Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean

被引:919
|
作者
Falkowski, PG
机构
[1] Oceanogr. and Atmosph. Sci. Division, Brookhaven National Laboratory, Upton
关键词
D O I
10.1038/387272a0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Over geological time, photosynthetic carbon fixation in the oceans has exceeded respiratory oxidation of organic carbon. The imbalance between the two processes has resulted in the simultaneous accumulation of oxygen in, and drawdown of carbon dioxide from, the Earth's atmosphere, and the burial of organic carbon in marine sediments(1-3). It is generally assumed that these processes are limited by the availability of phosphorus(4,5), which is supplied by continental weathering and fluvial discharge(5-7). Over the past two million years,decreases in atmospheric carbon dioxide concentrations during glacial periods correlate with increases in the export of organic carbon from surface waters to the marine sediments(8-11), but variations in phosphorus fluxes appear to have been too small to account for these changes(12,13). Consequently, it has been assumed that total oceanic primary productivity remained relatively constant during glacial-to-interglacial transitions, although the fraction of this productivity exported to the sediments somehow increased during glacial periods(12,14). Here I present an analysis of the evolution of biogeochemical cycles which suggests that fixed nitrogen, not phosphorus, limits primary productivity on geological timescales. Small variations in the ratio of nitrogen fixation to denitrification can significantly change atmospheric carbon dioxide concentrations on glacial-to-interglacial timescales. The ratio of these two processes appears to be determined by the oxidation state of the ocean and the supply of trace elements, especially iron.
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页码:272 / 275
页数:4
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