ARCTIC Mackenzie River Driftwood- A Dendrochronological Study

ABSTRACT. As part of a geqeral study of arctic driftwood, 206 samples of driftwood logs from the Mackenzie delta area were analyzed by dendrochronological methods (tree-ring studies). The aim was to detect the origin of the wood. Three forest stands in the delta were also sampled, and tree-ring chro...

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Main Author: Olafur Eggertsson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1993
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.8219
http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.8219 2023-05-15T14:19:36+02:00 ARCTIC Mackenzie River Driftwood- A Dendrochronological Study Olafur Eggertsson The Pennsylvania State University CiteSeerX Archives 1993 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.8219 http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.8219 http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf text 1993 ftciteseerx 2016-01-08T10:18:37Z ABSTRACT. As part of a geqeral study of arctic driftwood, 206 samples of driftwood logs from the Mackenzie delta area were analyzed by dendrochronological methods (tree-ring studies). The aim was to detect the origin of the wood. Three forest stands in the delta were also sampled, and tree-ring chronologies were constructed. The Mackenzie driftwood can be divided into four groups: 1) driftwood originating from the upper Mackenzie delta area with individual logs having up to 600 tree rings, 2) driftwood originating near the southern limit of the delta, 3) Wood with relatively few tree rings with possible origin in the Liard River drainage area, and 4) driftwood samples not datable with any available chronologies. Three driftwood samples from the Coast of Greenland could be correlated with tree-ring chronologies from the Mackenzie delta area and another three were correlated with chronologies from Alaska. American driftwood has not been detected in collections from Svalbard and Iceland, although more than 200 samples have been analyzed from each area. This indicates that some American driftwood is trans-ported from the Beaufort and Bering seas to the North Atlantic Ocean, probably via the western part of the East Greenland Current,. This wood is deposited on the Coast of Greenland. American driftwood probably does not reach the islands in the central and eastern North Atlantic. Text Arctic Arctic East Greenland east greenland current Greenland Iceland Liard River Mackenzie Delta Mackenzie river North Atlantic Svalbard Alaska Unknown Arctic Greenland Liard ENVELOPE(-67.417,-67.417,-66.850,-66.850) Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Mackenzie River Svalbard
institution Open Polar
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language English
description ABSTRACT. As part of a geqeral study of arctic driftwood, 206 samples of driftwood logs from the Mackenzie delta area were analyzed by dendrochronological methods (tree-ring studies). The aim was to detect the origin of the wood. Three forest stands in the delta were also sampled, and tree-ring chronologies were constructed. The Mackenzie driftwood can be divided into four groups: 1) driftwood originating from the upper Mackenzie delta area with individual logs having up to 600 tree rings, 2) driftwood originating near the southern limit of the delta, 3) Wood with relatively few tree rings with possible origin in the Liard River drainage area, and 4) driftwood samples not datable with any available chronologies. Three driftwood samples from the Coast of Greenland could be correlated with tree-ring chronologies from the Mackenzie delta area and another three were correlated with chronologies from Alaska. American driftwood has not been detected in collections from Svalbard and Iceland, although more than 200 samples have been analyzed from each area. This indicates that some American driftwood is trans-ported from the Beaufort and Bering seas to the North Atlantic Ocean, probably via the western part of the East Greenland Current,. This wood is deposited on the Coast of Greenland. American driftwood probably does not reach the islands in the central and eastern North Atlantic.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Olafur Eggertsson
spellingShingle Olafur Eggertsson
ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
author_facet Olafur Eggertsson
author_sort Olafur Eggertsson
title ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
title_short ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
title_full ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
title_fullStr ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
title_full_unstemmed ARCTIC Mackenzie River Driftwood- A Dendrochronological Study
title_sort arctic mackenzie river driftwood- a dendrochronological study
publishDate 1993
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.8219
http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf
long_lat ENVELOPE(-67.417,-67.417,-66.850,-66.850)
ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Arctic
Greenland
Liard
Mackenzie Delta
Mackenzie River
Svalbard
geographic_facet Arctic
Greenland
Liard
Mackenzie Delta
Mackenzie River
Svalbard
genre Arctic
Arctic
East Greenland
east greenland current
Greenland
Iceland
Liard River
Mackenzie Delta
Mackenzie river
North Atlantic
Svalbard
Alaska
genre_facet Arctic
Arctic
East Greenland
east greenland current
Greenland
Iceland
Liard River
Mackenzie Delta
Mackenzie river
North Atlantic
Svalbard
Alaska
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.8219
http://pubs.aina.ucalgary.ca/arctic/Arctic47-2-128.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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