<?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%">Polidorou, M.</style></author><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">DRINIA, H.</style></author><author><style face="normal" font="default" size="100%">Tsourou, T.</style></author><author><style face="normal" font="default" size="100%">Salomon, F.</style></author><author><style face="normal" font="default" size="100%">Blue, L.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Palaeogeography and geomorphological evolution of Akrotiri Salt Lake, Lemesos, Cyprus</style></title><secondary-title><style face="normal" font="default" size="100%">RCG2019 “Geomorphology of Climatically and Tectonically Sensitive Areas”</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><pub-location><style face="normal" font="default" size="100%">Athens - Greece</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;Akrotiri Salt Lake is located 5km west of the city of Lemesos, in the southern-most part of the&amp;nbsp;island of Cyprus. The palaeogeographic evolution of the Akrotiri Salt Lake presents a great&amp;nbsp;scientific interest, especially during the Holocene where the eustatic movements combined&amp;nbsp;with local active tectonics and climate changes have developed a unique geomorphological&amp;nbsp;environment. The Salt Lake, today a closed lagoon, which is depicted in Venetian maps&amp;nbsp;(Bordon AD 1528) as being connected to the sea, can provide evidence of the geological&amp;nbsp;settings and landscape evolution of the area. In this study, we investigate the development of&amp;nbsp;Akrotiri Salt Lake through a series of cores which penetrated the Holocene sediment&amp;nbsp;sequence. Sedimentological, micropaleontological (benthic foraminifera and ostracods)&lt;/div&gt;
&lt;div&gt;analyses and geochronological studies performed on deposited sediments, identifying the&amp;nbsp;complexity of the evolution of the Salt Lake and the progressive change of the area from&amp;nbsp;maritime space to an open bay and finally to a closed Salt Lake.&lt;/div&gt;</style></abstract></record></records></xml>