Geospatial Health (May 2011)

Effect of soil surface salt on the density and distribution of the snail Bithynia siamensis goniomphalos in northeast Thailand

  • Apiporn Suwannatrai,
  • Kulwadee Suwannatrai,
  • Surat Haruay,
  • Supawadee Piratae,
  • Chalida Thammasiri,
  • Panita Khampoosa,
  • Jutharat Kulsantiwong,
  • Sattrachai Prasopdee,
  • Pairat Tarbsripair,
  • Rasamee Suwanwerakamtorn,
  • Somsak Sukchan,
  • Thidarut Boonmars,
  • John B. Malone,
  • Michael T. Kearney,
  • Smarn Tesana

DOI
https://doi.org/10.4081/gh.2011.170
Journal volume & issue
Vol. 5, no. 2
pp. 183 – 190

Abstract

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Opisthorchis viverrini infection is associated with human cholangiocarcinoma and northeast Thailand has the highest incidence of this disease in the world. Bithynia siamensis goniomphalos is the major freshwater snail intermediate host of O. viverrini in this area and an analysis based on geographical information systems was used to determine the effect of variation in soil surface salt on the density and distribution of this snail. A malacological survey was carried out in 56 water bodies in the Khorat basin, northeast Thailand at locations with various soil surface salt levels. Mollusk samples were collected from 10 ecologically representative water body sites with 10-20 sampling stations in each. The shoreline of clear, shallow water bodies was found to be the preferred B. s. goniomphalos habitat. The snails were exclusively found in water with salinity levels ranging between 0.05 and 22.11 parts per thousand (ppt), which supports the notion that B. s. goniomphalos prefers water with some saline content over pure, freshwater. The highest snail population densities were in rice fields, ponds, road-side ditches and canals within a water salinity range of 2.5-5.0 ppt. However, the presence of B. s. goniomphalos was negatively correlated with water salinity (P ≤0.05), both with regard to density and distribution. The areas with the highest density of B. s. goniomphalos were those with less than 1% soil surface salt (potential index = 0.314), while the lowest densities were found in areas exceeding 50% soil surface salt (potential index = 0.015).

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