Estimates of oceanic mesozooplankton production: a comparison using the Bermuda and Hawaii time-series data

Citation:
Roman, MR, Adolf HA, Landry MR, Madin LP, Steinberg DK, Zhang X.  2002.  Estimates of oceanic mesozooplankton production: a comparison using the Bermuda and Hawaii time-series data. Deep-Sea Research (Part II, Topical Studies in Oceanography). 49:175-192.

Keywords:

ANW, Atlantic, Bermuda, ASFA 1: Biological Sciences & Living Resources, bermuda, carbon cycle, comparative studies, Copepoda, copepods, Faecal pellets, growth rate, ISE, USA, Hawaii, K 03012:Protozoa, marine, Microbiology Abstracts C: Algology, Mycology & Protozoology, O 1070:Ecology/Community Studies, Oceanic Abstracts, oceans, particulate flux, production, Q1 01461:Plankton, Q1 01482:Ecosystems and energetics, secondary production, sedimentation, time series analysis, USA, Hawaii, zooplankton

Abstract:

Mesozooplankton growth rates were estimated for the Hawaiian (HOT) and Bermuda (BATS) ocean time-series stations using the empirical model of Hirst and Lampitt (Marine Biology 132 (1998) 247), which predicts copepod growth rate from temperature and body size. Using this approach we derived seasonal and annual estimates of mesozooplankton production as well as rates of mesozooplankton ingestion and egestion using assumed growth and assimilation efficiencies for the period 1994-1997. Annual mesozooplankton production estimates at HOT (average 0.79 mol C m super(-2) yr super(-1)) were higher than production estimates at BATS (average 0.33 mol C m super(-2) yr super(-1)) due to both higher mesozooplankton biomass and higher estimated mesozooplankton individual growth rates. Annual primary production at the two sites was similar (average 14.92 mol C m super(-2) yr super(-1) at HOT and 13.43 mol C m super(-2) yr super(-1) at BATS). Thus, mesozooplankton production was a greater fraction of primary production at HOT (0.05) as compared to BATS (0.02). Mesozooplankton potentially contributed more to the gravitational flux of carbon at HOT, where the ratio of the average annual estimate of mesozooplankton fecal pellet carbon production/annual estimate of carbon flux at the base of the euphotic zone was 1.03 compared to the same ratio of 0.39 at BATS. Mortality estimates were similar to estimates of mesozooplankton production when compared over the entire study period. The higher mesozooplankton biomass and derived rate parameters at HOT compared to BATS may be due to the more episodic nature of nutrient inputs at BATS, which could result in mismatches between increases in phytoplankton production and the grazing/production response by mesozooplankton. In addition, there is evidence to suggest that there are periodic blooms of gelatinous macrozooplankton (salps) at BATS that may not be captured sufficiently by the monthly sampling program. Thus the gelatinous zooplankton would add to the overall grazing impact on the phytoplankton at BATS as well as the contribution of zooplankton to the gravitational flux of biogenic material via fecal pellet production.

Notes:

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DOI:

10.1016/S0967-0645(01)00099-6