Pelagic community responses to a deep-water front in the California Current Ecosystem: overview of the A-Front Study

• Published in: Journal of Plankton Research
• Main Authors: Landry, Michael R., Ohman, Mark D., Goericke, Ralf, Stukel, Michael R., Barbeau, Katherine A., Bundy, Randelle, Kahru, Mati
• Format: Text
• Language: English
• Published: Oxford University Press 2012
• Subjects: ORIGINAL ARTICLES; Subarctic
• Online Access: http://plankt.oxfordjournals.org/cgi/content/short/34/9/739; https://doi.org/10.1093/plankt/fbs025

In October 2008, we investigated pelagic community composition and biomass, from bacteria to fish, across a sharp frontal gradient overlying deep waters south of Point Conception, California. This north–south gradient, which we called A-Front, was formed by the eastward flow of the California Current and separated cooler mesotrophic waters of coastal upwelling origin to the north, from warm oligotrophic waters of likely mixed subarctic–subtropical origin to the south. Plankton biomass and phytoplankton growth rates were two to three times greater on the northern side, and primary production rates were elevated 5-fold to the north. Compared with either of the adjacent waters, the frontal interface was strongly enriched and uniquely defined by a subsurface bloom of large diatoms, elevated concentrations of suspension-feeding zooplankton, high bioacoustical estimates of pelagic fish and enhanced bacterial production and phytoplankton biomass and photosynthetic potential. Such habitats, though small in areal extent, may contribute disproportionately and importantly to regional productivity, nutrient cycling, carbon fluxes and trophic ecology. As a general introduction to the A-Front study, we provide an overview of its design and implementation, a brief summary of major findings and a discussion of potential mechanisms of plankton enrichment at the front.