Stable carbon isotope as a signal index for monitoring grassland degradation.
Sci Rep 2016;
6:31399. [PMID:
27527910 PMCID:
PMC4985657 DOI:
10.1038/srep31399]
[Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/15/2016] [Accepted: 07/19/2016] [Indexed: 11/10/2022] Open
Abstract
Grassland degradation due to overgrazing is common in many areas of the world. This study analyzed the potential of the stable carbon isotope (δ13C) value as a structural microcosmic index to monitor processes of grassland degradation. The δ13C values of plant leaves, roots and soils in non-grazed (NG) and over-grazed (OG) grassland were measured from samples collected from the seven types of grassland in China. We found that the leaf δ13C values of palatable species (δ13Cleaf) and root δ13C values (δ13Croot) in OG grasslands were reduced compared with those from NG grasslands. Furthermore, the δ13Cleaf and δ13Csoil were positive correlation with elevation and latitude, δ13Croot was negative correlation with them at high altitude (3000~5000m), and δ13Croot and δ13Csoil were negative correlation with them at low altitude (0~2000m), respectively. Consequently, tracing of the δ13C variations in grassland ecosystem can provide a powerful tool to evaluate the degree of grassland degradation.
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