Ecology of Endolithic Bivalve Mollusks from Ko Chang, Thailand

泰国象岛内生双壳类软体动物的生态学

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Abstract

Cheewarat Printrakoon, Thamasak Yeemin, and Paul Valentich-Scott (2016) The objective of this study was to examine the ecology of coral boring bivalves from four islands southeast of Ko Chang, Trat Province, Thailand. A total of 11 bivalve families containing 18 species were recorded in the survey, including six reported for this first time in the region. Members of the Mytilidae comprised the highest bivalve diversity with five species recorded. The five most abundant species were Leiosolenus lima (Jousseaume in Lamy), Lithophaga teres (Philippi), Botula cinnamomea (Gmelin), Coralliophaga coralliophaga (Gmelin), and Gastrochaena cuneiformis Spengler. Ecological analysis showed that Ko Bai Dung had the highest density of boring bivalves, with 196.29 ± 118.24 individual/ m(2). Density of coral boring bivalves was variable; the highest density was recorded for Coralliophaga coralliophaga (85.18 ± 74.35 individual/m(2)) at Ko Bai Dung. The highest diversity of boring bivalves was found on Ko Phrao Nok, and in dead coral. Multivariate analyses did not reveal a clear differences in the boring bivalve community composition between sites, or with coral age, or with coral species, however dead coral was well-grouped at 50% similarity. The number of species and number of specimens of boring bivalves in this study was significantly positively correlated with coral age. The maximum number of boring bivalve specimens was found in the oldest coral (11 years old) and in dead Porites host corals. Following the same trend of all dominant boring bivalves, corals more than nine years old showed the highest frequency distribution and the largest shell length. The distribution of shell height frequency showed Leiosolenus lima and Lithophaga teres had more variation in shell height than the other five dominant boring bivalve species. Endolithic bivalves are one of the main bioeroders in the coral biome. The ecologic data presented in this study can be used as one indicator of coral reef status, including bioerosion and nutrient recycling in coral ecosystems.

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