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  • Crania Brachiopod


    Images:

    DPS Ammonite

    Taxonomy

    Inarticulate Brachiopod

    Kingdom: Animalia
    Phylum: Brachiopoda
    Class: Craniata
    Order: Craniida
    Family: Craniidae
    Genus: Crania
    Species: Crania modesta
    Author Citation White and St. John 1867

    Geological Time Scale

    Eon: Phanerozoic
    Era: Paleozoic
    Period: Carboniferous
    Sub Period: Pennsylvanian
    Epoch: Middle
    International Age: Moscovian

    Stratigraphy

    Naco Formation

    Provenance

    Collector: DPS Ammonite
    Acquired by: Field Collection

    Dimensions

    Length: 4.8 mm
    Width: 4.6 mm

    Location

    Canyon Creek
    Gila County
    Arizona
    United States

    Comments

    Crania

     

    Crania modesta is a rare calcium carbonate Pennsylvanian inarticulate brachiopod. The shell is very thin and the ornamentation of the shell below shows through. You can see the interior of a near circular 4.6 by 4.8 mm pedicle valve that attached itself to aLinoproductus prattenianus (photo #1). A bryozoan also covers the front and back of the Linoproductus (photos #2 & #4). Photo #2 is a different photo of the same Crania as in photo #1. The Crania has a thickened rim and a sub central knob. Rowell (1965, p. 289) lists Crania as the only Pennsylvanian genus with a calcified pedicle valve as stated by Sutherland (1973, p. 16).

     

     

    The presence of a large bryozoan colony on the backside of the Linoproductus valve (photo #4) suggests why only the pedicle valve of the Crania was preserved. The entire Linoproductus shell with the Crania and small bryozoan colony on top (photo #2) was flipped over allowing the bryozoan to grow on the other side. The brachial valve dissolved away or was broken off from exposure before it was buried. The brachial valve was probable very thin like the pedicle valve.

     

    Taxonomy from GBIF.

     

    Photo 3 from plate 11, figure 17 from Mudge 1962.

     

    Mudge, M. R., Yochelson, E. L., Douglas, R. C. et al. 1962. Stratigraphy and Paleontology of the Uppermost Pennsylvanian and Lowermost Permian Rocks in Kansas. United States Geological Survey Professional Paper 323:1-213. 

     

    https://pubs.usgs.gov/pp/0323/report.pdf

     

     

    Rowell, A. J. 1965. Inarticulata. In: R.C. Moore (ed.), Treatise on Invertebrate Paleontology. Part H. Brachiopoda, H260–H296. Geological Society of America and University of Kansas Press, Boulder.

     

    Sutherland, P. K. and F. H. Harlow. 1973. Pennsylvanian brachiopods and biostratigraphy in southern Sangre de Cristo Mountains, New Mexico. Memoirs of the New Mexico Bureau of Mines and Mineral Resources 27:1–171. 

    Free download:

    https://geoinfo.nmt.edu/publications/monographs/memoirs/27/

     

    First description in: 

     

    White, C. A. and St. John, O. H. 1867. Descriptions of new sub-Carboniferous and Coal Mesures fossils collected upon the geological survey of Iowa, together with a notice of new generic characters observed in two species of brachiopods. Transactions of the Chicago Academy of Sciences 1:115-127.

     

     

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    User Feedback


    Tidgy's Dad

    Posted

    Splendid find, sir! Panama.gif.697aa7fa724a5fffe6b6fe07f88d5459.gif:brachiopod::b_love1:

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    DPS Ammonite

    Posted

    DE55AC67-E9B9-44D7-98ED-FDE7B4C4F4D6.jpeg.b5dd7627d89a549acced01fa420b63fc.jpeg

     

     

    This is the backside of photo 2.  Including photo 4 supports an interesting likely aspect of the taphonomy. It illustrates the community of epibonts that the Crania belonged to. One probable reason that both valves of the Crania are not present is that the whole piece on a Linoproductus valve was not rapidly buried, but was flipped over so that the larger bryozoan colony could grow on the other side. The top Crania valve dissolved or was broken off due to exposure.

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    Tidgy's Dad

    Posted

    The usual reason that many craniids are found as only the ventral valve is that they are inarticulate brachiopods so have no articulation teeth, sockets, hinge etc. The ventral valve is cemented firmly to the substrate or host but, as only muscles hold the two valves together, once these have rotted away, the dorsal valve often becomes detached.  

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