skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #119217:

The Norwegian Sea record of the last interglacial to glacial transition / Jean-Claude Duplessy, Laurent D. Labeyrie.

Title: The Norwegian Sea record of the last interglacial to glacial transition / Jean-Claude Duplessy, Laurent D. Labeyrie.
Author(s): Duplessy, Jean-Claude.
Labeyrie, Laurent D.
Date: 1992.
Publisher: Berlin: Springer
In: Start of a glacial. (1992.),
Abstract: Analysis of δ¹⁸O record of benthic foraminifera in deep sea cores shows that, at end of Eemian interglacial (isotopic substage 5e), continental ice sheets grew significantly, culminating in maximum of isotopic substage 5d. Ice volume was then about half of that of last glacial maximum, indicating that 5e/5d transition marks inception of glaciation over northern hemisphere. Subpolar planktonic foraminifera almost disappeared during second half of 5e, suggesting cooling of surface waters, which preceded development of continental ice sheets. As high temperatures prevailed south of Greenland--Iceland--Faeroes strait, thermal contrast between warm North Atlantic and cold Norwegian Sea reinforced natural cyclogenesis, producing heavy snowstorms over subpolar continents.
Notes:

In: Start of a glacial / George J. Kukla, Ellen Went, eds.

Keywords: 551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
551.588.5 -- Climate, relationship with ice.
551.336 -- Ice ages.
551.79 -- Quaternary.
E9 -- Glaciology: meteorology and climatology.
(*60) -- Arctic Ocean and adjacent waters.
(*615) -- Norwegian Sea.
SPRI record no.: 119217

MARCXML

LDR 01959naa#a2200000#a#4500
001 SPRI-119217
005 20221003040734.0
007 ta
008 221003s1992####gw#ab##|#####|0||#0#eng#d
035 ## ‡aSPRI-119217
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aDuplessy, Jean-Claude.
245 14 ‡aThe Norwegian Sea record of the last interglacial to glacial transition /‡cJean-Claude Duplessy, Laurent D. Labeyrie.
260 ## ‡aBerlin :‡bSpringer,‡c1992.
300 ## ‡ap. 173-183 :‡bdiags., map.
490 0# ‡aNATO ASI Series. Series I: Global environmental change ;‡v3
500 ## ‡aIn: Start of a glacial / George J. Kukla, Ellen Went, eds.
520 3# ‡aAnalysis of δ¹⁸O record of benthic foraminifera in deep sea cores shows that, at end of Eemian interglacial (isotopic substage 5e), continental ice sheets grew significantly, culminating in maximum of isotopic substage 5d. Ice volume was then about half of that of last glacial maximum, indicating that 5e/5d transition marks inception of glaciation over northern hemisphere. Subpolar planktonic foraminifera almost disappeared during second half of 5e, suggesting cooling of surface waters, which preceded development of continental ice sheets. As high temperatures prevailed south of Greenland--Iceland--Faeroes strait, thermal contrast between warm North Atlantic and cold Norwegian Sea reinforced natural cyclogenesis, producing heavy snowstorms over subpolar continents.
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*615) -- Norwegian Sea.‡2udc
700 1# ‡aLabeyrie, Laurent D.
773 0# ‡7nnam ‡aGeorge J. Kukla, Ellen Went, eds. ‡tStart of a glacial. ‡dBerlin : Springer, 1992. ‡wSPRI-119215
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003