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Record #140877:

Holocene climatic changes in Greenland / Bent Fredskild.

Title: Holocene climatic changes in Greenland / Bent Fredskild.
Author(s): Fredskild, Bent.
Date: 1996.
Publisher: Copenhagen: Danish Polar Center
In: Paleo-Eskimo Cultures of Greenland - new perspectives in Greenlandic archaeology. (1996.), Vol. 19
Abstract: Botanical indications of Holocene climatic changes in Greenland are summarized. Most information comes from pollen and macrofossil analyses of lake sediments and peat. Main trend, supported by Ice Cap cores, is clear: in West Greenland, temperature reached that of today c. 6000 BC, to peak some millenia later. In north, increase came later. C. 2000 BC, temperature began to decrease, and with fluctuations became colder until Little Ice Age. In East Greenland increase and decrease were millenium earlier. In central West Greenland sea temperature was higher during mid Holocene.
Notes:

In: The Paleo-Eskimo Cultures of Greenland - new perspectives in Greenlandic archaeology. Vol. 19 / Bjarne Grønnow, John Pind.

Keywords: 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
551.583 -- Climatic changes.
551.583.2 -- Climatic changes, historic.
551.794 -- Holocene.
56 -- Palaeontology.
581.081.3 -- Pollen analysis.
903 -- Archaeology.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
SPRI record no.: 140877

MARCXML

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005 20220924210735.0
007 ta
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035 ## ‡aSPRI-140877
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aFredskild, Bent.
245 10 ‡aHolocene climatic changes in Greenland /‡cBent Fredskild.
260 ## ‡aCopenhagen :‡bDanish Polar Center,‡c1996.
300 ## ‡ap. 243-251 :‡bdiags.
500 ## ‡aIn: The Paleo-Eskimo Cultures of Greenland - new perspectives in Greenlandic archaeology. Vol. 19 / Bjarne Grønnow, John Pind.
520 3# ‡aBotanical indications of Holocene climatic changes in Greenland are summarized. Most information comes from pollen and macrofossil analyses of lake sediments and peat. Main trend, supported by Ice Cap cores, is clear: in West Greenland, temperature reached that of today c. 6000 BC, to peak some millenia later. In north, increase came later. C. 2000 BC, temperature began to decrease, and with fluctuations became colder until Little Ice Age. In East Greenland increase and decrease were millenium earlier. In central West Greenland sea temperature was higher during mid Holocene.
650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.2 -- Climatic changes, historic.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a581.081.3 -- Pollen analysis.‡2udc
650 07 ‡a903 -- Archaeology.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
773 0# ‡7p1am ‡aGrønnow, Bjarne. ‡tPaleo-Eskimo Cultures of Greenland - new perspectives in Greenlandic archaeology. ‡dCopenhagen : Danish Polar Center, 1996. ‡gVol. 19 ‡wSPRI-139544
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924