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Identification of the Changbaishan ‘Millennium’ (B-Tm) eruption deposit in the Lake Suigetsu (SG06) sedimentary archive, Japan: Synchronisation of hemispheric-wide palaeoclimate archives

Abstract:

The B-Tm tephra, dispersed during the highly explosive Changbaishan ‘Millennium’ eruption (ca. 940–950 CE) and a key marker layer within the Greenland ice cores, has now been identified in the Lake Suigetsu (SG06) sedimentary sequence, central Japan. The major element geochemistry of the volcanic glasses within this tephra layer are compared to a new glass dataset from the distal type-locality (Tomakomai Port, Hokkaido) and other published ‘Millennium’ eruption/B-Tm deposits, to verify this c...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher's version

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Publisher copy:
10.1016/j.quascirev.2016.08.022

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Department:
Oxford, SSD, School of Archaeology, Archaeology Research Lab
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Author
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Department:
Oxford, SSD, School of Archaeology, Archaeology Research Lab
Role:
Author
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Department:
Oxford, SSD, School of Archaeology, Archaeology Research Lab
Role:
Author
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Grant:
NE/D00289/1; NE/F003048/1; NE/L002612/1
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Grant:
ECF-2014-438; ECF-2015-396
Publisher:
Elsevier Publisher's website
Journal:
Quaternary Science Reviews Journal website
Volume:
150
Pages:
301-307
Publication date:
2016-08-25
Acceptance date:
2016-08-16
DOI:
ISSN:
0277-3791 and 1873-457X
Pubs id:
pubs:652834
URN:
uri:c33dcf4c-064b-4495-8a0f-7a57557dfe73
UUID:
uuid:c33dcf4c-064b-4495-8a0f-7a57557dfe73
Local pid:
pubs:652834

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