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Understanding the ecology of the abyssal sediment community and constituent metazoan macrofauna is important because they influence carbon and nutrient cycle processes at the seafloor through remineralization, bioturbation, and burial of the sunken material.

Results from a 10-year study in the abyssal NE Pacific found that climate-driven variations in food availability were linked to total metazoan macrofauna abundance, phyla composition, rank-abundance distributions, and remineralization over seasonal and interannual scales.

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Appreciating how climate can influence deep-sea communities and biogeochemical cycles is essential in evaluating how they may vary in the future.

Current evidence suggests that climate change is resulting in significant alterations of oceanographic conditions worldwide including increased sea-surface temperatures, stronger stratification, and increased acidity (1, 2).Most spatial studies have effectively compared sediment fauna abundance across a gradient of spatial variation in surface production (10–16).For example, a metaanalysis of samples collected from 1961 to 1985 in the western North Atlantic found that the principal pattern of macrofauna abundance was related to depth-corrected POC flux as determined from the more modern sea-viewing wide field-of-view sensor (Sea Wi FS) ocean color data (13).Diverse faunal groups inhabit deep-sea sediments over much of Earth's surface, but our understanding of how interannual-scale climate variation alters sediment community components and biogeochemical processes remains limited.The vast majority of deep-sea communities depend on a particulate organic carbon food supply that sinks from photosynthetically active surface waters. Yuji Sugihara, Hiromichi Tsumori, Hiroshi Yoshioka, Shigeatsu Serizawa, Imaging measurement of whitecaps at sea observation tower, Coastal Engineering 2004, Vol.1, R. Murillo (ed.), Taylor & Francis, London, pp.263-270, 2005.04.

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