<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Pavlopoulos, K.</style></author><author><style face="normal" font="default" size="100%">Vassilopoulos, A.</style></author><author><style face="normal" font="default" size="100%">Triantafyllou, M.</style></author><author><style face="normal" font="default" size="100%">Vouvalidis, K.</style></author><author><style face="normal" font="default" size="100%">Syrides, G.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Palaeoenvironmental evolution of Vigla western Naxos (Cyclades, Greece), depositional environment and sea level changes in Upper Holocene.</style></title><secondary-title><style face="normal" font="default" size="100%">European Geosciences Union, General Assembly</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2-7 May</style></date></pub-dates></dates><pub-location><style face="normal" font="default" size="100%">Vienna, Austria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;The study area of Vigla coastal zone is located at the W coast of Naxos, the largest island of Cycladic plateau.&amp;nbsp;The study of sea-land interactions during Holocene in relation to the eustatic sea level oscillations as well as the&amp;nbsp;geomorphologic observations and analyses on deposited sediments, aims to reveal the paleogeographic evolution&amp;nbsp;of the landscape and its impact to the overall cultural development of the area.&amp;nbsp;A geomorphological mapping of the coastal area along with the drilling of three boreholes has been accomplished.&amp;nbsp;Moreover, a micro faunal analysis has been performed. Five samples of plant material, chart coal and shells were&amp;nbsp;dated using AMS and Conventional radiocarbon techniques providing temporal control of the sediments.&amp;nbsp;Sea level rise along with sea-land interactions to the landscape evolution and the transgression of sea in 5000 BP&amp;nbsp;have been verified.&lt;/div&gt;</style></abstract></record></records></xml>