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作 者:Mashura Shammi Xiangliang Pan Khan M.G. Mostofa Daoyong Zhang Cong-Qiang Liu
机构地区:[1]Laboratory af Bioremediation, Department of Environmental Pollution and Process Control, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences Urumqi 830011, China [2]Department of Environmental Sciences, Jahangirnagar University, Dhaka 1342, Bangladesh [3]Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China [4]State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China [5]University of Chinese Academy of Sciences, Beijing 100049, China
出 处:《Science Bulletin》2017年第11期764-766,共3页科学通报(英文版)
基 金:financially supported by National Natural Science Foundation of China(U1503281 and U1403181);the Key Construction Program of the National ‘‘985” Project,Tianjin University,China;Partial funding for this research Search Project;Mashura Shammi was supported by the CAS–TWAS President’s Fellowship program 2013
摘 要:Cyanobacteria are the Earth’s oldest oxygenic photoautotrophs and have had major impacts on shaping the biosphere.Their long evolutionary history($3.5 bya)has enabled them to adapt to geochemical and climatic changes and,more recently,anthropogenic modifications of aquatic environments,including nutrient overenrichment(eutrophication),water diversion,withdrawal。Cyanobacteria are the Earth's oldest oxygenic photoautotrophs and have had major impacts on shaping the biosphere. Their long evolutionary history (-3.5 bya) has enabled them to adapt to geochemical and climatic changes and, more recently, anthropogenic modifications of aquatic environments, including nutrient overenrichment (eutrophication), water diversion, withdrawal, and salinisation [1].
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