Prasad,M.B.K. and Ramanathan,AL.(2010): Characterization of phosphorus fractions in the sediments of a tropical intertidal mangrove ecosystem. Wetlands Ecol. Manage., 18, 165-175.

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wAbstract
@Solid phases of phosphorus fractions in the surface and core sediments were studied to understand the biogeochemical cycling and bioavailability of phosphorus in the Pichavaram intertidal mangrove sediments of India. Total P in surface and core sediments ranged between 451-552 and 459-736ƒΚg g-1 respectively and Fe bound P was the dominant fraction. Low levels of Fe bound P in the mangrove zone than the two estuarine zones may be because of high salinity inhibition of phosphate adsorption onto the Fe-oxides/hydroxides. Post-depositional reorganization of P was observed in surface sediments, converting organic P and Fe bound P into the authigenic P. High High levels of organic P in the mangrove zone is primarily due to intensive cycling and degradation of organic matter and adsorption of phosphate on the organic molecules. The burial rates and regeneration efficiency of P in the intertidal mangrove ecosystem ranged from 5.41 to 7.27ƒΚmol P cm-2 year-1 and 0.122 to 0.233ƒΚmol P cm-2 year-1, respectively. High burial efficiency (ΰ99“) of P proves the earlier observation of limiting nature of P for the biological productivity. Further, bioavailable P (exchangeable P + Fe bound P + organic P) constituted a considerable proportion of sedimentary P pool of which an average accounted for 55 and 50“ in surface and core sediments respectively. The results indicate that significant amount of P is locked in sediments in the form of authigenic P and detrital P which makes P as a limiting nutrient for the biological productivity.

Keywords: Phosphorus; Sequential extraction; Organic P; Mangrove; Indiax

Introduction
Materials and methods
@Research area description
@Sample collection and pretreatment
@Sequential extraction of phosphorus
@Analytical methods
Results
@Sediment characteristics
@Phosphorus fractions in sediments
Discussion
@Phosphorus speciation in surface sediments
@Phosphorus fractions in core sediments
@Phosphorus burial rate and regeneration efficiency
@Bioavailable phosphorus
Summary and conclusion
Acknowledgement
References


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