Triarthrus beckii

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Vendor: Gold Bugs

SKU Number: SQ3171573

A large and inflated Triarthrus beckii from the Middle Ordovician, Denley Limestone of Herkimer, New York.

This species is normally confined to its flattened, grainy form in the Lower Utica Shale unit. Rare inflated specimens of this species with black exoskeleton are found in the limestone layers of the Denley.

Full dimensions are listed below.

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Vendor: Gold Bugs

SKU Number: SQ3171573

A large and inflated Triarthrus beckii from the Middle Ordovician, Denley Limestone of Herkimer, New York.

This species is normally confined to its flattened, grainy form in the Lower Utica Shale unit. Rare inflated specimens of this species with black exoskeleton are found in the limestone layers of the Denley.

Full dimensions are listed below.

Vendor: Gold Bugs

SKU Number: SQ3171573

A large and inflated Triarthrus beckii from the Middle Ordovician, Denley Limestone of Herkimer, New York.

This species is normally confined to its flattened, grainy form in the Lower Utica Shale unit. Rare inflated specimens of this species with black exoskeleton are found in the limestone layers of the Denley.

Full dimensions are listed below.

Specimen Details
Species Name: Triarthrus beckii Order / Family: Ptychopariida / Olenidae Age: Middle Ordovician Locality: Herkimer Co., New York Formation: Denely Limestone
Matrix Dimensions
Dimensions: In Centimeters Length: 9.80 cm Width: 8.00 cm Thickness: 3.00 cm Weight: 326 grams
Specimen Dimensions
Dimensions: In Centimeters Length: 2.03 cm Width: 0.20 cm Thickness: Negligible Weight: 326 grams
Shipping Dimensions
Dimensions: In Inches Length: 10.0 inches Width: 7.0 inches Height: 3.0 inches Weight: Under 1.0 lbs
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Additional Information

T. beckii and T. eatoni have long been considered closely related and possibly synonymous. Recent comparative analysis showed that there is no sharp distinction between the two, but that they seem to represent opposing morphotypes.

T. beckii dominates earlier in the distribution and in shallow water, while T. eatoni does so later and in deeper waters. It is probable that the transgression of the sea level aided the eventual disappearance of the T. beckii morph. The occurrence of the supposed pluriform species continued for more than two million years.

References:

Charles Emerson Beecher
Triarthrus eatoni
Markus Martin
Gold Bugs
Beecher's Trilobite Bed


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