The marine δ18O record overestimates continental ice volume during Marine Isotope Stage 3-Reference-Cited by-同舟云学术

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The marine δ18O record overestimates continental ice volume during Marine Isotope Stage 3

Published:2022-05 Issue: Volume:212 Page:103814
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Dalton April S.,Pico Tamara,Gowan Evan J.,Clague John J.,Forman Steven L.,McMartin Isabelle,Sarala Pertti,Helmens Karin F.

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference176 articles.

1. The salinity, temperature, and δ18O of the glacial deep ocean;Adkins;Science,2002

2. Meltwater flooding events in the Gulf of Mexico revisited: Implications for rapid climate changes during the last deglaciation;Aharon;Paleoceanography,2003

3. Re-dating the Pilgrim Interstadial with OSL: a warmer climate and smaller ice sheet during the Swedish Middle Weichselian (MIS 3)?;Alexanderson;Boreas,2010

4. New dates from the Riipiharju interstadial site, northernmost Sweden [conference abstract];Alexanderson,2011

5. Constraining the age of the last interglacial–glacial transition in the Hudson Bay lowlands (Canada) using U–Th dating of buried wood;Allard;Quat. Geochronol.,2012

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1. Defining the Sheldon Creek Formation, a Middle Wisconsinan (MIS 3) till in Iowa, USA;Journal of Quaternary Science;2024-06-07

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3. Relative abundance and biometry of Bolivina ordinaria on the northern continental slope of the Pelotas basin during the late Quaternary;Marine Micropaleontology;2024-04

4. Growth of the Laurentide and Innuitian ice sheets during MIS 5 recorded in distal marine sediment;Quaternary Science Reviews;2024-03

5. Loess chronology and composition as interpreted through the lens of fossiliferous lake sediments in central Illinois, USA;Geological Society of America Bulletin;2024-02-27

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