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IRMNG name detailsCalciroda Meyer, 1952 †
1435897 (urn:lsid:irmng.org:taxname:1435897)
uncertain > nomen dubium (composite trace fossil)
Genus
marine,
fossil only
Neue Jb. Geol. Paleont., B
page(s): 455 [details]
Taxonomic remark From Wisshak et al., 2019: Calciroda Mayer, 1952 and its type ichnospecies C. kraichgoviae Mayer, 1952 consists of...
Taxonomic remark From Wisshak et al., 2019: Calciroda Mayer, 1952 and its type ichnospecies C. kraichgoviae Mayer, 1952 consists of ‘branched, horizontal tunnels running along the surface of organism hard parts, sometimes going vertically into the depth’ [original diagnosis, translated]. No holotype was designated, but the fgured specimens indicate an overlapping or cross-cutting relationship of individual tunnels instead of true branching, in addition to unbranched specimens. Plewes (1996: pl. 13, Fig. 5) studied Mayer’s type material and confrmed that ‘…both branching points and avoidance by tunnels can be seen…’; she regarded Calciroda as junior synonym of Talpina von Hagenow, 1840. In comparison with the recently rediscovered type material of Talpina and its revision (Wisshak et al. 2017: Fig. 2.1), the branched specimens of the dubious (because composite) and partly eroded trace fossil C. kraichgoviae can be assigned to Talpina ramosa von Hagenow, 1840, whereas the unbranched specimens belong to Trypanites solitarius (von Hagenow, 1840). [details]
IRMNG (2023). Calciroda Meyer, 1952 †. Accessed at: https://www.irmng.org/aphia.php?p=taxdetails&id=1435897 on 2024-05-15
Date action by
original description
Neue Jb. Geol. Paleont., B
page(s): 455 [details] basis of record Neave, S. A. and successors. (1939-2004). Nomenclator Zoologicus, vols. 1-10 online. [developed by uBio, hosted online at MBLWHOI Library]. , available online at http://ubio.org/NomenclatorZoologicus/ note: as Conodonta [details] source of synonymy Wisshak, M.; Knaust, D.; Bertling, M. (2019). Bioerosion ichnotaxa: review and annotated list. <em>Facies.</em> 65: 24., available online at https://doi.org/10.1007/s10347-019-0561-8 [details] status source Wisshak, M.; Knaust, D.; Bertling, M. (2019). Bioerosion ichnotaxa: review and annotated list. <em>Facies.</em> 65: 24., available online at https://doi.org/10.1007/s10347-019-0561-8 [details] name verified source Neave, S. A. and successors. (1939-2004). Nomenclator Zoologicus, vols. 1-10 online. [developed by uBio, hosted online at MBLWHOI Library]. , available online at http://ubio.org/NomenclatorZoologicus/ [details] extant flag source NZ cross ref or inferred from publ. title [details] From other sources
Taxonomic remark From Wisshak et al., 2019: Calciroda Mayer, 1952 and its type ichnospecies C. kraichgoviae Mayer, 1952 consists of ‘branched, horizontal tunnels running along the surface of organism hard parts, sometimes going vertically into the depth’ [original diagnosis, translated]. No holotype was designated, but the fgured specimens indicate an overlapping or cross-cutting relationship of individual tunnels instead of true branching, in addition to unbranched specimens. Plewes (1996: pl. 13, Fig. 5) studied Mayer’s type material and confrmed that ‘…both branching points and avoidance by tunnels can be seen…’; she regarded Calciroda as junior synonym of Talpina von Hagenow, 1840. In comparison with the recently rediscovered type material of Talpina and its revision (Wisshak et al. 2017: Fig. 2.1), the branched specimens of the dubious (because composite) and partly eroded trace fossil C. kraichgoviae can be assigned to Talpina ramosa von Hagenow, 1840, whereas the unbranched specimens belong to Trypanites solitarius (von Hagenow, 1840). [details]
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