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Record #200853:

Holocene climate variations at the entrance to a warm Arctic fjord: evidence from Kongsfjorden trough, Svalbard / Kari Skirbekk, and 4 others.

Title: Holocene climate variations at the entrance to a warm Arctic fjord: evidence from Kongsfjorden trough, Svalbard / Kari Skirbekk, and 4 others.
Author(s): Skirbekk, Kari.
Date: 2010.
Publisher: London: Geological Society
In: Fjord systems and archives. (2010.),
Abstract: Investigates sediment core (NPo5-11-21GC) from Kongsfjorden trough, which spans last 12 ka. Core site currently experiences seasonal inflow of Atlantic Water (AW) masses and may provide record of past variations in AW inflow to Arctic. Uses lithological analysis and benthic foraminifera to reconstruct palaeoceanographic development in area. Results show that cold and harsh conditions prevailed during late part of Younger Dryas and that site was in proximity to glaciers.
Notes:

In: Fjord systems and archives / J.A. Howe, and 3 others.

Keywords: 550.822 -- Geological drilling and coring.
551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.468.2 -- Fjords, oceanography.
551.794 -- Holocene.
551.583.3 -- Climatic changes, Quaternary.
551.588.5 -- Climate, relationship with ice.
574 -- Ecology.
56 -- Palaeontology.
593.12 -- Foraminifera and amoebozoa.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 200853

MARCXML

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001 SPRI-200853
005 20221007171810.0
007 ta
008 221007s2010####enkab##|#####|0||#0#eng#d
035 ## ‡aSPRI-200853
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSkirbekk, Kari.
245 10 ‡aHolocene climate variations at the entrance to a warm Arctic fjord :‡bevidence from Kongsfjorden trough, Svalbard /‡cKari Skirbekk, and 4 others.
260 ## ‡aLondon :‡bGeological Society,‡c2010.
300 ## ‡ap. 289-304 :‡bill., diags., table, maps.
500 ## ‡aIn: Fjord systems and archives / J.A. Howe, and 3 others.
520 3# ‡aInvestigates sediment core (NPo5-11-21GC) from Kongsfjorden trough, which spans last 12 ka. Core site currently experiences seasonal inflow of Atlantic Water (AW) masses and may provide record of past variations in AW inflow to Arctic. Uses lithological analysis and benthic foraminifera to reconstruct palaeoceanographic development in area. Results show that cold and harsh conditions prevailed during late part of Younger Dryas and that site was in proximity to glaciers.
530 ## ‡aAlso issued online ‡uurn:doi:10.1144/SP344.20‡uhttps://dx.doi.org/10.1144/SP344.20
650 07 ‡a550.822 -- Geological drilling and coring.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.468.2 -- Fjords, oceanography.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a593.12 -- Foraminifera and amoebozoa.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
773 0# ‡7p1am ‡aHowe, J. A. ‡tFjord systems and archives. ‡dLondon : Geological Society, 2010. ‡wSPRI-199569
916 ## ‡a2012/12/20 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221007 ‡bJW