Vectibalanus erisma

(Redirected from Vectibalanus mortoni)

Taxonavigation

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Taxonavigation: Balanoidea 

Superregnum: Eukaryota
Cladus: Unikonta
Cladus: Opisthokonta
Cladus: Holozoa
Regnum: Animalia
Subregnum: Eumetazoa
Cladus: Bilateria
Cladus: Nephrozoa
Cladus: Protostomia
Cladus: Ecdysozoa
Cladus: Panarthropoda
Phylum: Arthropoda
Cladus: Pancrustacea
Superclassis: Multicrustacea
Classis: Thecostraca
Subclassis: Cirripedia
Infraclassis: Thoracica
Superordine: Thoracicalcarea
Subordo: Balanomorpha
Superfamilia: Balanoidea

Familia: Archaeobalanidae
Subfamilia: Archaeobalaninae
Genusː †Vectibalanus
Species: †Vectibalanus erisma

Name

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  • Vectibalanus erisma (Sowerby, 1846): Pl. 648, fig. 2
    • Original genus: Balanus
    • Stratigraphic and geographic distribution: Middle Eocene (Bartonian) to lower Oligocene (Rupelian), Hampshire, UK
    • Type locality: Barton Clay Formation, Barton, Hampshire, UK
    • Typus: lectotype NHMUK In. 17027; paralectotype NHMUK In. 17028
    • ZooBank: 51043359-D9AB-44E7-A13F-593C1C59E6E1
    • Provisionally synonymized by Gale, Tracey & Trif, 2022: 90

Synonymy

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  • Archaeobalanus semicanaliculatus Menesini, 1971: 28
    • Original status: valid species
    • Stratigraphic and geographic distribution: Eocene; Bartonian, Oligocene, Paris Basin
    • Type locality: 'Marinesian', Bartonian, near Paris
    • Typus: Lectotype shell in Menesini, 1971; pl. 2, fig. 1; apparently not registered; selected by Gale, 2020
    • ZooBank: 950FB46F-3FA0-4431-8CEA-683514B2AD96
  • Vectibalanus mortoni Gale, 2021: 19
    • Stratigraphic and geographic distribution: Middle Eocene (Bartonian), Hampshire, UK
    • Type locality: middle Eocene, Barton Formation, Highcliffe Member, Barton, Hampshire, UK
    • Typus: holotype NHMUK IC 1913; paratypes NHMUK IC 1908-1912, 1914, 1915
    • ZooBank: 665F5417-EF35-483C-9A14-9878E6D3728C
    • Synonymized by Gale, Tracey & Trif, 2022: 90

References

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  • Sowerby, J. de C. 1846: The Mineral Conchology of Great Britain. London. pt. 113: 57-80, pl. 644-648. BHLReference page.  [See p. Pl. 648, fig. 2, original mention]