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<dc:title>Enviromagnetic study of Late Quaternary environmental evolution in Lower Volga loess sequences, Russia</dc:title>
<dc:creator>Költringer, Chiara</dc:creator>
<dc:creator>Stevens, Thomas</dc:creator>
<dc:creator>Bradák, Balázs</dc:creator>
<dc:creator>Almqvist, Bjarne</dc:creator>
<dc:creator>Kurbanov, Redzhep</dc:creator>
<dc:creator>Snowball, Ian</dc:creator>
<dc:creator>Yarovaya, Sofya</dc:creator>
<dc:subject>Lower Volga loess</dc:subject>
<dc:subject>Caspian Sea</dc:subject>
<dc:subject>Environmental magnetism</dc:subject>
<dc:subject>Magnetic proxies</dc:subject>
<dc:subject>Atelian regression</dc:subject>
<dc:subject>Last glaciation</dc:subject>
<dc:description>The late Quaternary development of the Lower Volga region of Russia is characterized by an alternating influence of marine&#xd;
and continental environments resulting from fluctuations in Caspian Sea level during the last glaciation. However, sediments&#xd;
deposited under continental conditions have received very little research attention compared to the under- and overlying&#xd;
marine deposits, such that even their origin is still in debate. Detailed magnetic mineralogical analyses presented here&#xd;
show clear similarities to loess. The results suggest that climate during the time of loess deposition, the Atelian regression&#xd;
(27–80 ka, MIS 4–3), was dry and cool, similar to the modern-day Northern Caspian lowland. The magnetic properties&#xd;
recorded in the loess-paleosol sequences of the Lower Volga also point to short episodes of potentially more humid and&#xd;
warmer climate during the late Atelian. The new findings in regard to the local Caspian climate and environmental evolution&#xd;
support decreased river discharge from the Russian Plain and Siberian Plain as the dominant factor causing the low Caspian&#xd;
sea level stand during the Atelian, although local-regional climate changes might have had an additional influence.</dc:description>
<dc:date>2021-11-04T12:13:55Z</dc:date>
<dc:date>2021-11-04T12:13:55Z</dc:date>
<dc:date>2021-09</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:identifier>0033-5894</dc:identifier>
<dc:identifier>http://hdl.handle.net/10259/6099</dc:identifier>
<dc:identifier>10.1017/qua.2020.73</dc:identifier>
<dc:language>eng</dc:language>
<dc:relation>Quaternary Research. 2021, V. 103, p. 49 - 73</dc:relation>
<dc:relation>https://doi.org/10.1017/qua.2020.73</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/VR//2017-03888/SE</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/RSF//19-77-10077/RU</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/RFBR//18-00-00470/RU</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/Junta de Castilla y León//BU235P18//Análisis arqueomagnéticos en materiales arqueológicos quemados de edad holocena y pleistocena</dc:relation>
<dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
<dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
<dc:rights>Atribución 4.0 Internacional</dc:rights>
<dc:publisher>Cambridge University Press</dc:publisher>
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