The arctic regions are north of the tree line, but nev-ertheless wood is quite plentiful. Most of this wood in Greenland is driftwood that has floated across the Arctic Ocean, to be eventually deposited on beaches. Following previous deglaciations and isostatic rebound, raised beaches are common, an...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.628.4165 2023-05-15T14:35:56+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.4165 http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.4165 http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf text ftciteseerx 2016-01-08T15:19:57Z The arctic regions are north of the tree line, but nev-ertheless wood is quite plentiful. Most of this wood in Greenland is driftwood that has floated across the Arctic Ocean, to be eventually deposited on beaches. Following previous deglaciations and isostatic rebound, raised beaches are common, and driftwood may be common below the marine limit. Most driftwood is of postglacial age, but pre-Holocene driftwood has been reported from Greenland and elsewhere in the Arctic. Some of the pre-Holocene wood derives from trees that grew in the Arctic in the past, when climates were warmer than at the present. Best known are the Late Cretaceous and Early Tertiary diverse floras that com-prise many warmth-demanding species including vines, but the wood from these time periods is more or less Text Arctic Arctic Ocean Greenland Unknown Arctic Arctic Ocean Greenland Nev ENVELOPE(-6.623,-6.623,62.108,62.108) |
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Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
The arctic regions are north of the tree line, but nev-ertheless wood is quite plentiful. Most of this wood in Greenland is driftwood that has floated across the Arctic Ocean, to be eventually deposited on beaches. Following previous deglaciations and isostatic rebound, raised beaches are common, and driftwood may be common below the marine limit. Most driftwood is of postglacial age, but pre-Holocene driftwood has been reported from Greenland and elsewhere in the Arctic. Some of the pre-Holocene wood derives from trees that grew in the Arctic in the past, when climates were warmer than at the present. Best known are the Late Cretaceous and Early Tertiary diverse floras that com-prise many warmth-demanding species including vines, but the wood from these time periods is more or less |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.4165 http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf |
long_lat |
ENVELOPE(-6.623,-6.623,62.108,62.108) |
geographic |
Arctic Arctic Ocean Greenland Nev |
geographic_facet |
Arctic Arctic Ocean Greenland Nev |
genre |
Arctic Arctic Ocean Greenland |
genre_facet |
Arctic Arctic Ocean Greenland |
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http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.4165 http://www.geus.dk/publications/review-greenland-97/gsb180p155-158.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766308671538593792 |