Temporal variability of particulate organic carbon in the lower Changjiang (Yangtze River) in the post-Three Gorges Dam period: Links to anthropogenic and climate impacts

被引:41
|
作者
Wu, Ying [1 ]
Bao, Hongyan [1 ]
Yu, Hao [2 ]
Zhang, Jing [1 ]
Kattner, Gerhard [3 ]
机构
[1] E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China
[2] State Ocean Adm Peoples Republ China, Inst North Sea Marine Engn Prospecting, North China Sea Branch, Qingdao, Peoples R China
[3] Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Bremerhaven, Germany
关键词
ASIAN SUMMER MONSOON; VEGETATION INDEX; LIGNIN PHENOL; STABLE CARBON; SEDIMENT LOAD; MATTER; CHINA; LAND; TRANSPORT; DEGRADATION;
D O I
10.1002/2015JG002927
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Suspended particles from the lower Changjiang were collected monthly from 2003 to 2011, which corresponds to the three construction periods of the Three Gorges Dam. Organic carbon (%OC), organic carbon to total nitrogen molar ratio, stable carbon isotope, and terrestrial biomarkers were examined. Rating curve studies were applied for the temporal trend analysis. The composition of particulate lignin phenols exhibited clear annual and periodic variations but only minor seasonal changes. Lignin phenol ratios (vanillyl/syringyl and cinnamyl/vanillyl) indicated that the terrigenous organic matter (OM) was primarily composed of woody and nonwoody tissue derived from angiosperm plants. The low-lignin phenol yields (A8) in combination with higher acid to aldehyde ratios reflected a substantial contribution from soil OM to the particle samples or modifications during river transport. The temporal shift of the lignin phenol vegetation index with the sediment load during the flood seasons revealed particulate organic matter (POM) erosion from soils and the impact of hydrodynamic processes. The dam operations affected the seasonal variability of terrigenous OM fluxes, although the covariation of lignin and sediment loads with discharged water implies that unseasonal extreme conditions and climate change most likely had larger influences, because decreases in the sediment load and lignin flux alter the structure and composition of particulate OM (POM) on interannual time scales, indicating that they may be driven by climate variability. The modification of the composition and structure of POM will have significant impacts on regional carbon cycles and marine ecosystems.
引用
收藏
页码:2194 / 2211
页数:18
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