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<title>Enviromagnetic study of Late Quaternary environmental evolution in Lower Volga loess sequences, Russia</title>
<creator>Költringer, Chiara</creator>
<creator>Stevens, Thomas</creator>
<creator>Bradák, Balázs</creator>
<creator>Almqvist, Bjarne</creator>
<creator>Kurbanov, Redzhep</creator>
<creator>Snowball, Ian</creator>
<creator>Yarovaya, Sofya</creator>
<subject>Lower Volga loess</subject>
<subject>Caspian Sea</subject>
<subject>Environmental magnetism</subject>
<subject>Magnetic proxies</subject>
<subject>Atelian regression</subject>
<subject>Last glaciation</subject>
<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.</description>
<date>2021-11-04</date>
<date>2021-11-04</date>
<date>2021-09</date>
<type>info:eu-repo/semantics/article</type>
<identifier>0033-5894</identifier>
<identifier>http://hdl.handle.net/10259/6099</identifier>
<identifier>10.1017/qua.2020.73</identifier>
<language>eng</language>
<relation>Quaternary Research. 2021, V. 103, p. 49 - 73</relation>
<relation>https://doi.org/10.1017/qua.2020.73</relation>
<relation>info:eu-repo/grantAgreement/VR//2017-03888/SE</relation>
<relation>info:eu-repo/grantAgreement/RSF//19-77-10077/RU</relation>
<relation>info:eu-repo/grantAgreement/RFBR//18-00-00470/RU</relation>
<relation>info:eu-repo/grantAgreement/Junta de Castilla y León//BU235P18//Análisis arqueomagnéticos en materiales arqueológicos quemados de edad holocena y pleistocena</relation>
<rights>http://creativecommons.org/licenses/by/4.0/</rights>
<rights>info:eu-repo/semantics/openAccess</rights>
<rights>Atribución 4.0 Internacional</rights>
<publisher>Cambridge University Press</publisher>
</thesis></metadata></record></GetRecord></OAI-PMH>