Reconciling the paradox that the heterotrophic waters of the East China Sea shelf act as a significant CO2sink during the summertime: Evidence and implications-Reference-Cited by-同舟云学术

Reconciling the paradox that the heterotrophic waters of the East China Sea shelf act as a significant CO2sink during the summertime: Evidence and implications

Published:2009-08-06 Issue:15 Volume:36 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Chou Wen-Chen¹,Gong Gwo-Ching¹,Sheu David D.²,Jan Sen³,Hung Chin-Chang¹,Chen Chung-Chi⁴

Affiliation:

1. Institute of Marine Environmental Chemistry and Ecology; National Taiwan Ocean University; Keelung; Taiwan

2. Institute of Marine Geology and Chemistry; National Sun Yat-Sen University; Kaohsiung; Taiwan

3. Institute of Hydrological and Oceanic Sciences; National Central University; Jungli; Taiwan

4. Department of Life Science; National Taiwan Normal University; Taipei; Taiwan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference19 articles.

1. The concentration and isotopic fractionation of oxygen dissolved in freshwater in equilibrium with the atmosphere;Benson;Limnol. Oceanogr.,1984

2. SCOPE Rep.;Chen,2004

3. Importance of planktonic community respiration on the carbon balance of the East China Sea in summer;Chen;Global Biogeochem. Cycles,2006

4. Hypoxia in the East China Sea: One of the largest coastal low-oxygen areas in the world;Chen;Mar. Environ. Res.,2007

5. Transport of the South China Sea subsurface water outflow and its influence on carbon chemistry of Kuroshio waters off southeastern Taiwan;Chou;J. Geophys. Res.,2007

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