Geochemical multielement signatures of glacial and interglacial facies of the Okhotsk Sea deepwater sediments during the past 350 kyr: A response to global climate changes at the orbital and millennial scales-Reference-Cited by-同舟云学术

Geochemical multielement signatures of glacial and interglacial facies of the Okhotsk Sea deepwater sediments during the past 350 kyr: A response to global climate changes at the orbital and millennial scales

Published:2015-03 Issue:3 Volume:30 Page:303-316
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Chebykin Eugene P.¹²,Gorbarenko Sergey A.³,Stepanova Ol'ga G.¹,Panov Vsevolod S.⁴,Goldberg Evgeny L.¹⁴

Affiliation:

1. Limnological Institute; Siberian Branch of the Russian Academy of Sciences; Irkutsk Russia

2. Institute of the Earth Crust; Siberian Branch of the Russian Academy of Sciences; Irkutsk Russia

3. V.I. Il'ichev Pacific Oceanology Institute; Far East Branch of the Russian Academy of Sciences; Vladivostok Russia

4. Institute of Archeology and Ethnography; Siberian Branch of the Russian Academy of Sciences; Novosibirsk Russia

Funder

Russian Academy of Sciences

Integrative Project of the Siberian and Far East Branches of the Russian Academy of Sciences

RFBR

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014PA002718/fullpdf

Reference49 articles.

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3. Peculiarities of capture and carrying of detritus by sea ice in the Sea of Okhotsk [in Russian];Archikov;Tikhookean. Geol.,1986

4. A routine method for oxide and hydroxide interference corrections in ICP-MS chemical analysis of environmental and geological samples;Aries;Geostand. Newsl.,2000

5. Distribution of benthic foraminifera in upper Quaternary sediments of the Deryugin Basin (Sea of Okhotsk);Barash;Oceanology,2008

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