Wintertime phytoplankton bloom in the Subarctic Pacific supported by continental margin iron.

Lam, P. J., J. K. B. Bishop, C. C. Henning, M. A. Marcus, G. A. Waychunas, I. Y. Fung

Global Biogeochemical Cycles
20, GB1006, doi:10.1029/2005GB002557.

Abstract. Heightened biological activity was observed in February 1996 in the high-nutrient low-chlorophyll (HNLC) subarctic North Pacific Ocean, a region that is thought to be iron-limited. Here we provide evidence supporting the hypothesis that Ocean Station Papa (OSP) in the subarctic Pacific received a lateral supply of particulate iron from the continental margin off the Aleutian Islands in the winter, coincident with the observed biological bloom. Synchrotron X-ray analysis was used to describe the physical form, chemistry, and depth distributions of iron in size fractionated particulate matter samples. The analysis reveals that discrete micron-sized iron-rich hot spots are ubiquitous in the upper 200 m at OSP, more than 900 km from the closest coast. The specifics of the chemistry and depth profiles of the Fe hot spots trace them to the continental margins. We thus hypothesize that iron hot spots are a marker for the delivery of iron from the continental margin. We confirm the delivery of continental margin iron to the open ocean using an ocean general circulation model with an iron-like tracer source at the continental margin. We suggest that iron from the continental margin stimulated a wintertime phytoplankton bloom, partially relieving the HNLC condition.

Figure: Iron Sress Index from Fung et al. 2000

This iron stress calculation included iron sources from upwelling of deep sea water and dust delivery. We've shown that input of iron derived from the contiental margin can be important and sometimes stealthy. Our study site was 50N 145W.

Return to ...

Ocean Biogeochemical Processes Home Page