The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska

Abstract We present a multi‐proxy reconstruction from a well‐preserved vegetation surface (ca. 32 000 14 C a BP) from the Fox Permafrost tunnel near Fairbanks, Alaska. A thick litter layer of plant material on the vegetation surface is consistent with the vegetation lacking evidence of disturbance....

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Published in:Journal of Quaternary Science
Main Authors: Wooller, Matthew J., Zazula, Grant D., Blinnikov, Misha., Gaglioti, Benjamin. V., Bigelow, Nancy. H., Sanborn, Paul., Kuzmina, Svetlana., La Farge, Catherine.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
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Online Access:http://dx.doi.org/10.1002/jqs.1497
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spelling crwiley:10.1002/jqs.1497 2024-06-02T08:13:06+00:00 The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska Wooller, Matthew J. Zazula, Grant D. Blinnikov, Misha. Gaglioti, Benjamin. V. Bigelow, Nancy. H. Sanborn, Paul. Kuzmina, Svetlana. La Farge, Catherine. 2011 http://dx.doi.org/10.1002/jqs.1497 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1497 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1497 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 26, issue 7, page 746-756 ISSN 0267-8179 1099-1417 journal-article 2011 crwiley https://doi.org/10.1002/jqs.1497 2024-05-03T11:23:00Z Abstract We present a multi‐proxy reconstruction from a well‐preserved vegetation surface (ca. 32 000 14 C a BP) from the Fox Permafrost tunnel near Fairbanks, Alaska. A thick litter layer of plant material on the vegetation surface is consistent with the vegetation lacking evidence of disturbance. Plant macrofossils and graminoid cuticle analysis show the presence of a graminoid assemblage consistent with phytolith data. The pollen data indicate that trees were not local to the site and that Artemisia sp. was present in the region. The insect and bryophyte reconstructions are consistent with the vascular plant reconstruction, indicating the site was at least periodically wet. δ 13 C values from the graminoids present show a large range encompassing both the wet and dry range displayed by modern graminoids in Alaska. Sequential δ 13 C analyses conducted along the length of leaves attached to the vegetation surface indicate a seasonal shift towards relatively higher water use efficiency. The lower water use efficiency earlier in the growing season may have stemmed from the use of winter season meltwater by plants at the site – a scenario consistent with the site's cryostratigraphy. Our multi‐proxy reconstruction contributes to the limited palaeoecological data available for graminoid‐dominated vegetation present in Eastern Beringia and particularly the interior of Alaska during the mid‐Wisconsinan interstadial. Copyright © 2011 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost Alaska Beringia Wiley Online Library Fairbanks Journal of Quaternary Science 26 7 746 756
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract We present a multi‐proxy reconstruction from a well‐preserved vegetation surface (ca. 32 000 14 C a BP) from the Fox Permafrost tunnel near Fairbanks, Alaska. A thick litter layer of plant material on the vegetation surface is consistent with the vegetation lacking evidence of disturbance. Plant macrofossils and graminoid cuticle analysis show the presence of a graminoid assemblage consistent with phytolith data. The pollen data indicate that trees were not local to the site and that Artemisia sp. was present in the region. The insect and bryophyte reconstructions are consistent with the vascular plant reconstruction, indicating the site was at least periodically wet. δ 13 C values from the graminoids present show a large range encompassing both the wet and dry range displayed by modern graminoids in Alaska. Sequential δ 13 C analyses conducted along the length of leaves attached to the vegetation surface indicate a seasonal shift towards relatively higher water use efficiency. The lower water use efficiency earlier in the growing season may have stemmed from the use of winter season meltwater by plants at the site – a scenario consistent with the site's cryostratigraphy. Our multi‐proxy reconstruction contributes to the limited palaeoecological data available for graminoid‐dominated vegetation present in Eastern Beringia and particularly the interior of Alaska during the mid‐Wisconsinan interstadial. Copyright © 2011 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Wooller, Matthew J.
Zazula, Grant D.
Blinnikov, Misha.
Gaglioti, Benjamin. V.
Bigelow, Nancy. H.
Sanborn, Paul.
Kuzmina, Svetlana.
La Farge, Catherine.
spellingShingle Wooller, Matthew J.
Zazula, Grant D.
Blinnikov, Misha.
Gaglioti, Benjamin. V.
Bigelow, Nancy. H.
Sanborn, Paul.
Kuzmina, Svetlana.
La Farge, Catherine.
The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
author_facet Wooller, Matthew J.
Zazula, Grant D.
Blinnikov, Misha.
Gaglioti, Benjamin. V.
Bigelow, Nancy. H.
Sanborn, Paul.
Kuzmina, Svetlana.
La Farge, Catherine.
author_sort Wooller, Matthew J.
title The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
title_short The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
title_full The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
title_fullStr The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
title_full_unstemmed The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska
title_sort detailed palaeoecology of a mid‐wisconsinan interstadial (ca. 32 000 14 c a bp) vegetation surface from interior alaska
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/jqs.1497
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1497
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1497
geographic Fairbanks
geographic_facet Fairbanks
genre permafrost
Alaska
Beringia
genre_facet permafrost
Alaska
Beringia
op_source Journal of Quaternary Science
volume 26, issue 7, page 746-756
ISSN 0267-8179 1099-1417
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op_doi https://doi.org/10.1002/jqs.1497
container_title Journal of Quaternary Science
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