摘要
Due to different photosynthetic process,there is obvious difference in δ 13 C values between C 3 plants and C 4 plants.It is a useful method to trace with stable carbon isotopes in soil organic matter when studying turning ecosystems,where C 3 plants (or C 4 plants)are planted instead of C 4 plants (or C 3 plants).This paper intends to review and synthesize the recent advances in the research of this subject.
Due to different photosynthetic process,there is obvious difference in δ 13 C values between C 3 plants and C 4 plants.It is a useful method to trace with stable carbon isotopes in soil organic matter when studying turning ecosystems,where C 3 plants (or C 4 plants)are planted instead of C 4 plants (or C 3 plants).This paper intends to review and synthesize the recent advances in the research of this subject.
出处
《生态学杂志》
CAS
CSCD
北大核心
2002年第2期58-60,70,共4页
Chinese Journal of Ecology
基金
国家自然科学基金 ( 4 98330 0 2和 49772 175 )
中国科学院知识创新工程项目 (KZCX2 -10 5 )
环境地球化学国家重点实验室创新领域项目联合资助
