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Opetiosaurus

species of reptile

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 15, 2025
Entity authorityQ45269867
Source-derived summary

Opetiosaurus is an extinct genus of Late Cretaceous marine or semiaquatic lizard classified as part of the family Aigialosauridae within the Mosasauroidea. Exclusively found in deposits of Cenomanian age near Hvar, Croatia, the genus contain one valid species, O. bucchichi. It was a small reptile measuring 1 metre (3.3 ft) long.

The genus was diagnosed as congenetic with Aigialosaurus by Dutchak and Caldwell (2009), being re-diagnosed as "Aigialosaurus bucchichi" and only separated by some minor anatomical differences between specimens of the two species. Madzia & Cau (2017) show that the two species are not necessarily more closely related to each other than either is to more derived mosasauroids, suggesting not only that Opetiosaurus is a valid genus, but also calling the validity of the Aigialosauridae as a monophyletic group into question.

Editorial summary

Begin with the source’s own compact description: “Opetiosaurus” is species of reptile. The dossier treats that line as a proposition to test through Opetiosaurus, species and reptile, not as a finished interpretation.

Editorial reviewA practical orientation to terminology and classification, particularly when read beside dated observations, specimens or technical literature. The current lead gives the account dated anchors—2009, 2017—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Opetiosaurus, species and reptile is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “species of reptile” supplies a clear boundary for inquiry. It also exposes the unanswered questions: who defined that boundary, when it became stable and which sources sit outside it.

Evidence profile

Stable identifiers, scientific names and standards terminology offer the best bridge between this overview and specialist evidence. The source revision retrieved here is dated Aug 15, 2025. The linked authority identifier is Q45269867. None of the 0 selected statements returned an explicit reference. The first chronological checks are 2009 and 2017.

Critical limits

A general summary may omit uncertainty, sample limits or methodological disagreement that is explicit in the technical record. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Check terminology, classification and the date of the cited evidence. Scientific names and technical consensus can change while older records retain historical value.

Best used for
  • Current terminology
  • Classification context
  • Finding cited technical literature
Verify next

Primary datasets, specimen catalogues, standards bodies and the most recent peer-reviewed literature.

Three-step research path

  1. Establish the record: confirm the title “Opetiosaurus”, its source revision and the description used here.
  2. Expand the search: follow Opetiosaurus primary sources, Opetiosaurus archive and Opetiosaurus research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

Questions for further research

  1. Which source most directly establishes the central claim about “Opetiosaurus”?
  2. Is the terminology current, historical or disputed?
  3. Which observation, specimen, dataset or publication supports the account?
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Source & attribution

This entry incorporates text from Opetiosaurus” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.