Poster's note : relevant to OIF http://m.pnas.org/content/early/2016/05/11/1600616113.abstract
Ocean dynamics, not dust, have controlled equatorial Pacific productivity over the past 500,000 years Gisela Winckler Robert F. Anderson Samuel L. Jaccard Franco Marcantonioea April 8, 2016 Significance The equatorial Pacific is a key oceanographic region in Earth’s climate system. Biological production in this region is limited, in part, by the lack of the micronutrient iron. Atmospheric dust is a source of iron, as is upwelling of ocean waters from below. A longstanding question has been whether biological productivity has responded to variable dust supply over ice age cycles. We use geochemical proxies in three sediment cores spanning the breadth of the equatorial Pacific to show that biological productivity did not respond to dustier ice age conditions. Rather than atmospheric iron supply, we infer that ocean dynamics, linking the equatorial Pacific to nutrient supply from the Southern Ocean, played a crucial role in regulating equatorial Pacific productivity. Abstract Biological productivity in the equatorial Pacific is relatively high compared with other low-latitude regimes, especially east of the dateline, where divergence driven by the trade winds brings nutrient-rich waters of the Equatorial Undercurrent to the surface. The equatorial Pacific is one of the three principal high-nutrient low-chlorophyll ocean regimes where biological utilization of nitrate and phosphate is limited, in part, by the availability of iron. Throughout most of the equatorial Pacific, upwelling of water from the Equatorial Undercurrent supplies far more dissolved iron than is delivered by dust, by as much as two orders of magnitude. Nevertheless, recent studies have inferred that the greater supply of dust during ice ages stimulated greater utilization of nutrients within the region of upwelling on the equator, thereby contributing to the sequestration of carbon in the ocean interior. Here we present proxy records for dust and for biological productivity over the past 500 ky at three sites spanning the breadth of the equatorial Pacific Ocean to test the dust fertilization hypothesis. Dust supply peaked under glacial conditions, consistent with previous studies, whereas proxies of export production exhibit maxima during ice age terminations. Temporal decoupling between dust supply and biological productivity indicates that other factors, likely involving ocean dynamics, played a greater role than dust in regulating equatorial Pacific productivity. climate change export production iron fertilization carbon eolian dust -- You received this message because you are subscribed to the Google Groups "geoengineering" group. To unsubscribe from this group and stop receiving emails from it, send an email to [email protected]. To post to this group, send email to [email protected]. Visit this group at https://groups.google.com/group/geoengineering. For more options, visit https://groups.google.com/d/optout.
