Enhancements of Himalayan and Tibetan Erosion and the Produced Organic Carbon Burial in Distal Tropical Marginal Seas During the Quaternary Glacial Periods: An Integration of Sedimentary Records-Reference-Cited by-同舟云学术

Enhancements of Himalayan and Tibetan Erosion and the Produced Organic Carbon Burial in Distal Tropical Marginal Seas During the Quaternary Glacial Periods: An Integration of Sedimentary Records

Published:2021-03 Issue:3 Volume:126 Page:
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Xu Zhaokai¹²³⁴^ORCID,Wan Shiming¹²⁴,Colin Christophe⁵^ORCID,Clift Peter D.⁶^ORCID,Chang Fengming¹²³^ORCID,Li Tiegang²⁷,Chen Hongjin¹⁸,Cai Mingjiang¹⁸,Yu Zhaojie¹²³^ORCID,Lim Dhongil⁹^ORCID

Affiliation:

1. CAS Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences Qingdao China

2. Laboratory for Marine Geology Pilot National Laboratory for Marine Science and Technology Qingdao China

3. Center for Ocean Mega‐Science Chinese Academy of Sciences Qingdao China

4. CAS Center for Excellence in Quaternary Science and Global Change Xi'an China

5. Laboratoire Geosciences Paris‐Sud (GEOPS) CNRS‐Université de Paris‐Sud Université Paris‐Saclay Orsay Cedex France

6. Department of Geology and Geophysics Louisiana State University Baton Rouge LA USA

7. Key Laboratory of Marine Sedimentology and Environmental Geology First Institute of Oceanography Ministry of Natural Resources Qingdao China

8. University of Chinese Academy of Sciences Beijing China

9. South Sea Research Institute Korea Institute of Ocean Science & Technology Geoje Republic of Korea

Funder

National Natural Science Foundation of China

Korea Institute of Ocean Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JF005828

Reference60 articles.

1. Glacial-Interglacial Indian Summer Monsoon Dynamics

2. Integrating Suspended Sediment Flux in Large Alluvial River Channels: Application of a Synoptic Rouse‐Based Model to the Irrawaddy and Salween Rivers

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4. Insolation values for the climate of the last 10 million years

5. Large-river delta-front estuaries as natural "recorders" of global environmental change

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