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Paraonychoplecia inversa

Strophomenata - Orthotetida - Triplesiidae

Taxonomy
Paraonychoplecia inversa was named by Percival (1991). It is a 3D body fossil. Its type locality is L137. Quondong, Bowan Park, which is in an Eastonian offshore shelf limestone in the Daylesford Limestone Formation of Australia. It is the type species of Paraonychoplecia.

Synonymy list
YearName and author
1991Paraonychoplecia inversa Percival

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Protostomia
Spiralia
superphylumLophotrochozoa
Lophophorata
PanbrachiopodaCarlson and Cohen 2020
phylumBrachiopodaCuvier 1805
RankNameAuthor
subphylumRhynchonelliformeaWilliams et al. 1996
classStrophomenataWilliams et al 1996
orderOrthotetidaWaagen 1884
suborderTriplesiidinaMoore 1952
superfamilyTriplesioideaSchuchert 1913
familyTriplesiidaeSchuchert 1913
genusParaonychoplecia
speciesinversa

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.

Paraonychoplecia inversa Percival 1991
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
Composition: low Mg calcitep
Environment: marineuc
Locomotion: stationaryp
Attached: yesp
Life habit: low-level epifaunalp
Diet: suspension feederp
Vision: blindc
Created: 2010-02-15 05:25:57
Modified: 2010-02-15 07:25:57
Source: c = class, p = phylum, uc = unranked clade
References: Nesnidal et al. 2013, Aberhan et al. 2004

Age range: Eastonian or 452.70000 to 449.50000 Ma

Collections (3 total)


Time interval Ma Country or state Original ID and collection number
Eastonian452.7 - 449.5Australia (New South Wales) Paraonychoplecia inversa (2745 type locality: 2749 166850)