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Found 4 results

  1. From the album: MY FOSSIL Collection - Dpaul7

    Scaphopods -Three LAEVIDENTALIUM Matrices Chesterian Zone of the Bangor Limestone Formation in northern Alabama Mississippian Period - (ca 325,000,000 years old) Dentaliida is one of the two orders of scaphopod mollusks, commonly known as elephant's tusk shells. The order Dentaliida contains most of the larger scaphopods, and is distinguished from the other order (the Gadilidae) by the shape of its shell (the Dentaliid shell tapers uniformly from anterior to posterior; the Gadilid one has an anterior shell opening slightly smaller than the shell's widest point), the shape of th
  2. From the album: MY FOSSIL Collection - Dpaul7

    Scaphopods -Three LAEVIDENTALIUM Matrices Chesterian Zone of the Bangor Limestone Formation in northern Alabama Mississippian Period - (ca 325,000,000 years old) Dentaliida is one of the two orders of scaphopod mollusks, commonly known as elephant's tusk shells. The order Dentaliida contains most of the larger scaphopods, and is distinguished from the other order (the Gadilidae) by the shape of its shell (the Dentaliid shell tapers uniformly from anterior to posterior; the Gadilid one has an anterior shell opening slightly smaller than the shell's widest point), the shape of th
  3. From the album: MY FOSSIL Collection - Dpaul7

    Scaphopods -Three LAEVIDENTALIUM Matrices Chesterian Zone of the Bangor Limestone Formation in northern Alabama Mississippian Period - (ca 325,000,000 years old) Dentaliida is one of the two orders of scaphopod mollusks, commonly known as elephant's tusk shells. The order Dentaliida contains most of the larger scaphopods, and is distinguished from the other order (the Gadilidae) by the shape of its shell (the Dentaliid shell tapers uniformly from anterior to posterior; the Gadilid one has an anterior shell opening slightly smaller than the shell's widest point), the shape of th
  4. HI all, Our latest finds from the acid fines from our new site on the Mogollon Rim - Scaphopods (Tusk Shells) from the Permian Fort Apache Limestone East of Payson. A minor but very important faunal element in the upper early Permian Fort Apache Limestone are Scaphopods - Or more commonly known today as "Tusk Shells". These mollusks were conical tubes - some linearly ribbed some smooth, with both ends open for water current movement. Fortunately for us, In 1963 White, in his monumental GSA Memoir 89 had found the smooth scaphopods, and identified them as Plagioglypta. W
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