Stable oxygen and carbon isotopes in modern benthic foraminifera from the Laptev Sea shelf: implications for reconstructing proglacial and profluvial environments in the Arctic-Reference-Cited by-同舟云学术

Stable oxygen and carbon isotopes in modern benthic foraminifera from the Laptev Sea shelf: implications for reconstructing proglacial and profluvial environments in the Arctic

Published:2004-06 Issue:3-4 Volume:51 Page:285-300
ISSN:0377-8398
Container-title:Marine Micropaleontology
language:en
Short-container-title:Marine Micropaleontology

Author:

Bauch H.A.,Erlenkeuser H.,Bauch D.,Mueller-Lupp T.,Taldenkova E.

Publisher

Elsevier BV

Subject

Paleontology,Oceanography

Reference64 articles.

1. The role of sea ice and other freshwater in the Arctic circulation;Aagaard;Journal of Geophysical Research,1989

2. Diatom-inferred salinity records from the Arctic Siberian Margin: implications for fluvial runoff patterns during the Holocene;Bauch;Paleoceanography,2003

3. Freshwater balance and the sources of deep and bottom waters in the Arctic Ocean inferred from the distribution of H218O;Bauch;Progress in Oceanography,1995

4. Depositional environment of the Laptev Sea (Arctic Siberia) during the Holocene;Bauch;Boreas,1999

5. Siberian shelf sediments contain clues to paleoclimate forcing;Bauch;EOS Transactions,2000

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