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Blastozoa

Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)Not linked to a GBIF record.
PaleoBioDB ID (PBDB)120078https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=120078
Ranksubphylum (PBDB)
Taxonomy (PBDB)Life : Animalia : Echinodermata : Blastozoa
Classification
(PBDB,GBIF)
RankNameAuthor
-Eukaryota
-OpisthokontaCavalier-Smith 1987
kingdomAnimalia
-TriploblasticaLankester 1877
-NephrozoaJondelius et al. 2002
-DeuterostomiaGrobben 1908
-Ambulacraria
phylumEchinodermataKlein 1754
subphylumBlastozoaSprinkle 1973
Opinions (PBDB)
NameRankOpinionEvidenceAuthor
Blastozoasubphylumbelongs to Echinodermatastated with evidenceBockelie, 1984
Blastozoasubphylumbelongs to Echinodermatastated without evidenceZhao et al., 2008
Status (PBDB)extant
Taxon Size (PBDB)776
Extant Size (PBDB)6 (0.77%)
First Recorded Appearance530 - 516 Ma
Cambrian
Environmentmarine (based on Echinodermata)
Motilitystationary (based on Blastozoa)
Dietsuspension feeder (based on Blastozoa)
Reproductiondispersal=water,planktonic (based on Echinodermata)
Ontogenyaccretion,addition of parts (based on Echinodermata)
Ecospace CommentsLIFE HISTORY: Erect, non-motile attached/unattached, suspension feeder according to Bambach et al (2007).
Taphonomyhigh Mg calcite (based on Echinodermata)
Primary Reference (PBDB)Y. Zhao, R. L. Parsley, and J. Peng. 2008. Basal Middle Cambrian short-stalked eorinoids from the Kali Biota: Guizhou Province, China. Journal of Paleontology 82(2):415-422

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Coronoidea
class
listed (PBDB)83466 Ma
Middle Ordovician
433 Ma
Silurian
Eocrinoidea
class
listed (PBDB)224530 Ma
Cambrian
433 Ma
Silurian
Paracrinoidea
class
listed (PBDB)116468 Ma
Middle Ordovician
458 Ma
Late/Upper Ordovician
Rhombifera
class
listed (PBDB)613513 Ma
Cambrian
0 Ma
Extant
Soluta
class
listed (PBDB)49516 Ma
Cambrian
419 Ma
Early/Lower Devonian
Blastoidea
subclass
listed (PBDB)479461 Ma
Middle Ordovician
252 Ma
Permian
Parablastoidea
order
listed (PBDB)41479 Ma
Early/Lower Ordovician
458 Ma
Middle Ordovician
Rhombifera
order
listed (PBDB)136479 Ma
Early/Lower Ordovician
427 Ma
Silurian
Felbabkacystidae
family
listed (PBDB)2513 Ma
Cambrian
513 Ma
Cambrian
Lepidocystidae
family
listed (PBDB)6516 Ma
Cambrian
513 Ma
Cambrian

Synonymy List

YearName and Author
1973Blastozoa Sprinkle
1984Blastozoa Bockelie
2006Blastozoa Parsley and Zhao p. 1063
2008Blastozoa Zhao et al. p. 419
2008Blastozoa Zuykov et al.
2014Blastozoa Noailles et al. p. 459
2018Blastozoa Lefebvre and Lerosey-Aubril

References

Zhao Y., Parsley R. L., et al (2008) Basal Middle Cambrian short-stalked eorinoids from the Kali Biota: Guizhou Province, China, Journal of Paleontology 82 2, 415-422
Bockelie J. F. (1984) The Diploporita of the Oslo region, Norway, Palaeontology 27 1, 1-68
Parsley R. L., Zhao Y.-L. (2006) Long stalked eocrinoids in the basal Middle Cambrian Kaili Biota, Taijiang County, Guizhou Province, China, Journal of Paleontology 80 6, 1058-1071
Zuykov M. A., Terentiev S. S., et al (2008) New endemic brachiopod and echinoderm genera from the Upper Ordovician of the St. Petersburg region, northwestern Russia, Geological Society of Sweden, Geologiska Föreningen 130 2, 87-93
Noailles F., Lefebvre B., et al (2014) A probable case of heterochrony in the solutan Dendrocystites Barrande, 1887 (Echinodermata: Blastozoa) from the Upper Ordovician of the Prague Basin (Czech Republic) and a revision of the family Dendrocystitidae Bassler, 1938, Bulletin of Geosciences 89 3, 451-476 doi:10.3140/bull.geosci.1475
Lefebvre B., Lerosey-Aubril R. (2018) Laurentian origin of solutan echinoderms: new evidence from the Guzhangian (Cambrian Series 3) Weeks Formation of Utah, USA, Geological Magazine 155 5, 1190-1204 doi:10.1017/S0016756817000152
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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