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Ecosystem responses to anthropogenic and natural forcing over the last 100 years in the coastal areas of the East China Sea

Datos Bibliográficos

ID12265502
AutoresLei Xing (0000-0002-7147-5252, Ocean University of China), Meixun Zhao (0000-0001-9450-6448, Ocean University of China, autor de correspondencia), Ting Zhang (0000-0002-6840-1367, Ocean University of China), Meng Yu (0000-0002-3769-0979, Ocean University of China), Shan-Shan Duan (Ocean University of China), Shanshan Duan (Ocean University of China), Rongping Zhang (0000-0001-6448-7493, Ocean University of China), Chih-An Huh (Institute of Earth Sciences, Academia Sinica, Taiwan), Wen‐Hsuan Liao (0000-0002-3687-3423, Research Center for Environmental Changes, Academia Sinica), Wen-Hsuan Liao (Research Center for Environmental Changes, Academia Sinica, Taiwan), Xuwen Feng (Second Institute of Oceanography)
Año2016
Volumen26
Número5
Páginas669-677
Fecha de publicación2016-01-22
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaThe Holocene (JOURNAL)
Identificadores de la revistaISSN: 0959-6836 • E-ISSN: 1477-0911
EditorialSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683615618248
OpenAlexW2340193413
IdiomaEN
Citas recibidas5
Referencias citadas53

Ecosystem changes of the coastal areas of the East China Sea (ECS) during the past 30 years have been characterized by increased productivity and increased occurrences of dinoflagellate red tides; both were commonly attributed to be caused by anthropogenic input of nutrients. However, climate-driven regime shifts were found in the Pacific, but they have not been observed in the ECS owing to the lack of continuous high resolution data. Hence, it is still a challenge to distinguish the influences of anthropogenic activities and climate changes on ECS shelf ecosystem. We compare phytoplankton biomarker (brassicasterol, dinosterol, and alkenones) data of five box cores from the coastal area of the ECS, which afford phytoplankton productivity and community structure records at decadal-scale resolution for the last 100 years. Phytoplankton productivity in all cores increased during the past 50 years, but community structure changes showed different trends. Relative diatom contribution revealed a decreasing trend during the past ca. 50 years in cores DH5-1 and CJ43 collected near the Changjiang Estuary, which were likely caused by increased N/Si and N/P ratios, providing conditions more favorable for dinoflagellates growth. In contrast, the relative diatom contribution increased in cores 32, 34, and DH6-3 further away and south of the Changjiang Estuary, suggesting limited influence of the Changjiang water. Instead, diatom increasing trend is likely caused by increased supply of phosphorus and silicate, as a result of larger Kuroshio intrusion flux and the corresponding strengthened coastal upwelling. Therefore, both anthropogenic activities and climate-driven coastal upwelling have contributed to increased productivities, but these two forcing mechanisms have resulted in contrasting community structure changes at different sites in the coastal area of the ECS

Biogenic silica · Biology · Diatom · Ecosystem · Estuary · Marine ecosystem · Nutrient · Phytoplankton · Productivity · Upwelling · Environmental Science · Geology and Paleoclimatology Research · Marine and coastal ecosystems · Methane Hydrates and Related Phenomena · Ecology · Geology · Oceanography

  • Multiple lipid biomarkers record organic matter sources and paleoenvironmental changes in the East China Sea coast over the past 160 years

    Open Access•Lilei Chen, Feng Li et al.•The Holocene•2020

  • Biogenic Silica and Organic Carbon Records in Zhoushan Coastal Sea over the Past One Hundred Years and Their Environmental Indications

    Open Access•Hao Xu, Shangwei Jiang et al.•International Journal of…•2020

  • Spatiotemporal temperature variations in the East China Sea shelf during the Holocene in response to surface circulation evolution

    Open Access•Zineng Yuan, Xiaotong Xiao et al.•Quaternary International•2018

  • Late-Holocene variation in vertical thermal gradient from the coastal East China Sea

    Open Access•Yuxin He, Bangqi Hu et al.•The Holocene•2018

  • Phytoplankton productivity and community structure variations over the last 160 years in the East China Sea coast in response to natural and human-induced environmental changes

    Open Access•Lilei Chen, Jian Liu et al.•The Holocene•2019

  • The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment

    Open Access•P G Appleby, Frank Oldfield•CATENA•1978

Obras citantes distintas5
Citas por año0,63
Intervalo de citas2018 - 2020 (3)
Velocidad de citaciónhistorical
Altamente citadoNo
Tipos de citaNeutras: 5
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