Siddall, Mark (2005). Paleoclimate: The riddle of the sediments. Nature, 437(7055), pp. 39-41. Nature Publishing Group 10.1038/437039a
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The ratio of oxygen isotopes contained in the signal in deep-sea sediments can tell us a great deal about past ice-volume variations. The challenge is to disentangle the different contributions to the signal.
Item Type: |
Journal Article (Further Contribution) |
|---|---|
Division/Institute: |
08 Faculty of Science > Physics Institute > Climate and Environmental Physics |
UniBE Contributor: |
Siddall, Mark |
Subjects: |
500 Science > 530 Physics |
ISSN: |
0028-0836 |
Publisher: |
Nature Publishing Group |
Language: |
English |
Submitter: |
BORIS Import 2 |
Date Deposited: |
17 Aug 2021 09:45 |
Last Modified: |
05 Dec 2022 15:52 |
Publisher DOI: |
10.1038/437039a |
BORIS DOI: |
10.48350/158218 |
URI: |
https://boris.unibe.ch/id/eprint/158218 |
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