scholarly journals Environments of Ocean and Primary Productivity during the Late Quaternary. Millennial-scale Large and Abrupt Climatic Changes-Global system dynamics in response to Dansgaad-Oeschger Cycles.

1998 ◽  
Vol 107 (2) ◽  
pp. 218-233 ◽  
Author(s):  
Ryuji TADA
Keyword(s):  
System Dynamics ◽  
Primary Productivity ◽  
Late Quaternary ◽  
Climatic Changes ◽  
Global System ◽  
Millennial Scale

scholarly journals Millennial-Scale Response of a Western Mediterranean River to Late Quaternary Climate Changes: A View from the Deep Sea

2014 ◽  
Vol 122 (6) ◽  
pp. 687-703 ◽  
Author(s):  
Lucile Bonneau ◽  
Stéphan J. Jorry ◽  
Samuel Toucanne ◽  
Ricardo Silva Jacinto ◽  
Laurent Emmanuel
Keyword(s):  
Deep Sea ◽  
Climate Changes ◽  
Late Quaternary ◽  
Western Mediterranean ◽  
Mediterranean River ◽  
Quaternary Climate ◽  
Scale Response ◽  
Quaternary Climate Changes ◽  
Millennial Scale

scholarly journals Abrupt climate changes during Termination III in Southern Europe

2017 ◽  
Vol 114 (38) ◽  
pp. 10047-10052 ◽  
Author(s):  
Carlos Pérez-Mejías ◽  
Ana Moreno ◽  
Carlos Sancho ◽  
Miguel Bartolomé ◽  
Heather Stoll ◽  
...  
Keyword(s):  
High Resolution ◽  
Water Availability ◽  
Climate Changes ◽  
Late Quaternary ◽  
Marine Isotope Stage ◽  
Southern Europe ◽  
Vegetation Productivity ◽  
Common Features ◽  
Sequence Of Events ◽  
Millennial Scale

The Late Quaternary glacial–interglacial transitions represent the highest amplitude climate changes over the last million years. Unraveling the sequence of events and feedbacks at Termination III (T-III), including potential abrupt climate reversals similar to those of the last Termination, has been particularly challenging due to the scarcity of well-dated records worldwide. Here, we present speleothem data from southern Europe covering the interval from 262.7 to 217.9 kyBP, including the transition from marine isotope stage (MIS) 8 to MIS 7e. High-resolution δ13C, δ18O, and Mg/Ca profiles reveal major millennial-scale changes in aridity manifested in changing water availability and vegetation productivity. uranium–thorium dates provide a solid chronology for two millennial-scale events (S8.1 and S8.2) which, compared with the last two terminations, has some common features with Heinrich 1 and Heinrich 2 in Termination I (T-I).

Glacial advances in southeastern Tibet during late Quaternary and their implications for climatic changes

2010 ◽  
Vol 218 (1-2) ◽  
pp. 58-66 ◽  
Author(s):  
Zhou Shangzhe ◽  
Wang Jie ◽  
Xu Liubing ◽  
Wang Xiaoli ◽  
Patrick M. Colgan ◽  
...  
Keyword(s):  
Late Quaternary ◽  
Climatic Changes ◽  
Southeastern Tibet

Millennial-scale vegetation and climatic changes from an Early to Mid-Holocene lacustrine archive in Central Ganga Plains using multiple biotic proxies

2020 ◽  
Vol 243 ◽  
pp. 106474 ◽  
Author(s):  
Pavani Misra ◽  
Anjum Farooqui ◽  
Rajiv Sinha ◽  
Sonal Khanolkar ◽  
Sampat K. Tandon
Keyword(s):  
Climatic Changes ◽  
Millennial Scale

Responses of Non-volant Mammals to Late Quaternary Climatic Changes in the Wet Tropics Region of North-eastern Australia

1997 ◽  
Vol 24 (5) ◽  
pp. 493 ◽  
Author(s):  
J. W. Winter
Keyword(s):  
Late Quaternary ◽  
Temperature Tolerance ◽  
Climatic Changes ◽  
Glacial Period ◽  
Profound Influence ◽  
Eastern Australia ◽  
North Eastern ◽  
Sclerophyll Forest ◽  
Wet Tropics ◽  
Glacial Periods

It is generally recognised that the distribution of vertebrates in rainforest and wet sclerophyll forest of the Wet Tropics region of north-eastern Australia is profoundly influenced by the formation of two rainforest refugia at the height of Pleistocene glacial periods. Anomalies in the distribution of non-volant mammals indicate that other events may be equally important. In this paper, past geographical occurrence of non-volant mammals is examined by equating the mammals’ known temperature tolerance with palaeoclimatic temperature zones. It is hypothesised that dispersal and vicariant phases taking place since the most recent glacial period have had a profound influence on current patterns of distribution. A major dispersal phase of cool-adapted species occurred after the glacial period, and continuous populations were subsequently fragmented into upland isolates by expansion of warm rainforest during the late post-glacial period. These upland isolates remain substantially unchanged to the present day. Species shared either with New Guinea or south-eastern Australia arrived in the region during the most recent post-glacial period. Clarification of periods of vicariance and dispersal provides a conceptual framework for testing relative divergences of populations within and between regions.

scholarly journals Late Quaternary environmental and climatic changes in central Europe as inferred from the composition of organic matter in annually laminated maar lake sediments

2004 ◽  
Vol 5 (11) ◽  
pp. n/a-n/a ◽  
Author(s):  
Andreas Fuhrmann ◽  
Thomas Fischer ◽  
Andreas Lücke ◽  
Achim Brauer ◽  
Bernd Zolitschka ◽  
...  
Keyword(s):  
Organic Matter ◽  
Lake Sediments ◽  
Central Europe ◽  
Late Quaternary ◽  
Climatic Changes ◽  
Maar Lake
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