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Record #104750:

The enigma of oxygen isotope stage 5 in the central Fram Strait / S.E.I. Köhler, R.F. Spielhagen.

Title: The enigma of oxygen isotope stage 5 in the central Fram Strait / S.E.I. Köhler, R.F. Spielhagen.
Author(s): Köhler, S. E. I.
Spielhagen, R. F.
Date: 1990.
Publisher: Dordrecht: Kluwer Academic
In: Geological history of the polar oceans : Arctic versus Antarctic. (1990.),
Abstract: Stable oxygen isotope stratigraphy for last 150 ka is established in sedimentary cores from this region. Radiometric ages obtained by U/Th method in one core provide absolute time framework. δ¹⁸O record from substage 5a in central Fram Strait is represented by lighter δ¹⁸O ratios than substage 5e. This probably reflects lower salinities of uppermost water column due to intense melting of icebergs and/or supply of meltwater from adjacent land masses rather than higher sea surface temperatures.
Notes:

In: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds.

Keywords: 551.337 -- Chronology of the Pleistocene and recent periods.
551.336 -- Ice ages.
551.79 -- Quaternary.
550.93 -- Geochronology.
551.461.8 -- Palaeo-oceanography.
551.33 -- Glacial geology.
C -- Oceanography, hydrography and hydrology.
(*60) -- Arctic Ocean and adjacent waters.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 104750

MARCXML

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001 SPRI-104750
005 20221129101242.0
007 ta
008 221129s1990####ne#ab##|#####|0||#0#eng#d
035 ## ‡aSPRI-104750
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aKöhler, S. E. I.
245 14 ‡aThe enigma of oxygen isotope stage 5 in the central Fram Strait /‡cS.E.I. Köhler, R.F. Spielhagen.
260 ## ‡aDordrecht :‡bKluwer Academic,‡c1990.
300 ## ‡ap. 489-497 :‡bdiags., map.
490 0# ‡aNATO ASI Series. Series C, Mathematical and Physical Sciences ;‡v308
500 ## ‡aIn: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds.
520 3# ‡aStable oxygen isotope stratigraphy for last 150 ka is established in sedimentary cores from this region. Radiometric ages obtained by U/Th method in one core provide absolute time framework. δ¹⁸O record from substage 5a in central Fram Strait is represented by lighter δ¹⁸O ratios than substage 5e. This probably reflects lower salinities of uppermost water column due to intense melting of icebergs and/or supply of meltwater from adjacent land masses rather than higher sea surface temperatures.
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
700 1# ‡aSpielhagen, R. F.
773 0# ‡7nnam ‡aUlrich Bleil, Jörn Thiede, eds. ‡tGeological history of the polar oceans : Arctic versus Antarctic. ‡dDordrecht : Kluwer Academic, 1990. ‡wSPRI-104236
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221129