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MEPS 719:41-63 (2023)  -  DOI: https://doi.org/10.3354/meps14393

Phytoplankton transport out of the euphotic zone by frontal subduction and gravitational sinking in the Santa Barbara Channel, CA, USA

Libe Washburn1,2,*, Mark A. Brzezinski1,3, Chris Gotschalk1,#, Kyle Mylonakis4, Carlos Garcia-Cervera5, Li Kui1

1Marine Science Institute, University of California, Santa Barbara, CA 93106-6150, USA
2Department of Geography, University of California, Santa Barbara, CA 93106-6150, USA
3Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA 93106-6150, USA
4Protopia AI, 600 Congress Avenue, Austin, TX 78701, USA
5Department of Mathematics, University of California, Santa Barbara, CA 93106-6150, USA
*Corresponding author:
#Retired

ABSTRACT: Production of particulate organic carbon (POC) in nutrient-rich coastal waters over continental shelves, its export to depth, and its transport to deeper ocean waters is a poorly quantified component of the global carbon cycle. A critical step in quantifying this vertical transport is identifying shelf processes that export phytoplankton out of the euphotic zone. During cruises of the Santa Barbara Coastal Long Term Ecological Research project, we discovered substantial chlorophyll a (chl a) below the euphotic zone in the Santa Barbara Channel, a part of the southern California Current System. Observations from towed, undulating vehicles revealed deep chlorophyll layers near fronts where upwelled waters from central California converged with lower-density waters from the Southern California Bight. The mean fraction ± 1 standard deviation (SD) of chlorophyll biomass below the euphotic zone spanning the entire Santa Barbara Channel was ~7 ± 9% during 13 cruises averaged across all seasons. In one spring cruise, the fraction was ~30%, and in other cruises the layers were absent. Phytoplankton export out of the euphotic zone by subduction was indicated by spatial coherence between chl a and sloping density surfaces. Vertical plumes of chl a crossing density surfaces indicated enhanced gravitational export within cyclonic eddies. Chl a in water samples below the euphotic zone, away from fronts and cyclonic flows, suggested additional phytoplankton export. Our results emphasize the importance of subduction in the export of phytoplankton and POC out of the euphotic zone in coastal upwelling systems.


KEY WORDS: Fronts · Subduction · Flux · Particulate organic carbon · Phytoplankton · Sinking particles · POC · Chlorophyll


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Cite this article as: Washburn L, Brzezinski MA, Gotschalk C, Mylonakis K, Garcia-Cervera C, Kui L (2023) Phytoplankton transport out of the euphotic zone by frontal subduction and gravitational sinking in the Santa Barbara Channel, CA, USA. Mar Ecol Prog Ser 719:41-63. https://doi.org/10.3354/meps14393

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