Changing Concentrations of CO, CH4, C5H8, CH3Br, CH3I, and Dimethyl Sulfide during the Southern Ocean Iron Enrichment Experiments
Oceanic iron (Fe) fertilization experiments have advanced the understanding of how Fe regulates biological productivity and air-sea carbon dioxide ( CO2) exchange. However, little is known about the production and consumption of halocarbons and other gases as a result of Fe addition. Besides metabol...
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Veröffentlicht in: | Proceedings of the National Academy of Sciences - PNAS 2004-06, Vol.101 (23), p.8537-8541 |
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