Paleoclimate Change
Paleoclimate Change is a scientific construct that denotes the systematic variation in Earth's climatic conditions over the Quaternary period, particularly during the Pleistocene epoch, as reconstructed from geological, biological, and geochemical proxy evidence relevant to the environmental contexts of Paleolithic human evolution and behavior.
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2017–2026
336
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Chinese Academy of Sciences
Beijing, China
43 h-index
404 publications
25.9K citations

Centre National de la Recherche Scientifique
Paris, France
40 h-index
164 publications
19.8K citations
United States Geological Survey
Reston, United States
27 h-index
61 publications
5.6K citations
China University of Geosciences
Wuhan, China
27 h-index
125 publications
7.1K citations
University of Arizona
Tucson, United States
26 h-index
61 publications
6.3K citations
Institute of Tibetan Plateau Research
Beijing, China
23 h-index
102 publications
8K citations
University of Michigan
Ann Arbor, United States
23 h-index
39 publications
4.8K citations
University of Colorado Boulder
Boulder, United States
23 h-index
39 publications
4.9K citations
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