Format

Send to

Choose Destination
Mar Pollut Bull. 2006 Dec;52(12):1625-33. Epub 2006 Aug 9.

Organic carbon and nitrogen stable isotopes in the intertidal sediments from the Yangtze Estuary, China.

Author information

1
Department of Geography, Key Laboratory of Geographical Information Science of the Ministry of Education, East China Normal University, No. 3663 Zhongshan North Road, Shanghai 200062, PR China. mliu@geo.ecnu.edu.cn <mliu@geo.ecnu.edu.cn>

Abstract

The natural isotopic compositions and C/N elemental ratios of sedimentary organic matter were determined in the intertidal flat of the Yangtze Estuary. The results showed that the ratios of carbon and nitrogen stable isotopes were respectively -29.8 per thousand to -26.0 per thousand and 1.6 per thousand-5.5 per thousand in the flood season (July), while they were -27.3 per thousand to -25.6 per thousand and 1.7 per thousand-7.8 per thousand in the dry season (February), respectively. The delta(13)C signatures were remarkably higher in July than in February, and gradually increased from the freshwater areas to the brackish areas. In contrast, there were relatively complex seasonal and spatial changes in stable nitrogen isotopes. It was also reflected that delta(15)N and C/N compositions had been obviously modified by organic matter diagenesis and biological processing, and could not be used to trace the sources of organic matter at the study area. In addition, it was considered that the mixing inputs of terrigenous and marine materials generally dominated sedimentary organic matter in the intertidal flat. The contribution of terrigenous inputs to sedimentary organic matter was roughly estimated according to the mixing balance model of stable carbon isotopes.

PMID:
16901511
DOI:
10.1016/j.marpolbul.2006.06.008
[Indexed for MEDLINE]

Supplemental Content

Full text links

Icon for Elsevier Science
Loading ...
Support Center