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  • Glycymeris Clam Internal Mold


    Images:

    I_gotta_rock

    Taxonomy

    Bittersweet Clam

    Kingdom: Animalia
    Phylum: Mollusca
    Class: Bivalvia
    Order: Arcida
    Family: Glycymerididae
    Genus: Gycymeris
    Species: Gycymeris mortoni
    Author Citation (Conrad, 1869)

    Geological Time Scale

    Eon: Phanerozoic
    Era: Mesozoic
    Period: Cretaceous
    Sub Period: None
    Epoch: Late

    Stratigraphy

    Monmouth Group
    Mount Laurel Formation

    Provenance

    Collector: Heather Siple
    Date Collected: 01/21/2021
    Acquired by: Field Collection

    Dimensions

    Thickness: 4 mm
    Diameter: 10 mm

    Location

    Reedy Point Spoils, North Side
    New Castle
    Delaware
    United States

    Comments

    Glycymeris clams have ridges along the inside edge of the valves that extend past the cardinal area. Internal molds tend to include these teeth, making them very distinctive. 

     

    As of the time this was posted, this was the only member of the genus listed in the Paleobio Database for the Cretaceous period and it is only listed as being found in NJ. However, Stuart Weller (1907) and Horace G Richards (1958) not only include them in the C and D Canal zone, but identify three different species for the region. This one is the most common and the only one THEY found outside of NJ.

     

    This is most likely from the Mount Laurel formation. It was found among the Mount Laurel index fossils. However, Navesink Formation fossils are also found in pockets in this spoils area, so the possibility that this came from the Navesink and got mixed up with the Mount Laurel material from constant human activity cannot be ruled out.




    User Feedback


    Nice! The steinkerns look like they have a bit of shell clinging to them. Don't remember any preservation like this back in the day (1970s - 80s). Are there new spoils? This and the gastropod remind me of the Bigg's Farm? material.

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    There are no new spoils accessible. The new dredge material from earlier this century went to an island in the middle of the DE River because it was too toxic for people to be poking through.  

    This is from the 1980 spoils east of the Biggs Farm. It's all the same two formations, though - Mt Laurel and Navesink. Even at the Biggs Farm, there are hints of white shell clinging to some of the fossils, It's just hard to see on something smaller than an Anomia oyster. Thing is, as I mentioned in the details about the gastropod, the shell material usually permineralized into black phosphate instead of stabilizing into calcite.

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