Abstract
A variety of infaunal marine polychaete and hemichordate species produce brominated secondary metabolites, particularly bromophenols, bromopyrroles, and bromobenzylalcohols. Rates of14C-4-bromophenol respiration and assimilation by sediment microflora were determined in intact cores taken from a site inhabited by the bromophenol-producing polychaete, Notomastus lobatus, and from a similar site having very low levels of bromophenols. Rates were similar at both locations, ranging from 6 to 87 pmole ml−1 h−1 for respiration, and from 13 to 35 pmole ml−1 h−1 for assimilation. Respiration rates exhibited strong seasonal variation, consistent with results of temperature response experiments, while assimilation rates showed less seasonal variation. Calculated areal rates of bromophenol degradation (to a sediment depth of 6 cm) ranged from 2.0 to 7.8 μmole m−2 h−1, equivalent to 350–1,250 μg m−2 h−1, indicating an important role for sediment bacteria in turnover of these compounds. Similar rates of bromophenol degradation at bromophenol-containing and non-bromophenol-containing locations show that adaptation of sediment bacteria by prior exposure to bromophenols is not required for degradation of these compounds.
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Received: 8 December 1995; Revised: 29 July 1996
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Steward, C., Lovell, C. Respiration and Assimilation of 4-Bromophenol by Estuarine Sediment Bacteria . Microb Ecol 33 , 198 –205 (1997). https://doi.org/10.1007/s002489900022
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DOI: https://doi.org/10.1007/s002489900022