MEPS 373:239-247 (2008)  -  doi:10.3354/meps07801

Contribution to the Theme Section ‘Effects of ocean acidification on marine ecosystems’


Ocean acidification: documenting its impact on calcifying phytoplankton at basin scales

William M. Balch1,*, Victoria J. Fabry2

1Bigelow Laboratory for Ocean Sciences, PO Box 475, W. Boothbay Harbor, Maine 04575, USA
2Department of Biological Sciences, California State University San Marcos, San Marcos, California 92096-0001, USA

ABSTRACT: In this paper, we evaluate several approaches to discern the impact of ocean acidification on calcifying plankton, over basin scales. We focus on estimates of the standing stock of particulate inorganic carbon (PIC) associated with calcifying plankton since it is thought that these organisms will be the most sensitive to ocean acidification. Chemical techniques provide the greatest accuracy and precision for measuring the concentration of PIC in seawater, but basin-scale chemical surveys are formidably expensive due to the high costs of ship time and analytical instrumentation. Optical techniques, while not yet as precise as chemical methods, provide the opportunity to rapidly sample over much greater spatial scales, with large numbers of samples contributing to each PIC determination (which reduces the SE of each mean determination). Optical measurements from autonomous platforms (buoys and gliders) will provide important depth resolution of PIC, which is otherwise not accessible to ocean color satellites. We propose a strategy for future PIC measurements that employs both optical and chemical measurements on the same water samples. This will ensure adequate knowledge of the PIC backscattering cross-section, critical for satellite PIC determinations at basin scales.

KEY WORDS: Coccolithophores · Ocean acidification · Calcium carbonate · Calcite · Coccolith · Ocean backscattering

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Cite this article as: Balch WM, Fabry VJ (2008) Ocean acidification: documenting its impact on calcifying phytoplankton at basin scales. Mar Ecol Prog Ser 373:239-247

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