Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal

Abstract Understanding the past dynamics of large-scale atmospheric systems is crucial for our knowledge of the palaeoclimate conditions in Europe. Southeastern Europe currently lies at the border between Atlantic, Mediterranean, and continental climate zones. Past changes in the relative influence...

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Autores principales: Igor Obreht, Ulrich Hambach, Daniel Veres, Christian Zeeden, Janina Bösken, Thomas Stevens, Slobodan B. Marković, Nicole Klasen, Dominik Brill, Christoph Burow, Frank Lehmkuhl
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Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/d78f704ac11445e3b19c75087c395815
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spelling oai:doaj.org-article:d78f704ac11445e3b19c75087c3958152021-12-02T15:04:51ZShift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal10.1038/s41598-017-06285-x2045-2322https://doaj.org/article/d78f704ac11445e3b19c75087c3958152017-07-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-06285-xhttps://doaj.org/toc/2045-2322Abstract Understanding the past dynamics of large-scale atmospheric systems is crucial for our knowledge of the palaeoclimate conditions in Europe. Southeastern Europe currently lies at the border between Atlantic, Mediterranean, and continental climate zones. Past changes in the relative influence of associated atmospheric systems must have been recorded in the region’s palaeoarchives. By comparing high-resolution grain-size, environmental magnetic and geochemical data from two loess-palaeosol sequences in the Lower Danube Basin with other Eurasian palaeorecords, we reconstructed past climatic patterns over Southeastern Europe and the related interaction of the prevailing large-scale circulation modes over Europe, especially during late Marine Isotope Stage 3 (40,000–27,000 years ago). We demonstrate that during this time interval, the intensification of the Siberian High had a crucial influence on European climate causing the more continental conditions over major parts of Europe, and a southwards shift of the Westerlies. Such a climatic and environmental change, combined with the Campanian Ignimbrite/Y-5 volcanic eruption, may have driven the Anatomically Modern Human dispersal towards Central and Western Europe, pointing to a corridor over the Eastern European Plain as an important pathway in their dispersal.Igor ObrehtUlrich HambachDaniel VeresChristian ZeedenJanina BöskenThomas StevensSlobodan B. MarkovićNicole KlasenDominik BrillChristoph BurowFrank LehmkuhlNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-10 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Igor Obreht
Ulrich Hambach
Daniel Veres
Christian Zeeden
Janina Bösken
Thomas Stevens
Slobodan B. Marković
Nicole Klasen
Dominik Brill
Christoph Burow
Frank Lehmkuhl
Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
description Abstract Understanding the past dynamics of large-scale atmospheric systems is crucial for our knowledge of the palaeoclimate conditions in Europe. Southeastern Europe currently lies at the border between Atlantic, Mediterranean, and continental climate zones. Past changes in the relative influence of associated atmospheric systems must have been recorded in the region’s palaeoarchives. By comparing high-resolution grain-size, environmental magnetic and geochemical data from two loess-palaeosol sequences in the Lower Danube Basin with other Eurasian palaeorecords, we reconstructed past climatic patterns over Southeastern Europe and the related interaction of the prevailing large-scale circulation modes over Europe, especially during late Marine Isotope Stage 3 (40,000–27,000 years ago). We demonstrate that during this time interval, the intensification of the Siberian High had a crucial influence on European climate causing the more continental conditions over major parts of Europe, and a southwards shift of the Westerlies. Such a climatic and environmental change, combined with the Campanian Ignimbrite/Y-5 volcanic eruption, may have driven the Anatomically Modern Human dispersal towards Central and Western Europe, pointing to a corridor over the Eastern European Plain as an important pathway in their dispersal.
format article
author Igor Obreht
Ulrich Hambach
Daniel Veres
Christian Zeeden
Janina Bösken
Thomas Stevens
Slobodan B. Marković
Nicole Klasen
Dominik Brill
Christoph Burow
Frank Lehmkuhl
author_facet Igor Obreht
Ulrich Hambach
Daniel Veres
Christian Zeeden
Janina Bösken
Thomas Stevens
Slobodan B. Marković
Nicole Klasen
Dominik Brill
Christoph Burow
Frank Lehmkuhl
author_sort Igor Obreht
title Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
title_short Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
title_full Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
title_fullStr Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
title_full_unstemmed Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal
title_sort shift of large-scale atmospheric systems over europe during late mis 3 and implications for modern human dispersal
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/d78f704ac11445e3b19c75087c395815
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