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Atmospheric iron supply and enhanced vertical carbon flux in the NE subarctic Pacific: Is there a connection?
Author(s) -
Boyd P. W.,
Wong C. S.,
Merrill J.,
Whitney F.,
Snow J.,
Harrison P. J.,
Gower J.
Publication year - 1998
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 - 10.1029/98gb00745
Subject(s) - oceanography , subarctic climate , biological pump , sediment trap , pelagic zone , biogenic silica , iron fertilization , phytoplankton , bloom , algal bloom , environmental science , photic zone , diatom , flux (metallurgy) , chlorophyll a , deep sea , geology , nutrient , water column , ecology , chemistry , biology , biochemistry , organic chemistry
Recent studies have confirmed the relationship between iron supply and phytoplankton growth rates in all three high‐nitrate low‐chlorophyll (HNLC) oceanic provinces. However, there is little evidence, so far, of the role of iron in altering the efficiency of the biological pump via increased downward export of particulate organic carbon (POC). The NE subarctic Pacific is unique among HNLC regions in that long time series pelagic observations and deep‐moored sediment trap records exist which may provide the best opportunity thus far to test aspects of the iron hypothesis. Episodic elevated levels of chlorophyll a (> 2.0 μg L −1 ) were observed 6 times between 1964 and 1976 at the former site of Ocean Station Papa (OSP). In addition, between 1984 and 1990 on at least three occasions, concurrent pulses of POC and biogenic silica were recorded in deep‐moored traps at OSP. Possible explanations for these events, such as lateral advection of more productive waters, iron‐mediated blooms, or grazing by salp swarms are discussed and tested using an existing downward POC flux model. Owing to the episodic nature of such events, no available data are sufficiently comprehensive to unequivocally rule out any of these explanations. Nevertheless, from the data available, the occurrence of pelagic or deep water pulses, approximately once every 3 years, are most consistent with iron‐mediated diatom blooms, and of the sinking of POC and biogenic silica (from such a bloom) to depth, respectively. A comparison of the timing of these iron‐mediated pulses with that of the transport probabilities of atmospheric dust supply from Asia and Alaska provides an opportunity to assess the likelihood of a coupling between the atmosphere and the ocean.