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Methane-derived carbon flows through methane-oxidizing bacteria to higher trophic levels in aquatic systems
被引:70
|作者:
Deines, Peter
Bodelier, Paul L. E.
Eller, Gundula
机构:
[1] Max Planck Inst Limnol, Dept Physiol Ecol, D-24306 Plon, Germany
[2] Netherlands Inst Ecol, NIOO, KNAW, Ctr Limnol,Dept Microbial Wetland Ecol, NL-3631 AC Nieuwersluis, Netherlands
关键词:
D O I:
10.1111/j.1462-2920.2006.01235.x
中图分类号:
Q93 [微生物学];
学科分类号:
071005 ;
100705 ;
摘要:
Recent investigations have shown that biogenic methane can be a carbon source for macro invertebrates in freshwater food webs. Stable carbon isotopic signatures, used to infer an organism's food source, indicated that methane can play a major role in the nutrition of chironomid larvae. However, the pathway of methane-derived carbon into invertebrate biomass is still not confirmed. It has been proposed that chironomid larvae ingest methane-oxidizing bacteria (MOB), but this has not been experimentally demonstrated to date. Using C-13-labelled methane we could show for the first time that chironomid larvae assimilate methane-derived carbon through MOB. Chironomid larval biomass was significantly C-13-enriched after dwelling for 10 days in lake sediment enriched with labelled methane. Moreover, phospholipid fatty acids diagnostic for MOB were detected in larval tissue and were significantly C-13-enriched, which encompasses the C-13-Uptake predicted for a methane-based nutrition. Additionally, chironomid larvae fed on sediment and water-column derived MOB biomass.
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页码:1126 / 1134
页数:9
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