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Acanthoparypha

Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)4633433https://www.gbif.org/species/4633433
PaleoBioDB ID (PBDB)21422https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=21422
Rankgenus
Taxonomy (GBIF,PBDB)Life : Animalia : Arthropoda : Trilobita : Phacopida : Cheiruridae : Acanthoparypha
Taxonomic Status (GBIF)accepted
Classification
(PBDB,GBIF)
RankNameAuthor
-Eukaryota
-OpisthokontaCavalier-Smith 1987
kingdomAnimalia
-Bilateria
-EubilateriaAx 1987
-ProtostomiaGrobben 1908
-Ecdysozoa
-Panarthropoda
phylumArthropodaLatreille 1829
subphylumMandibulata
classTrilobitaWalch 1771
orderPhacopidaSalter 1864
suborderCheirurinaHarrington and Leanza 1957
familyCheiruridaeHawle and Corda 1847
subfamilyAcanthoparyphinaeWhittington and Evitt 1953
genusAcanthoparyphaWhittington & Evitt 1954
Scientific NameAcanthoparypha Whittington & Evitt, 1954
Name Published InMem. Geol. Soc. Amer., No. 59
Opinions (PBDB)
NameRankOpinionEvidenceAuthor
Acanthoparyphagenusbelongs to Acanthoparyphinaestated with evidenceWhittington and Evitt, 1953
Acanthoparyphagenusbelongs to Cheiruridaestated without evidenceJell and Adrain, 2002
Acanthoparyphagenusbelongs to Phacopidasecond handSepkoski, 2002
Status (PBDB)extinct
Taxon Size (PBDB)7
First Recorded Appearance472 - 464 Ma
Ordovician
Last Recorded Appearance458 - 450 Ma
Late/Upper Ordovician
Environmentmarine (based on Trilobita)
Motilityfast-moving (based on Trilobita)
Visionwell-developed
Dietcarnivore (based on Cheiruridae)
Ontogenymolting,addition of parts (based on Trilobita)
Ecospace CommentsBODY SIZE: Data from Harrington et al. (1959).
Taphonomymajor spines
Primary Reference (PBDB)H. B. Whittington and W.R., I.I. Evitt. 1953. Silicified Middle Ordovician trilobites. Geological Society of America Memoir 59:1-139

Fossil Distribution

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Acanthoparypha chiropyga
species
accepted (GBIF)
listed (PBDB)
1461 Ma
Middle Ordovician
461 Ma
Middle Ordovician
Acanthoparypha echinoderma
species
accepted (GBIF)
listed (PBDB)
5468 Ma
Middle Ordovician
468 Ma
Middle Ordovician
Acanthoparypha evitti
species
accepted (GBIF)
listed (PBDB)
8472 Ma
Early/Lower Ordovician
468 Ma
Middle Ordovician
Acanthoparypha goniopyga
species
accepted (GBIF)
listed (PBDB)
4461 Ma
Middle Ordovician
461 Ma
Middle Ordovician
Acanthoparypha perforata
species
accepted (GBIF)
listed (PBDB)
5461 Ma
Middle Ordovician
461 Ma
Middle Ordovician
Acanthoparypha subcircularis
species
accepted (GBIF)
listed (PBDB)
2461 Ma
Middle Ordovician
461 Ma
Middle Ordovician

Synonymy List

YearName and Author
1953Acanthoparypha Whittington and Evitt pp. 72-73
2002Acanthoparypha Jell and Adrain p. 336
2002Acanthoparypha Sepkoski, Jr.

References

Whittington H. B., Evitt W.R., II. (1953) Silicified Middle Ordovician trilobites, Geological Society of America Memoir 59, 1-139
Jell P. A., Adrain J. M. (2002) Available generic names for trilobites, Memoirs of the Queensland Museum 48 2, 331-553
Sepkoski, Jr. J. J. (2002) A compendium of fossil marine animal genera, Bulletins of American Paleontology 363, 1-560
Nomenclator Zoologicus. A list of the names of genera and subgenera in zoology from the tenth edition of Linnaeus, 1758 to the end of 2004. Digitised by uBio from vols. 1-9 of Neave (ed.), 1939-1996 plus supplementary digital-only volume. http://ubio.org/NomenclatorZoologicus (as at 2006). - via The Interim Register of Marine and Nonmarine Genera
SN2000: Brands, S. J. (compiler) 1989-2005. Systema Naturae 2000. Amsterdam, The Netherlands (2006 version). Available online at http://sn2000.taxonomy.nl/. - via The Interim Register of Marine and Nonmarine Genera
extinct group - via The Interim Register of Marine and Nonmarine Genera
Mem. Geol. Soc. Amer., No. 59 - via The Interim Register of Marine and Nonmarine Genera
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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