scholarly journals Diverse responses of common vole (Microtus arvalis) populations to Late Glacial and Early Holocene climate changes – Evidence from ancient DNA

2020 ◽  
Vol 233 ◽  
pp. 106239 ◽  
Author(s):  
Mateusz Baca ◽  
Danijela Popović ◽  
Katarzyna Baca ◽  
Anna Lemanik ◽  
Karolina Doan ◽  
...  
Keyword(s):  
Ancient Dna ◽  
Climate Changes ◽  
Common Vole ◽  
Late Glacial ◽  
Early Holocene ◽  
Microtus Arvalis ◽  
Holocene Climate

scholarly journals Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)

2013 ◽  
Vol 392 ◽  
pp. 335-349 ◽  
Author(s):  
T. Vegas-Vilarrúbia ◽  
P. González-Sampériz ◽  
M. Morellón ◽  
G. Gil-Romera ◽  
A. Pérez-Sanz ◽  
...  
Keyword(s):  
Climate Changes ◽  
Late Glacial ◽  
Early Holocene ◽  
Holocene Climate ◽  
Vegetation Responses ◽  
Ne Spain

Late-glacial and Early Holocene climate and environment from stable isotopes in Welsh tufa

Quaternaire ◽  
2006 ◽  
pp. 31-42 ◽  
Author(s):  
E. R. Garnett ◽  
J. E. Andrews ◽  
Richard C. Preece ◽  
P. F. Dennis
Keyword(s):  
Stable Isotopes ◽  
Late Glacial ◽  
Early Holocene ◽  
Holocene Climate

Cladocera response to Late Glacial to Early Holocene climate change in a South Carpathian mountain lake

Hydrobiologia ◽  
2011 ◽  
Vol 676 (1) ◽  
pp. 223-235 ◽  
Author(s):  
János Korponai ◽  
Enikő Katalin Magyari ◽  
Krisztina Buczkó ◽  
Sanda Iepure ◽  
Tadeusz Namiotko ◽  
...  
Keyword(s):  
Climate Change ◽  
Late Glacial ◽  
Early Holocene ◽  
Mountain Lake ◽  
Holocene Climate ◽  
Holocene Climate Change ◽  
Carpathian Mountain

Early Holocene hydrology and environments of the Ner River (Poland)

2016 ◽  
Vol 85 (2) ◽  
pp. 187-203 ◽  
Author(s):  
Piotr Kittel ◽  
Mateusz Płociennik ◽  
Ryszard K. Borόwka ◽  
Daniel Okupny ◽  
Dominik Pawłowski ◽  
...  
Keyword(s):  
Climate Changes ◽  
Late Glacial ◽  
Reference Points ◽  
Early Holocene ◽  
Oxbow Lake ◽  
Pollen Data ◽  
Overbank Sediments ◽  
Winter Temperatures ◽  
Organic Deposits ◽  
Boreal Period

The Ner River valley (central Poland) underwent substantial transformation during the Weichselian–Holocene transition as a result of fluvial processes and climate changes, resulting in the establishment of its present shape in the Holocene. A multiproxy study based on organic deposits from a palaeochannel fill (Lutomiersk–Koziówki) shows that after the channel was cut off during the late glacial termination, it became a shallow oxbow, fed by local springs. In the Boreal period, the oxbow lake was also fed by precipitation and became a telmatic environment overgrown by rush and swamp vegetation. Finally, it was covered by overbank deposits. The first flooding phase (9900–9600 cal. BP) was followed by the accumulation of overbank sediments (after 9500 cal. BP) and flooding increased after ca. 9300–9000 cal. BP. Pollen data provide information on the regional vegetation context for local and regional changes. In the Atlantic period, an increase in both summer and winter temperatures is inferred from the pollen data, corresponding to an expansion of thermophilous deciduous forests. While in general, flooding phases of the Early Holocene are poorly recognised in Eastern Europe, the Lutomiersk–Koziówki site may be considered as one of the reference points for this phenomenon in the region.

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