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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 |
LDR 01790naa#a2200000#a#4500 001 SPRI-202475 005 20231207024741.0 007 ta 008 231207s2011####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# ‡a20231207 ‡bJW