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  • Pentlandia macroptera (TRAQUAIR, 1888)


    Images:

    oilshale

    Taxonomy

    Lungfish

    Kingdom: Animalia
    Phylum: Chordata Haeckel 1874
    Class: Sarcopterygii
    Order: Dipnomorpha Ahlberg 1991
    Family: Phaneropleuridae Huxley 1861
    Genus: Pentlandia
    Species: Pentlandia macroptera
    Author Citation (TRAQUAIR, 1888)

    Geological Time Scale

    Eon: Phanerozoic
    Era: Paleozoic
    Period: Devonian
    Sub Period: None
    Epoch: Middle
    International Age: Givetian

    Stratigraphy

    John o'Groats Sandstone Group
    Last House Formation

    Biostratigraphy

    John o'Groats fish bed

    Provenance

    Acquired by: Purchase/Trade

    Dimensions

    Length: 20 cm

    Location

    John o'Groats
    Caithness County
    Scotland
    United Kingdom

    Comments

    Grammatically incorrect form: Pentlandia macropterus.

    Taxonomy from Challands & Blaauwen, 2016.

    Emended diagnosis from Challands & Blaauwen, 2016, p. 3: "A medium-sized dipnoan (up to 40 cm) in which the I-bones do not meet medially posterior to the B-bone. The B-bone is 1.2 times as long as it is wide. The paired C-bones are 1.7 times long as they are wide. There are two paired Y-bones that lie lateral to the I-bone and contact the operculum along with bone 4, the J-bone, and the X-bone. Only one suboperculum is present. The X-bone carries the bifurcation for the supraorbital and infraorbital lateral line. There are six circumorbital bones, bone 3 being positioned dorsally and the largest. An A-bone is present posterior to the B-bone. The parasphenoid is short with a poorly developed posterior stalk. The entopterygoids are thin and L-shaped and carry subtriangular tooth plates with up to 12 rows of dentine-covered cusps. The lateral margins of the A-bone contact dorsal protuberances of the I-bone. The posterior dorsal fin is 17% of the total length of the animal with the anterior-most portion supported by a basal plate that carries three radials. Cosmine is not present on any scales or dermal bones. M-, O-, and P-bones are present in the snout region anterolateral to the E-bones but anterior to these bones the snout is unossified or poorly ossified and is not preserved in all but the largest specimens."

    Reconstruction from Challands & Blaauwen, 2016, p. 40:

    1889405653_PentlandiaReconstr.JPG.1bc3265eb086b1b64fcb380aaf254973.JPG

    Identified by oilshale.

    References:

    Challands, T. and Blaauwen, Jan den (2016) A redescription of the Middle Devonian dipnoan Pentlandia macroptera Traquair, 1889, and an assessment of the Phaneropleuridae. Zoological Journal of the Linnean Society. p. 1-47. doi: 10.1111/zoj.12491

    Volume 16: Fossil Fishes of Great Britain. Chapter 6: Mid-Devonian fossil fishes sites of Scotland. Site: JOHN O'GROATS, CAITHNESS (GCR ID: 353)

    Emma Jude, Zerina Johanson, Anton Kearsley and Matt Friedman(2014): Early evolution of the lungfish pectoral-fin endoskeleton: evidence from the Middle Devonian (Givetian) Pentlandia macroptera. Frontiers in Earth Science, 2014, Vol. 2, Article 18




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