Evidence for sea level and monsoonally driven variations in terrigenous input to the northern East China Sea during the last 24.3 ka-Reference-Cited by-同舟云学术

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Evidence for sea level and monsoonally driven variations in terrigenous input to the northern East China Sea during the last 24.3 ka

Published:2015-06 Issue:6 Volume:30 Page:642-658
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Chang Fengming¹^ORCID,Li Tiegang¹,Xiong Zhifang¹,Xu Zhaokai¹

Affiliation:

1. Key Laboratory of Marine Geology and Environment, Institute of OceanologyChinese Academy of Sciences Qingdao China

Funder

Knowledge Innovation Engineering Project of Chinese Academy of Sciences

National Special Project for “Global Change and Air-Sea Interaction”

National Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014PA002733

Reference120 articles.

1. Younger Dryas ice-marginal deposits in Norway

2. Climatic changes during the last deglaciation recorded in sediment cores from the northeastern Brazilian Continental Margin

3. U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years

4. Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge

5. Deglacial Meltwater Pulse 1B and Younger Dryas Sea Levels Revisited with Boreholes at Tahiti

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