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Chasmocarcininae

Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)Not linked to a GBIF record.
PaleoBioDB ID (PBDB)225772https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=225772
Ranksubfamily (PBDB)
Taxonomy (PBDB)Life : Animalia : Arthropoda : Malacostraca : Decapoda : Chasmocarcinidae : Chasmocarcininae
Classification
(PBDB,GBIF)
RankNameAuthor
-Eukaryota
-OpisthokontaCavalier-Smith 1987
kingdomAnimalia
-Bilateria
-EubilateriaAx 1987
-ProtostomiaGrobben 1908
-Ecdysozoa
-Panarthropoda
phylumArthropodaLatreille 1829
subphylumMandibulata
-Pancrustacea
subphylumCrustaceaBrünnich 1772
classMalacostracaLatreille 1802
superorderEucaridaCalman 1904
orderDecapodaLatreille 1802
-MeiuraSaint Laurent 1980
infraorderBrachyuraLatreille 1802
-Eubrachyurade Saint Laurent 1980
-HeterotremataGuinot 1977
superfamilyGoneplacoideaMacLeay 1838
familyChasmocarcinidaeSerene 1964
subfamilyChasmocarcininaeSerene 1964
Opinions (PBDB)
NameRankOpinionEvidenceAuthor
Chasmocarcininaesubfamilybelongs to Goneplacidaestated without evidenceFeldmann and Wilson, 1988
Chasmocarcininaesubfamilybelongs to Chasmocarcinidaestated without evidenceSchweitzer et al., 2010
Status (PBDB)extant
Taxon Size (PBDB)28
Extant Size (PBDB)2 (7.1%)
First Recorded Appearance56.0 - 41.3 Ma
Eocene
Motilityactively mobile (based on Malacostraca)
Visionwell-developed (based on Malacostraca)
Dietcarnivore (based on Decapoda)
Taphonomychitin (based on Malacostraca)
Primary Reference (PBDB)C. E. Schweitzer, R. M. Feldmann, and A. Garassino, H. Karasawa, and G. Schweigert. 2010. Systematic list of fossil decapod crustacean species. Crustaceana Monographs 10:1-222

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Chasmocarcinus
genus
accepted (GBIF)
listed (PBDB)
356.0 Ma
Paleocene
0 Ma
Extant
Collinsius
genus
accepted (GBIF)
listed (PBDB)
1033.9 Ma
Oligocene
33.9 Ma
Oligocene
Falconoplax
genus
accepted (GBIF)
listed (PBDB)
255.8 Ma
Eocene
23.0 Ma
Miocene
Gillcarcinus
genus
accepted (GBIF)
listed (PBDB)
247.8 Ma
Eocene
47.8 Ma
Eocene
Mioplax
genus
accepted (GBIF)
listed (PBDB)
Orthakrolophos
genus
accepted (GBIF)
listed (PBDB)
1147.8 Ma
Eocene
5.33 Ma
Miocene

Synonymy List

YearName and Author
1964Chasmocarcininae Serene
1988Chasmocarcininae Feldmann and Wilson p. 484
2001Chasmocarcininae Schweitzer and Feldmann p. 338
2003Chasmocarcininae Collins et al. p. 218
2003Chasmocarcininae Karasawa and Kato p. 142
2004Chasmocarcininae Schweitzer et al. p. 102
2004Chasmocarcininae Schweitzer and Karasawa p. 73
2010Chasmocarcininae Schweitzer et al.
2017Chasmocarcininae Luque et al. p. 18

References

Schweitzer C. E., Feldmann R. M., et al (2010) Systematic list of fossil decapod crustacean species, Crustaceana Monographs 10, 1-222
Feldmann R. M., Wilson M. T. (1988) Eocene decapod crustaceans from Antartica, Geological Society of America, Memoir 169, 465-488
Schweitzer C. E., Feldmann R. M. (2001) Differentiation of the fossil Hexapodidae Miers, 1886 (Decapoda: Brachyura) from similar forms, Journal of Paleontology 75 2, 330-345
Collins J. S. H., Lee C., et al (2003) Miocene and Pleistocene Crabs (Crustacea, Decapoda) from Sabah and Sarawak, Journal of Systematic Palaentology 1, 187-226
Schweitzer C. E., Feldmann R. M., et al (2004) New Decapoda (Crustacea) from the middle and late Eocene of Pakistan and a revision of Lobonotus A. Milne Edwards, 1864, University of Michigan Contributions from the Musuem of Paleontology 31 4, 89-118
Schweitzer C. E., Karasawa H. (2004) Revision of Amydrocarcinus and Palaeograpsus (Decapoda: Brachyura: Xanthoidea) with definition of three new genera, Paleontological Research 8 1, 71-86
Luque J., Schweitzer C. E., et al (2017) Checklist of fossil decapod crustaceans from tropical America. Part I: Anomura and Brachyura, Nauplius 25, e2017025 doi:10.1590/2358-2936e2017025
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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