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Record #186985:

Lake sediments from Store Koldewey, northeast Greenland, as archive of Late Pleistocene and Holocene climatic and environmental changes / Martin Klug, and 5 others.

Title: Lake sediments from Store Koldewey, northeast Greenland, as archive of Late Pleistocene and Holocene climatic and environmental changes / Martin Klug, and 5 others.
Author(s): Klug, Martin.
Date: 2009.
In: Boreas. (2009.), Vol. 38(1) (2009)
Abstract: Investigates 2.9 m sedimentary record from small lake (Duck Lake) located on Store Koldewey. Sediments are investigated for geophysical and biogeochemical characteristics, and for fossil chironomid assemblages. Finds that organic matter began to accumulate in lake at 9.1 cal. kyr BP, which provides minimum age for deglaciation of basin; also that organic matter accumulation in lake remained low during Early Holocene, possibly due to late plant immigration and lack of nutrient availability, but increased during Middle and Late Holocene, when temperatures gradually decreased.
Notes:

Boreas. Vol. 38(1) :59-71 (2009).

Keywords: 556 -- Hydrology.
556.55 -- Lakes and ponds.
556.555.6 -- Lakes, sediments.
574 -- Ecology.
56 -- Palaeontology.
574.5 -- Marine and freshwater ecology.
574.523 -- Food chains and networks, aquatic.
F -- Biological sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*387) -- North Greenland.
SPRI record no.: 186985

MARCXML

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001 SPRI-186985
005 20221006125432.0
007 ta
008 221006s2009####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-186985
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aKlug, Martin.
245 10 ‡aLake sediments from Store Koldewey, northeast Greenland, as archive of Late Pleistocene and Holocene climatic and environmental changes /‡cMartin Klug, and 5 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 59-71 :‡bill., diags., tables.
500 ## ‡aBoreas. Vol. 38(1) :59-71 (2009).
520 3# ‡aInvestigates 2.9 m sedimentary record from small lake (Duck Lake) located on Store Koldewey. Sediments are investigated for geophysical and biogeochemical characteristics, and for fossil chironomid assemblages. Finds that organic matter began to accumulate in lake at 9.1 cal. kyr BP, which provides minimum age for deglaciation of basin; also that organic matter accumulation in lake remained low during Early Holocene, possibly due to late plant immigration and lack of nutrient availability, but increased during Middle and Late Holocene, when temperatures gradually decreased.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2008.00038.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2008.00038.x
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡a556.55 -- Lakes and ponds.‡2udc
650 07 ‡a556.555.6 -- Lakes, sediments.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a574.5 -- Marine and freshwater ecology.‡2udc
650 07 ‡a574.523 -- Food chains and networks, aquatic.‡2udc
650 07 ‡aF -- Biological sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*387) -- North Greenland.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 38(1) (2009) ‡wSPRI-56035
916 ## ‡a2009/08/11 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221006 ‡bJW