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Record #140877:
- #140877
Main publication details
MARC recordHolocene 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 |
LDR 01771naa#a2200000#a#4500 001 SPRI-140877 005 20230607094620.0 007 ta 008 230607s1996####dk#a###|#####|0||#0#eng#d 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# ‡a20230607