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2017 ; 7
(1
): 5848
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Shift of large-scale atmospheric systems over Europe during late MIS 3 and
implications for Modern Human dispersal
#MMPMID28725004
Obreht I
; Hambach U
; Veres D
; Zeeden C
; Bösken J
; Stevens T
; Markovi? SB
; Klasen N
; Brill D
; Burow C
; Lehmkuhl F
Sci Rep
2017[Jul]; 7
(1
): 5848
PMID28725004
show ga
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.