Ostracod palaeoecology and environmental change in the L aptev and K ara seas ( S iberian A rctic) during the last 18 000 years-Reference-Cited by-同舟云学术

Ostracod palaeoecology and environmental change in the L aptev and K ara seas ( S iberian A rctic) during the last 18 000 years

Published:2012-04-20 Issue:4 Volume:41 Page:557-577
ISSN:0300-9483
Container-title:Boreas
language:en
Short-container-title:Boreas

Author:

Stepanova Anna¹,Taldenkova Ekaterina²,Bauch Henning A.³

Affiliation:

1. Borisyak Paleontological Institute RAS Profsoyuznaya, 123 Moscow 117997 Russia

2. Geographical FacultyLomonosov Moscow State University Leninskie Gory, 1 Moscow 119991 Russia

3. Mainz Academy for Science, Humanities and Literature, c/o GEOMAR Helmholtz Centre for Ocean Research Wischhofstrasse 1‐3 24148 Kiel Germany

Funder

BMBF and Russian Ministry for Education and Science

Russian Foundation for Basic Research

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2012.00254.x

Reference70 articles.

1. Alvarez Zarikian C. A. Blackwelder P. L. Hood T. Nelsen T. A.&Featherstone C.2000:Ostracods as indicators of natural and anthropogenically‐induced changes in coastal marine environments.Coasts at the Millenium Proceedings of the 17th International Conference of the Coastal Society Portland USA July 9–12 2000 896–905.

2. Glacial–interglacial variability in deep sea ostracod assemblage composition at IODP Site U1314 in the subpolar North Atlantic

3. Depositional environment of the Laptev Sea (Arctic Siberia) during the Holocene

4. Chronology of the Holocene transgression at the North Siberian margin

5. Ostracode Distribution and Biofacies, Newfoundland Continental Slope and Rise

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