Search Results - (Author, Cooperation:H. Kawahata)
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1T. Watanabe ; A. Suzuki ; S. Minobe ; T. Kawashima ; K. Kameo ; K. Minoshima ; Y. M. Aguilar ; R. Wani ; H. Kawahata ; K. Sowa ; T. Nagai ; T. Kase
Nature Publishing Group (NPG)
Published 2011Staff ViewPublication Date: 2011-03-11Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsKeywords: Animals ; *Anthozoa/metabolism ; Atmosphere ; *Climate ; El Nino-Southern Oscillation/*history ; Entropy ; Fossils ; History, Ancient ; Oxygen Isotopes ; Pacific Ocean ; Philippines ; Salinity ; Seasons ; Seawater/analysis ; *Temperature ; Time FactorsPublished by: -
2Staff View
ISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
3Ohkouchi, N. ; Kawahata, H. ; Murayama, M. ; Okada, M. ; Nakamura, T. ; Taira, A.
Amsterdam : ElsevierStaff ViewISSN: 0012-821XSource: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002Topics: GeosciencesPhysicsType of Medium: Electronic ResourceURL: -
4Staff View
ISSN: 1432-0975Keywords: Key words Carbon budget ; Nutrients ; Total carbon dioxide ; Fringing reef ; Ground waterSource: Springer Online Journal Archives 1860-2000Topics: BiologyGeosciencesNotes: Abstract Measurements of CO2 system parameters and nutrients showed the potential influence of terrestrial inputs on the carbon budget of a fringing coral reef on Ishigaki Island, Japan. Land-derived freshwaters, including river and ground water, make a relatively large contribution (0.5–1.2% by volume) to the water circulation of the reef. These terrestrial waters exhibit extremely high fugacity of CO2 (fCO2 up to 6400 μatm), reflecting enrichments in total alkalinity and dissolved inorganic carbon. Since the dissolved inorganic C:P ratio is anomalously high in terrestrial waters compared with the mean C:P ratios of primary production, excess carbon could be released into the atmosphere. Terrestrial inputs deliver a large quantity of C relative to P. The study site was a source of CO2 at the time of measurement. Such a situation is likely to prevail all year round, and it may occur elsewhere.Type of Medium: Electronic ResourceURL: -
5Staff View
ISSN: 1432-0975Source: Springer Online Journal Archives 1860-2000Topics: BiologyGeosciencesNotes: Abstract. Precise measurements of the partial pressure of CO2 (PCO2) in oceanic and lagoonal surface waters from Palau Barrier Reef and Majuro Atoll were taken to ascertain the net effect of these coral reef systems on air-sea CO2 exchange. PCO2 in the surface water in the lagoon of Palau Barrier Reef and Majuro Atoll was 48 and 14 μatm higher than in the surrounding oceanic water, respectively. A total carbon dioxide vs. total alkalinity diagram indicates that calcification is mainly responsible for CO2 evasion in these coral reef systems.Type of Medium: Electronic ResourceURL: