Biological 12C–13C fractionation increases with increasing community-complexity in soil microcosms
Biological 12C–13C fractionation increases with increasing community-complexity in soil microcosms
复制标题
生物 12C–13C 分馏随着土壤微观世界中群落复杂性的增加而增加
DOI:
10.1016/j.soilbio.2013.10.030
复制
发表时间:
2014
影响因子:
9.7
通讯作者:
F. Ekelund
中科院分区:
文献类型:
--
作者:
Weijun Yang;J. Magid;S. Christensen;R. Rønn;P. Ambus;F. Ekelund
Isotope fractionation is a ubiquitous phenomenon in natural ecosystems. When chemical elements move through food chains, natural isotope ratios change because biological processes tend to discriminate against heavier isotopes. This effect can be used to trace flows of matter, estimate process-rates and determine the trophic level of organisms in biological systems. While it is widely accepted that 15N-accumulates in natural food-chains, it is disputed to which extent this is the case for13C. We constructed sand-microcosms inoculated with a dilution series of soil organisms and amended with glucose as the source of organic carbon. We demonstrated that the proportion of13C in respiratory CO2correlated inversely with community complexity. Our results therefore suggest that increasing community complexity, with increasing synergy, competition and predation, facilitates increasing12C–13C isotopic fractionation.