<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sergio R. Dillenburg</style></author><author><style face="normal" font="default" size="100%">Eduardo G. Barboza</style></author><author><style face="normal" font="default" size="100%">Maria Luiza C. C. Rosa</style></author><author><style face="normal" font="default" size="100%">Felipe Caron</style></author><author><style face="normal" font="default" size="100%">Rodrigo Cancelli</style></author><author><style face="normal" font="default" size="100%">Cristiane B. Santos-Fischer</style></author><author><style face="normal" font="default" size="100%">Renato P. Lopes</style></author><author><style face="normal" font="default" size="100%">MATIAS DO NASCIMENTO RITTER</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Sedimentary records of Marine Isotopic Stage 3 (MIS 3) in southern Brazil</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1007/s00367-019-00574-2</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">40</style></volume><pages><style face="normal" font="default" size="100%">1099 - 1108</style></pages><isbn><style face="normal" font="default" size="100%">1432-1157</style></isbn><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;In this paper, a reinterpretation of the older 14C ages of the Pleistocene substrate of the Holocene barrier-lagoon system of three coastal localities in southern Brazil is presented (Hermenegildo, Cassino, and Curumim). Sedimentological, geochronological, palynological, and diatom analyses of a sedimentary deposit formed in an estuarine/shallow marine environment are examined. This sedimentary deposit is presently found between 22 and 25 m depth below sea level in the Pinheira coastal plain. Results from all studied sites indicate that the deposit was formed under a former sea level of Marine Isotopic Stage 3 (MIS 3) that may have oscillated in the study region between 5 and 23 m depth below present sea level, from 36.2 to 47.7 ka. These results are reinforced by studies of nearby sites, including southeast Brazil. The Pleistocene substrate of the Holocene lagoonal-barrier system, at depths lower than 5 m below sea level, seems to correspond to sedimentary deposits of the Pleistocene barrier formed during MIS 5, while at depths greater than 5 m below sea level, they might correspond to sedimentary deposits that were formed during the relative high sea levels of MIS 3.&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">6</style></issue><notes><style face="normal" font="default" size="100%">n/a</style></notes></record></records></xml>