Open AccessIncorporation of plant residue–derived carbon into the microeukaryotic community in a rice field soil revealed by DNA stable‐isotope probing
Author(s) -
Murase Jun,
Shibata Manami,
Lee Chol Gyu,
Watanabe Takeshi,
Asakawa Susumu,
Kimura Makoto
Publication year - 2012
Publication title -
fems microbiology ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.377
H-Index - 155
eISSN - 1574-6941
pISSN - 0168-6496
DOI - 10.1111/j.1574-6941.2011.01224.x
Subject(s) - stable isotope probing , biology , botany , soil carbon , soil organic matter , ascomycota , organic matter , fungus , fusarium , soil water , bacteria , ecology , microorganism , biochemistry , genetics , gene
The microbial decomposition of plant residue is a central part of the carbon cycle in soil ecosystems. Here, we explored the microeukaryotic community responsible for the uptake of plant residue carbon in a rice field soil through DNA ‐based stable‐isotope probing ( SIP ) using dried rice callus labelled with 13 C as a model substrate. Molecular fingerprinting with PCR ‐ DGGE showed that the total eukaryotic community in soil under drained (upland) conditions distinctly changed within 3 days after the callus was applied and stable thereafter. The predominant group of eukaryotes that incorporated callus carbon were fungi affiliated with the M ucoromycotina ( M ortierella ), A scomycota ( G alactomyces , E leutherascus , G ibberella and F usarium ) and Z oopagomycotina ( S yncephalis ). ‘ F ungus‐like’ protists such as P ythium (stramenopiles) and P olymyxa ( C ercozoa ) were also involved in carbon flow from the callus. Some of these fungi and ‘fungus‐like’ protists took up soil organic matter with time, which suggested a priming effect of the callus on the eukaryotic community. Our results demonstrated the usefulness of SIP not only to trace the carbon flow from fresh organic matter but also to study the effect of fresh organic matter on the utilization of soil organic matter by the microbial community.