Meltwater discharge during the Holocene from the Wilkes subglacial basin revealed by beryllium isotope analysis of marine sediments-Reference-Cited by-同舟云学术

Meltwater discharge during the Holocene from the Wilkes subglacial basin revealed by beryllium isotope analysis of marine sediments

Published:2019-10-02 Issue:8 Volume:34 Page:603-608
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J. Quaternary Sci.

Author:

Behrens Bethany¹²,Miyairi Yosuke¹,Sproson Adam D.¹,Yamane Masako³,Yokoyama Yusuke¹²⁴⁵

Affiliation:

1. Atmosphere and Ocean Research InstituteUniversity of Tokyo Kashiwa Chiba Japan

2. Graduate Programme on Environmental ScienceUniversity of Tokyo Komaba Meguro Tokyo Japan

3. Institute for Space‐Earth Environmental ResearchNagoya University, Furocho, ChikusaNagoya Aichi Japan

4. Department of Earth and Planetary Science, Graduate School of ScienceUniversity of Tokyo Hongo Bunkyō Tokyo Japan

5. Japan Agency for Marine‐Earth Science and Technology (JAMSTEC), NatsushimachoYokosuka Kanagawa Prefecture Japan

Funder

Japan Society for the Promotion of Science

Ministry of Education, Culture, Sports, Science and Technology

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3148

Reference35 articles.

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2. Volcanic and solar activity, and atmospheric circulation influences on cosmogenic 10Be fallout at Vostok and Concordia (Antarctica) over the last 60years

3. Glacial ice and atmospheric forcing on the Mertz Glacier Polynya over the past 250 years

4. Holocene glacial discharge fluctuations and recent instability in East Antarctica

5. Ocean as the main driver of Antarctic ice sheet retreat during the Holocene

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