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Record #180610:

Послеледниковое развитие бентосных фораминифер в южной части Берингова моря

Title: Послеледниковое развитие бентосных фораминифер в южной части Берингова моря
Title, transliterated: Poslelednikovoe razvitie bentosnykh foraminifer v i︠u︡zhnoĭ chasti Beringova mori︠a︡ / T.A. Khusid, I.A. Basov, S.A. Gorbarenko.
Translated title: Postglacial evolution of benthic foraminifera in the southern Bering Sea.
Author(s): Khusid, T. A.
Basov, I. A.
Gorbarenko, S. A.
Date: 2005.
Language: Russian.
In: Arktika i Antarktika. (2005.), Vol. 4(38) (2005)
Abstract: Studies of benthic foraminifera in uppermost Pleistocene-Holocene sediments from southern Bering Sea reveal substantial quantitative and compositional variations with time that reflect changes in hydrological characteristics of basin over last 22,000 years. Periods marked by highest productivity of both foraminifera and diatoms correspond to two deglaciation phases by brief Younger Dryas cooling.
Notes:

Arktika i Antarktika. Vol. 4(38) :103-114 (2005).

Keywords: 56 -- Palaeontology.
574.5 -- Marine and freshwater ecology.
574.583 -- Plankton.
551.461.8 -- Palaeo-oceanography.
F -- Biological sciences.
(*662) -- Bering Sea and Strait.
SPRI record no.: 180610

MARCXML

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001 SPRI-180610
005 20220924221524.0
007 ta
008 220924s2005####xx#ab#|##|###|0||#0|rus#d
035 ## ‡aSPRI-180610
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aKhusid, T. A.
242 10 ‡aPostglacial evolution of benthic foraminifera in the southern Bering Sea.‡yeng
245 10 ‡6880-02‡aPoslelednikovoe razvitie bentosnykh foraminifer v i︠u︡zhnoĭ chasti Beringova mori︠a︡ /‡cT.A. Khusid, I.A. Basov, S.A. Gorbarenko.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2005.
300 ## ‡ap. 103-114 :‡bill., map.
500 ## ‡aArktika i Antarktika. Vol. 4(38) :103-114 (2005).
520 3# ‡aStudies of benthic foraminifera in uppermost Pleistocene-Holocene sediments from southern Bering Sea reveal substantial quantitative and compositional variations with time that reflect changes in hydrological characteristics of basin over last 22,000 years. Periods marked by highest productivity of both foraminifera and diatoms correspond to two deglaciation phases by brief Younger Dryas cooling.
546 ## ‡aIn Russian.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a574.5 -- Marine and freshwater ecology.‡2udc
650 07 ‡a574.583 -- Plankton.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡aF -- Biological sciences.‡2local
651 #7 ‡a(*662) -- Bering Sea and Strait.‡2udc
700 1# ‡6880-03‡aBasov, I. A.
700 1# ‡6880-04‡aGorbarenko, S. A.
773 0# ‡6880-05‡7nnas ‡tArktika i Antarktika. ‡gVol. 4(38) (2005) ‡wSPRI-175680
880 1# ‡6100-01/(N‡aХусид, Т. А.
880 10 ‡6245-02/(N‡aПослеледниковое развитие бентосных фораминифер в южной части Берингова моря /‡cТ.А. Хусид, И.А. Басов, С.А. Горбаренко.
880 1# ‡6700-03/(N‡aБасов, И. А.
880 1# ‡6700-04/(N‡aГорбаренко, С. А.
880 0# ‡6773-05/(N‡7nnas ‡tАрктика и Антарктика. ‡gVol. 4(38) (2005) ‡wSPRI-175680
916 ## ‡a2007/11/14 -- IW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924 ‡bIW