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Record #202475:

Chironomids as indicators of the Holocene climatic and environmental history of two lakes in northeast Greenland / Steffi Schmidt, and 5 others.

Title: Chironomids as indicators of the Holocene climatic and environmental history of two lakes in northeast Greenland / Steffi Schmidt, and 5 others.
Author(s): Schmidt, Steffi.
Date: 2011.
In: Boreas. (2011.), Vol. 40(1) (2011)
Abstract: Investigates two Holocene sediment sequences from Arctic lakes on Store Koldewey, island in north-east Greenland, for fossil chironomid assemblages. Uses canonical correspondence analysis to compare assemblages from Store Koldewey with chironomid assemblages and environmental conditions presently found in Canadian Arctic lake and, hence, to infer environmental changes for north-east Greenland. Temperature development inferred by chironomids, with cool Early Holocene, warmer Mid-Holocene and relatively cool Late Holocene, is supported by other palaeoclimate records from region.
Notes:

Boreas. Vol. 40(1) :116-130 (2011).

Keywords: 551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
551.794 -- Holocene.
556.555.6 -- Lakes, sediments.
56 -- Palaeontology.
574 -- Ecology.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*387) -- North Greenland.
SPRI record no.: 202475

MARCXML

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001 SPRI-202475
005 20220926195852.0
007 ta
008 220926s2011####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-202475
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSchmidt, Steffi.
245 10 ‡aChironomids as indicators of the Holocene climatic and environmental history of two lakes in northeast Greenland /‡cSteffi Schmidt, and 5 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2011.
300 ## ‡ap. 116-130 :‡bill., diags., tables, map.
500 ## ‡aBoreas. Vol. 40(1) :116-130 (2011).
520 3# ‡aInvestigates two Holocene sediment sequences from Arctic lakes on Store Koldewey, island in north-east Greenland, for fossil chironomid assemblages. Uses canonical correspondence analysis to compare assemblages from Store Koldewey with chironomid assemblages and environmental conditions presently found in Canadian Arctic lake and, hence, to infer environmental changes for north-east Greenland. Temperature development inferred by chironomids, with cool Early Holocene, warmer Mid-Holocene and relatively cool Late Holocene, is supported by other palaeoclimate records from region.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2010.00173.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2010.00173.x
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a556.555.6 -- Lakes, sediments.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡aD -- Atmospheric 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. 40(1) (2011) ‡wSPRI-56035
916 ## ‡a2013/02/26 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220926 ‡bJW