Organic matter degradation in surface sediments of the Changjiang estuary: Evidence from amino acids

Kui Wang; Jianfang Chen; Haiyan Jin; Hongliang Li; Weiyan Zhang

doi:10.1016/j.scitotenv.2018.04.242

Organic matter degradation in surface sediments of the Changjiang estuary: Evidence from amino acids

Sci Total Environ. 2018 Oct 1:637-638:1004-1013. doi: 10.1016/j.scitotenv.2018.04.242. Epub 2018 May 13.

Authors

Kui Wang¹, Jianfang Chen², Haiyan Jin³, Hongliang Li⁴, Weiyan Zhang⁵

Affiliations

¹ Key Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China. Electronic address: wangkui@sio.org.cn.
² Key Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China. Electronic address: jfchen@sio.org.cn.
³ Key Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China. Electronic address: jinhaiyan@sio.org.cn.
⁴ Key Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China. Electronic address: lihongliang@sio.org.cn.
⁵ Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China.

PMID: 29801197
DOI: 10.1016/j.scitotenv.2018.04.242

Abstract

Organic matter degradation is a key component of the processes of carbon preservation and burial in seafloor sediments. The aim of this study was to explore organic matter degradation state within the open-shelf Changjiang Estuary of the East China Sea, using an amino acids-based degradation index (DI) in conjunction with information about organic matter source (marine versus terrestrial), bottom water oxygenation state, and sediment grain size. The relative molar percentages of 17 individual amino acids (characterized using principal component analysis) in surface sediments indicate that organic matter is degraded to varying extents across the estuary seabed. Sediments with DI >0 (relatively labile) were found mostly within a coastal hypoxic area. Sediments of DI less than -1 (relatively refractory) were found near the Changjiang River mouth and the northern and southern parts of the central shelf. We consider DI to be a more reliable indicator of degradation than simple ratios of AAs. DI was inversely correlated with the proportion of terrestrial organic material (F_t) in the sediments, indicating that relatively fresh/labile organic matter was generally associated with marine sources. DI was significantly correlated with F_t and bottom water apparent oxygen utilization (AOU_bot) together. The parameter DI and the (labile) amino acid tyrosine were highest in hypoxic areas, suggesting the presence of relatively fresh organic matter, probably due to a combination of marine-source inputs and better preservation of organic matter in the silt and clay sediments of these areas (as compared to sandy sediments). Less degraded organic matter with high amino acids was also favorable to benthic animals. Overall, sedimentary estuarine organic matter was least degraded in areas characterized by marine sources of organic matter, low-oxygen conditions, and fine-grained sediments.

Keywords: Amino acid; Degradation; Sediment.

MeSH terms

Amino Acids / analysis
China
Environmental Monitoring*
Estuaries*
Geologic Sediments / chemistry*
Water Pollutants, Chemical / analysis*

Substances

Amino Acids
Water Pollutants, Chemical