4.6 Article

Within-day and seasonal patterns of microphytobenthos biomass determined by co-measurement of sediment and water column chlorophylls in the intertidal mudflat of Nanaura, Saga, Ariake Sea, Japan

Journal

ESTUARINE COASTAL AND SHELF SCIENCE
Volume 72, Issue 1-2, Pages 42-52

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ecss.2006.10.005

Keywords

microphytobenthos biomass; chlorophyll; tidal flat; Ariake Sea

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The microphytobenthos biomass was examined at a fixed site on the Nanaura mudflat, Ariake Sea over 9 months at intervals of 2-3 weeks. During the course of 16 surveys, samples were collected in daytime at intervals of < 1 h for measurement of chlorophylls (Chl a and pheopigments) in sediment (during exposure; n = 98) and water column (during ebb, n = 86; flood, it = 95). We found a clear temporal pattern in within-day sediment Chl a indicating net increase of microphytobenthos biomass in surface sediment during a single-daytime exposure. The significant biomass increase was clearly observed during the winter period, but weakened during the rest of the periods. Pheopigments in sediment showed much greater within-day variation compared to corresponding Chl a, with relatively great fluctuation from summer to early fall. However, during fall-winter periods, the sediment pheopigments showed within-day variation, similar to corresponding Chl a, indicating a biomass-dependent degradation approaching winter season. Overall, winter peak of Chl a (176 mg m(-2)) and summer peak of pheopigments (596 mg m(-2)) in sediment were characteristic in the Nanaura mudflat, Ariake Sea. In general, seasonal patterns for water column chlorophylls were similar to those for sediment chlorophylls, with winter peak of Chl a (174 mu g L-1) and summer maximum of pheopigments (206 mu g L-1), respectively. Typically, monthly mean water Chl a (during flood) was significantly correlated with monthly mean sediment Chl a (during exposure), indicating an entrainment of sediment Chl a to the water column during flood by tidal resuspension. Calculations indicated that ca. 66% of Chl a in the water column could be benthic-derived from the surface sediment, on average (n = 181), supporting a significant contribution of microphytobenthos biomass and production in intertidal mudflat ecosystem. (c) 2006 Elsevier Ltd. All rights reserved.

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