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Carbon Cycling in the East China Sea

The ECS is one of the largest continental shelves in the world and has high primary production all year round, as observed on the Coastal Zone Color Scanner images. As a transition zone between the Asian continent and the open ocean, this shelf sea is a very active site of carbon cycling. Some measurements of the partial pressure of CO2 (FCO2) nd other carbon parameters have been conducted by other studies since the 1990s primarily in the central and southern part of the ECS. [Pg.431]

Shiah, P. K., Gong, G. C., and Chen, C. C. (2003). Seasonal and spatial variation of bacterial production in the continental shelf of the East China Sea Possible controlhng mechanisms and potential roles in carbon cycling. Deep Sea Res. Part II—Top. Stud. Oceanogr. 50, 1259—1309. [Pg.1131]

See other pages where Carbon Cycling in the East China Sea is mentioned: [Pg.84]    [Pg.431]    [Pg.431]    [Pg.433]    [Pg.435]    [Pg.437]    [Pg.439]    [Pg.441]    [Pg.443]    [Pg.445]    [Pg.447]    [Pg.449]    [Pg.451]    [Pg.453]    [Pg.455]    [Pg.457]    [Pg.459]    [Pg.461]    [Pg.463]    [Pg.465]    [Pg.84]    [Pg.431]    [Pg.431]    [Pg.433]    [Pg.435]    [Pg.437]    [Pg.439]    [Pg.441]    [Pg.443]    [Pg.445]    [Pg.447]    [Pg.449]    [Pg.451]    [Pg.453]    [Pg.455]    [Pg.457]    [Pg.459]    [Pg.461]    [Pg.463]    [Pg.465]    [Pg.103]    [Pg.108]    [Pg.632]    [Pg.86]    [Pg.593]    [Pg.647]    [Pg.425]   


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