(Article of periodic en Anglais - 1996)

Document title

Stable isotope and lithologic evidence of late-Glacial and Holocene oceanography of the Northwestern Pacific and its marginal seas

Authors(s) and Affiliation(s)

(1) Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences, Vladivostok, RUSSIE, FEDERATION DE


Stable isotopes, geochemical, lithological, and micropaleontological results from cores from the far northwest (FNW) Pacific and the Okhotsk and Bering seas are used to reconstruct the regional environment for the last glaciation, the deglacial transition, and the Holocene. During deglaciation, accumulation of the coarse terrigenous component decreased in sediments of the Bering Sea and the FNW Pacific before the north Pacific terminal event T1ANP, probably as a result of rising sea level and opening of the Bering Strait


Article of periodic

published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV

Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)

Millesime : 1996, vol. 46, no3 [pp. 230-250]

Bibliographic references : 40 ref.

Collation : Illustration ;



INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1997.
Refdoc record number (ud4) : 5967189 : Permanent link - XML version
Powered by Pxxo