A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale-Reference-Cited by-同舟云学术

A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale

Published:2018-07 Issue:7 Volume:33 Page:778-794
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Baggenstos Daniel¹^ORCID,Severinghaus Jeffrey P.¹^ORCID,Mulvaney Robert²^ORCID,McConnell Joseph Robert³^ORCID,Sigl Michael³^ORCID,Maselli Olivia³^ORCID,Petit Jean‐Robert⁴,Grente Benjamin⁴,Steig Eric J.⁵^ORCID

Affiliation:

1. Scripps Institution of OceanographyUC San Diego La Jolla CA USA

2. British Antarctic Survey, Natural Environment Research Council Cambridge UK

3. Department of Hydrologic Sciences, Desert Research Institute Reno NV USA

4. University Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE Grenoble France

5. Department of Earth and Space SciencesUniversity of Washington Seattle WA USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2017PA003297

Reference98 articles.

1. Dust composition changes from Taylor Glacier (East Antarctica) during the last glacial-interglacial transition: A multi-proxy approach

2. The impact of glacier retreat from the Ross Sea on local climate: Characterization of mineral dust in the Taylor Dome ice core, East Antarctica

3. Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica

4. Atmospheric CO2and climate from 65 to 30 ka B.P.

5. Interpreting last glacial to Holocene dust changes at Talos Dome (East Antarctica): implications for atmospheric variations from regional to hemispheric scales

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