Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska

Abstract Last interglacial sediments in unglaciated Alaska and Yukon (eastern Beringia) are commonly identified by palaeoecological indicators and stratigraphic position ∼2–5 m above the regionally prominent Old Crow tephra (124 ± 10 ka). We demonstrate that this approach can yield erroneous age ass...

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Published in:Journal of Quaternary Science
Main Authors: REYES, ALBERTO V., ZAZULA, GRANT D., KUZMINA, SVETLANA, AGER, THOMAS A., FROESE, DUANE G.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
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Online Access:http://dx.doi.org/10.1002/jqs.1464
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spelling crwiley:10.1002/jqs.1464 2024-06-02T08:12:42+00:00 Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska REYES, ALBERTO V. ZAZULA, GRANT D. KUZMINA, SVETLANA AGER, THOMAS A. FROESE, DUANE G. 2011 http://dx.doi.org/10.1002/jqs.1464 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1464 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1464 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 26, issue 3, page 345-352 ISSN 0267-8179 1099-1417 journal-article 2011 crwiley https://doi.org/10.1002/jqs.1464 2024-05-03T11:41:00Z Abstract Last interglacial sediments in unglaciated Alaska and Yukon (eastern Beringia) are commonly identified by palaeoecological indicators and stratigraphic position ∼2–5 m above the regionally prominent Old Crow tephra (124 ± 10 ka). We demonstrate that this approach can yield erroneous age assignments using data from a new exposure at the Palisades, a site in interior Alaska with numerous exposures of last interglacial sediments. Tephrochronology, stratigraphy, plant macrofossils, pollen and fossil insects from a prominent wood‐rich organic silt unit are all consistent with a last interglacial age assignment. However, six 14 C dates on plant and insect macrofossils from the organic silt range from non‐finite to 4.0 14 C ka BP, indicating that the organic silt instead represents a Holocene deposit with a mixed‐age assemblage of organic material. In contrast, wood samples from presumed last interglacial organic‐rich sediments elsewhere at the Palisades, in a similar stratigraphic position with respect to Old Crow tephra, yield non‐finite 14 C ages. Given that local permafrost thaw since the last interglaciation may facilitate reworking of older sediments into new stratigraphic positions, minimum constraining ages based on 14 C dating or other methods should supplement age assignments for last interglacial sediments in eastern Beringia that are based on palaeoecology and stratigraphic association with Old Crow tephra. Copyright © 2011 John Wiley & Sons, Ltd. Article in Journal/Newspaper Old Crow permafrost Alaska Beringia Yukon Wiley Online Library Palisades ENVELOPE(159.167,159.167,-82.833,-82.833) The Palisades ENVELOPE(159.167,159.167,-82.833,-82.833) Yukon Journal of Quaternary Science 26 3 345 352
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Last interglacial sediments in unglaciated Alaska and Yukon (eastern Beringia) are commonly identified by palaeoecological indicators and stratigraphic position ∼2–5 m above the regionally prominent Old Crow tephra (124 ± 10 ka). We demonstrate that this approach can yield erroneous age assignments using data from a new exposure at the Palisades, a site in interior Alaska with numerous exposures of last interglacial sediments. Tephrochronology, stratigraphy, plant macrofossils, pollen and fossil insects from a prominent wood‐rich organic silt unit are all consistent with a last interglacial age assignment. However, six 14 C dates on plant and insect macrofossils from the organic silt range from non‐finite to 4.0 14 C ka BP, indicating that the organic silt instead represents a Holocene deposit with a mixed‐age assemblage of organic material. In contrast, wood samples from presumed last interglacial organic‐rich sediments elsewhere at the Palisades, in a similar stratigraphic position with respect to Old Crow tephra, yield non‐finite 14 C ages. Given that local permafrost thaw since the last interglaciation may facilitate reworking of older sediments into new stratigraphic positions, minimum constraining ages based on 14 C dating or other methods should supplement age assignments for last interglacial sediments in eastern Beringia that are based on palaeoecology and stratigraphic association with Old Crow tephra. Copyright © 2011 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author REYES, ALBERTO V.
ZAZULA, GRANT D.
KUZMINA, SVETLANA
AGER, THOMAS A.
FROESE, DUANE G.
spellingShingle REYES, ALBERTO V.
ZAZULA, GRANT D.
KUZMINA, SVETLANA
AGER, THOMAS A.
FROESE, DUANE G.
Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
author_facet REYES, ALBERTO V.
ZAZULA, GRANT D.
KUZMINA, SVETLANA
AGER, THOMAS A.
FROESE, DUANE G.
author_sort REYES, ALBERTO V.
title Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
title_short Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
title_full Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
title_fullStr Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
title_full_unstemmed Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska
title_sort identification of last interglacial deposits in eastern beringia: a cautionary note from the palisades, interior alaska
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/jqs.1464
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1464
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1464
long_lat ENVELOPE(159.167,159.167,-82.833,-82.833)
ENVELOPE(159.167,159.167,-82.833,-82.833)
geographic Palisades
The Palisades
Yukon
geographic_facet Palisades
The Palisades
Yukon
genre Old Crow
permafrost
Alaska
Beringia
Yukon
genre_facet Old Crow
permafrost
Alaska
Beringia
Yukon
op_source Journal of Quaternary Science
volume 26, issue 3, page 345-352
ISSN 0267-8179 1099-1417
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/jqs.1464
container_title Journal of Quaternary Science
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