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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #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

LDR 01718naa#a2200000#a#4500
001 SPRI-104749
005 20240419024443.0
007 ta
008 240419s1990####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# ‡a20240419