Decadal variations in diatoms and dinoflagellates on the inner shelf of the East China Sea, China

被引:6
作者
Abate, Rediat [1 ,2 ,4 ]
Gao Yahui [1 ,2 ,3 ]
Chen Changping [1 ,2 ,3 ]
Liang Junrong [1 ,2 ,3 ]
Mu Wenhua [3 ]
Kifile, Demeke [5 ]
Chen Yanghang [1 ,2 ]
机构
[1] Xiamen Univ, Sch Life Sci, Xiamen 361102, Peoples R China
[2] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China
[3] Xiamen Univ, Key Lab, Minist Educ Coastal & Wetland Ecosyst, Coll Environm & Ecol, Xiamen 361102, Peoples R China
[4] Arba Minch Univ, Coll Nat Sci, POB 21, Arba Minch, Ethiopia
[5] Univ Addis Ababa, Dept Zool Sci, POB 117, Addis Ababa, Ethiopia
基金
中国国家自然科学基金;
关键词
anthropogenic impact; benthic diatoms; pigment signature; nutrient concentration; Three Gorges Dam construction; YANGTZE-RIVER ESTUARY; REGIME SHIFTS; ENVIRONMENTAL IMPLICATIONS; PHYTOPLANKTON DYNAMICS; SEDIMENTARY RECORDS; CLIMATE-CHANGE; PACIFIC; NORTH; NUTRIENT; MARINE;
D O I
10.1007/s00343-017-6029-1
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Diatoms and dinoflagellates are two major groups of phytoplankton that flourish in the oceans, particularly in coastal zone and upwelling systems, and their contrasting production have been reported in several world seas. However, this information is not available in the coastal East China Sea (ECS). Thus, to investigate and compare the decadal trends in diatoms and dinoflagellates, a sediment core, 47 cm long, was collected from the coastal zone of the ECS. Sediment chlorophyll-a (Chl-a), phytoplankton-group specific pigment signatures of diatoms and dinoflagellates, and diatom valve concentrations were determined. The sediment core covered the period from 1961 to 2011 AD. The chlorophyll-a contents ranged from 2.32 to 73 mu g/g dry sediment (dw) and averaged 9.81 mu g/g dw. Diatom absolute abundance ranged from 29152 to 177501 valve/gram (v/g) dw and averaged 72137 v/g dw. Diatom valve and diatom specific pigment marker concentrations were not significantly correlated. Peridinin increased after the 1980s in line with intensified use of fertilizer and related increases in nutrient inputs into the marine environment. The increased occurrence of dinoflagellate dominance after the 1980s can be mostly explained by the increase in nutrients. However, the contribution of dinoflagellates to total phytoplankton production (Chl-a) decreased during the final decade of this study, probably because of the overwhelming increase in diatom production that corresponded with the construction of the Three Gorges Dam (TGD) and related light availability. Similarly, the mean ratio of fucoxanthin/peridinin for the period from 1982 to 2001 was 6% less than for 1961 to 1982, while the ratio for 2001 to 2011 was 45.3% greater than for 1982 to 2001. The decadal variation in the fucoxanthin/peridinin ratio implies that dinoflagellate production had been gradually increasing until 2001. We suggest that the observed changes can be explained by anthropogenic impacts, such as nutrient loading and dam construction.
引用
收藏
页码:1374 / 1386
页数:13
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