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Large 3D Triarthrus with Soft Tissue Preservation Pyrite Legs + Antennae from New York

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Large 3D Triarthrus with Soft Tissue Preservation Pyrite Legs + Antennae from New York
$1,350.00

Availability: Out of stock

Triarthrus eatoni (HALL, 1838)

Whetstone Gulf Formation, Lewis County, New York

Late Ordovician Period - 450 million years old

A true museum quality fossil from one of the most rare fossil sites in the world. Presented here is a trilobite (Triarthrus eatoni) with its legs and antennae present. What makes this specimen really stand out from 99% of the trilobites found in the Whetstone Fm., is that this trilobite is still inflated and was prepared to show the concave shell of the trilobite, with antennae and legs! Incredibly hard to prepare any specimen in this fashion and would be a center piece for any trilobite collection.

Specimen will come with Riker Mount, Upclose Photo, and ID Label for display.

Trilobite : 0.75 inch

Matrix : 3.55 x 2.8 in
Description

Details

Triarthrus eatoni (HALL, 1838)
Whetstone Gulf Formation, Lewis County, New York

An amazing and remarkable discovery made in the mid 2000's brought to light one of the most mysterious and talked about trilobite localities known from upstate New York, Beecher's Pyrite Trilobite Beds. Having been closed to collectors for over a century, many of Beecher's original sites had been lost and over taken back by the forest, these trilobites come from this recent discovery made nearby by a local collector.

The remarkably well-preserved fossils are about 1 - 3 cm long, and suggest the animal was intact with a shell along with the delicate parts of limbs and antennae protruding from the shell. The fossil was preserved in pyrite and was examined using X-Ray and CT Scan techniques.

From the middle Ordovician, these fossils are estimated to be about 450 million years old.

Several theories as to why these fossil trilobites preserved so delicately are made known when you look closely at the specimens themselves, they are not made up of sheets of pyrite, but rather thousands of small orbs. These "orbs" show a body form of an ancient sulfur bacteria that may have either (1) lived symbiotically with the trilobite in life or (2) covered the body of the animal once deceased and once covered quickly in mud, preserving the living shape of the trilobite in the soft mud.

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