High tide of the warm Pliocene: Implications of global sea level for Antarctic deglaciation-Reference-Cited by-同舟云学术

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High tide of the warm Pliocene: Implications of global sea level for Antarctic deglaciation

Published:2012-03-19 Issue:5 Volume:40 Page:407-410
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geology

Author:

Miller K. G.,Wright J. D.,Browning J. V.,Kulpecz A.,Kominz M.,Naish T. R.,Cramer B. S.,Rosenthal Y.,Peltier W. R.,Sosdian S.

Publisher

Geological Society of America

Subject

Geology

Reference22 articles.

1. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2

2. High eustatic sea level during the middle Pliocene:Evidence from the southeastern U.S. Atlantic Coastal Plain

3. Impact effects and regional tectonic insights: Backstripping the Chesapeake Bay impact structure

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1. Geologically constrained 2-million-year-long simulations of Antarctic Ice Sheet retreat and expansion through the Pliocene;Nature Communications;2024-08-15

2. Pliocene–Pleistocene warm-water incursions and water mass changes on the Ross Sea continental shelf (Antarctica) based on foraminifera from IODP Expedition 374;Journal of Micropalaeontology;2024-07-11

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4. The changes in south Asian summer monsoon circulation during the mid-Piacenzian warm period;Climate Dynamics;2024-03-25

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