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Record #131404:

Land biotas of the last interglacial/glacial cycle, Jameson Land, East Greenland / O. Bennike, Jens Böcher.

Title: Land biotas of the last interglacial/glacial cycle, Jameson Land, East Greenland / O. Bennike, Jens Böcher.
Author(s): Bennike, O.
Böcher, Jens.
Date: 1994.
In: Boreas. (1994.), Vol. 23(4) (1994)
Abstract: Macrofossil plant and insect remains from nearshore marine sediments in Jameson Land show that land biotas of last interglacial stage were more diverse than those of Holocene. Rich dwarf shrub heaths with diverse assemblage of ericaceous plants occupied low land areas with copses of Betula pubescens on sheltered sites. Many southern extra-limital species were present and summer temperature was 5°C higher than today. Beetles were of palaearctic type. Some fossils from Hugin Sø interstade point to mean summer temperature 3-4°C lower than today.
Notes:

Boreas. Vol. 23(4) :479-487 (1994).

Keywords: 551.1/.4 -- Geology.
551.336 -- Ice ages.
551.583.3 -- Climatic changes, Quaternary.
551.79 -- Quaternary.
56 -- Palaeontology.
58 -- Botany.
595.7 -- Insecta.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*381) -- East Greenland.
(*381.4) -- Kong Christian den Xs Land.
SPRI record no.: 131404

MARCXML

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007 ta
008 240419s1994####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-131404
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100 1# ‡aBennike, O.
245 10 ‡aLand biotas of the last interglacial/glacial cycle, Jameson Land, East Greenland /‡cO. Bennike, Jens Böcher.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 479-487 :‡bill., diags., tables, maps.
500 ## ‡aBoreas. Vol. 23(4) :479-487 (1994).
520 3# ‡aMacrofossil plant and insect remains from nearshore marine sediments in Jameson Land show that land biotas of last interglacial stage were more diverse than those of Holocene. Rich dwarf shrub heaths with diverse assemblage of ericaceous plants occupied low land areas with copses of Betula pubescens on sheltered sites. Many southern extra-limital species were present and summer temperature was 5°C higher than today. Beetles were of palaearctic type. Some fossils from Hugin Sø interstade point to mean summer temperature 3-4°C lower than today.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a58 -- Botany.‡2udc
650 07 ‡a595.7 -- Insecta.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*381) -- East Greenland.‡2udc
651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc
700 1# ‡aBöcher, Jens.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 23(4) (1994) ‡wSPRI-56035
917 ## ‡aUnenhanced record from Muscat, imported 2019
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