Sedimentary responses to sea-level rise and Kuroshio Current intrusion since the Last Glacial Maximum: Grain size and clay mineral evidence from the northern South China Sea slope-Reference-Cited by-同舟云学术

Sedimentary responses to sea-level rise and Kuroshio Current intrusion since the Last Glacial Maximum: Grain size and clay mineral evidence from the northern South China Sea slope

Published:2016-05 Issue: Volume:450 Page:111-121
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Liu Jianguo,Xiang Rong,Kao S.-J.,Fu Shaoying,Zhou Liping

Funder

National Program on Global Change and Air-Sea Interaction

Strategic Priority Research Program of the Chinese Academy of Sciences

Knowledge Innovation Program of the Chinese Academy of Sciences

National Key Project for Basic Research of China

National Natural Science of China

Guangzhou Marine Geological Survey

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference73 articles.

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3. Sediment sources and East Asian monsoon intensity over the last 450ky. Mineralogical and geochemical investigations on South China Sea sediments;Boulay;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2005

4. East Asian Monsoon Variability on Orbital- and Millennial-to-subdecadal Time Scales;Buehring,2001

5. Grain size and geochemistry of surface sediments in northwestern continental shelf of the South China Sea;Cai;Environ. Earth Sci.,2013

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