globalchange  > 气候变化与战略
DOI: 10.1016/j.scitotenv.2019.136052
论文题名:
Changing riverine organic C:N ratios along the Pearl River: Implications for estuarine and coastal carbon cycles
作者: Liu Q.; Liang Y.; Cai W.-J.; Wang K.; Wang J.; Yin K.
刊名: Science of the Total Environment
ISSN: 489697
出版年: 2020
卷: 709
语种: 英语
英文关键词: Anthropogenic perturbation ; Coastal ocean carbon cycle ; Organic C:N ratio ; Pearl River ; Riverine organic carbon flux
Scopus关键词: Biogeochemistry ; Budget control ; Estuaries ; Gems ; Marine biology ; Nitrogen ; Phytoplankton ; Rivers ; Anthropogenic perturbation ; C:N ratio ; Coastal ocean ; Organic carbon fluxes ; Pearl River ; Organic carbon ; fresh water ; inorganic compound ; organic carbon ; organic matter ; organic nitrogen ; anthropogenic source ; carbon cycle ; carbon flux ; carbon isotope ratio ; carbon sink ; nitrogen cycle ; perturbation ; Article ; carbon cycle ; carbon source ; correlational study ; estuary ; priority journal ; seashore ; stream (river) ; urban area ; water sampling ; China ; Guangdong ; Zhujiang Estuary
英文摘要: In the traditional view, riverine organic matter typically has a higher C:N ratio than marine phytoplankton 6.7:1 and has therefore been thought to be a carbon source in estuaries and coastal waters. Thus, a decrease in the riverine organic C:N ratio to <6.7:1 would potentially switch riverine organic matter from a coastal carbon source to sink. However, few studies have paid an attention to such a change. Our field investigation showed that organic C:N ratio was 11.8:1 in the pristine upstream section of a natural reserve, but decreased after the river passed through several urban cities, reaching 5.0:1 in near the Pearl River estuary. Along the river, dissolved inorganic nitrogen, total organic carbon and nitrogen all increased and they were highly negatively correlated with organic C:N ratios. The observation has a great implication that organic matter with a decreased C:N ratio from the Pearl River would potentially switch from a coastal carbon source of 2.8 × 1011 g C/year to a sink of 2.2 × 1011 g C/year. This carbon sink (2.2 × 1011 g C/year) contributes to 56% of the previous estimate of the Pearl River estuarine-coastal net carbon sink. Such a decrease in organic C:N ratio also occurs in some other large rivers, which should be considered in the assessment of global coastal carbon budgets and metabolic balance. © 2019 The Authors
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被引频次[WOS]:31   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/158656
Appears in Collections:气候变化与战略

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作者单位: School of Marine Sciences/Guangdong Key Laboratory of Marine Resources and Coastal Engineering, Sun Yat-Sen University, Guangzhou, 510275, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China; School of Marine Science and Policy, University of Delaware, Newark, DE 19716, United States; National Marine Environmental Monitoring Center, Ministry of Ecology and Environment, Dalian, 116023, China

Recommended Citation:
Liu Q.,Liang Y.,Cai W.-J.,et al. Changing riverine organic C:N ratios along the Pearl River: Implications for estuarine and coastal carbon cycles[J]. Science of the Total Environment,2020-01-01,709
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