<?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%">Ratopoulou, M.</style></author><author><style face="normal" font="default" size="100%">Rousakis, G.,</style></author><author><style face="normal" font="default" size="100%">Triantaphyllou, M.,</style></author><author><style face="normal" font="default" size="100%">Gogou, A.,</style></author><author><style face="normal" font="default" size="100%">Bouloubassi, I.,</style></author><author><style face="normal" font="default" size="100%">Dimiza, M.,</style></author><author><style face="normal" font="default" size="100%">Parinos, C.,</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%">A paleoceanographic approach of MIS5e interglacial deposits at the western margin of Cyclades plateau</style></title><secondary-title><style face="normal" font="default" size="100%">11th Panhellenic Symposium on Oceanography and Fisheries</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://okeanos-dspace.hcmr.gr/handle/123456789/2707?show=full</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Proceeding</style></volume><pages><style face="normal" font="default" size="100%">1001-1004</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Paleoceanographic proxies, such as marine micropaleontology, sedimentology and organic geochemistry have&lt;br&gt;been performed in the sediment record of SK-3 gravity core (total length 217cm, water depth 249m) in order to&lt;br&gt;provide possible determination of late interglacial-Holocene the paleoenvironmental changes, at the south&lt;br&gt;western margin of Cyclades plateau in the SW Aegean Sea. The sediment core exhibits two sapropels layer; the&lt;br&gt;first one is associated with sapropel S1. The second sapropelic layer which we focus on represents anoxic&lt;br&gt;conditions during the high sea-level warm event associated with sapropel S5 deposition.&lt;/p&gt;</style></abstract></record></records></xml>