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3.6" Silurian Fossil Brittle Star (Protaster) - New York
This is a 3.6" wide fossil brittle star (Protaster) from the Silurian-aged Rochester Shale of New York.
Caleb’s Quarry is in the Rochester Shale Formation, which is a primary source of over 200 richly detailed species that tell the ecologic story of the Early Silurian. This famous strata is known for its especially beautiful and rare assemblage of echinoderms. The calcareous mudstones and grainstones were transported from the relic Appalachian Mountains, which were uplifted and then eroded into the shallow but deepening warm seas of the Atlantic foreland basin during the Early Silurian.
While the rocks around Lockport, NY have been worked for trilobites since the 1830s, the opening of Caleb's quarry in 1991 has significantly added to the quantity and quality of the material available. Working this quarry is unquestionably difficult since it spends much of the year under water. Many hours of detailed preparation under microscope are required to extract and repair the trilobites found there.
Brittle stars are seafloor denizens belonging to the genus Protaster. These echinoderms are ornamented with flexible, whip-like arms that lurched them across the sea floor: one arm would have pressed ahead, while the other four acted as two pairs of opposite levers, thrusting the body forward.
Protaster is in the class Ophiuroidae, which is closely related to starfish. The ophiuroids diverged in the Early Ordovician, about 500 million years ago, resulting in over 2,000 species of brittle stars living today. The Rochester Shale is known for the excellent preservation of Protaster detail in its Lower Silurian strata (425 mya). They often fell apart after death, making a cluster of intact specimens a rare discovery.
There are several fascinating details regarding the Ophiuridoid body plan:
A brittle star's skeleton is made up of embedded ossicles, which are microcrystals of calcite arranged in a three-dimensional lattice known as a stereom. Occicles fuse together into an armor-like test that forms part of the endoskeleton.
The crystals and the spaces between them produce a light and tough honeycomb structure.
Modern Ophiurides establish that Protaster had no eyes or other specialized sense organs. However, they likely had several types of sensitive nerve endings in their epidermis.
Their tube feet might have sensed light as well as odors.
The disk of Protaster contains all of the internal organs that conducted digestion and reproduction.
The underside of the disk contains the mouth, which is also the anus. Ingestion and egestion occur in the same area.
While the rocks around Lockport, NY have been worked for trilobites since the 1830s, the opening of Caleb's quarry in 1991 has significantly added to the quantity and quality of the material available. Working this quarry is unquestionably difficult since it spends much of the year under water. Many hours of detailed preparation under microscope are required to extract and repair the trilobites found there.
Brittle stars are seafloor denizens belonging to the genus Protaster. These echinoderms are ornamented with flexible, whip-like arms that lurched them across the sea floor: one arm would have pressed ahead, while the other four acted as two pairs of opposite levers, thrusting the body forward.
Protaster is in the class Ophiuroidae, which is closely related to starfish. The ophiuroids diverged in the Early Ordovician, about 500 million years ago, resulting in over 2,000 species of brittle stars living today. The Rochester Shale is known for the excellent preservation of Protaster detail in its Lower Silurian strata (425 mya). They often fell apart after death, making a cluster of intact specimens a rare discovery.
There are several fascinating details regarding the Ophiuridoid body plan:
SPECIES
Protaster sp.
LOCATION
Middleport, New York
FORMATION
Rochester Shale
SIZE
Starfish: 3.6" wide, Shale: 3.9x3.8"
CATEGORY
SUB CATEGORY
ITEM
#270241
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