Journal article
The potential of sedimentary foraminiferal rare earth element patterns to trace water masses in the past
- Abstract:
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Dissolved rare earth element (REE) concentration data from intermediate and deep seawater form an array characterized by higher middle-REE enrichments (MREE/MREE*) in the North Atlantic and a progressive increase in heavy-to-light REE ratios (HREE/LREE) as water masses age. The REEs in foraminifera are fractionated toward higher MREE/MREE* and lower HREE/LREE relative to seawater. Calculations based on a scavenging model show that the REE patterns in uncleaned core-top foraminifera resemble t...
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- Publication status:
- Published
- Peer review status:
- Peer reviewed
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- Files:
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(Accepted manuscript, pdf, 1.9MB)
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- Publisher copy:
- 10.1002/2016GC006782
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Authors
Funding
Bibliographic Details
- Publisher:
- Wiley Publisher's website
- Journal:
- Geochemistry, Geophysics, Geosystems Journal website
- Volume:
- 18
- Issue:
- 4
- Pages:
- 1550–1568
- Publication date:
- 2017-03-17
- Acceptance date:
- 2017-03-14
- DOI:
- EISSN:
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1525-2027
- Source identifiers:
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691387
Item Description
- Pubs id:
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pubs:691387
- UUID:
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uuid:3993d566-dc38-45dc-8f5c-530485fb3a52
- Local pid:
- pubs:691387
- Deposit date:
- 2017-04-27
Terms of use
- Copyright holder:
- American Geophysical Union
- Copyright date:
- 2017
- Notes:
- © 2017. American Geophysical Union. All Rights Reserved. This is the accepted manuscript version of the article. The final version is available online from Wiley at: [10.1002/2016GC006782]
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