Eemian and Early Weichselian vegetation and climate history in Central Europe: A case study from the Klinge section (Lusatia, eastern Germany)

2008 ◽  
Vol 151 (1-2) ◽  
pp. 72-78 ◽  
Author(s):  
E.Yu. Novenko ◽  
M. Seifert-Eulen ◽  
T. Boettger ◽  
F.W. Junge
Keyword(s):  
Central Europe ◽  
Climate History ◽  
Eastern Germany ◽  
Vegetation And Climate

Vegetation and climate history reconstructed from an alpine lake in central Tienshan Mountains since 8.5 ka BP

2015 ◽  
Vol 432 ◽  
pp. 36-48 ◽  
Author(s):  
Xiao-zhong Huang ◽  
Chun-zhu Chen ◽  
Wan-na Jia ◽  
Cheng-bang An ◽  
Ai-feng Zhou ◽  
...  
Keyword(s):  
Alpine Lake ◽  
Climate History ◽  
Vegetation And Climate

scholarly journals Littoral landforms and pedosedimentary sequences indicating late Holocene lake-level changes in northern central Europe — A case study from northeastern Germany

Geomorphology ◽  
2014 ◽  
Vol 216 ◽  
pp. 58-78 ◽  
Author(s):  
Knut Kaiser ◽  
Mathias Küster ◽  
Alexander Fülling ◽  
Martin Theuerkauf ◽  
Elisabeth Dietze ◽  
...  
Keyword(s):  
Central Europe ◽  
Lake Level ◽  
Late Holocene ◽  
Lake Level Changes ◽  
Northeastern Germany

The role of bilingual instructors in the implementation of ERC standards in Eastern and Central Europe. Case study of Ukraine

Resuscitation ◽  
2010 ◽  
Vol 81 (2) ◽  
pp. S105
Author(s):  
L. Duniec ◽  
J. Szymański ◽  
T. Łazowski ◽  
J. Andres
Keyword(s):  
Central Europe

Holocene Vegetation and Climate History of the Northern Bighorn Basin, Southern Montana

2002 ◽  
Vol 58 (2) ◽  
pp. 171-181 ◽  
Author(s):  
Mark E. Lyford ◽  
Julio L. Betancourt ◽  
Stephen T. Jackson
Keyword(s):  
Climate Change ◽  
Great Basin ◽  
Rocky Mountain ◽  
Bighorn Basin ◽  
Downward Movement ◽  
Climate History ◽  
Juniperus Osteosperma ◽  
Rocky Mountain Region ◽  
History Of ◽  
Vegetation And Climate

AbstractRecords of Holocene vegetation and climate change at low elevations (<2000 m) are rare in the central Rocky Mountain region. We developed a record of Holocene vegetation and climate change from 55 14C-dated woodrat middens at two low-elevation sites (1275 to 1590 m), currently vegetated by Juniperus osteosperma woodlands, in the northern Bighorn Basin. Macrofossil and pollen analyses show that the early Holocene was cooler than today, with warming and drying in the middle Holocene. During the Holocene, boreal (Juniperus communis, J. horizontalis) and montane species (J. scopulorum) were replaced by a Great Basin species (J. osteosperma). J. osteosperma colonized the east side of the Pryor Mountains 4700 14C yr B.P. Downward movement of lower treeline indicates wetter conditions between 4400 and 2700 14C yr B.P. Increased aridity after 2700 14C yr B.P. initiated expansion of J. osteosperma from the east to west side of the Pryor Mountains.

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