Scytalocrinus disparilis
Vendor: Fossil Soup
SKU Number: SQ8073618
An absolutely perfect and beautiful individual Scytalocrinus disparilis, Edwardsville Formation, Mississippian, Carboniferous, Crawsfordsville, Montgomery County, Indiana, USA.
The stalk and the crown are beautifully preserved. The stalk is formed of numerous calcarious plates called ossicles that flow towards the crown. The crown is composed of cup shaped sets of plates in a pentaradial pattern around the crinoid. This part of the crown is known as the calyx. The arms that extend from the calyx are called brachia. There are lateral unbranched extensions of plates that protrude from the arms called pinnules.
The crinoids from the world famous location of Crawfordsville, Indiana are about 320 Million Years Old.
This specimen has a crown of about 5.20 cm and a total length of about 12+ cm.
Full dimensions are listed below.
Vendor: Fossil Soup
SKU Number: SQ8073618
An absolutely perfect and beautiful individual Scytalocrinus disparilis, Edwardsville Formation, Mississippian, Carboniferous, Crawsfordsville, Montgomery County, Indiana, USA.
The stalk and the crown are beautifully preserved. The stalk is formed of numerous calcarious plates called ossicles that flow towards the crown. The crown is composed of cup shaped sets of plates in a pentaradial pattern around the crinoid. This part of the crown is known as the calyx. The arms that extend from the calyx are called brachia. There are lateral unbranched extensions of plates that protrude from the arms called pinnules.
The crinoids from the world famous location of Crawfordsville, Indiana are about 320 Million Years Old.
This specimen has a crown of about 5.20 cm and a total length of about 12+ cm.
Full dimensions are listed below.
Vendor: Fossil Soup
SKU Number: SQ8073618
An absolutely perfect and beautiful individual Scytalocrinus disparilis, Edwardsville Formation, Mississippian, Carboniferous, Crawsfordsville, Montgomery County, Indiana, USA.
The stalk and the crown are beautifully preserved. The stalk is formed of numerous calcarious plates called ossicles that flow towards the crown. The crown is composed of cup shaped sets of plates in a pentaradial pattern around the crinoid. This part of the crown is known as the calyx. The arms that extend from the calyx are called brachia. There are lateral unbranched extensions of plates that protrude from the arms called pinnules.
The crinoids from the world famous location of Crawfordsville, Indiana are about 320 Million Years Old.
This specimen has a crown of about 5.20 cm and a total length of about 12+ cm.
Full dimensions are listed below.
Additional Information
Sea urchins belong to the Phylum Echinodermata and includes crinoids, brittle stars and sea cucumbers. The first echinoderms appear in the Lower Cambrian period.
It has been suggested that he ancestor of all echinoderms was a simple bi-laterally symmetrical animal with a mouth, gut and anus. This ancestral organism adopted an attached mode of life with suspension feeding, and developed radial symmetry. Even so, the larvae of all echinoderms are bilaterally symmetrical, and all develop radial symmetry at metamorphosis. Like their ancestor, the starfish and crinoids still attach themselves to the seabed while changing to their adult form.
