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BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems

Macropetalichthyidae

Description

Petalichthyida is an extinct order of small, flattened placoderm fish. They are typified by their splayed pectoral fins, exaggerated lateral spines, flattened bodies, and numerous tubercles that decorated all of the plates and scales of their armor. They reached a peak in diversity during the Early Devonian and were found throughout the world, particularly in Europe (especially in Germany), North America, Asia, South America, and Australia. The petalichthids Lunaspis and Wijdeaspis are among the best known. The earliest and most primitive known petalichthyid is Diandongpetalichthys, which is from earliest Devonian-aged strata of Yunnan. The presence of Diandongpetalichthys, along with other primitive petalichthyids including Neopetalichthys and Quasipetalichthys, and more advanced petalichthyids, suggest that the order may have arisen in China, possibly during the late Silurian.


Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)3240794https://www.gbif.org/species/3240794
Rankfamily
Taxonomy (GBIF)Life : Animalia : Chordata : Macropetalichthyidae
Taxonomic Status (GBIF)accepted
Classification
(GBIF)
RankNameAuthor
familyMacropetalichthyidae
Scientific NameMacropetalichthyidae
Wikipediahttps://en.wikipedia.org/wiki/Macropetalichthyidae

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Lunaspis
genus
accepted (GBIF)No associated record in PBDB

References

Benton, M.J. (ed). (1993). The Fossil Record 2. Chapman & Hall, London, 845 pp. - via The Interim Register of Marine and Nonmarine Genera
Museum Victoria KEmu database (Oct 2006) - 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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