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Record #72411:
Структура танатоценоса планктонных фораминифер как индикатор океанских круговоротов и фронтов
Title: | Структура танатоценоса планктонных фораминифер как индикатор океанских круговоротов и фронтов |
Title, transliterated: | Struktura tanatot︠s︡enosa planktonnykh foraminifer kak indikator okeanskikh krugovorotov i frontov / N.S. Osʹkina, N.S. Bli︠u︡m. |
Translated title: | The structure of the thanatocoenosis of planktonic foraminifera as an indicator of oceanic gyres and fronts. |
Author(s): | Osʹkina, N. S. Bli︠u︡m, N. S. |
Date: | 1984. |
Language: | Russian. |
In: | Okeanologii︠a︡. (1984.), Vol. 24(6) (1984) |
Abstract: | Distribution of planktonic foraminifera thanatocoenoses in Atlantic Ocean studied. Normal type was found to be formed in central parts of gyres, whereas contrasting type was formed in frontal zones. Reconstructs location of oceanic gyres and fronts during maximum of last glaciation 18,000 years ago. With reference also to southern polar region. |
Notes: | Okeanologii︠a︡. Vol. 24(6) :942-947 (1984). English summary, p.947. |
Keywords: | 551.336 -- Ice ages. 551.461.8 -- Palaeo-oceanography. 574.583 -- Plankton. 593.12 -- Foraminifera and amoebozoa. C -- Oceanography, hydrography and hydrology. (*60) -- Arctic Ocean and adjacent waters. (*80) -- Southern Ocean. |
SPRI record no.: | 72411 |
LDR 02067naa#a2200000#a#4500 001 SPRI-72411 005 20240418163043.0 007 ta 008 240418s1984####xx#ab#|##|###|0||#0|rus#d 035 ## ‡aSPRI-72411 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aOsʹkina, N. S. 242 14 ‡aThe structure of the thanatocoenosis of planktonic foraminifera as an indicator of oceanic gyres and fronts.‡yeng 245 10 ‡6880-02‡aStruktura tanatot︠s︡enosa planktonnykh foraminifer kak indikator okeanskikh krugovorotov i frontov /‡cN.S. Osʹkina, N.S. Bli︠u︡m. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1984. 300 ## ‡ap. 942-947 :‡bdiags., maps. 500 ## ‡aOkeanologii︠a︡. Vol. 24(6) :942-947 (1984). 500 ## ‡aEnglish summary, p.947. 520 3# ‡aDistribution of planktonic foraminifera thanatocoenoses in Atlantic Ocean studied. Normal type was found to be formed in central parts of gyres, whereas contrasting type was formed in frontal zones. Reconstructs location of oceanic gyres and fronts during maximum of last glaciation 18,000 years ago. With reference also to southern polar region. 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 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc 650 07 ‡a574.583 -- Plankton.‡2udc 650 07 ‡a593.12 -- Foraminifera and amoebozoa.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*80) -- Southern Ocean.‡2udc 700 1# ‡6880-03‡aBli︠u︡m, N. S. 773 0# ‡6880-04‡7nnas ‡tOkeanologii︠a︡. ‡gVol. 24(6) (1984) ‡wSPRI-37085 880 1# ‡6100-01/(N‡aОськина, Н. С. 880 10 ‡6245-02/(N‡aСтруктура танатоценоса планктонных фораминифер как индикатор океанских круговоротов и фронтов /‡cН.С. Оськина, Н.С. Блюм. 880 1# ‡6700-03/(N‡aБлюм, Н. С. 880 0# ‡6773-04/(N‡7nnas ‡tОкеанология. ‡gVol. 24(6) (1984) ‡wSPRI-37085 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418