Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems

Rivers play an important role in carbon (C) exchange between terrestrial and oceanic water bodies and the atmosphere. The aim of this study was to systematically quantify fluxes in riverine C export and C exchange in the air–sea interface of marine ecosystems in China. Results show that annual C tra...

Full description

Bibliographic Details
Main Authors: Yang Gao, Tiantian Yang, Yafeng Wang, Guirui Yu
Format: Article
Language:English
Published: Taylor & Francis Group 2017-03-01
Series:Ecosystem Health and Sustainability
Subjects:
Online Access:http://dx.doi.org/10.1002/ehs2.1265
id doaj-ec5d1efa60f74134b07b09ee23012279
record_format Article
spelling doaj-ec5d1efa60f74134b07b09ee230122792021-04-02T11:40:59ZengTaylor & Francis GroupEcosystem Health and Sustainability2096-41292332-88782017-03-013310.1002/ehs2.126511879073Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystemsYang Gao0Tiantian Yang1Yafeng Wang2Guirui Yu3University of Chinese Academy of SciencesUniversity of CaliforniaChinese Academy of SciencesUniversity of Chinese Academy of SciencesRivers play an important role in carbon (C) exchange between terrestrial and oceanic water bodies and the atmosphere. The aim of this study was to systematically quantify fluxes in riverine C export and C exchange in the air–sea interface of marine ecosystems in China. Results show that annual C transport from rivers to coastal ecosystems in China can reach up to 64.35 TgC, which accounts for approximately 4.8%–8.1% of global C transport from river systems. In the Bohai Sea, particulate inorganic carbon is the main form of C influx, and it can reach up to 20.79 TgC/yr. Conversely, dissolved inorganic carbon is the main form of C influx into the East China Sea, and it can reach up to 10.52 TgC/yr, which is 42.6% of the total annual C imported into the East China Sea. China's marine ecosystems including the Yellow Sea, the Bohai Sea, the East China Sea, and the South China Sea can absorb 65.06 TgC/yr from the atmosphere.http://dx.doi.org/10.1002/ehs2.1265air–sea interfacecarbon fluxcarbon transportChina Seasriverine carbon
collection DOAJ
language English
format Article
sources DOAJ
author Yang Gao
Tiantian Yang
Yafeng Wang
Guirui Yu
spellingShingle Yang Gao
Tiantian Yang
Yafeng Wang
Guirui Yu
Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
Ecosystem Health and Sustainability
air–sea interface
carbon flux
carbon transport
China Seas
riverine carbon
author_facet Yang Gao
Tiantian Yang
Yafeng Wang
Guirui Yu
author_sort Yang Gao
title Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
title_short Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
title_full Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
title_fullStr Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
title_full_unstemmed Fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
title_sort fate of river‐transported carbon in china: implications for carbon cycling in coastal ecosystems
publisher Taylor & Francis Group
series Ecosystem Health and Sustainability
issn 2096-4129
2332-8878
publishDate 2017-03-01
description Rivers play an important role in carbon (C) exchange between terrestrial and oceanic water bodies and the atmosphere. The aim of this study was to systematically quantify fluxes in riverine C export and C exchange in the air–sea interface of marine ecosystems in China. Results show that annual C transport from rivers to coastal ecosystems in China can reach up to 64.35 TgC, which accounts for approximately 4.8%–8.1% of global C transport from river systems. In the Bohai Sea, particulate inorganic carbon is the main form of C influx, and it can reach up to 20.79 TgC/yr. Conversely, dissolved inorganic carbon is the main form of C influx into the East China Sea, and it can reach up to 10.52 TgC/yr, which is 42.6% of the total annual C imported into the East China Sea. China's marine ecosystems including the Yellow Sea, the Bohai Sea, the East China Sea, and the South China Sea can absorb 65.06 TgC/yr from the atmosphere.
topic air–sea interface
carbon flux
carbon transport
China Seas
riverine carbon
url http://dx.doi.org/10.1002/ehs2.1265
work_keys_str_mv AT yanggao fateofrivertransportedcarboninchinaimplicationsforcarboncyclingincoastalecosystems
AT tiantianyang fateofrivertransportedcarboninchinaimplicationsforcarboncyclingincoastalecosystems
AT yafengwang fateofrivertransportedcarboninchinaimplicationsforcarboncyclingincoastalecosystems
AT guiruiyu fateofrivertransportedcarboninchinaimplicationsforcarboncyclingincoastalecosystems
_version_ 1721571760208347136