Robotic observations of high wintertime carbon export in California coastal waters

James K B Bishop,Michael B Fong,Todd J Wood

doi:10.5194/bg-13-3109-2016

Abstract

Abstract. Biologically mediated particulate organic and inorganic carbon (POC and PIC) export from surface waters is the principal determinant of the vertical oceanic distribution of pH and dissolved inorganic carbon and thus sets the conditions for air–sea exchange of CO2; exported organic matter also provides the energy fueling communities in the mesopelagic zone. However, observations are temporally and spatially sparse. Here we report the first hourly-resolved optically quantified POC and PIC sedimentation rate time series from an autonomous Lagrangian Carbon Flux Explorer (CFE), which monitored particle flux using an imaging optical sedimentation recorder (OSR) at depths below 140 m in the Santa Cruz Basin, CA, in May 2012, and in January and March 2013. Highest POC vertical flux ( ∼ 100–240 mmol C m−2 d−1) occurred in January, when most settling material was millimeter- to centimeter-sized aggregates but when surface biomass was low; fluxes were ∼ 18 and ∼ 6 mmol C m−2 d−1, respectively, in March and May, under high surface biomass conditions. An unexpected discovery was that January 2013 fluxes measured by CFE were 20 times higher than that measured by simultaneously deployed surface-tethered OSR; multiple lines of evidence indicate strong undersampling of aggregates larger than 1 mm in the latter case. Furthermore, the January 2013 CFE fluxes were about 10 times higher than observed during multiyear sediment trap observations in the nearby Santa Barbara and San Pedro basins. The strength of carbon export in biologically dynamic California coastal waters is likely underestimated by at least a factor of 3 and at times by a factor of 20.

Highlights

Phytoplankton account for half of global net photosynthesis (Field et al, 1998), or about 50 Pg C yr−1, yet they live for a week before being removed from the euphotic zone through grazing or abiotic aggregation processes
While most phytoplankton carbon is recycled in the surface layer, recent model- and observation-based estimates (Henson et al, 2011; Yao and Schlitzer, 2013; Siegel et al, 2014) suggest that globally 5 to 12 Pg C yr−1 is exported below the euphotic zone as sinking particulate organic and inorganic carbon (POC and PIC) in fecal pellets, amorphous large aggregates, and independently sinking carapaces and calcareous shells (e.g., Bishop et al, 1978; Alldredge and Silver, 1988; Turner, 2015)
We describe direct in situ observations of carbon export in biologically dynamic ocean waters near the California coast obtained using a fully autonomous ocean profiling Carbon Flux Explorer (CFE; Fig. 1a) that we have developed

Summary

Introduction

Phytoplankton account for half of global net photosynthesis (Field et al, 1998), or about 50 Pg C yr−1, yet they live for a week before being removed from the euphotic zone through grazing or abiotic aggregation processes. While most phytoplankton carbon is recycled in the surface layer, recent model- and observation-based estimates (Henson et al, 2011; Yao and Schlitzer, 2013; Siegel et al, 2014) suggest that globally 5 to 12 Pg C yr−1 is exported below the euphotic zone as sinking particulate organic and inorganic carbon (POC and PIC) in fecal pellets, amorphous large aggregates, and independently sinking carapaces and calcareous shells (e.g., Bishop et al, 1978; Alldredge and Silver, 1988; Turner, 2015). Together with siliceous diatom frustules and radiolarian tests, biogenic carbonates are a major factor governing the excess density, and sinking rate, of aggregate particles carrying POC downward from

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Discussion

Conclusion