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The impact of glaciation and climate change on biogeochemical cycling and landscape development
geochemistry phosphorus sediment glacial lake
2015/1/16
Lake cores from Dry Lake, California and Crystal Lake, Illinois were analyzed to identify climate variability and characterize landscape response to glacial/deglacial climate transitions.
Geochemica...
The Phylogeography of Marstonia Lustrica: Understanding the Relationship Between Glaciation and the Evolution and Distribution of a Rare Snail
gastropod glacier Marstonia phylogenetics phylogeography snail
2014/12/9
Marstonia lustrica is a poorly understood aquatic snail, relatively rare throughout its range and listed in the State of Massachusetts as Endangered (MNHESP 2010, Hershler et. al 1987). It is the nort...
Geomorphologic Structure, Characteristics and Processes in the Cangshan Mountains: Explanations for the Formation and Development of the Dali Glaciation
The Dali Glaciation Step-Like Landform Cangshan Mountain
2013/3/6
The area around Cangshan Mountain, located on the southeastern fringes of the Tibetan Plateau, is a key region in terms of revealing the processes involved in the uplifting of the Tibetan Plateau, plu...
Tropical cooling and the onset of North American glaciation
tropical North American glaciation
2008/11/5
We offer a test of the idea that gradual cooling in the eastern tropical Pacific led to cooling of North America and the initiation of glaciation ~3 Myr ago. Using modern climate data we estimate how...
Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains
in Yunnan Province
2007/8/24
Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of ...
The glacial extent and glacial advance/retreat asynchroncity in East Asia during Last Glaciation
2007/8/24
New dates for last glacial cycle in Tibetan bordering mountains and in East Asia show the glacial extent during the early/middle (MIS3-4) stage is larger than that of the late stage (MIS2)...