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Jainemys pisdurensis
Taxonomy
Carteremys pisdurensis was named by Jain (1977). Its type specimen is ISI R200, a partial skull, and it is a 3D body fossil. Its type locality is Pisdura Hill (sandstone), which is in a Maastrichtian terrestrial claystone/sandstone in the Lameta Formation of India.
It was recombined as Shweboemys pisdurensis by Jain (1986); it was recombined as Jainemys pisdurensis by Joyce and Bandyopadhyay (2020).
It was recombined as Shweboemys pisdurensis by Jain (1986); it was recombined as Jainemys pisdurensis by Joyce and Bandyopadhyay (2020).
Synonymy list
Year | Name and author |
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1977 | Carteremys pisdurensis Jain |
1986 | Shweboemys pisdurensis Jain |
2020 | Jainemys pisdurensis Joyce and Bandyopadhyay |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Jainemys pisdurensis Jain 1977
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Diagnosis
Reference | Diagnosis | |
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W. G. Joyce and S. Bandyopadhyay 2020 | Jainemys pisdurensis furthermore differs from podocnemidids by lacking an interorbital groove and an interparietal scale. Among kurmademydines, Jainemys pisdurensis can be differentiated from Kurmademys kallamedensis by having a more elongate skull, a greater posterior extension of the frontals, more anteroposteriorly elongate palatines that only contribute minorly to the triturating surfaces, remnants of the vomer between the maxillae, presence of a prootic and opisthotic contact in the upper temporal fossa, which hinders contact between the quadrate and supraoccipital, a more equilaterally pentagonal basisphenoid, and a much smaller fossa pterygoidea and from Sankuchemys sethnai by having a more elongate skull, a greater posterior extension of the frontals, presence of a prootic and opisthotic contact in the upper temporal fossa, which hinders a contact between the quadrate and supraoccipital, broader triturating surfaces, by lacking a posterior vomeral process that contacts the palatines, and by having more expanded palatines, a more equally sided pentagonal basisphenoid, and a shorter basioccipital. |
Measurements
No measurements are available
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Source: subo = suborder, c = class, subp = subphylum | |||||
References: Hendy et al. 2009, Carroll 1988, Uetz 2005 |
Age range: Maastrichtian or 72.10000 to 66.00000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Maastrichtian | India (Maharashtra) | Carteremys pisdurensis (type locality: 60397) |