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THESIS APPROVAL

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1989), such an approaching of shadow or an occurring of vibration may signal a lifethreatening<br />

attack by a predator. As a defense, the worms sense these stimuli and<br />

initiate a rapid escape response in which reflexively withdraws their tail by sudden<br />

contraction.<br />

L. hoffmeisteri adopt a vertical position in the sediment with their anterior<br />

part in the mud and their posterior end free in the water. This burrowing behavior is<br />

normally found in most oligochaete due to their feeding habit. It is well known that<br />

oligochaete worms have a complete digestive tract with a mouth and an anus<br />

(Brinkhurst and Jamieson, 1971). Fragment of dead organisms and small decaying<br />

materials settled down on the sediments become a valid food source for the worms<br />

(Brinkhurst and Churan, 1969). From this observation, undigested materials ingested<br />

by worms at the front end of the body were passed through the gut, and the exceed<br />

particles were finally laid down onto the Petri dish via the hind end of the body.<br />

Kaster et al. (1984), Ewald et al. (1997) and Othman et al. (2002) reported that<br />

oligochaetes feed by ingesting sediment-anterior end buried in the sediment, and<br />

posterior end protruding out of thin tubes into the sediment-water interface where the<br />

defeacted materials are deposited, in a manner similar to this observation. Due to<br />

bringing sediment from depth to the sediment surface in the form of fecal pellets via<br />

feeding habit by such animals, it is suggests that conveyor belt species like<br />

oligochaetes seem to be an organism playing an important role in both modifying and<br />

recycling sediment materials.<br />

Cluster of L. hoffmeisteri on the sediment surface was obviously seen in<br />

this observation. According to the worm penetration, they comprehensively pierced<br />

as deep as 4-5 cm but mostly condensed near the first centimeter of the sediment.<br />

This result was similar to Fisher et al. (1980), demonstrated that tubificid worms<br />

preferred to feed on the level of sediment from 5-9 cm. Based on these results, it is<br />

implied that accumulation of organic matter near the top of the sediment layer may be<br />

a factor affecting aggregation of worm on foraging food particles.<br />

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