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Testing models of past ocean chemistry using foraminifera 15 N/ 14 N
Author(s) -
Altabet Mark A.,
Curry William B.
Publication year - 1989
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/gb003i002p00107
Subject(s) - foraminifera , interglacial , glacial period , oceanography , deep sea , deglaciation , ocean current , geology , environmental science , holocene , benthic zone , paleontology
Previous models have attempted to explain glacial to interglacial changes in atmospheric pCO 2 by invoking changes in the ocean's nutrient concentration or regional changes in nutrient utilization. Nitrogen is limiting to primary production and has a residence time in the ocean compatible with glacial to interglacial variations. But up to now, there has been no geological indicator for glacial to interglacial changes in the ocean's nitrogen cycle. We propose that 15 N/ 14 N ratios for the organic matrix of preserved foraminifera yield an interpretable δ 15 N record. We have developed models to study the relationship between plausible changes in the ocean's nitrogen cycle and resulting changes in the 15 N/ 14 N ratio of dissolved NO 3 − . Our model results demonstrate that 15 N/ 14 N ratios exhibit excursions during periods in which the oceans are accumulating or losing nitrogen regardless of the means by which these changes occur. Foraminifera 15 N/ 14 N results for a Pacific and an Atlantic core provide evidence against wide spread glacial anoxia, a consequence of many models of ocean chemistry. We suggest that increasing shelf‐sediment denitrification upon deglaciation reduced nitrogen concentrations in the modern ocean. Ambiguities between the two foraminifera 15 N/ 14 N records indicate that local effects associated with changes in hydrography or ecology need to be studied further.