Stream food web fueled by methane-derived carbon

被引:58
|
作者
Kohzu, A
Kato, C
Iwata, T
Kishi, D
Murakami, M
Nakano, S
Wada, E
机构
[1] Kyoto Univ, Ctr Ecol Res, Otsu, Shiga 5202113, Japan
[2] Hokkaido Univ, Tomakomai Res Stn, Tomakomai, Hokkaido 0530035, Japan
[3] Yamanashi Univ, Dept Ecosocial Syst Engn, Kofu, Yamanashi 4008511, Japan
[4] RIHN, Kyoto 6020878, Japan
关键词
backwater pool; carbon isotope ratio; hyporheic zone; macroinvertebrates; methane gas; methanotrophic bacteria; nitrogen isotope ratio; stream food web;
D O I
10.3354/ame036189
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Food webs driven by energy from the oxidation of methane are now recognized to be omnipresent in terrestrial and freshwater ecosystems (e.g. lakes, soils and peat bogs), as well as in deep-sea hydrothermal vents and cold seeps. However, the incorporation of methane-derived carbon into stream food webs has never been reported. Here we present the first circumstantial evidence from stable carbon and nitrogen isotope ratios that a stream food web composed of aquatic macro-invertebrates is partly sustained by methanotrophs or chemoautotrophs that gain carbon respired by methane-oxidizing bacteria. Methane-derived carbon seems to enter stream communities around anoxic habitats such as backwater pools and hyporheic zones. Because these reductive habitats exist in many streams, food webs partly sustained by methane-derived carbon are likely to be ubiquitous in lotic ecosystems.
引用
收藏
页码:189 / 194
页数:6
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