Responses of summer phytoplankton community to drastic environmental changes in the Changjiang (Yangtze River) estuary during the past 50 years

2014 ◽  
Vol 54 ◽  
pp. 1-11 ◽  
Author(s):  
Zhibing Jiang ◽  
Jingjing Liu ◽  
Jianfang Chen ◽  
Quanzhen Chen ◽  
Xiaojun Yan ◽  
...  
2012 ◽  
Vol 9 (6) ◽  
pp. 6261-6291 ◽  
Author(s):  
F. Cheng ◽  
X. Song ◽  
Z. Yu ◽  
D. Liu

Abstract. Two sediment cores from the Changjiang (Yangtze) River estuary and its adjacent East China Sea were collected and studied for eutrophication history using paleoecological records of environmental changes over the last century. A multiproxy approach by using biological and geochemical analyses revealed changes in diatom assemblages, total organic carbon (TOC), total nitrogen (TN) and biogenic silica (BSi) and give an indication of nutrient in status and trends in Changjiang River estuary and its adjacent East China Sea. The diatom assemblages in the two cores generally increased gradually from the 1970s, and accelerated from the 1990s until now, reflecting the increased eutrophication and causing large algae blooms/red tides. The TOC, TN and BSi showing the similar trends, supported the interpretation of the eutrophication process indicated by diatom analyses. The two cores were located in different sea areas of the East China Sea, and we discuss their relative changes based on their environment characteristics. We also discuss the potential effect of anthropogenic influences and ongoing projects on eutrophication in the Changjiang River and its adjacent East China Sea.


2016 ◽  
Vol 13 (4) ◽  
pp. 631
Author(s):  
Xiaoyong Duan ◽  
Yanxia Li ◽  
Xianguo Li ◽  
Yi Gao ◽  
Dahai Zhang

Environmental contextThe concentrations of n-alkanes, phthalates and alkylphenols in a dated sediment core from the Yangtze River estuary steadily increased, with evident peaks in c. 1980 and c. 2000. Most of the phthalates and alkylphenols in the core originated from direct industrial and municipal discharges into the lower reaches of the Yangtze River, whereas the n-alkanes were mainly from aquatic and terrestrial plants. The Yangtze River discharge plays an important role in the sedimentary records of organic compounds. AbstractThe depositional records of phthalate esters (PAEs), alkylphenols (APs) and n-alkanes in the Yangtze River Estuary over the past century were constructed using a dated sediment core to help reconstruct the environmental history. The n-alkane concentrations increased steadily. All the samples had a resolved lower-alkane pattern with well-defined even-over-odd predominance. The n-alkanes originated largely from aquatic and terrestrial plants (83.6%), the remainder being contributed by way of biotransformation in the land soil and river (16.4%). The down-core concentration profiles of PAEs and APs increased rapidly, with evident peaks in the 1980s and c. 2000. PAE and AP homologues were dominated by dibutyl phthalate and nonylphenol respectively, originating mainly from industrial and municipal discharges (79.5%). Long-range transportation from the upper and middle reaches played a much smaller role (20.5%), especially in recent decades. The changes in the Yangtze River discharge and the modification of the water system played important roles in the transport of organic compounds, especially after the 1950s.


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