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Mysterious 'crystals': found attached to the epidermal peritoneum of marine tubificid (Annelida, clitellata) species
Marine tubificids are abundant and diverse in the carbonate sediments of Bermuda, as well as in many other tropical and subtropical locations. Recently, during microscopic observations of living specimens, crystal-like structures were observed attached to the coelomic peritoneum and in the coelomic...
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Published in: | Hydrobiologia 2001-11, Vol.463 (1-3), p.115-122 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Online Access: | Get full text |
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Summary: | Marine tubificids are abundant and diverse in the carbonate sediments of Bermuda, as well as in many other tropical and subtropical locations. Recently, during microscopic observations of living specimens, crystal-like structures were observed attached to the coelomic peritoneum and in the coelomic cavity of some Bermuda species, including phallodrilines of the genera Aktedrilus and Pectinodrilus,and a rhyacodriline of the genus Heterodrilus. Similar structures were not seen in tubificid species of Thallasodrilides and other limnodriloidines, a second species of Heterodrilus, a tubificine of the genusTubificoides, a phallodriline of the genus Bathydrilus,nor in a number of marine enchytraeid genera and species found in Bermuda. The crystal-like structures have two needle arms, each about 5-10 μm long and about 0.5 μm in diameter, meeting at an obtuse angle. At the junction of the arms, there is a small membrane-bound `knob', about 1 μm in diameter, which may be continuous with the coelomic peritoneum. The numbers of `crystals' per individual worm are estimated at 100-400 per body segment, or well over 2 × 10^sup 3^ in an adult worm. `Crystals' are found: throughout the length of the worms, in all individuals of species in which `crystals' occur, and over the range of environmental conditions where these species are found in Bermuda. Simple digestions with hypochlorite, weak and dilute acids, and staining with nuclear and cytoplasmic stains indicate that the composition of the knob is organic and the arms inorganic. The fluorescent tracer Calcein (Sigma) was not incorporated into any structures during a 24-h bath incubation of living worms, and the `crystals' do not show birefringence when viewed between crossed polarizing filters. These last two results do not support an hypothesis that these are calcium carbonate `crystals'. Geographically, the crystal-like structures are widespread, and have also been observed in a species of immature (unidentified) marine tubificid from Rottnest Island, Western Australia.[PUBLICATION ABSTRACT] |
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ISSN: | 0018-8158 1573-5117 |
DOI: | 10.1023/A:1013195306432 |