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| '''''Tardisia''''' is |
'''''Tardisia''''' is an extinct genus of ] arthropod known from the upper Carboniferous ] in northern ]. It is the youngest known member of the ] outside of the ], at almost 100 million years younger than the next youngest in the ] and ].<ref name=tardisia>{{cite journal |last1=McCoy |first1=Victoria E. |last2=Herrera |first2=Fabiany |last3=Wittry |first3=Jack |last4=Mayer |first4=Paul |last5=Lamsdell |first5=James C. |title=A possible vicissicaudatan arthropod from the Late Carboniferous Mazon Creek Lagerstätte |journal=Geological Magazine |date=2025 |volume=162 |doi=10.1017/S001675682400044X}}</ref> | ||
| == Description == | == Description == | ||
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| == Etymology == | == Etymology == | ||
| ''Tardisia'' is named after the TARDIS from the TV show '']'', in reference to the large stratigraphic gap between it and the next youngest vicissicaudatans. The specific name ''broedeae'' honours Irene Broede, a Mazon Creek fossil collector.<ref name=tardisia/> | ''Tardisia'' is named after the ] from the TV show '']'', in reference to the large stratigraphic gap between it and the next youngest vicissicaudatans. The specific name ''broedeae'' honours Irene Broede, a Mazon Creek fossil collector.<ref name=tardisia/> | ||
| == References == | == References == | ||
Revision as of 14:19, 14 January 2025
Extinct genus of artiopod
| Tardisia Temporal range: Moscovian PreꞒ Ꞓ O S D C P T J K Pg N | |
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| Fossils of Tardisia | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| (unranked): | †Artiopoda |
| (unranked): | †Vicissicaudata |
| Genus: | †Tardisia McCoy et al, 2025 |
| Species: | †T. broedeae |
| Binomial name | |
| †Tardisia broedeae McCoy et al, 2025 | |
Tardisia is an extinct genus of vicissicaudatan arthropod known from the upper Carboniferous Mazon Creek fossil beds in northern Illinois. It is the youngest known member of the artiopoda outside of the trilobites, at almost 100 million years younger than the next youngest in the Hunsrück Slate and Severnaya Zemlya Formation.
Description
Tardisia lacks eyes, with a head shield (the frontal end is lost on the holotype, but according to descriptions and the paratype it was likely sub-semicircular) smaller than the first tergite. The trunk comprises seven tergites in the thorax, four with overlapping margins, and a postabdomen composed of the eighth segment, which lacks wide pleurae and instead bears a pair of caudal appendages. The trunk’s width slightly increases with the widest section (roughly 6 6 mm (0.24 in) wide) being the third tergite, afterwards steadily decreasing towards the posterior. Each segment is around 1 mm (0.039 in) long. The postabdomen bears a shield-shaped telson, slightly wider than long, alongside two caudal appendages at least 6 mm (0.24 in) long and narrowing towards their tips. These appendages have bulbous anterior ends and were likely heavily sclerotized due to them being the only appendages preserved. It is unclear whether they were movable in life.
Classification
| Artiopoda |
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Tardisia is likely a vicissicaudatan, due to sharing features such as the number of trunk segments and the postabdomen ending in caudal appendages. While it is unusual in lacking eyes, many cheloniellids also lack eyes, such as Duslia and Neostrabops. Tardisia, while closest resembling cheloniellids, has some key differences from this group. Its postabdomen and telson are much larger, alongside lacking a well-defined axis. In addition, the tergopleurae of cheloniellids have an unusual radial arrangement that Tardisia lacks. Because of this, Tardisia is likely the sister group of cheloniellids.
Etymology
Tardisia is named after the TARDIS from the TV show Doctor Who, in reference to the large stratigraphic gap between it and the next youngest vicissicaudatans. The specific name broedeae honours Irene Broede, a Mazon Creek fossil collector.
References
- ^ McCoy, Victoria E.; Herrera, Fabiany; Wittry, Jack; Mayer, Paul; Lamsdell, James C. (2025). "A possible vicissicaudatan arthropod from the Late Carboniferous Mazon Creek Lagerstätte". Geological Magazine. 162. doi:10.1017/S001675682400044X.