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Record #144030:

Late Quaternary glacial history and palaeoceanographic reconstructions along the East Greenland continental margin: Evidence from high-resolution records of stable isotopes and ice-rafted debris / Seung-Il Nam.

Title: Late Quaternary glacial history and palaeoceanographic reconstructions along the East Greenland continental margin: Evidence from high-resolution records of stable isotopes and ice-rafted debris / Seung-Il Nam.
Author(s): Nam, Seung-Il.
Date: 1997.
In: Berichte zur Polarforschung = Reports on Polar Research. (1997.), Vol. 241 (1997)
Abstract: Analyses were performed in order to reconstruct climatic and oceanographic conditions in late Quaternary and to link terrestrial and deep- sea climatic records. 16 gravity and 2 box cores were taken from margin between 69 and 72 deg. N on three W-E transects from shelf to deep sea. Glaciomarine sediments are dominated by terrestrially derived components and biogenic components are low. Processes are influenced by fluctuations in extent of Greenland Ice Sheet, sea ice cover, rate of iceberg drifting, meltwater input and changes in East Greenland Current.
Notes:

Berichte zur Polarforschung = Reports on Polar Research. Vol. 241 :1-157 (1997).

Keywords: 551.3.051 -- Sedimentation and stratification.
551.324.6 -- Land ice, fluctuation.
551.326.5 -- Floating ice, extraneous matter.
551.461.8 -- Palaeo-oceanography.
551.79 -- Quaternary.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 144030

MARCXML

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001 SPRI-144030
005 20221002014153.0
007 ta
008 221002s1997####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-144030
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aNam, Seung-Il.
245 10 ‡aLate Quaternary glacial history and palaeoceanographic reconstructions along the East Greenland continental margin :‡bEvidence from high-resolution records of stable isotopes and ice-rafted debris /‡cSeung-Il Nam.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1997.
300 ## ‡ap. 1-157 :‡bdiags., tables, maps.
500 ## ‡aBerichte zur Polarforschung = Reports on Polar Research. Vol. 241 :1-157 (1997).
520 3# ‡aAnalyses were performed in order to reconstruct climatic and oceanographic conditions in late Quaternary and to link terrestrial and deep- sea climatic records. 16 gravity and 2 box cores were taken from margin between 69 and 72 deg. N on three W-E transects from shelf to deep sea. Glaciomarine sediments are dominated by terrestrially derived components and biogenic components are low. Processes are influenced by fluctuations in extent of Greenland Ice Sheet, sea ice cover, rate of iceberg drifting, meltwater input and changes in East Greenland Current.
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a551.326.5 -- Floating ice, extraneous matter.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
773 0# ‡7nnas ‡tBerichte zur Polarforschung = Reports on Polar Research. ‡gVol. 241 (1997) ‡wSPRI-64232
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221002