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Marine Ecology Progress Series

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MEPS 329:23-42 (2007)  -  doi:10.3354/meps329023

Temporal and spatial variability of photosynthetic parameters and community respiration in Long Island Sound

Nicole L. Goebel1,2,*, James N. Kremer1

1Department of Marine Sciences, University of Connecticut at Avery Point, Groton, Connecticut 06340, USA
2Present address: Ocean Sciences Department, University of California, Santa Cruz, California 95062, USA

ABSTRACT: Photosynthetic parameters and community respiration were measured throughout 3 seasons at 8 stations in central and western Long Island Sound during 2002 and 2003. Light-dark bottle oxygen change was measured in a photosynthesis–irradiance (P–I) series for water from the mixed layer, and respiration was measured for surface, pycnocline, and near bottom water. PI curves were fitted numerically to calculate biomass-specific rates of maximum photosynthesis at light saturation (PBm), photosynthetic efficiency at low irradiance (αB) and plankton community respiration (Rc). The temporal and spatial variability of these fitted parameters, the derived parameter Ik, and the concentration of phytoplankton pigments were described in relation to each other and to environmental factors. Concentrations of chlorophyll (chl) and phaeopigments (phaeo), and Rc reached maxima in summer and significantly decreased seaward along the length of the Sound. Photosynthetic parameters also reached maxima in summer, however there was no significant spatial variability. In surface waters, the average (±SD) of PBm (1.3 ± 0.4 mmol O2 [mg chl]–1 h–1) demonstrated the lowest variability, compared to chl (6.9 ± 4.9 mg m–3), phaeo (3.5 ± 2.5 mg m–3), αB (10.9 ± 5.4 µmol O2 [mg chl]–1 h–1 [µE m–2 s–1]–1), Ik (132.6 ± 71.9 µE m–2 s–1), and Rc (1.4 ± 0.9 mmol O2 m–3 h–1). Chl and PBm both varied with total daily insolation and with average irradiance of the photic zone, while PBm was also correlated with temperature. Although PBm and chl increased during summer, their peaks did not occur simultaneously. Temporal trends in αB were less clear-cut than for PBm and chl, but αB was correlated with light properties of the water column. Plankton community respiration was high in surface waters and decreased with depth. Based on the relationship between Rc and chl, algal-related rates of respiration (Ra) were estimated at ~50% of total plankton community respiration. Our results do not support the common method of estimating algal respiration based on PBm.

KEY WORDS: Productivity · Primary production · Respiration · Oxygen · Chlorophyll · Phytoplankton community · Long Island Sound

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