DOI: 10.1002/gbc.20033
Scopus记录号: 2-s2.0-84881096749
论文题名: Amounts, isotopic character, and ages of organic and inorganic carbon exported from rivers to ocean margins: 1. Estimates of terrestrial losses and inputs to the Middle Atlantic Bight
作者: Hossler K ; , Bauer J ; E
刊名: Global Biogeochemical Cycles
ISSN: 8866236
出版年: 2013
卷: 27, 期: 2 起始页码: 331
结束页码: 346
语种: 英语
英文关键词: coastal ocean
; DIC
; DOC
; POC
; river exports
Scopus关键词: Coastal ocean
; DIC
; Dissolved organic C
; DOC
; Net primary productivity
; POC
; Terrestrial ecosystems
; Watersheds draining
; Aging of materials
; Ecosystems
; International trade
; Oceanography
; Rivers
; biogeochemistry
; carbon isotope
; coastal water
; continental margin
; dissolved inorganic carbon
; dissolved organic carbon
; estuarine front
; freshwater input
; heterotrophy
; net primary production
; particulate organic carbon
; Atlantic Ocean
; Middle Atlantic Bight
英文摘要: Rivers transport carbon (C) from terrestrial ecosystems to the coastal ocean, providing significant heterotrophic support within both rivers and receiving coastal waters. The amounts and ages of these terrestrial-river- coastal ocean C fluxes, however, are still poorly constrained. To address this uncertainty, a study of eight rivers discharging to the Middle Atlantic Bight (MAB) was undertaken. The rivers were sampled periodically over 2 years for concentrations and δ13C and Δ14C signatures of particulate organic C (POC), dissolved organic C (DOC), and dissolved inorganic C (DIC). For the watersheds draining to the MAB, it was estimated that ∼3800 Gg of terrestrial organic C (OC) and 700 Gg of terrestrial inorganic C was removed annually by fluvial transport. Of the terrestrial OC loss, ∼64% was contemporary C representing approximately 1% of the annual terrestrial net primary productivity. Net fluvial C inputs to the MAB shelf were estimated to be ∼70 Gg·yr-1 of POC, 280 Gg·yr-1 of DOC, and 800 Gg·yr-1 of DIC. Terrestrial C, as opposed to in situ produced river C, comprised the majority of the riverine POC and DOC flux and around half of the total C flux. A smaller but significant fraction (<25%) of the river C flux was further composed of aged materials deriving from fossil C and aged soil OC. The timing of fluvial OC inputs to the MAB, which appear to be temporally offset from peak MAB primary production, could help support the net heterotrophy that has been observed there during periods of low productivity. ©2013. American Geophysical Union. All Rights Reserved. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/77611
Appears in Collections: 气候变化事实与影响
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作者单位: Aquatic Biogeochemistry Laboratory, Department of Evolution, Ecology and Organismal Biology, Ohio State University, 1314 Kinnear Road, Columbus, OH 43212-1156, United States
Recommended Citation:
Hossler K,, Bauer J,E. Amounts, isotopic character, and ages of organic and inorganic carbon exported from rivers to ocean margins: 1. Estimates of terrestrial losses and inputs to the Middle Atlantic Bight[J]. Global Biogeochemical Cycles,2013-01-01,27(2)