Water column dissolution of aragonite in the Pacific Ocean
Pelagic pteropods are an important component of the oceanic CO 2 system. Their shells appear to be a principal source of excess alkalinity in the upper water column of the North Pacific Ocean. Dissolution of aragonite must therefore be taken account of in generating models of the oceanic CO 2 system...
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| Veröffentlicht in: | Nature (London) 1984-01, Vol.312 (5992), p.321-326 |
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| container_end_page | 326 |
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| container_issue | 5992 |
| container_start_page | 321 |
| container_title | Nature (London) |
| container_volume | 312 |
| creator | Byrne, Robert H. Acker, James G. Betzer, Peter R. Feely, Richard A. Cates, Marion H. |
| description | Pelagic pteropods are an important component of the oceanic CO
2
system. Their shells appear to be a principal source of excess alkalinity in the upper water column of the North Pacific Ocean. Dissolution of aragonite must therefore be taken account of in generating models of the oceanic CO
2
system and is also an important cause of sample loss from long-term sediment traps deployed in undersaturated seawater. |
| doi_str_mv | 10.1038/312321a0 |
| format | Article |
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| fulltext | fulltext |
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| ispartof | Nature (London), 1984-01, Vol.312 (5992), p.321-326 |
| issn | 0028-0836 1476-4687 |
| language | eng |
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| source | SpringerLink Journals; Nature Journals Online |
| subjects | Earth sciences Earth, ocean, space Exact sciences and technology Geochemistry Humanities and Social Sciences Marine Mineralogy multidisciplinary Pteropoda Science Science (multidisciplinary) Silicates Water geochemistry |
| title | Water column dissolution of aragonite in the Pacific Ocean |
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