Titlebook: Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continenta; Jing Zhang Book 2015 Springer Intern

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Ambivalenzen der digitalen Transformationical for a quantitative understanding of global biogeochemical cycles. This chapter summarizes the spatial variation of organic matter and biomarkers from the watershed to the shelf. Monthly data collected from the downstream of the watershed help to elucidate the seasonal variation of biomarkers (e

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Paresh Wankhade,Kevin Mackway-Joneshave been colonized by various types of salt marsh vegetation. As the Changjiang Estuary is located adjacent to the megacity of Shanghai, human activities exert substantial pressures on the coastal wetlands and cause coastal ecosystem degeneration and consequent decreases or loss in ecosystem servic

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https://doi.org/10.1007/978-3-662-47312-2, zooplankton, benthic macro-invertebrate, and fish faunas. During recent decades, the marine ecosystems in this area have experienced marked disturbances induced by human activities and changing climate. An increase in the abundance of dinoflagellates constitutes the most important change in phytop

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https://doi.org/10.1007/978-3-662-49885-9veloped and the densely populated areas in China. Over the last 30 years, these areas have experienced rapid urbanization and industrialization. With increasing incomes and improved living standards in China, so tourism, traffic, and related industries have also developed rapidly. The rapid urbaniza

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Book 2015ronment, the East China Sea. The studies in this volume bridges the watersheds of the river and the marginal sea through a combined approach of hydro-dynamics, geochemistry, sedimentary processes, ecology and fishery. The response of ecosystem to the external driving forces is examined via process-o

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Changjiang Estuary Sediment Transport Dynamics,scharges acting on the estuary and their variations in the past half century. There is an ongoing decrease in sediment discharge since the 1980s, which has accelerated since 2003 when the Three Gorges Dam (TGD) commenced operation. In situ flocculation of suspended sediment is detected in the freshw