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The Ostracod Cyprideis torosa develops nodes on its calcified carapace in brackish waters and is therefore widely used in paleontology as a marker for lower saline waters. The formation of nodes in lower saline waters was investigated with SEM and TEM analyses and micro-cryoscopic measurements of the inner osmoregulation. Noding is considered a failure in osmoregulation, which causes the pillars connecting the inner and outer epidermal cell layer to rupture during the molting process. As a result, the still flexible shell develops protrusions, which then persist as nodes after subsequent calcification.
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Tom
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19--24
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Bibliogr.18 poz.
Bibliografia
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- Triebel E. 1941. Fossile Arten der Ostracoden-Gattung Paracyprideis Klie. Senckenbergiana 23, 153–164.
- van Harten D. 2000. Variable noding in Cyprideis torosa (Ostracoda, Crustacea): an overview, experimental results and a model from catastrophe theory. Hydrobiologia 419, 131–139.
- Vesper B. 1972. Zum Problem der Buckelbildung bei Cyprideis torosa (Jones, 1850) (Crustacea, Ostracoda, Cytheridae). Mitteilungen des hamburgischen zoologischen Museums und Instituts 68, 79–94.
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Bibliografia
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bwmeta1.element.baztech-article-BPW9-0007-0022