melilitic, alkaline and calc-alkaline lamprophyric rocks. Centenary celebration of the first description of polzenites by K.H. Scheumann'.- Rapprich V &#038; Holub FV&#060;br /&#062;* Revision of Scheumann's classification of melilitic lamprophyres and related melilitic rocks in light of new analytical data.- Ulrych J, Adamovic J, Krmicek L, Ackerman L &#038; Balogh K&#060;br /&#062;* The camptonites in the multiple intrusion of Platja Fonda (Girona, NE Spain): mechanisms of intrusion and geochemistry.- Esteve S, Enrique P &#038; Galan G&#060;br /&#062;* Late Variscan calc-alkaline lamprophyres in the Krupka ore district, Eastern Krusne hory/Erzgebirge: their relationship to Sn-W mineralization.- Stemprok M, Dolejs D &#038; Holub FV&#060;br /&#062;* Temporal relationships between Mg-K mafic magmatism and catastrophic melting of the Variscan crust in the southern part of Velay Complex (Massif Central, France).- Couzinie S, Moyen J-F, Villaros A, Paquette J-L, Scarrow JH &#038; Marignac C&#060;br /&#062;* Phlogopite/matrix, clinopyroxene/matrix and clinopyroxene/phlogopite trace-element partitioning in a calc-alkaline lamprophyre: new constrains from the Krizanovice minette dyke (Bohemian Massif).- Krmicek L, Halavinova M, Romer RL, Vasinova Galiova M &#038; Vaculovic T</description>
 <category>Journal</category>
 <author>jgeosci@jgeosci.org</author>
<pubDate>Sun, 2 March 2014 00:00:00 GMT</pubDate>
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<item>
 <title>Carnets de Geologie [Notebooks on Geology], Letter, vol. 14, n&#186; 3</title>
 <link>http://paleopolis.rediris.es/cg/1403/</link>
 <description>Francesco Sciuto.- Acanthocythereis colini nomen novum for A. reticulata Sciuto, 2014.- In Sciuto (2014), a new species, Acanthocythereis reticulata, was described from the Upper Pliocene sediments of NE Sicily and belonging to the Family Trachyleberididae Sylvester-Bradley, 1948- Handle-ID: http://hdl.handle.net/2042/53523</description>
 <category>Letter</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Fri, 28 Feb 2014 18:36:23 GMT</pubDate>
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<item>
 <title>Carnets de Geologie [Notebooks on Geology], Article, vol. 14, n&#186; 2</title>
 <link>http://paleopolis.rediris.es/cg/1402/</link>
 <description>Robert W. Scott.- A Cretaceous chronostratigraphic database: construction and applications.- Timing and rates of tectonic events, evolutionary processes, and oceanographic and paleoclimatic changes must be based on high-precision numerical age calibration of stages defined in Global Stratotype and Section Points (GSSPs). The Cretaceous Chronostratigraphic Database (CRETCSDB3) is an objective, testable database that calibrates select Cretaceous events and enables high-resolution chronostratigraphic correlations. CRETCSDB3 is a compilation of more than 3500 taxa and marker beds in nearly 300 published sections calibrated to a mega-annum (Ma) scale. The database spans the Jurassic/Cretaceous and the Cretaceous/Paleogene boundaries. Construction of CRETCSDB3 began by plotting bioevents in the Kalaat Senan, Tunisia, Cenomanian-Turonian section to the 1989 time scale. The sedimentology, sequence stratigraphy, and biostratigraphy of this section were precisely documented and stage boundaries defined biostratigraphically. Additional sections with radiometrically dated beds were graphed to constrain the accuracy of the numerical scale. Ranges of first and last occurrences are calibrated to mega-annums of Cretaceous stages defined by GSSPs or reference sections. This database serves as a look-up table for interpolation and age calibration of other stratigraphic sections. The age ranges of some taxa and marker beds are preliminary and may be extended as new sections are added to the database. CRETCSDB3 tested the numeric age calibration of the Albian/Cenomanian boundary. This boundary in North Texas accurately correlates with the GSSP in France by ammonites, planktic foraminifers and dinoflagellates. This stage boundary in North Texas correlates with the 97.88&#177;0.69 Ma Clay Spur Bentonite in Wyoming by sequence stratigraphy and cosmopolitan dinoflagellates. The inconsistency between this age and the current 100.5 Ma date of the 2012 Geologic Time Scale remains to be evaluated independently.- Handle-ID: http://hdl.handle.net/2042/53522</description>
 <category>Article</category>
 <author>carnetsdegeologie@hotmail.com</author>
 <pubDate>Fri, 28 Feb 2014 18:31:20 GMT</pubDate>
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<item>
<title>Oceanologia No. 56(1)/2014</title>
<link>http://iopan.gda.pl/oceanologia/56_1.html</link>
<description>*Simple statistical formulas for estimating biogeochemical properties of suspended particulate matter in the southern Baltic Sea potentially useful for optical remote sensing applications .- Wo&#378;niak  S&#322;awomir B. &#060;br /&#062;*Biometry and reproductive biology of Pseudonereis anomala Gravier 1901 (Polychaeta: Nereididae) on the Alexandria coast, Egypt .-  Hamdy Rasha, Dorgham Mohamed Moussa,El-Rashidy Hoda Hassan, Atta Manal Mohamed &#060;br /&#062;*Principal Component and Cluster Analysis for determining diversification of bottom morphology based on bathymetric profiles from Brepollen (Hornsund, Spitsbergen).- Moskalik Mateusz, T&#281;gowski Jaros&#322;aw, Grabowiecki Piotr, &#379;ulichowska Monika &#060;br /&#062;*Sediment deposition and accumulation rates determined by sediment trap and<sup>210</sup>Pb isotope methods in the Outer Puck Bay (Baltic Sea).- Szmytkiewicz Angelika, Zalewska Tamara &#060;br /&#062;*Effect of accessory pigment composition on the absorption characteristics of a dinoflagellate bloom in a coastal embayment.- Vijayan Anil Kumar, Somayajula Srikanth Ayyala &#060;br /&#062;*Non-native crab Rhithropanopeus harrisii (Gould, 1984) - a new component of the benthic communities in the Gulf of Gda&#324;sk (southern Baltic Sea).- Hegele-Drywa Joanna, Normant Monika &#060;br /&#062;*Evadne anonyx G. O. Sars, 1897 - the first record of this Ponto-Caspian cladoceran in the Gulf of Gda&#324;sk (Baltic Sea). -  Bielecka Luiza, Mudrak-Cegio&#322;ka Stella, Kalarus Marcin &#060;br /&#062;*First record of a new alien species Limnodrilus cervix Brinkhurst, 1963 (Annelida, Clitellata) in the Vistula Lagoon (Southern Baltic Sea). - Dumnicka El&#380;bieta, Jab&#322;o&#324;ska-Barna Izabela, Rychter Agata &#060;br /&#062;*First record of brown colouration of Atlantic cod (Gadus morhua, L.) from the North Sea. - Rybczyk Agnieszka, Czerniejewski Przemys&#322;aw, Rokicka-Praxmajer Joanna</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Tue, 28 Jan 2014 09:49:33 GMT</pubDate>
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<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, vol. 14, n&#186; 1</title>
<link>http://paleopolis.rediris.es/cg/1401/</link>
<description>Francesco Sciuto.- Ostracods of the Upper Pliocene - Pleistocene Punta Mazza succession (NE Sicily) with special focus on the Family Trachyleberididae Sylvester-Bradley, 1948, and description of a new species.- The ostracod associations of the Upper Pliocene-Pleistocene sedimentary succession out-cropping at Punta Mazza (Milazzo, Sicily NE) have been investigated. The ostracod fauna is often well-preserved and well-diversified: there 42 species belonging to 24 genera have been found. The association consists almost exclusively of bathyal taxa such as Bythocypris obtusata (Sars), B. bosquetiana (Brady), Henryhowella ex H. profunda Bonaduce et al. group, Quasibuntonia radiatopora (Seguenza), Retibythere (Bathybythere) scaberrima Brady, Pseudocythere caudata Sars and Bythocythere mylaensis Sciuto. Also, the Krithe group is well-represented with Krithe compressa (Seguenza) and K. pernoides (Bornemann). Further taxa such as Cytheropteron testudo Sars are rare. Almost all species, especially those belonging to Trachyleberididae Sylvester-Bradley are described, illustrated and commented on, including a new species, Acanthocythereis reticulata n.sp., found in the lower part of the section in Upper Pliocene sediment, is proposed as new. Finally, a specimen belonging to the genus Quasibuntonia Ruggieri is currently given in open nomenclature.- 1401.- Handle-ID: http://hdl.handle.net/2042/****</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Sat, 25 Jan 2014 14:05:28 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A09</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A09/</link>
<description>Olev Vinn &#038; Mark A. Wilson.- Silurian cornulitids of Estonia (Baltica).- Seven species of cornulitids are systematically described from the Silurian of Saaremaa and Hiiumaa islands, Estonia. There are three species of cornulitids in the Rhuddanian, three in the Sheinwoodian, single species in the Gorstian and Ludfordian, and three species in the Pridoli. Cornulitids have a facies range from pelletal limestones of shoal environments to deeper ramp marls. Endobiotic cornulitid symbionts occur in stromatoporoids found in shoal and open shelf zones. Gregarious aggregates are restricted to the limestones of the open shelf zone possibly because of higher nutrient levels in open shelf zone waters as compared to those of the deeper ramp. Unattached free forms are especially common in offshore deeper ramp marls presumably due to their adaption to life on a soft bottom. Solitary attached forms occur in all facies zones where cornulitids are present. Because the life modes of cornulitids are closely associated with particular facies zones, they are useful tools for paleoecological reconstructions.- CG2013_A09.- Handle-ID: http://hdl.handle.net/2042/53034</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Wed, 25 Dec 2013 12:02:34 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Book, CG2013_B02</title>
<link>http://paleopolis.rediris.es/cg/CG2013_B02/</link>
<description>Zbigniew Kota&#324;ski.- Anisian Dasycladales from Upper Silesia and adjacent regions.- Anisian Dasycladales (calcareous algae) from the Diplopora Dolomite of the Upper Silesia and adjacent regions of S Poland are revised. All previously reported taxa are critically reviewed and illustrated. New paleontological samples were collected from 74 outcrops and from 45 boreholes. The abundant material includes both specimens visible on fractured rock surfaces and thin-sectioned ones; 24 species of Dasycladales are identified, including three new species: Oligoporella chrzanowensis n.sp., Physoporella polonoandalusica n.sp., and Salpingoporella krupkaensis n.sp. Best-preserved specimens are illustrated in 39 plates. The identified species were compared with Alpine and Carpathian forms of stratigraphic importance. Six Dasycladalean local horizons are defined. The Pelsonian-Illyrian boundary occurs in the middle part of the Diplopora Dolomite. Its uppermost part, despite the presence of Diplopora annulata, belongs to the Illyrian, not to the Fassanian, as also corroborated by conodont correlations. The peculiar state of preservation (internal moulds and double tubes) is discussed; it is due to early syngenetic dolomitisation. The palaeoenvironment of the algae is determined as sublittoral. Dasycladales flourished upon a peri-Tethyan carbonate platform, widely connected with the Alpine-Carpathian seas. Five palaeoecological assemblages are recognized, differing in their bathymetric and turbulence conditions, and living in marine shoals and shallow basins separating them. The Upper Silesian platform was separated from the hypersaline Germanic Basin of the Middle Muschelkalk by banks and oolite and bioclastic barriers, blocking dispersal of marine biota. A wide connection existed with the Alpine-Carpathian seas, allowing immigration of High-Tatric, Kri&#382;na and even South Alpine flora to the Upper Silesian Carbonate Platform.- CG2013_B02.- Handle-ID: http://hdl.handle.net/2042/53036</description>
<category>Book</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Wed, 25 Dec 2013 11:50:58 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L07</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L07/</link>
<description>Bruno Granier.- Dissocladella hauteriviana Masse in Masse et al., 1999 (non Masse, 1976), another lower Urgonian Dasycladalean alga revisited.- First ascribed to the Triploporellacean genus Dissocladella (Pia in Rao &#038; Pia, 1936), the species D. hauteriviana Masse in Masse et al., 1999, was supposedly characterized by a thallus bearing whorls of laterals each consisting of a stumpy primary with a tuft of four slim secondaries at its top. A restudy of the laterals proves that they split, not only once, but several times, and stepwisely decrease in diameter. The species is re-ascribed to the Family Thyrsoporellaceae in a new combination to the genus Deloffrella Granier &#038; Michaud, 1987. Its known stratigraphic range is rather short (Late Valanginian-earliest Barremian). In addition, it disappears earlier than its companion Polyphysacean alga, i.e., Clypeina paucicalcarea (Conrad, 1970), and its geographical distribution is broader, which makes it a good index fossil for lower Urgonian carbonate platform series.- CG2013_L07.- Handle-ID: http://hdl.handle.net/2042/53035</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Wed, 25 Dec 2013 11:48:36 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, Jean-Paul_Colin</title>
<link>http://paleopolis.rediris.es/cg/Jean-Paul_Colin/</link>
<description>Pierre Carbonel, Maria Cristina Cabral &#038; Dan L. Danielopol.- Obituary notice: Jean-Paul Colin.- Jean-Paul Colin (1948 - 2013) passed away at the end of this summer and his departure is a cruel loss for our community, not only as a scientist of international repute, but also as an outstanding organizer and, for a number of us, as a good friend. Following his PhD degree in micropaleontology from the University of Paris VI in 1973, he spent his entire career in the exploration branch of the oil industry, first with EXXON in Houston and B&#232;gles from 1974 to 1989, and then with ESSO REP in B&#232;gles from 1989 to 2000. Initially, he worked on biostratigraphical micropaleontology, and later focused on ostracods, sequence stratigraphy and stratigraphic syntheses. From 2000 and until recently, he provided consultancy to several oil companies. Jean-Paul Colin also gave training courses to PETROBRAS and PETROCI, as well as workshops in Brazil (UNISINOS, S&#227;o Leopoldo; University of Bras&#237;lia; PETROBRAS, Rio de Janeiro) and Portugal (University of Lisbon). He taught applied micropaleontology in ENSEGID Bordeaux 3 and was a Research Associate at the University of Lisbon. His scientific work has never slowed down. Throughout his career and into retirement, he published or contributed to more than 300 publications and presentations at international conferences. Many times he was invited as a member for thesis juries in France and abroad. He was an internationally recognized authority on ostracods, especially those of the Cretaceous, but also had an excellent knowledge of the whole group throughout the post-Paleozoic time interval. Jean-Paul Colin was a great field and laboratory naturalist and as a scientific partner was always open to often lively discussion. His enthusiasm for the ostracods was huge and it was a pleasure to discuss with him. His special qualities were: that he was familiar with all the relevant literature; he had an encyclopedic memory; he always knew where to find the necessary literature and was able to comment on the specimens under investigation. He quickly identified the interesting and unusual subjects to be published. Being a very friendly person, he helped ostracodologists worldwide who went to him with questions, particularly the young. Besides these activities, Jean-Paul Colin was member of the editorial board of several international journals: A Stereo Atlas of Ostracod Shells, African Geosciences Journal, Annales de Pal&#233;ontologie, Open Journal of Paleontology, and the Paleontology Journal. He was associate editor of Carnets de G&#233;ologie and Revue de Micropal&#233;ontologie. Jean-Paul Colin was a member of several scientific societies (Soci&#233;t&#233; G&#233;ologique de France, The Micropalaeontological Society, The International Paleontologists Association, Association des Pal&#233;ontologues Fran&#231;ais, Association des G&#233;ologues du Sud-Ouest). He was also actively involved for many years in the life of the R&#233;serve Naturelle de Saucats-La Br&#232;de (Natural Reserve of Saucats-La Br&#232;de). After 2000, he was the soul and inspiration for the meetings of the Ostracodologistes de Langue fran&#231;aise that he opened up beyond the French-speaking community. He will remain a focal point for the community and a facilitator hard to replace.- Jean-Paul_Colin.- Handle-ID: http://hdl.handle.net/2042/51849</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 22 Nov 2013 11:29:07 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L06</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L06/</link>
<description>Josep A. Moreno-Bedmar &#038; G&#233;rard Delanoy.- About the generic attribution of Megatyloceras casei Humphrey, 1949 (Ammonoidea, Ancyloceratina), from the Aptian of Mexico.- In the present work we review the generic attribution of the Mexican ammonoid species Megatyloceras casei Humphrey, 1949, through a careful examination of the holotype housed in the University of Michigan and with reference to new biostratigraphic data from the type locality. We assign here this species to the subfamily Cheloniceratinae and to the genus Epicheloniceras Casey, 1954.- CG2013_L06.- Handle-ID: http://hdl.handle.net/2042/51826</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 11 Nov 2013 11:00:43 GMT</pubDate>
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<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A08</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A08/</link>
<description>Christian C. Emig.- Daniel &#338;hlert (1849-1920) : biographie scientifique et bibliographie.- Daniel &#338;hlert a fait toute sa carri&#232;re &#224; Laval (Mayenne, France). Ses fonctions de biblioth&#233;caire de la ville de Laval, puis de conservateur des mus&#233;es d'arch&#233;ologie et d'histoire naturelle de Laval, lui laissaient une ind&#233;pendance pour se consacrer &#224; la pal&#233;ontologie et &#224; la g&#233;ologie. Avec son &#233;pouse Pauline, ils partageaient leurs recherches entre des &#233;tudes sur le terrain dans la Mayenne et la Sarthe et de longs s&#233;jours &#224; Paris, surtout &#224; la Sorbonne. Les travaux d'&#338;hlert ont principalement port&#233; sur les peuplements des mers pal&#233;ozo&#239;ques du Maine, de l'Anjou et du Cotentin. &#338;hlert se consacra plus particuli&#232;rement &#224; l'&#233;tude des Crino&#239;des, des Trilobites et surtout des Brachiopodes. Dans leur collection, d&#233;pos&#233;e au Mus&#233;e des Sciences &#224; Laval, on compte plus de 20 nouveaux genres avec plus de 150 nouvelles esp&#232;ces d'invert&#233;br&#233;s. L'&#339;uvre g&#233;ologique et stratigraphique d'&#338;hlert est largement originale ; elle ne concerne pratiquement que des terrains pal&#233;ozo&#239;ques des d&#233;partements de la Mayenne et de la Sarthe et, accessoirement, des d&#233;partements de l'Orne et de l'Ille-et-Vilaine. En 1884, il devient collaborateur au Service de la Carte g&#233;ologique de France. Une centaine de publications s'&#233;chelonnent de 1877 pour s'arr&#234;ter brutalement en 1911 avec le d&#233;c&#232;s de son &#233;pouse Pauline. La liste de tous ses travaux est fournie.- CG2013_A08.- Handle-ID: http://hdl.handle.net/2042/51825</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 11 Nov 2013 11:00:07 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A07</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A07/</link>
<description>Bruno Granier, Rajka Radoi&#269;i&#263; &#038; Katica Drobne.- Revision of the Jesse Harlan Johnson Collection. Part 1. Some fossil Dasycladales from Guatemala.- This first report is a revision of fossil calcareous green algae (Dasycladales) described from the Upper Cretaceous and Paleocene series of Guatemala. Among other things in their 1965 paper J.H. Johnson and H.V. Kaska introduced three new species originally referred to the genera Acroporella, Cylindroporella, and Cymopolia. One species, which has previously been referred to the genus Cylindroporella, is a foraminifer.- CG2013_A07.- Handle-ID: http://hdl.handle.net/2042/51824</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 11 Nov 2013 11:03:55 GMT</pubDate>
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<item>
<title>Oceanologia No. 55(4)/2013</title>
<link>http://iopan.gda.pl/oceanologia/55_4.html</link>
<description>* Synoptic conditions governing upwelling along the Polish Baltic coast.- Bednorz Ewa, P&#243;&#322;rolniczak Marek , Czernecki Bartosz &#060;br /&#062;* Seasonal variability in the Baltic Sea level.- Stramska Ma&#322;gorzata, Kowalewska-Kalkowska Halina, &#346;wirgo&#324; Marek &#060;br /&#062;* Acoustic noise generation under plunging breaking waves.- Klusek Zygmunt, Lisimenka Aliaksandr &#060;br /&#062;* Impact of ship-borne nitrogen deposition on the Gulf of Finland ecosystem: an evaluation.- UUrmas Raudsepp, Jaan Laanemets, Ilja Maljutenko, Marke Hongisto, Jukka-Pekka Jalkanen &#060;br /&#062;* Impact of the inflow of Vistula river waters on the pelagic zone in the Gulf of Gda&#324;sk.- Wielgat-Rychert Magdalena, Ameryk Anetta, Jarosiewicz Anna, Kownacka Janina, Rychert Krzysztof, Krzysztof, Zalewski Mariusz, Agatova Alina, Lapina Natalia, Torgunova Nadezhda &#060;br /&#062;* Rotifer trophic state indices as ecosystem indicators in brackish coastal waters.- Gutkowska Agnieszka, Paturej Ewa, Kowalska Ewa &#060;br /&#062;* Epibiotic mites associated with the invasive Chinese mitten crab &#060;i&#062;Eriocheir sinensis&#060;/i&#062; - new records of Halacaridae from Poland.- Normant Monika, Zawal Andrzej, Chatterjee Tapas, W&#243;jcik Dagmara &#060;br /&#062;* Effect of temperature on two reef-building corals &#060;i&#062;Pocillopora damicornis&#060;/i&#062; and &#060;i&#062;P. verrucosa&#060;/i&#062; in the Red Sea.- Al-Sofyani Abdulmohsin A., Floos Yahya A.M.&#060;br /&#062;* Sedimentation from suspension and sediment accumulation rate in the River Vistula prodelta, Gulf of Gda&#324;sk (Baltic Sea).- Damrat Mateusz, Zaborska Agata, Zaj&#261;czkowski Marek &#060;br /&#062;* Geochemical and acoustic evidence for the occurrence of methane in sediments of the Polish sector of the southern Baltic Sea.- Brodecka Aleksandra, Majewski Piotr, Bola&#322;ek Jerzy, Klusek Zygmunt &#060;br /&#062;* Dinoflagellate cyst distribution in recent sediments along the south-east coast of India.- Narale Dhiraj Dhondiram, Patil S. Jagadish, Chandrashekar Arga Anil</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Fri, 08 Nov 2013 12:11:55 GMT</pubDate>
</item>

<item>
<title>Journal of GEOsciences, Volume 58, Issue 3 (2013)</title>
<link>http://www.jgeosci.org/issue-58-3</link>
<description>* Memorial of Professor Zdenek Pouba (1922-2011).- Pertold Z&#060;br /&#062;
* Foreword to the thematic set on 'Mineral deposits and ore-forming processes in spatial, temporal and geodynamic context (a special issue in honor of Professor Zdenek Pouba)'.- Dolejs D, Jelinek E &#038; Johan Z&#060;br /&#062;* Platinum-group elements (PGE) and their principal carriers in metal-rich black shales: an overview with a new data from Mo-Ni-PGE black shales (Zunyi region, Guizhou Province, south China).- Pasava J, Zaccarini F, Aiglsperger T &#038; Vymazalova A&#060;br /&#062;* Origin of mantle peridotites from the Vourinos Ophiolite Complex, Greece, as deduced from Cr-spinel morphological and chemical variations.- Kapsiotis AN&#060;br /&#062;* Age and tectonic setting of magmatic sulfide Cu-Ni mineralization in the Eastern Tianshan Orogenic Belt, Xinjiang, Central Asia.- Han C, Xiao W, Zhao G, Su B, Ao S, Zhang J &#038; Wan B&#060;br /&#062;* SIMS U-Pb zircon dating and Re-Os isotopic analysis of the Hulu Cu-Ni deposit, eastern Tianshan, Central Asian Orogenic Belt, and its geological significance.- Han C, Xiao W, Zhao G, Su B-X, Sakyi PA, Ao S, Wan B, Zhang J &#038; Zhang Z&#060;br /&#062;* Geology and Re-Os molybdenite geochronology of the Kuriskova U-Mo deposit (Western Carpathians, Slovakia).- Kohut M, Trubac J, Novotny L, Ackerman L, Demko R, Bartalsky B &#038; Erban V&#060;br /&#062;* Fluid inclusion study of the Horni Luby cinnabar deposit, Saxothuringian Zone, Bohemian Massif: clues for the metamorphic remobilization of mercury.- Velebil D &#038; Zacharias J</description>
<category>Journal</category>
<author>jgeosci@jgeosci.org</author>
<pubDate>Tue, 15 Oct 2013 00:00:00 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 55(3)/2013</title>
<link>http://iopan.gda.pl/oceanologia/55_3.html</link>
<description>
* Anthropogenic radionuclides 137Cs and 90Sr in the southern Baltic Sea ecosystem.- Zalewska Tamara, Supli&#324;ska Maria &#060;br /&#062;* Activation of the operational ecohydrodynamic model (3D CEMBS) - the hydrodynamic part.- Dzierzbicka-G&#322;owacka Lidia, Janecki Maciej, Nowicki Artur, Jakacki Jaromir &#060;br /&#062;* Activation of the operational ecohydrodynamic model (3D CEMBS) - the ecosystem module.- Dzierzbicka-G&#322;owacka Lidia, Janecki Maciej, Nowicki Artur, Jakacki Jaromir &#060;br /&#062;* Observations of the aerosol particle number concentration in the marine boundary layer over the south-eastern Baltic Sea.- By&#269;enkien&#279; Steigvil, Ulevicius Vidmantas, Prokop&#269;iuk Nina, Jasinevi&#269;ien&#279; Dalia &#060;br /&#062;* UV absorption reveals mycosporine-like amino acids (MAAs) in Tatra mountain lake phytoplankton:.- Ficek Dariusz, Dera Jerzy, Wo&#378;niak Bogdan&#060;br /&#062;* Vulnerability assessment of southern coastal areas of Iran to sea level rise: evaluation of climate change impact:.- Goharnejad Hamid, Shamsai Abolfazl, Hosseini Seyed Abbas &#060;br /&#062;* Short-term changes in specific conductivity in Polish coastal lakes (Baltic Sea basin).- Cie&#347;li&#324;ski Roman &#060;br /&#062;* Comparison of the impacts of climate change and anthropogenic disturbances on the El Arish coast and seaweed vegetation after ten years in 2010, North Sinai, Egypt.- El Shoubaky Gihan Ahmed &#060;br /&#062;* Upwelling dynamics in the Baltic Sea studied by a combined SAR/infrared satellite data and circulation model analysis.- Gurova Evgenia, Lehmann Andreas, Ivanov Andrei &#060;br /&#062;* Red tides of the dinoflagellate Noctiluca scintillans associated with eutrophication in the Sea of Marmara (the Dardanelles, Turkey).- Turkoglu Muhammet &#060;br /&#062;* Protozoa in a stressed area of the Egyptian Mediterranean coast of Damietta, Egypt.- Dorgham Mohamed Moussa, El-Tohamy Wael Salah, Aziz Nagwa Elsayed Abdel, El-Ghobashi Ahmed, Qin Jian G. &#060;br /&#062;* Biocontamination of the western Vistula Lagoon (south-eastern Baltic Sea, Poland).- Jab&#322;o&#324;ska-Barna Izabela, Rychter Agata, Kruk Marek</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Fri, 02 Aug 2013 11:48:08 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L05</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L05/</link>
<description>Patricia Vallati.- Paleotropical pollen grains from the Neuqu&#233;n Group, Patagonia, Argentina.- This paper discusses the presence of elater-bearing pollen grains and other characteristic paleotropical palynomorphs in the mid to Late Cretaceous Neuqu&#233;n Group at the El Zampal locality, south of Mendoza Province, Argentina. The elaterates characterize the equatorial paleofloristic province in the Albian-Cenomanian. The species Elateroplicites africaensis is present in the pollen assemblage recovered from the lower section of the Huincul Formation, a basal unit of the studied Neuqu&#233;n Group. It represents the first record of elater-bearing pollen grains in Argentina and marks their southernmost extension. Other conspicuous paleotropical elements recorded in different lithostratigraphic units of the Neuqu&#233;n Group include gymnospermous polyplicate pollen grains and angiosperm pollen, including two species of the periporate pollen genus Cretacaeiporites and the triporate pollen species Confossia vulgaris. The paleobiogeographic and biostratigraphic significance of the paleotropical sporomorph record in the Cretaceous palynofloras of the Neuqu&#233;n Group at El Zampal is herein discussed.- CG2013_L05.- Handle-ID: http://hdl.handle.net/2042/51218</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 02 Aug 2013 10:37:31 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L04</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L04/</link>
<description>Felix Schlagintweit, Ioan I. Bucur, Koorosh Rashidi &#038; Behnam Saberzadeh.- Praeorbitolina claveli n.sp. (benthic Foraminifera) from the Lower Aptian sensu lato (Bedoulian) of Central Iran.- The new orbitolinid foraminifer, Praeorbitolina claveli n.sp., is described from the Lower Aptian (Bedoulian) of Central Iran. It is characterized by an eccentric embryonic apparatus displaying both a subdivided subembryonic zone and a deuteroconch. The Barremian-Aptian orbitolinid association of this area has a typical northern Tethyan character (e.g., "association &#224; Valserina" of Cherchi and Schroeder, 1973).- CG2013_L04.- Handle-ID: http://hdl.handle.net/2042/51217</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 02 Aug 2013 10:35:09 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A06</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A06/</link>
<description>Pierre-Olivier Mojon, Antonio Musolino, Stefan Bucher &#038; Bernard Claude.- Nouvelles donn&#233;es sur les ammonites du Valanginien - Hauterivien de la r&#233;gion stratotypique de Neuch&#226;tel (Jura suisse) : implications biostratigraphiques.- De nouvelles donn&#233;es sur les ammonites du Valanginien sup&#233;rieur - Hauterivien inf&#233;rieur apportent des pr&#233;cisions sur le sch&#233;ma biostratigraphique du Cr&#233;tac&#233; inf&#233;rieur de la r&#233;gion stratotypique de Neuch&#226;tel (Jura suisse). Ainsi, Stoicoceras pitrei (Busnardo, 1966) du Calcaire roux limoniteux peut &#234;tre rapport&#233;e &#224; la partie sup&#233;rieure de la biozone &#224; Saynoceras verrucosum (sous-zone &#224; Karakaschiceras pronecostatum) du Valanginien sup&#233;rieur. Dans l'Hauterivien inf&#233;rieur, Olcostephanus (O.) variegatus Paquier, 1900, de la partie sup&#233;rieure des Marnes bleues d'Hauterive et Saynella cf. clypeiformis (d'Orbigny, 1841) des Marnes d'Uttins (sommet de la partie inf&#233;rieure de la Pierre jaune de Neuch&#226;tel) &#233;largissent l'extension de la biozone &#224; Lyticoceras nodosoplicatum par rapport &#224; la biozone &#224; Crioceratites loryi indiqu&#233;e par Saynella neocomiensis (Baumberger, 1905) et un unique sp&#233;cimen de Crioceratites cf. gr. loryi (Sarkar, 1955) trouv&#233; en 1907.- CG2013_A06.- Handle-ID: http://hdl.handle.net/2042/51216</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 02 Aug 2013 10:26:18 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A05</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A05/</link>
<description>Philippe Quereilhac.- &#201;tude de l'esp&#232;ce Ochetoceras (Ochetoceras) canaliculatum (de Buch, 1831) (Oxfordien moyen, Zone &#224; Transversarium).- L'esp&#232;ce Ochetoceras (Ochetoceras) canaliculatum (de Buch, 1831), discut&#233;e ici, est certainement la plus repr&#233;sentative de la Zone &#224; Transversarium (Oxfordien moyen) dans le Domaine t&#233;thysien (Province m&#233;diterran&#233;enne). Elle appara&#238;t dans la Sous-Zone &#224; Parandieri et semble dispara&#238;tre dans la Sous-Zone &#224; Stenocycloides (Oxfordien sup&#233;rieur, base de la Zone &#224; Bifurcatus). Elle est fortement repr&#233;sent&#233;e dans les populations ammonitiques et poss&#232;de une large extension g&#233;ographique. Une analyse montre qu'elle se trouve toujours associ&#233;e &#224; des esp&#232;ces d&#233;nomm&#233;es Ochetoceras (Ochetoceras) hispidum [M] (Oppel, 1863) et Glochiceras (Glochiceras) subclausum [m] (Oppel, 1863) ; de nombreux auteurs ont pens&#233; depuis longtemps qu'il s'agissait d'une seule et m&#234;me esp&#232;ce. Ces trois "esp&#232;ces" sont donc r&#233;unies sous la d&#233;nomination Ochetoceras (Ochetoceras) canaliculatum (de Buch, 1831) : le macroconque correspondant aux "morphes" canaliculatum et hispidum est polymorphique, &#233;voluant d'un p&#244;le mince vers un p&#244;le &#233;pais ; quant au "morphe" subclausum, il s'agit d'un microconque dimorphique sexuel. - CG2013_A05.- Handle-ID: http://hdl.handle.net/2042/51215</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 02 Aug 2013 10:22:25 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A04</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A04/</link>
<description>Bruno Granier, Bernard Clavel, Michel Moullade, Robert Busnardo, Jean Charollais, Guy Tronchetti &#038; Pierre Desjacques.- L'Estellon (Baronnies, France), a "Rosetta Stone" for the Urgonian biostratigraphy.- Shallow-water assemblages of transported ("freshly reworked") bioclasts (mainly orbitolinids and dasycladales) are observed in the deeper facies of the "Vocontian Trough" (SE France). There these benthic assemblages can be directly correlated with ammonite zones. These new finds give an Early Barremian age to the earliest record of Palorbitolina lenticularis as well as those of four so-called "typical Early Aptian" representatives of the genus Orbitolinopsis. Actually most orbitolinid species recorded from the Late Barremian interval are now found present in Lower Barremian strata at L'Estellon. Some currently used correlation schemes for the Urgonian platforms, that are based on partial stratigraphic distribution ranges for the orbitolinids, --and consequently derived conclusions and hypotheses-- require at least in-depth revisions when they are not definitively refuted- CG2013_A04.- Handle-ID: http://hdl.handle.net/2042/51213</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 22 Jul 2013 17:26:45 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A03</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A03/</link>
<description>Robert Busnardo, Bruno Granier, Bernard Clavel &#038; Jean Charollais.- Ammonitofaune du Barr&#233;mien de la coupe de L'Estellon (Baronnies, SE France) : r&#233;sultats biostratigraphiques pr&#233;liminaires.- L'&#233;tude de l'ammonitofaune de la coupe de L'Estellon (d&#233;partement de la Dr&#244;me, France) permet de dater les &#233;pisodes de la s&#233;dimentation gravitaire dans ce secteur de la "Fosse vocontienne". Ils couvrent pratiquement l'ensemble du Barr&#233;mien, depuis la Zone &#224; Nicklesi jusqu'&#224; celle &#224; Giraudi. Nous n'y avons pas caract&#233;ris&#233; de res&#233;dimentation b&#233;doulienne, la "barre b&#233;doulienne" auct. correspondant au Barr&#233;mien terminal.- CG2013_A03.- Handle-ID: http://hdl.handle.net/2042/51212</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 22 Jul 2013 17:21:33 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L03</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L03/</link>
<description>Olev Vinn.- Cornulitid tubeworms from the Ordovician of eastern Baltic.- Nine species of cornulitids are systematically described here from the Ordovician of Estonia. The earliest species, Cornulites semiapertus, appears in the late Darriwilian (Middle Ordovician), the next two species appear in the Sandbian and there are a further six new species in the Katian, which indicates a rapid diversification of cornulitids in the Late Ordovician of Baltica. All the studied cornulitids from the Ordovician of Estonia occur in relatively shallow-water normal-marine sediments of a carbonate platform. The cornulitids are found encrusting mostly brachiopod shells (both syn vivo and post mortem).- CG2013_L03.- Handle-ID: http://hdl.handle.net/2042/51214</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Mon, 22 Jul 2013 17:16:38 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 55(2)/2013</title>
<link>http://iopan.gda.pl/oceanologia/55_2.html</link>
<description>
* Sea salt in aerosols over the southern Baltic. Part 1. The generation and transportation of marine particles.- Lewandowska Anita Urszula, Falkowska Lucyna Miros&#322;awa &#060;br /&#062;
* Sea salt in aerosols over the southern Baltic. Part 2. The neutralizing properties of sea salt and ammonia.- Lewandowska Anita Urszula, Falkowska Lucyna Miros&#322;awa &#060;br /&#062;* Recent multiyear trends in the Baltic Sea level .- Stramska Ma&#322;gorzata, Chudziak Natalia &#060;br /&#062;* Herbivory on macro-algae affects colonization of beach-cast algal wrack by detritivores but not its decomposition .- Eereveld Philip, H&#252;bner Lena, Schaefer Gesa , Zimmer Martin &#060;br /&#062;* Annual spatio-temporal variation of the euphotic depth in the SW-Finnish archipelago, Baltic Sea .- Luhtala Hanna, Tolvanen Harri, Kalliola Risto &#060;br /&#062;* Seasonal proximate and fatty acid variations of some seaweeds from the northeastern Mediterranean coast .- Polat Sevim, Ozogul Yesim &#060;br /&#062;* Seven years of macroinfauna monitoring at Ladeira beach (Corrubedo Bay, NW Spain) after the<i>Prestige</i> oil spill .- Junoy Juan, Castellanos Carolina, Vi&#233;itez Jos&#233; Manuel, Riera Rodrigo &#060;br /&#062;* Interannual variability in the population dynamics of the main mesozooplankton species in the Gulf of Gda&#324;sk (southern Baltic Sea): Seasonal and spatial distribution .- Dzierzbicka-G&#322;owacka Lidia, Kalarus Marcin, &#379;mijewska Maria Iwona &#060;br /&#062;* Seasonal variations in the biochemical composition of some common seaweed species from the coast of Abu Qir Bay, Alexandria, Egypt.- Khairy Hanan M., El-Shafay Shimaa M. &#060;br /&#062;* Spatial distribution of biological and physical sediment parameters in the western Gulf of Gda&#324;sk .- Katarzyna Huzarska &#060;br /&#062;* Optical water types of the Nordic Seas and adjacent areas .- Aas Eyvind , Niels Kristian H&#248;jerslev, Jo H&#248;kedal3, Kai S&#248;rensen4</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Mon, 27 May 2013 09:09:48 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Memoir, CG2013_M02</title>
<link>http://paleopolis.rediris.es/cg/CG2013_M02/</link>
<description>Michel Delamette &#038; Jean Albert Remy.- Mammif&#232;res et reptiles priaboniens du massif de Plat&#233; (Haute-Savoie, France).- Une lentille de calcaire marneux indur&#233; &#224; la base de la s&#233;rie tertiaire des Grandes Plati&#232;res (massif de Plat&#233;, Haute-Savoie) a livr&#233; la plus importante collection de restes de vert&#233;br&#233;s actuellement connue dans le Pal&#233;og&#232;ne des Alpes occidentales. Les mammif&#232;res ongul&#233;s sont repr&#233;sent&#233;s par 35 dents attribu&#233;es &#224; 9 taxons (4 p&#233;rissodactyles et 5 artiodactyles). Cette faune para&#238;t contemporaine de celle de La D&#233;bruge (niveau MP 18), dat&#233;e d'environ -35,5 MA. Le nouveau site, d&#233;nomm&#233; gisement des Perdrix, est situ&#233; stratigraphiquement &#224; 20-35 m en-dessous de celui dans lequel Weidmann et al. (1991) avaient mis au jour quelques restes de mammif&#232;res qu'ils ont attribu&#233;s au niveau MP 20. La nouvelle faune est donc plus ancienne d'environ 1,5 MA. Sa composition et la nature palustre du d&#233;p&#244;t sugg&#232;rent que les animaux concern&#233;s vivaient dans un environnement vari&#233; comportant des espaces bois&#233;s &#224; proximit&#233; de zones humides mar&#233;cageuses.- CG2013_M02.- Handle-ID: http://hdl.handle.net/2042/50056</description>
<category>Memoir</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Fri, 17 May 2013 17:13:00 GMT</pubDate>
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<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A02</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A02/</link>
<description>G&#233;rard Delanoy, Josep Anton Moreno-Bedmar, Jos&#233; J. Ruiz &#038; Domingo Tol&#243;s Ll&#225;dser.- Xerticeras gen. nov., a new genus of micromorphic heteromorph ammonite (Ancyloceratina, Ancyloceratidae) from the lower Aptian of Spain.- Biostratigraphical and paleontological studies of lower Aptian material from the Eastern Iberian Chain (Spain) have revealed the presence of a new genus of micromorphic heteromorph ammonite: Xerticeras gen. nov. (type species: Xerticeras salasi sp. nov.). This new taxon comes from the Deshayesites deshayesi and Dufrenoya furcata ammonite zones. The size difference observed in the population is considered due to sexual dimorphism.- CG2013_A02.- Handle-ID: http://hdl.handle.net/2042/49315</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Wed, 24 Apr 2013 17:09:37 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L02</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L02/</link>
<description>Olev Vinn &#038; Mark A. Wilson.- An event bed with abundant Skolithos burrows from the late Pridoli (Silurian) of Saaremaa (Estonia).- Abundant Skolithos burrows are here described from a possible regressive event bed at Ohesaare cliff (Pridoli), Saaremaa, Estonia. The vertical, cylindrical burrows are identified as Skolithos rather than Trypanites because they intercept and bypass rather than cut bioclasts in the limestone matrix. The absence of encrustation on the upper bedding surface also is evidence that these traces are soft-sediment burrows rather than hardground borings. We interpret this intensive bioturbation by Skolithos-producing organisms as an indicator of a shallow water paleoenvironment with high hydrodynamic energy.- CG2013_L02.- Handle-ID: http://hdl.handle.net/2042/49316</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Wed, 24 Apr 2013 17:03:33 GMT</pubDate>
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<item>
<title>Journal of GEOsciences, Volume 58, Issue 1 (2013)</title>
<link>http://www.jgeosci.org/issue-58-1</link>
<description>* Editorial.- Janousek V&#060;br /&#062; * Garnet pyroxenite in the Biskupice peridotite, Bohemian Massif: anatomy of a Variscan high-pressure cumulate.- Medaris GLJr, Jelinek E, Beard BL, Valley JW, Spicuzza MJ &#038; Strnad L&#060;br /&#062; * Geological position, mineral assemblages and contamination of granitic pegmatites in the Moldanubian Zone, Czech Republic; examples from the Vlastejovice region.- Novak M, Kadlec T &#038; Gadas P&#060;br /&#062; * Genesis of chromitites from Korydallos, Pindos Ophiolite Complex, Greece, based on spinel chemistry and PGE-mineralogy.- Kapsiotis AN&#060;br /&#062; * Note on the formula of brunogeierite and the first bond-valence parameters for Ge2+.- Cempirek J &#038; Groat LA</description>
<category>Journal</category>
<author>jgeosci@jgeosci.org</author>
<pubDate>Mon, 15 Apr 2013 00:00:00 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Article, CG2013_A01</title>
<link>http://paleopolis.rediris.es/cg/CG2013_A01/</link>
<description>Jacques Rey, Josep Anton Moreno-Bedmar, Michel Bilotte &#038; Ricardo Mart&#237;nez.- Nouvelles donn&#233;es pal&#233;ontologiques et stratigraphiques au passage Aptien &#8211; Albien dans les Pyr&#233;n&#233;es ari&#233;geoises (France).- La d&#233;couverte d'ammonites du passage Aptien - Albien (biozones &#224; Hypacanthoplites jacobi et &#224; Leymeriella tardefurcata), dans la s&#233;rie urgonienne de la couverture du massif de l'Arize invalide l'attribution ant&#233;rieure au Clansay&#233;sien inf&#233;rieur propos&#233;e sur des arguments pal&#233;ontologiques non contraints.- CG2013_A01.- Handle-ID: http://hdl.handle.net/2042/48733</description>
<category>Article</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Thu, 28 Feb 2013 16:45:33 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Letter, CG2013_L01</title>
<link>http://paleopolis.rediris.es/cg/CG2013_L01/</link>
<description>Bruno Granier.- Heteroporella ? paucicalcarea (Conrad, 1970), an Urgonian Dasycladalean alga revisited.- When the species Heteroporella ? paucicalcarea (Conrad, 1970) was erected it was left in open nomenclature. Later on new combinations were introduced but did not meet a general agreement among paleophycologists. Considering the current acception of the Dasycladalean families, we ascribe it to the Family Polyphysaceae and subsequently to the genus Clypeina (Michelin, 1845). Its known stratigraphic range is rather brief (Late Hauterivian-Early Barremian), which makes it a good index fossil in Urgonian carbonate platform series. Its geographical distribution is apparently restricted to Western Europe (France, Spain and Switzerland).- CG2013_L01.- Handle-ID: http://hdl.handle.net/2042/48737</description>
<category>Letter</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Thu, 28 Feb 2013 16:38:08 GMT</pubDate>
</item>

<item>
<title>Carnets de Geologie [Notebooks on Geology], Book, CG2013_B01</title>
<link>http://paleopolis.rediris.es/cg/CG2013_B01/</link>
<description>Bruno Granier &#038; Nestor J. Sander.- The XXIst Century (the 100th Anniversary) Edition of the "New studies on Triassic Siphoneae verticillatae" by Julius von Pia.- This 21st century edition of Julius von Pia's 1912 memoir entitled "Neue Studien &#252;ber die triadischen Siphoneae verticillatae" is brought to you by B. Granier (editing, photomicrographs) and N.J. Sander (translation). The artwork is due to A. Lethiers and B. Granier. The original 24 text-figures and 7 plates [II-VIII] were converted into 125 discrete photomicrographs, 5 figures and 56 videos.- CG2013_B01.- Handle-ID: http://hdl.handle.net/2042/48735</description>
<category>Book</category>
<author>carnetsdegeologie@hotmail.com</author>
<pubDate>Thu, 28 Feb 2013 16:40:57 GMT</pubDate>
</item>

<item>
<title>Oceanologia No. 55(1)/2013</title>
<link>http://iopan.gda.pl/oceanologia/55_1.html</link>
<description>
* Relationships between inherent optical properties in the Baltic Sea for application to the underwater imaging problem.- Levin Iosif, Darecki Miros&#322;aw, Sagan S&#322;awomir, Radomyslskaya Tamara &#060;br /&#062;* Validation of SeaWiFS and MODIS Aqua/Terra aerosol products in coastal regions of European marginal seas.- M&#233;lin Fr&#233;d&#233;ric, Zibordi Giuseppe, Carlund Thomas, Holben Brent N., Stefan Sabina &#060;br /&#062;* Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea.- Stramska Ma&#322;gorzata, Zuzewicz Agata &#060;br /&#062;* Comparison of primary productivity estimates in the Baltic Sea based on the DESAMBEM algorithm with estimates based on other similar algorithms.- Stramska Ma&#322;gorzata, Zuzewicz Agata &#060;br /&#062;* Surface wave generation due to glacier calving .- Massel Stanis&#322;aw R., Przyborska Anna &#060;br /&#062;* Modelling flow in the porous bottom of the Barents Sea shelf.- Massel Stanis&#322;aw R. &#060;br /&#062;* Influence of landfast ice on the hydrography and circulation of the Baltic Sea coastal zone .- Merkouriadi Ioanna, Lepp&#228;ranta Matti &#060;br /&#062;* Habitat modelling limitations - Puck Bay, Baltic Sea - a case study.- W&#281;s&#322;awski Jan Marcin, Kryla-Straszewska Lucyna, Piwowarczyk Joanna, Urba&#324;ski Jacek, Warzocha Jan, Kotwicki Lech, W&#322;odarska-Kowalczuk Maria, Wiktor J&#243;zef &#060;br /&#062;* Spatio-temporal variation of microphytoplankton in the upwelling system of the south-eastern Arabian Sea during the summer monsoon of 2009.- Thomas Lathika Cicily, Padmakumar K. B., Smitha B. R., Devi C. R. Asha, Nandan S. Bijoy, Sanjeevan V. N. &#060;br /&#062;* Summer mesozooplankton community of Moller Bay (Novaya Zemlya Archipelago, Barents Sea).- Dvoretsky Vladimir G., Dvoretsky Alexander G. &#060;br /&#062;* Seasonal fluxes of phosphate across the sediment-water interface in Edku Lagoon, Egypt.- Khalil Mona Kh., Rifaat Ahmed E. &#060;br /&#062;* First records of polychaetes new to Egyptian Mediterranean waters.- Dorgham Mohamed Moussa, Hamdy, Rasha, El-RashidyHoda Hassan, Atta Manal Mohamed &#060;br /&#062;* Compensatory growth of the bloom-forming dinoflagellate<i>Prorocentrum donghaiense</i> induced by nitrogen stress.- Cai Zhuoping, Duan Shunshan, Zhu Honghui</description>
<category>Journal</category>
<author>sabina@iopan.gda.pl</author>
<pubDate>Tue, 26 Feb 2013 13:04:47 GMT</pubDate>
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