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Nitrogen fixation in the Gulf of California and the Eastern Tropical North Pacific

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Title Nitrogen fixation in the Gulf of California and the Eastern Tropical North Pacific
Names White, Angelicque E. (creator)
Foster, Rachel A. (creator)
Benitez-Nelson, Claudia R. (creator)
Masque, Pere (creator)
Verdeny, Elisabet (creator)
Popp, Brian N. (creator)
Arthur, Karen E. (creator)
Prahl, Fredrick G. (creator)
Date Issued 2013-02 (iso8601)
Note This is the author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/progress-in-oceanography/.
Abstract Di-nitrogen (N₂) fixation plays a well-recognized role in the enhancement of primary production
and arguably particle export in oligotrophic regions of the subtropical and tropical oceans.
However, recent evidence suggests that N₂ fixation may also be significant in regions of the
surface ocean proximate to or overlying zones of intense subsurface denitrification. In this study,
we present results from a series of research cruises in the Gulf of California (GoCal) and
adjacent waters of the eastern tropical North Pacific (ETNP). Measurements included
microscopy, genomic analyses, incubations, stable isotopic measurements, and sediment traps
coupled with ²³⁸U:²³⁴Th disequilibria. Combined, these results suggest that N₂ fixing
microorganisms are present and active throughout the region, with larger sized Richelia and
Trichodesmium spp. recorded within the warmer waters at the entrance to and within the GoCal,
and smaller, unicellular diazotrophs observed in the cooler waters of the northern ETNP. N₂
fixation rates in the summer varied from 15-70 μmol N m⁻² d⁻¹, with episodic blooms
contributing as much as 795 μmol N m⁻² d⁻¹. While the estimated contribution of N₂ fixation to
particle export was highly variable, blooms of diatom-Richelia symbioses accounted for as much
as ~44% of the measured summer carbon flux at 100 m. Alternately, evaluation of the N isotopic
composition of sinking material and the magnitude of measured N₂ fixation rates indicate
negligible to small enhancements of new production when blooms of either colonial
Trichodesmium spp. or unicellular diazotrophs were encountered. Consistent with previous
research, we also found that while fluxes of C to sediment traps are similar in winter and summer
months, the efficiency of C export (export/surface productivity) in the GoCal region is elevated
during summer relative to the more productive diatom-dominated winter phase of the seasonal
cycle. The episodic and variable nature of N₂ fixation recorded in this region make it unlikely
that new production via diazotrophic activity is solely responsible for the observed patterns of C
transport efficiency; rather, we hypothesize that eolian inputs and/or efficient transport of
picocyanobacterial biomass via grazing or aggregation may further explain the enhanced export
efficiency observed in the GoCal summer. In sum, diazotrophy typically supports <10%, but as
much as 44% of export production. The high variability of direct measurements of N₂ fixation
implies that other mechanisms contribute to the seasonal invariance of C flux in this region. If
this region is indicative of other oxygen minima zones with active diazotrophs, our results
indicate that export-mediated feedback mechanisms between N₂ fixation and denitrification are
not as strong as previously hypothesized.
Genre Article
Topic Nitrogen fixation
Identifier White, A., Foster, R., Benitez-Nelson, C., Masque, P., Verdeny, E., Popp, B., . . . Prahl, F. (2013). Nitrogen fixation in the gulf of california and the eastern tropical north pacific. Progress in Oceanography, 109, 1-17. doi: 10.1016/j.pocean.2012.09.002

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