<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athanasiou, M.,</style></author><author><style face="normal" font="default" size="100%">Triantaphyllou, M.,</style></author><author><style face="normal" font="default" size="100%">Dimiza, M.,</style></author><author><style face="normal" font="default" size="100%">Gogou, A.,</style></author><author><style face="normal" font="default" size="100%">Roussakis, G.,</style></author><author><style face="normal" font="default" size="100%">Lykousis, V.,</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Paleoceanographic-Paleoclimatic variability during S1 sapropel deposition in the NE Mediterranean Sea: Calcareous nannoplankton implications</style></title><secondary-title><style face="normal" font="default" size="100%">10th Symposium on Oceanography and Fishery</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://users.uoa.gr/~mdimiza/pdf/proceedings%208.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Proceeding</style></volume><pages><style face="normal" font="default" size="100%">10 pp. (in Greek)</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Detailed quantitative analyses of calcareous nannofossils/coccolithophores performed on the deep sea deposits of the north eastern Mediterranean Sea; two gravity core from North Aegean Sea (SL 152) and south Cretan continental margin (HCMR 2/22), with a focus on the regional expression of sapropel S1 deposition. In both sites, higher values of &lt;em&gt;Florisphaera profunda&lt;/em&gt;, &lt;em&gt;Helicosphaera&lt;/em&gt; spp., &lt;em&gt;Braarudosphaera bigelowii&lt;/em&gt; and the concomitant increase of stratification S index, within sapropel intervals can be interpreted as the result of elevated marine production and enhanced inflow of fresh water input during the S1 period. A series of cooling events detected within the S1 depositional interval, may be linked to outbursts of cold northerly air masses and relevant pulses in the deep-intermediate water ventilation that caused the temporary cessation of S1 deposition between 7.8-7.5 ka uncal. BP in North Aegean and 8.1-7.8 ka uncal. BP at the south Cretan margin. During this interval the peak of &lt;em&gt;Braarudosphaera bigelowii&lt;/em&gt;, the decrease in abundance of &lt;em&gt;Florisphaera profunda&lt;/em&gt;, &lt;em&gt;Helicosphaera&lt;/em&gt; spp., &lt;em&gt;Rhabdosphaera&lt;/em&gt; spp. and a general increase in NPP are related to a shoaling of the nutricline and higher production in the surface layer.</style></abstract></record></records></xml>