Changes in the13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic CO2uptake-Reference-Cited by-同舟云学术

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Changes in the13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic CO2uptake

Published:2003-01-03 Issue:1 Volume:17 Page:4-1-4-20
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Quay P.¹,Sonnerup R.²,Westby T.¹,Stutsman J.¹,McNichol A.³

Affiliation:

1. School of Oceanography; University of Washington; Seattle Washington USA

2. Joint Institute for Study of the Atmosphere and Ocean; University of Washington; Seattle Washington USA

3. National Ocean Sciences AMS Facility; Wood Hole Oceanographic Institution; Woods Hole Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Reference53 articles.

1. Distributions of oxygen and carbon stable isotopes and CFC-12 in the water masses of the Southern Ocean at 30°E from South Africa to Antarctica: Results of the CIVA 1 cruise;Archambeau;J. Mar. Syst.,1998

2. The δ13C Suess effect in the world surface oceans and its implications for oceanic uptake of CO2: Analysis of observations at Bermuda;Bacastow;Global Biogeochem. Cycles,1996

3. Determination of the isotopic (13C/12C) discrimination by terrestrial biology from a global network of observations;Bakwin;Global Biogeochem. Cycles,1998

4. Global carbon sinks and their variability inferred from atmospheric O2 and δ13C;Battle;Science,2000

5. Carbon isotope fractionation by plankton in the Southern Ocean: relationship between δ13C of particulate organic carbon and dissolved carbon dioxide;Bentaleb;J. Mar. Syst.,1998

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