Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 16 June 2000:
Vol. 288. no. 5473, pp. 2028 - 2031
DOI: 10.1126/science.288.5473.2028

Reports

Assessment of Oceanic Productivity with the Triple-Isotope Composition of Dissolved Oxygen

Boaz Luz, * Eugeni Barkan

Plant production in the sea is a primary mechanism of global oxygen formation and carbon fixation. For this reason, and also because the ocean is a major sink for fossil fuel carbon dioxide, much attention has been given to estimating marine primary production. Here, we describe an approach for estimating production of photosynthetic oxygen, based on the isotopic composition of dissolved oxygen of seawater. This method allows the estimation of integrated oceanic productivity on a time scale of weeks.

The Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem 91904, Israel.
*   To whom correspondence should be addressed.


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Heavy Water Fractionation during Transpiration.
G. D. Farquhar, L. A. Cernusak, and B. Barnes (2007)
Plant Physiology 143, 11-18
   Full Text »    PDF »
Fractionation of the Three Stable Oxygen Isotopes by Oxygen-Producing and Oxygen-Consuming Reactions in Photosynthetic Organisms.
Y. Helman, E. Barkan, D. Eisenstadt, B. Luz, and A. Kaplan (2005)
Plant Physiology 138, 2292-2298
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)