Extra-lobal and complex dimorphic features in Middle Devonian palaeocopine ostracods

Becker, Gerhard; Braun, Willi K.

doi:10.1007/978-1-4020-6418-0_12

Cited by 1 publication

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References 12 publications

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“…Matern, 1929;Harris, 1931Harris, , 1957Bassler & Kellett, 1934;Keenan, 1951;Levinson, 1950Levinson, , 1951Levinson, , 1961Egorov, 1954;Jaanusson, 1957;Rome & Goreux, 1960;Adamczak, 1961;Jones, 1962;Zagora, 1966;Schallreuter, 1968Schallreuter, , 1977Schallreuter, , 1987Schallreuter, , 1995Warshauer & Berdan, 1982;Abushik, 1990;Whatley et al, 1993;Becker et al, 2004;Hoare & Merrill, 2004;Becker & Braun, 2007). Adamczak (1961) established the new suborder Eridostraca for such multilayered taxa as the Eridoconchinae Henningsmoen, 1953.…”

Section: Assignment Of Eridostracinesmentioning

confidence: 97%

Morphology and affinities of Eridostracina: Palaeozoic ostracods with moult retention

Olempska

2011

Hydrobiologia

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Ostracods are by far the most abundant living group of arthropods in the fossil record. Traditionally, eridostracines were classified as members of the Class Ostracoda. They have also been considered to represent extinct marine spinicaudatan (conchostracan) branchiopods. The ostracod affinity of the Eridostracina is evident in a number of features such as the muscle scars pattern, the hinge structure, the presence of an adductorial sulcus reflected as a ridge on the internal surface and the separation at the dorsal margin of successive valves. The eridostracines might be a polyphyletic group, containing aberrant representatives of ostracods, with ancestors probably among the conchoprimitid, leperditellid and beyrichioidean ostracod species. The Eridostracina represent an extinct group of small marine crustaceans with a multilayer structure of the calcified carapace, formed through the retention of unshed moults during the growth process. Details of the morphology of the eridostracine Cryptophyllus socialis from the Upper Devonian of Russia are reconstructed using the process of exfoliation of successive exuviae. 'Double-sided' hingement structures were found in the accumulated exuviae. It is suggested that the main function of these structures was the strengthening of the connection between the accumulated valves. The hingement of Cryptophyllus represents a vestigial structure, which has lost its original function as a pivot, a role documented in the ancestors of that genus. Tubular structures were found attached to the internal side of the calcite layer. It is suggested that they also represent vestigial pore canals, having lost their original function as sensory receptors. External surfaces of the attached exuviae bear imprints of the tubular structures of the overlying exuviae. These imprints originated probably due to the strong pressure of the new cuticle against the old one, during the very short moulting time. During this process, the freshly formed cuticle was at its final size, but still soft and non-calcified. A number of three-dimensionally preserved cell-like structures were recovered inside the interlayer chambers.

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Section: Assignment Of Eridostracinesmentioning

confidence: 97%

Morphology and affinities of Eridostracina: Palaeozoic ostracods with moult retention

Olempska

2011

Hydrobiologia

View full text Add to dashboard Cite

show abstract

Extra-lobal and complex dimorphic features in Middle Devonian palaeocopine ostracods

Cited by 1 publication

References 12 publications

Morphology and affinities of Eridostracina: Palaeozoic ostracods with moult retention

Morphology and affinities of Eridostracina: Palaeozoic ostracods with moult retention

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