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Glyptodynomene ✝

Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)4646606https://www.gbif.org/species/4646606
PaleoBioDB ID (PBDB)22454https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=22454
Rankgenus
Taxonomy (GBIF)Life : Animalia : Arthropoda : Malacostraca : Decapoda : Necrocarcinidae : Glyptodynomene
Taxonomy (PBDB)Life : Animalia : Arthropoda : Malacostraca : Decapoda : Glyptodynomene
Taxonomic Status (GBIF)accepted
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
-ThoracotremataGuinot 1977
superfamilyGrapsoideaMacLeay 1838
genusGlyptodynomeneVan Straelen 1944
Scientific NameGlyptodynomene Van Straelen, 1944
Opinions (PBDB)
NameRankOpinionEvidenceAuthor
Glyptodynomenegenusbelongs to Decapodasecond handSepkoski, 2002
Glyptodynomenegenusbelongs to Paranecrocarcininaestated without evidenceFraaije et al., 2008
Glyptodynomenegenusbelongs to Grapsoideastated without evidenceSchweitzer et al., 2010
Status (PBDB)extinct
Taxon Size (PBDB)3
First Recorded Appearance70.6 - 66.0 Ma
Late/Upper Cretaceous
Last Recorded Appearance70.6 - 66.0 Ma
Late/Upper Cretaceous
Motilityactively mobile (based on Malacostraca)
Visionwell-developed (based on Malacostraca)
Dietcarnivore (based on Decapoda)
Taphonomychitin (based on Malacostraca)
Primary Reference (PBDB)J. J. Sepkoski, Jr. 2002. A compendium of fossil marine animal genera. Bulletins of American Paleontology 363:1-560

Fossil Distribution

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Glyptodynomene alsasuensis ✝
species		accepted (GBIF)
listed (PBDB)
Glyptodynomene inornata ✝
species		accepted (GBIF)
listed (PBDB)		270.6 Ma
Late/Upper Cretaceous		70.6 Ma
Late/Upper Cretaceous

Synonymy List

YearName and Author
1944Glyptodynomene Van Straelen
2002Glyptodynomene Sepkoski, Jr.
2003Glyptodynomene Schweitzer et al. p. 18
2008Glyptodynomene Fraaije et al. p. 201
2010Glyptodynomene Schweitzer et al.
2014Glyptodynomene Karasawa et al. p. 233

References

Sepkoski, Jr. J. J. (2002) A compendium of fossil marine animal genera, Bulletins of American Paleontology 363, 1-560
Schweitzer C. E., Feldmann R. M., et al (2003) Cretaceous and Eocene Decapod Crustaceans from Southern Vancouver Island, British Columbia Canada, NRC Research Press, 1-66
Fraaije R. H. B., van Bakel B. W. M., et al (2008) New decapold crustaceans (Anomura, Brachyura) from mid-Cretaceous reefal deposits at Monte Orobe (Navarra, northern Spain), and comments on related type-Maastrichian materia, Sciences De La Terre 78, 193-208
Schweitzer C. E., Feldmann R. M., et al (2010) Systematic list of fossil decapod crustacean species, Crustaceana Monographs 10, 1-222
Karasawa H., Schweitzer C. E., et al (2014) Phylongeny and Classification of Raninoida (Decapoda: Brachyura), Journal of Crustacean Biology 34 2, 216-272
De Grave, S., Pentcheff, N.D., Ahyong, S.T., Chan, T.-Y., Crandall, K.A., Dworschak, P.C., Felder, D.L., Feldmann, R.M., Fransen, C.H.J.M., Goulding, L.Y.D., Lemaitre, R., Low, M.E.Y., Martin, J.W., Ng, P.K.L., Schweitzer, C.E., Tan, S.H., Tshudy, D. & Wetzer, R. (2009). A classification of living and fossil genera of decapod crustaceans. Raffles Bulletin of Zoology. supplement 21: 1-109. - via The Interim Register of Marine and Nonmarine Genera
Sepkoski, J. J., Jr. (2002). A compendium of fossil marine animal genera. Bulletins of American Paleontology. 363, 1-560. - 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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