Published March 30, 2003
| Supplemental Material
Journal Article
Open
An alternative age model for the Paleocene-Eocene thermal maximum using extraterrestrial ^3He
- Creators
- Farley, K. A.
- Eltgroth, S. F.
Abstract
A continuous age model for the brief climate excursion at the Paleocene–Eocene boundary has been constructed by assuming a constant flux of extraterrestrial ^3He (^3He_(ET)) to the seafloor. ^3He_(ET) measurements from ODP Site 690 provide quantitative evidence for the rapid onset (
Additional Information
© 2003 Elsevier Science B.V. Received 27 September 2002; received in revised form 5 January 2003; accepted 8 January 2003. We thank Tim Bralower for guidance, encouragement and helpful comments on the manuscript, Debbie Thomas for preparation of samples from Site 690, and constructive reviews by Jim Zachos and Franco Marcantonio. This work was supported by NSF EAR-9909448 and by a Fellowship from the David and Lucille Packard Foundation to K.A.F.[BARD]Attached Files
Supplemental Material - mmc1.xls
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Additional details
- Eprint ID
- 35478
- DOI
- 10.1016/S0012-821X(03)00017-7
- Resolver ID
- CaltechAUTHORS:20121115-093445626
- EAR-9909448
- NSF
- David and Lucile Packard Foundation Fellowship
- Created
-
2012-11-15Created from EPrint's datestamp field
- Updated
-
2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences