carbon mineralization;
fluorescence in situ hybridization;
marine sediment;
variability;
D O I:
10.1111/j.1574-6941.2003.tb01093.x
中图分类号:
Q93 [微生物学];
学科分类号:
071005 ;
100705 ;
摘要:
Spatiotemporal variation and metabolic activity of the microbial community were studied in coarse-grained Middle Atlantic Bight shelf sediments in relation to pools of dissolved and particulate carbon. Algal cells were present 8-11 cm into the sediment, probably due to hydrodynamically induced pore water flushing and sediment mixing. The coarse-grained (> 70 mum) fraction of the sediment held the major share (61-98%) of benthic bacteria. Bacterial and algal cell abundances, exoenzymatic activity, and [DOC] generally showed higher values in May/July 2001 than in August/December 2000. Carbohydrates and proteins were hydrolyzed at potential rates of 1-12 nmol cm(-3) h(-1) (beta-glucosidase) and 3-70 nmol cm(-1) h(-1) (aminopeptidase), respectively. Fluorescence in situ hybridization analyses of the benthic microbes assigned 45-56% of DAPI-stained cells to Eubacteria and less than 2% to Eukarya. The prokaryotic community was dominated by planctomycetes and members of the Cytophaga/Flavobacterium cluster. Near the sediment surface, iodonitrotetrazolium violet reducing cells, that are considered actively respiring, amounted to 15-29% of total bacteria. Despite a low organic content (particulate organic carbon <0.03%) and relatively low bacterial abundances (<10(9) cm(-3)), the Middle Atlantic Bight shelf sediments showed organic matter turnover rates that are comparable to those found in organic-rich finer-grained deposits. Our findings suggest a high biocatalytic filtration activity in these coarse permeable sediments. (C) 2002 Federation of European Microbiological Societies. Published by Elsevier Science B.V. All rights reserved.