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Biogeochemistry of Nitrous Oxide Production in the Red Mangrove (Rhizophora Mangle) Forest Sediments

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Biogeochemistry of Nitrous Oxide Production in the Red Mangrove (Rhizophora Mangle) Forest Sediments
BIOGEOCHEMISTRY OF NITROUS OXIDE PRODUCTION IN THE RED MANGROVE (Rhizophora mangle) FOREST SEDIMENTS

Jorge Bauza, Julio M. Morell and Jorge E. Corredor
Department of Marine Sciences
University of Puerto Rico
Mayaguez, Puerto Rico 00680

RUNNING HEAD: Nitrous Oxide in Mangrove Sediments

keywords: nitrous oxide, nitrification, mangrove forest

ABSTRACT The present study was undertaken to quantify the emission and distribution of nitrous oxide and to explore its relation with pertinent physical and chemical parameters of the red mangrove forest sediment. Rates of N2O evolution, which ranged from 0.052 to 1.37 ƒÝmole.m-2.h-1 (overall mean = 0.495 ƒÝmole.m-2.h-1), are comparable to those of other ecosystems that has been previously studied. A significant diel flux change in nitrous oxide emission was observed. Dissolved nitrous oxide concentration averaged 0.149 nmole.cm-3 (SD = 0.09, n = 54) with a range from 0.096 to 0.574 nmole.cm-3. Dissolved and exchangeable inorganic nitrogen was present mostly in the form of ammonium (from 199 to 272 nmole.cm-3) with lesser amounts of nitrate (overall mean = 29.0 nmole.cm-3). Redox potentials in the sediments generally decreased with depth, with a mean value of 377 mV at the sediment surfaces and lower mean value (159 mV) at 10 cm deep. We have explored the probable sources of nitrous oxide in the mangrove forest sediment using linear and multiple regression and correlation between the data obtained in this study and comparing this observations with previous studies of N2O metabolism. Our results, while not excluding the possibility of N2O production through denitrification, indicate that N2O is produced mainly by nitrification in sediments of this mangrove forest.

INTRODUCTION

Nitrous oxide is a trace gas produced under natural conditions by the processes of nitrification and denitrification as part of the biogeochemical cycle of nitrogen (Firestone and Davidson, 1989). It was not until



References: Bange, H.W., S. Rapsomaniris, and M.O. AnDreae. 1996. Nitrous oxide in coastal waters. Global Biogeochem. Cycles 10: 197-207. Boto, F.G. and Robertson, A.I. 1990. The relationship between nitrogen fixation and tidal exports of nitrogen in a tropical mangrove system. Estuarine, Coastal and Shelf Science 31:243-540. Boto, K. G. 1982. Nutrient and organic fluxes in mangroves. In: B. F. Clough (Ed.) Mangrove ecosystems in Australia, pp. 239-257. Australia National University Press, Australia. Boto, K. P. Saffigna and B. Clough. 1985. Role of nitrate in nitrogen nutrition of the mangrove Avicennia marina. Mar. Ecol. Prog. Ser. 21: 259-265. Capone, D.G. 1996. A biologically constrained estimate of oceanic N2O flux. In : D.D. Adams et al. (Eds.) Cycling of reduced gases in the hydrosphere. Mitt. Internat. Verein Limnol. 25: 105-114. Carrera, C. J. and A. E. Lugo. 1978. Los sistemas de manglares de Puerto Rico. Department of Natural Resources Publication. San Juan, Puerto Rico, 270 pp. Crutzen, P. J. 1976. Upper limits on atmospheric ozone reductions following application of fixed nitrogen to the soil Danielson and Sutherland, 1986. Porosity. In: C.A. Black et al. (Eds.) Methods of Soil Analysis. Part 1. Agronomy 9: 443-461. Davidson, E. A. 1993. Soil water content and the ratio of nitrous oxide to nitric oxide emitted from soil. In: R. S. Oremland (ed.). Biogeochemistry of global change: radiatively active trace gases, pp. 369-386. Chapman and Hall, New York. Delwiche, C.C. 1981. Atmospheric chemistry of nitrous oxide. In: Denitrification, nitrification, and Atmospheric Nitrous Oxide, pp Golley, F., H. T. Odum and R. F. Wilson. 1962. The structure and metabolism of a Puerto Rican red mangrove forest in May. Ecology. 43: 9-19. Goodroad, L. L., and D. R. Keeney. 1984. Nitrous oxide emission from forest marsh, and prairie ecosystems Goreau, T. J., W. A. Kapla, S. C. Wofsy, M. B. Mc Elroy, F. W. Valios, and S. W. Watson. 1980. Production of NO and N2O by nitrifying bacteria at reduced concentrations of oxygen. Appl. Environ. Microbiol. 40: 526-532. Hansen, J Hao, W. M., S. C. Wofsy, M. B. McElroy, J. M. Beer, and M. A. Togan. 1987. Sources of atmospheric nitrous oxide from combustion Hines, M. E. and W. B. Lyons. 1982. Biogeochemistry of nearshore Bermuda sediment. I. Sulfate reduction rates and nutrient regeneration. Mar. Ecol. Prog. Ser. 8: 87-94. Kaplan, W.A. 1983. Nitrification. In: E.J. Carpenter and D.G. Capone (Eds.) Nitrogen in the Marine Environment. Academic. N.Y. p.139-190. Keller, M., and W. A. Reiners. 1990. Emissions of nitrous oxide and nitric oxide from wet tropical forest soils. EOS 71: 1259. Koike, I. and K. Terauchi. 1996. Fine scaler distribution of nitrous oxide in marine sediments. Mar. Chem. 52: 185-193 Kristensen, E., M Kristensen, E., F. O. Andersen, and L. H. Kofeod. 1988. Preliminary assessment of benthic community metabolism in a southeast Asian mangrove swamp. Mar. Ecol. Prog. Ser. 48: 137-145. Levine, E.A Lugo, A.E., and S. C. Snedaker. 1974. The ecology of mangroves. Annual Review of Ecology and Systematic 5: 39-64. Lugo, A.E Martikainen, P. J. 1985. Nitrous oxide emission associated with autotrophic ammonium oxidation in acid coniferous forest soil Matson, P. A., and P. M. Vitousek. 1990. Ecosystem approach to a global nitrous oxide budget. Bioscience 40: 667-672. Matson, P.A.., P.M. Vitousek, G.P. Livingston, and N.A. Swanberg. 1990. Sources of variation in nitrous oxide flux from amazonian ecosystems. J. Geophy.Res. 95:16789-16798. Mosier, A.R. 1989. Chamber and isotope tecniques. In: M.O. Andreae and D.S. Chimel (ed.). Exchange of trace gases between terrestrial ecosystems and the atmosphere, pp. 175-187. John Wiley & Son. N.Y. Mosier, A.R. and L. Mack. 1980. Gas chromatographic system for precise, rapid analysis of nitrous oxide. Soil Sci. Soc. J. 44: 1121-1123. Nishio, T., I. Koike, and A. Hattori. 1983. Estimate of denitrification and nitrification in coastal and estuarine sediments. Appl. Environ. Microbiol. 45: 444-450. Rosenfeld, J .K. 1979. Interstitial water and sediment chemistry of two cores from Florida Bay. J. Sed. Petrol. 49: 989-994. Schmidt, J., W. Seiler, and R. Conrad. 1988. Emission of nitrous oxide Scholander, P. F. and S. I. Scholander. 1955. Gas exchange in the roots of mangroves. Amer. J. Bot. 42: 92-98. Seitzinger, S. P., S. W. Nixon, and M. E. Q. Pilson. 1984. Denitrification and nitrous oxide production in a coastal marine ecosystem. Limnol. Oceanogr. 29: 73-83. Smith, C. J., W. F. Wright, and W. H. Patrick. 1983. The effect of soil redox potential and pH on the reduction and production of nitrous oxide. J. Environ. Qual. 12: 186-188.

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