1999
DOI: 10.1016/s0065-2504(08)60194-4
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Ecology of Estuarine Macrobenthos

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Cited by 351 publications
(270 citation statements)
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References 139 publications
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“…The highest abundance and biomass of macrozoobenthos was observed in zone I, which was attributed to the highest trophic level and food availability. The food quantity and availability might be the limiting factors for benthic abundance and biomass in lacustrine benthic systems (Herman et al 1999;Sousa et al 2006;Zbikowski & Kobak 2007). As a consequence of abundant submerged macrophytes and the lowest trophic level, macrozoobenthos in zone II were characterized by diverse species richness and lower abundance.…”
Section: Discussionmentioning
confidence: 99%
“…The highest abundance and biomass of macrozoobenthos was observed in zone I, which was attributed to the highest trophic level and food availability. The food quantity and availability might be the limiting factors for benthic abundance and biomass in lacustrine benthic systems (Herman et al 1999;Sousa et al 2006;Zbikowski & Kobak 2007). As a consequence of abundant submerged macrophytes and the lowest trophic level, macrozoobenthos in zone II were characterized by diverse species richness and lower abundance.…”
Section: Discussionmentioning
confidence: 99%
“…These benthic algae are consequently an important carbon source for benthic heterotrophs (e.g. Admiraal et al, 1983;Herman et al, 1999;Hagerthey et al, 2002) and can significantly affect the exchange of oxygen and nutrients across the sediment-water interface (Risgaard-Petersen et al, 1994). The MPB, particularly diatoms and cyanophytes, has been reported to stabilize the sediment surface against re-suspension by the extrusion of extracellular polymeric substances (Holland et al, 1974;Paterson & Black, 1999;Staats et al, 2000).…”
Section: Introductionmentioning
confidence: 99%
“…An indicator of OM sources and the quality (degradation state) of the bulk OM pool: planktonic OM typically has C : N ratios of 5-10 (5-7 in fresh planktonic OM; Emery and Uchupy 1984) and fresh terrestrial OM usually has C : N ratios .20 (Burdige 2006). There is an assumption that increasing N (and decreasing C : N ratios) equates to higher nutritional value and preferential mineralisation, although N may become incorporated in recalcitrant compounds (for a review, see Herman et al 1999 (Glud 2008). Shown to correlate with the rate of OM input to the seabed (Henrichs 1992).…”
Section: Introductionmentioning
confidence: 99%