| Intro | | Search taxa | | Taxon tree | | Search literature | | Taxon match | | Homonyms | | Statistics | | Webservice | | Manual | | FAQ | | LifeWatch | | Download | | Log in |
IRMNG taxon detailsTreptichnus Miller, 1889 †
Plangtichnus Miller, 1889 † · unaccepted
fossil only
N. Amer. Geol. Pal.
page(s): 581 [details]
Taxonomic remark Ichnogenus (fossil burrows), with one species T. pedum an important stratigraphic marker for the base of the Cambrian...
Taxonomic remark Ichnogenus (fossil burrows), with one species T. pedum an important stratigraphic marker for the base of the Cambrian period. According to Vannier et al., 2010, possibly made by priapulid (or priapulid-like) worms. According to other sources, some traces attributed to Treptichnus in later epochs could have been made by Coleoptera or by Dipteran larvae. Listed as Col[eoptera] in Nomen. Zool. [details]
IRMNG (2021). Treptichnus Miller, 1889 †. Accessed at: https://www.irmng.org/aphia.php?p=taxdetails&id=1131923 on 2024-04-20
original description
N. Amer. Geol. Pal.
page(s): 581 [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/ [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] current name source Vannier, J.; Calandra, I.; Gaillard, C.; Żylińska, A. (2010). Priapulid worms: pioneer horizontal burrowers at the Precambrian-Cambrian boundary. <em>Geology.</em> 38(8): 711-714., available online at https://doi.org/10.1130/g30829.1 [details] extant flag source NZ cross ref or inferred from publ. title [details] original description (of Plangtichnus Miller, 1889 †) N. Amer. Geol. Pal. page(s): 580 [details] From other sources
Taxonomic remark Ichnogenus (fossil burrows), with one species T. pedum an important stratigraphic marker for the base of the Cambrian period. According to Vannier et al., 2010, possibly made by priapulid (or priapulid-like) worms. According to other sources, some traces attributed to Treptichnus in later epochs could have been made by Coleoptera or by Dipteran larvae. Listed as Col[eoptera] in Nomen. Zool. [details]
|
