Oxygen isotopes and sea level
From the time that detailed oxygen isotope records derived from foraminifera living in the constant-temperature environment of the abyssal ocean became available, there has been a discrepancy between the ice volume record that these records imply, and that derived from the altitude of dated coral te...
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| Veröffentlicht in: | Nature (London) 1986-11, Vol.324 (6093), p.137-140 |
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| container_title | Nature (London) |
| container_volume | 324 |
| creator | Chappell, J. Shackleton, N. J. |
| description | From the time that detailed oxygen isotope records derived from foraminifera living in the constant-temperature environment of the abyssal ocean became available, there has been a discrepancy between the ice volume record that these records imply, and that derived from the altitude of dated coral terraces around the world. Here, we re-examine the data and conclude that the temperature of the abyssal ocean has been an actively varying component of the climate system. |
| doi_str_mv | 10.1038/324137a0 |
| format | Article |
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| fulltext | fulltext |
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| ispartof | Nature (London), 1986-11, Vol.324 (6093), p.137-140 |
| issn | 0028-0836 1476-4687 |
| language | eng |
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| source | Nature; Springer Nature - Complete Springer Journals |
| subjects | Earth sciences Earth, ocean, space Exact sciences and technology Humanities and Social Sciences Isotope geochemistry Isotope geochemistry. Geochronology letter Marine Marine geology multidisciplinary Science Science (multidisciplinary) |
| title | Oxygen isotopes and sea level |
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