The distribution of late-Quaternary woody taxa in northern Eurasia: evidence from a new macrofossil database
The distribution of late-Quaternary woody taxa in northern Eurasia: evidence from a new macrofossil database
We present a database of late-Quaternary plant macrofossil records for northern Eurasia (from 23° to 180°E and 46° to 76°N) comprising 281 localities, over 2300 samples and over 13,000 individual records. Samples are individually radiocarbon dated or are assigned ages via age models fitted to sequences of calibrated radiocarbon dates within a section. Tree species characteristic of modern northern forests (e.g. Picea, Larix, tree-Betula) are recorded at least intermittently from prior to the last glacial maximum (LGM), through the LGM and Lateglacial, to the Holocene, and some records locate trees close to the limits of the Scandinavian ice sheet, supporting the hypothesis that some taxa persisted in northern refugia during the last glacial cycle. Northern trees show differing spatio-temporal patterns across Siberia: deciduous trees were widespread in the Lateglacial, with individuals occurring across much of their contemporary ranges, while evergreen conifers expanded northwards to their range limits in the Holocene.
2445-2464
Binney, Heather A.
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Willis, Katherine J.
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Edwards, Mary E.
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Bhagwat, Shonil A.
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Anderson, Patricia M.
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Andreev, Andrei A.
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Blaauw, Maarten
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Damblon, Freddy
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Haesaerts, Paul
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Kienast, Frank
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Kremenetski, Konstanin V.
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Krivonogov, Sergey K.
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Lozhkin, Anatoly V.
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MacDonald, Glen M.
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Novenko, Pirita Oksanen
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Sapelko, Tatiana
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Väliranta, Minna
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Vazhenina, Ludmila
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November 2009
Binney, Heather A.
6e994c91-6de7-4a8d-8f50-babf146c8691
Willis, Katherine J.
7ab089d1-4fd6-40aa-90d8-b55bf5ab0edb
Edwards, Mary E.
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Bhagwat, Shonil A.
394d7c39-9728-42f4-9bab-a1a336025860
Anderson, Patricia M.
f8889c66-d89d-4614-bf36-8259a4abb3b8
Andreev, Andrei A.
71380236-c845-4957-84c8-50532717101a
Blaauw, Maarten
42f13bb7-e011-40f3-a218-ff207204b833
Damblon, Freddy
9d3f9a65-c291-467b-9539-50adf25cdda5
Haesaerts, Paul
413e2724-2ee9-476b-b871-6330583c76b6
Kienast, Frank
5fd53907-539e-467c-9f67-4d49763cb12a
Kremenetski, Konstanin V.
d59a8e3c-7a01-4980-aff1-23f93f5a0fb1
Krivonogov, Sergey K.
c63ca5cc-60b7-4c73-ae12-809b36800ec3
Lozhkin, Anatoly V.
b65a539b-c522-42e1-8783-0443a1a0ef3f
MacDonald, Glen M.
dde0318f-886c-4c2d-99a4-d95399710ae7
Novenko, Pirita Oksanen
dc3f9293-533b-47d7-aa94-22bd5ac6adb1
Sapelko, Tatiana
160622ce-89b6-4910-94ad-d6d445e9a983
Väliranta, Minna
b1f894d6-b300-4a78-9187-621da2cd2056
Vazhenina, Ludmila
ff9b34bc-bc1b-430f-ad60-892cd7d9c061
Binney, Heather A., Willis, Katherine J., Edwards, Mary E., Bhagwat, Shonil A., Anderson, Patricia M., Andreev, Andrei A., Blaauw, Maarten, Damblon, Freddy, Haesaerts, Paul, Kienast, Frank, Kremenetski, Konstanin V., Krivonogov, Sergey K., Lozhkin, Anatoly V., MacDonald, Glen M., Novenko, Pirita Oksanen, Sapelko, Tatiana, Väliranta, Minna and Vazhenina, Ludmila
(2009)
The distribution of late-Quaternary woody taxa in northern Eurasia: evidence from a new macrofossil database.
Quaternary Science Reviews, 28 (23-24), .
(doi:10.1016/j.quascirev.2009.04.016).
Abstract
We present a database of late-Quaternary plant macrofossil records for northern Eurasia (from 23° to 180°E and 46° to 76°N) comprising 281 localities, over 2300 samples and over 13,000 individual records. Samples are individually radiocarbon dated or are assigned ages via age models fitted to sequences of calibrated radiocarbon dates within a section. Tree species characteristic of modern northern forests (e.g. Picea, Larix, tree-Betula) are recorded at least intermittently from prior to the last glacial maximum (LGM), through the LGM and Lateglacial, to the Holocene, and some records locate trees close to the limits of the Scandinavian ice sheet, supporting the hypothesis that some taxa persisted in northern refugia during the last glacial cycle. Northern trees show differing spatio-temporal patterns across Siberia: deciduous trees were widespread in the Lateglacial, with individuals occurring across much of their contemporary ranges, while evergreen conifers expanded northwards to their range limits in the Holocene.
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Published date: November 2009
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Local EPrints ID: 151395
URI: http://eprints.soton.ac.uk/id/eprint/151395
ISSN: 0277-3791
PURE UUID: e23b2703-7550-4389-bb6a-d9eb4830cf32
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Date deposited: 10 May 2010 15:55
Last modified: 14 Mar 2024 02:47
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Contributors
Author:
Heather A. Binney
Author:
Katherine J. Willis
Author:
Shonil A. Bhagwat
Author:
Patricia M. Anderson
Author:
Andrei A. Andreev
Author:
Maarten Blaauw
Author:
Freddy Damblon
Author:
Paul Haesaerts
Author:
Frank Kienast
Author:
Konstanin V. Kremenetski
Author:
Sergey K. Krivonogov
Author:
Anatoly V. Lozhkin
Author:
Glen M. MacDonald
Author:
Pirita Oksanen Novenko
Author:
Tatiana Sapelko
Author:
Minna Väliranta
Author:
Ludmila Vazhenina
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