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Record #140313:

North Atlantic sea surface conditions during the Younger Dryas cold event / Jean-Claude Duplessy, Laurent D. Labeyrie, M. Paterne.

Title: North Atlantic sea surface conditions during the Younger Dryas cold event / Jean-Claude Duplessy, Laurent D. Labeyrie, M. Paterne.
Author(s): Duplessy, Jean-Claude.
Labeyrie, Laurent D.
Paterne, M.
Date: 1996.
Publisher: Bath: Geological Society
In: Late Quaternary palaeoceanography of the North Atlantic Margins. (1996.),
Abstract: Map showing main trends of sea surface temperature field during Younger Dryas has been drawn from study of oxygen isotopic composition (δ¹⁸O) of planktonic foraminifera which deposited shells in isotopic equilibrium with ambient surface waters. Map shows no δ¹⁸O anomaly associated with continental ice-sheet melting, so rules out theories relating Younger Dryas cooling to injection of continental ice-sheet meltwater with very low δ¹⁸O value into North Atlantic. Conclusions about Arctic sea ice and its effect on climate in last deglaciation are suggested.
Notes:

In: Late Quaternary palaeoceanography of the North Atlantic Margins / John T. Andrews, William E.N. Austin, Helene Bergsten, Anne E. Jennings, eds.

Keywords: 54.027 -- Isotope analysis.
551.326.7 -- Sea ice.
551.336 -- Ice ages.
551.461.8 -- Palaeo-oceanography.
551.463.6 -- Sea water, thermal properties and heat flux.
551.465.5 -- Ocean currents.
593.12 -- Foraminifera and amoebozoa.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*61) -- North Atlantic Ocean.
SPRI record no.: 140313

MARCXML

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001 SPRI-140313
005 20220925114041.0
007 ta
008 220925s1996####enkab##|#####|0||#0#eng#d
035 ## ‡aSPRI-140313
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aDuplessy, Jean-Claude.
245 10 ‡aNorth Atlantic sea surface conditions during the Younger Dryas cold event /‡cJean-Claude Duplessy, Laurent D. Labeyrie, M. Paterne.
260 ## ‡aBath :‡bGeological Society,‡c1996.
300 ## ‡ap. 167-175 :‡bdiags., table, maps.
500 ## ‡aIn: Late Quaternary palaeoceanography of the North Atlantic Margins / John T. Andrews, William E.N. Austin, Helene Bergsten, Anne E. Jennings, eds.
520 3# ‡aMap showing main trends of sea surface temperature field during Younger Dryas has been drawn from study of oxygen isotopic composition (δ¹⁸O) of planktonic foraminifera which deposited shells in isotopic equilibrium with ambient surface waters. Map shows no δ¹⁸O anomaly associated with continental ice-sheet melting, so rules out theories relating Younger Dryas cooling to injection of continental ice-sheet meltwater with very low δ¹⁸O value into North Atlantic. Conclusions about Arctic sea ice and its effect on climate in last deglaciation are suggested.
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.463.6 -- Sea water, thermal properties and heat flux.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡a593.12 -- Foraminifera and amoebozoa.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc
700 1# ‡aLabeyrie, Laurent D.
700 1# ‡aPaterne, M.
773 0# ‡7nnam ‡aJohn T. Andrews, William E.N. Austin, Helene Bergsten, Anne E. Jennings, eds. ‡tLate Quaternary palaeoceanography of the North Atlantic Margins. ‡dBath : Geological Society, 1996. ‡wSPRI-138922
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220925