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Diurnal Changes in the Partial Pressure of Carbon Dioxide in Coral Reef Water
Abstract
Coral reefs are considered to be a source of atmospheric carbon dioxide because of their high calcium carbonate production and low net primary production. This was tested by direct measurement of diurnal changes in the partial pressure of carbon dioxide ( P co 2 ) in reef waters during two 3-day periods, one in March 1993 and one in March 1994, on Shiraho reef of the Ryukyu Islands, Japan. Although the P co 2 values in reef waters exhibited large diurnal changes ranging from 160 to 520 microatmospheres, they indicate that the reef flat area is a net sink for atmospheric carbon dioxide. This suggests that the net organic production rate of the reef community exceeded its calcium carbonate production rate during the observation periods.
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Citations
Cited by
GATTUSO, J.-P., ALLEMAND, D., & FRANKIGNOULLE, M. (1999) · American Zoologist · doi:10.1093/icb/39.1.160 · Cited by 709
Do we have enough pieces of the jigsaw to integrate CO2 fluxes in the coastal ocean?
Borges, A. V. (2005) · Estuaries · doi:10.1007/bf02732750 · Cited by 414
Ocean acidification and calcifying reef organisms: a mesocosm investigation
Jokiel, P. L., Rodgers, K. S., Kuffner, I. B., Andersson, A. J., Cox, E. F., & Mackenzie, F. T. (2008) · Coral Reefs · doi:10.1007/s00338-008-0380-9 · Cited by 389
Barker, S., Higgins, J. A., & Elderfield, H. (2003) · Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences · doi:10.1098/rsta.2003.1238 · Cited by 91
Metadata
- Authors
- Kayanne, H., Suzuki, A., & Saito, H.
- Venue
- Science
- Published
- 1995-07-14
- Volume
- 269
- Issue
- 5221
- Pages
- 214-216
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W1989395589
- Cited by
- 172
- References
- 0
- FWCI
- 11.40
- Type
- journal article
- Language
- en
- Open access
- closed
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- Kayanne, H., Suzuki, A., & Saito, H. (1995). Diurnal Changes in the Partial Pressure of Carbon Dioxide in Coral Reef Water. Science. https://doi.org/10.1126/science.269.5221.214
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