Robotic observations of high wintertime carbon export in California coastal waters
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 CO<sub>2</sub>; exported org...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2016-05-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/13/3109/2016/bg-13-3109-2016.pdf |
| _version_ | 1811241917371908096 |
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| author | J. K. B. Bishop M. B. Fong T. J. Wood |
| author_facet | J. K. B. Bishop M. B. Fong T. J. Wood |
| author_sort | J. K. B. Bishop |
| collection | DOAJ |
| description | 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 CO<sub>2</sub>; 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<sup>−2</sup> d<sup>−1</sup>) 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<sup>−2</sup> d<sup>−1</sup>, 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. |
| first_indexed | 2024-04-12T13:44:10Z |
| format | Article |
| id | doaj.art-c4441141553149c39b17fadddc922549 |
| institution | Directory Open Access Journal |
| issn | 1726-4170 1726-4189 |
| language | English |
| last_indexed | 2024-04-12T13:44:10Z |
| publishDate | 2016-05-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Biogeosciences |
| spelling | doaj.art-c4441141553149c39b17fadddc9225492022-12-22T03:30:45ZengCopernicus PublicationsBiogeosciences1726-41701726-41892016-05-0113103109312910.5194/bg-13-3109-2016Robotic observations of high wintertime carbon export in California coastal watersJ. K. B. Bishop0M. B. Fong1T. J. Wood2Department of Earth and Planetary Science, UC Berkeley, Berkeley, CA 94720, USADepartment of Chemistry, Scripps Institution of Oceanography, La Jolla, CA 92093, USAEarth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USABiologically 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 CO<sub>2</sub>; 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<sup>−2</sup> d<sup>−1</sup>) 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<sup>−2</sup> d<sup>−1</sup>, 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.http://www.biogeosciences.net/13/3109/2016/bg-13-3109-2016.pdf |
| spellingShingle | J. K. B. Bishop M. B. Fong T. J. Wood Robotic observations of high wintertime carbon export in California coastal waters Biogeosciences |
| title | Robotic observations of high wintertime carbon export in California coastal waters |
| title_full | Robotic observations of high wintertime carbon export in California coastal waters |
| title_fullStr | Robotic observations of high wintertime carbon export in California coastal waters |
| title_full_unstemmed | Robotic observations of high wintertime carbon export in California coastal waters |
| title_short | Robotic observations of high wintertime carbon export in California coastal waters |
| title_sort | robotic observations of high wintertime carbon export in california coastal waters |
| url | http://www.biogeosciences.net/13/3109/2016/bg-13-3109-2016.pdf |
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