Abstract
Phosphorus is a key macronutrient being strongly enriched in the deep ocean as a result of continuous export and remineralization of biomass from primary production. We show that phosphorus incorporated within the skeletons of the cosmopolitan cold-water coral Desmophyllum dianthus is directly proportional to the ambient seawater phosphorus concentration and thus may serve as a paleo-oceanographic proxy for variations in ocean productivity as well as changes in the residence times and sources of deep-water masses. The application of this tool to fossil specimens from the Mediterranean reveals phosphorus-enriched bottom waters at the end of the Younger Dryas period.
Original language | English |
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Pages (from-to) | 1788-1791 |
Number of pages | 4 |
Journal | Science |
Volume | 312 |
Issue number | 5781 |
DOIs | |
Publication status | Published - 23 Jun 2006 |