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Abstract
The work presents an extended database (n = 123) of total mercury (THg) in fine-grained sediment fraction (<63 μm) of core samples in 10 sampling stations of the Sundarban mangrove wetland, India, formed at the estuarine realm of the Hugli (Ganga) River. Results revealed a wide range of spatial, seasonal, and intertidal flat variations of THg (7.3 to 93.3 ng/g) with a definite enhancement level at the lower stretch of the estuary, which has extreme mangrove vegetation. An overall enrichment of THg in surface/subsurface layers of the core is tentatively explained by remobilization and resuspension of the metal from deeper sediments (36–40 cm). A strong positive correlation was observed between the Hg and clay fraction content of the sediments, while correlations of Hg with organic carbon was poor. Based on the index of geoaccumulation (Igeo), enrichment factor (EF), and anthropogenic factor (AF) values, it is suggested that the sediments of Sundarban were found to be less polluted with respect to total mercury. The data reported are a useful baseline for THg in Sundarban and would be of importance in future sediment quality studies.
Acknowledgements
The research work was supported jointly by the Council of Scientific and Industrial Research (CSIR), New Delhi, India (Sanction No. 09/028(0776)/2010-EMR I), and the Indo-Croatian Programme of Cooperation in Science and Technology (Sanction No. INT/CROATIA/P-7/05), Principal Investigators, S.K. Sarkar and H. Bilinski, and project of the Croatian Ministry of Science Education and Sport No. 098-0982934-2720, Principal Investigator I. Pižeta.