Sea level at the last glacial maximum, constrained by oxygen isotopic curves of planktonic foraminifera in the Japan Sea
Version of Record online: 11 DEC 2012
Copyright © 2012 John Wiley & Sons, Ltd.
Journal of Quaternary Science
Special Issue: WESTERN PACIFIC PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY: LAND-SEA LINKAGE AND VARIABILITY OF CENTENNIAL TO ORBITAL SCALES
Volume 27, Issue 9, pages 941–947, December 2012
How to Cite
Oba, T. and Irino, T. (2012), Sea level at the last glacial maximum, constrained by oxygen isotopic curves of planktonic foraminifera in the Japan Sea. J. Quaternary Sci., 27: 941–947. doi: 10.1002/jqs.2585
- Issue online: 11 DEC 2012
- Version of Record online: 11 DEC 2012
- Manuscript Accepted: 14 AUG 2012
- Manuscript Revised: 29 JUL 2012
- Manuscript Received: 20 AUG 2011
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