Hydrological variations on the Central Tibetan Plateau since the Last Glacial Maximum and their teleconnection to inter-regional and hemispheric climate variations

2015 ◽  
Vol 30 (1) ◽  
pp. 70-78 ◽  
Author(s):  
THOMAS KASPER ◽  
TORSTEN HABERZETTL ◽  
JUNBO WANG ◽  
GERHARD DAUT ◽  
STEFAN DOBERSCHÜtz ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Climate Variations ◽  
Last Glacial ◽  
Central Tibetan Plateau ◽  
The Last Glacial Maximum ◽  
The Last Glacial

scholarly journals Biogeochemical evidence for freshwater periods during the Last Glacial Maximum recorded in lake sediments from Nam Co, south-central Tibetan Plateau

2015 ◽  
Vol 55 (1) ◽  
pp. 67-82 ◽  
Author(s):  
Roman Witt ◽  
Franziska Günther ◽  
Stefan Lauterbach ◽  
Thomas Kasper ◽  
Roland Mäusbacher ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Lake Sediments ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Nam Co ◽  
Last Glacial ◽  
South Central ◽  
Central Tibetan Plateau ◽  
The Last Glacial Maximum ◽  
The Last Glacial

The Low Lake‐Level Record according to the Selin Co Stratigraphical Basis and Multi‐Proxies during the Last Glacial Maximum in the Central Tibetan Plateau

2018 ◽  
Vol 92 (5) ◽  
pp. 2058-2059 ◽  
Author(s):  
Chengjun ZHANG ◽  
Blaise DEMBELE ◽  
Wanyi ZHANG ◽  
Jingya ZHANG ◽  
Hansheng WANG ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Lake Level ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Central Tibetan Plateau ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Winter and summer monsoonal evolution in Gonghe Basin, northeastern Qinghai-Tibetan Plateau since the Last Glacial Maximum

2013 ◽  
Vol 5 (3) ◽  
pp. 282
Author(s):  
Liu Bing ◽  
Jin He-Ling ◽  
Sun Zhong ◽  
Su Zhi-Zhu ◽  
Zhang Cai-Xia
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
Gonghe Basin ◽  
The Last Glacial

A mitochondrial revelation of early human migrations to the Tibetan Plateau before and after the last glacial maximum

2010 ◽  
Vol 143 (4) ◽  
pp. 555-569 ◽  
Author(s):  
Zhendong Qin ◽  
Yajun Yang ◽  
Longli Kang ◽  
Shi Yan ◽  
Kelly Cho ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
The Tibetan Plateau ◽  
Last Glacial ◽  
Before And After ◽  
The Last Glacial Maximum ◽  
Early Human ◽  
The Last Glacial

scholarly journals Tree endurance on the Tibetan Plateau marks the world’s highest known tree line of the Last Glacial Maximum

2009 ◽  
Vol 185 (1) ◽  
pp. 332-342 ◽  
Author(s):  
Lars Opgenoorth ◽  
Giovanni G. Vendramin ◽  
Kangshan Mao ◽  
Georg Miehe ◽  
Sabine Miehe ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
The Tibetan Plateau ◽  
Tree Line ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Vegetation composition in Sanjiangyuan region compared with Hengduan Mountains (eastern Tibetan Plateau) since the Last Glacial Maximum revealed by plant metabarcoding of sedimentary ancient DNA

2021 ◽  
Author(s):  
Wei Shen ◽  
Sisi Liu ◽  
Kathleen R. Stoof-Leichsenring ◽  
Jeremy Courtin ◽  
Steffen Mischke ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Last Glacial Maximum ◽  
Beta Diversity ◽  
Glacial Maximum ◽  
Hengduan Mountains ◽  
Vegetation Composition ◽  
Eastern Tibetan Plateau ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

<p>The eastern Tibetan Plateau, particularly the Hengduan Mountains and Sanjiangyuan region, is a biodiversity hotspot also known for its sensitivity to climate change. How these vegetation communities assembled since the Last Glacial Maximum is still unclear. Here we present new results from plant metabarcoding of sediments from Lake Ximencuo (Nianbaoyeze Mountains, Sanjiangyuan region) covering the last 18 ka and compare them with records from Lake Naleng (Hengduan Mountains).  We investigate temporal changes of within-site and between-site alpha and beta diversities. Both sites show the highest richness between 14 and 10 ka when alpine meadows covered the areas while richness was rather low in forested periods during the early Holocene. Ordination results support that the vegetation composition was relatively low between-site beta-diversities indicate that the vegetation composition was relatively similar in the two study areas before the Holocene, particularly during the early late-glacial when alpine steppes dominated. The maximal between-site beta-diversity occurred between 10 and 8 ka when environmental filtering was most relevant, as suggested by the dominating turnover component. The nestedness component of beta-diversity reached a maximum during the middle Holocene indicating that between-site differences during this period possibly originated from e.g., dispersal limitation.</p>

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