<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Karkani, A.</style></author><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Giaime, M.</style></author><author><style face="normal" font="default" size="100%">Marriner, N.</style></author><author><style face="normal" font="default" size="100%">Maroukian, H.</style></author><author><style face="normal" font="default" size="100%">Morhange, C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Late Holocene palaeogeographical evolution of Paroikia Bay (Paros Island, Greece).</style></title><secondary-title><style face="normal" font="default" size="100%">Comptes Rendus Geoscience</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/pii/S163107131830052X</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">350</style></volume><pages><style face="normal" font="default" size="100%">202-211</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span&gt;&lt;span&gt;Although there is rich evidence for human occupation of Paros’ coastline, there is a dearth of data with regards to the evolution of the island's seaboard&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/paleoenvironments&quot; title=&quot;Learn more about Paleoenvironments&quot;&gt;palaeoenvironments&lt;/a&gt;. In this paper, we use sedimentological and palaeontological proxies of late&amp;nbsp;&lt;/span&gt;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/holocene&quot; title=&quot;Learn more about Holocene&quot;&gt;Holocene&lt;/a&gt;&amp;nbsp;coastal deposits from lagoonal environment to reconstruct the evolution of&amp;nbsp;&lt;/span&gt;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/coastal-landscape&quot; title=&quot;Learn more about Coastal Landscape&quot;&gt;coastal landscapes&lt;/a&gt;&lt;span&gt;&amp;nbsp;in Paroikia Bay (Paros Island, Greece). A semi-enclosed&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/lagoon&quot; title=&quot;Learn more about Lagoon&quot;&gt;lagoon&lt;/a&gt;&lt;span&gt;&amp;nbsp;existed in the northeastern part of Paroikia from at least 2915–2551 BC, which was gradually infilled after around 780–436 BC. Although it was not possible to chronologically constrain the timing of the infill, it is most likely relatively young, indicating anthropogenic effects. A correlation of our chronostratigraphic data with archaeological remains and tidal notches in the study area suggests that the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/subsidence&quot; title=&quot;Learn more about Subsidence&quot;&gt;subsidence&lt;/a&gt;&amp;nbsp;observed on Paros Island is linked to long-term subsidence in combination with vertical seismic displacements.&lt;/span&gt;&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record></records></xml>