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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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 |
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Open Polar |
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Wiley Online Library |
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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 |
container_volume |
26 |
container_issue |
3 |
container_start_page |
345 |
op_container_end_page |
352 |
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1800759218837389312 |