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Record #104749:

High resolution ¹⁰Be and ²³⁰Th stratigraphy of Late Quaternary sediments from the Fram Strait (core 23235) / A. Eisenhauer, and 8 others.

Title: High resolution ¹⁰Be and ²³⁰Th stratigraphy of Late Quaternary sediments from the Fram Strait (core 23235) / A. Eisenhauer, and 8 others.
Author(s): Eisenhauer, A.
Date: 1990.
Publisher: Dordrecht: Kluwer Academic
In: Geological history of the polar oceans : Arctic versus Antarctic. (1990.),
Abstract: Variation in concentration of these isotopes yielded stratigraphy at resolution comparable to δ¹⁸O method. Radioisotope stratigraphy is useful tool for understanding geological record in sediments from high latitudes, where δ¹⁸O stratigraphy is not available due to low carbonate contents. Coherent ratio of fluxes of ¹⁰Be and ²³⁰Th into sediments may be used to trace periods of enhanced scavenging of trace elements from water column as response to periods of stronger biological productivity.
Notes:

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

Keywords: 551.336 -- Ice ages.
551.79 -- Quaternary.
551.33 -- Glacial geology.
551.337 -- Chronology of the Pleistocene and recent periods.
E7 -- Glaciology: glacial geology and ice ages.
(*60) -- Arctic Ocean and adjacent waters.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 104749

MARCXML

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001 SPRI-104749
005 20231129110717.0
007 ta
008 231129s1990####ne#a###|#####|0||#0#eng#d
035 ## ‡aSPRI-104749
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aEisenhauer, A.
245 10 ‡aHigh resolution ¹⁰Be and ²³⁰Th stratigraphy of Late Quaternary sediments from the Fram Strait (core 23235) /‡cA. Eisenhauer, and 8 others.
260 ## ‡aDordrecht :‡bKluwer Academic,‡c1990.
300 ## ‡ap. 475-487 :‡bdiags., table.
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# ‡aVariation in concentration of these isotopes yielded stratigraphy at resolution comparable to δ¹⁸O method. Radioisotope stratigraphy is useful tool for understanding geological record in sediments from high latitudes, where δ¹⁸O stratigraphy is not available due to low carbonate contents. Coherent ratio of fluxes of ¹⁰Be and ²³⁰Th into sediments may be used to trace periods of enhanced scavenging of trace elements from water column as response to periods of stronger biological productivity.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
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# ‡a20231129