Eurypterus
remipes
Class Merostomata,
Order Eurypterida, Superfamily Eurypteroidea, Family Eurypteridae
Geological
Time: Upper Silurian, (~410 m.y.a.)
Size (25.4
mm = 1 inch): Eurypterus fossil
are 70 mm – 135 mm long; Matrix: 295 mm by 245 mm
Fossil Site:
Bertie Group, Fiddler’s Green Formation Phelps Waterlime, Herkimer
County, New York
Fossil Code:
KZC16
Price: Sold
Description:
While Eurypterids (“Sea Scorpions”) are uncommon
fossils worldwide, New York state is one of the few places where
conditions for preservation have been ideal. They were large
arthropod predators during the Silurian and Devonian, reaching
a maximum length
of 2 meters. The Eurypterid colonies of New York are distinctly
localized, with two being found above and
two below the salt beds of what was termed the Salina Series.
These colonies are presumed to be breeding pools of brackish
to partly open basins. They are the Otisville Basin (Colony O),
the Pittsford Pool (Colony P), the Herkimer Pool (Colony P),
and the Buffalo Pool (Colony P). These last two are the most
famous of them, yielding numerous fantastic specimens. Erypterus
remipes was a small example of the Merostomata, with specimens
having been found ranging from 8 mm to 280 mm in length. It is
presumed to have crawled along the seafloor, using its grasping
pincers to seize trilobites and other prey. This fine example
is a juvenile, and has the swimming paddles and some walking
legs preserved. The segmentation of the meso- and metasoma is
well detailed, and the specimen is well-centered on the dolostone
matrix. This is a fine example of a death assemblage of the fossil
designated the New York Sate Fossil by then Governor Mario Cuomo
in 1984. It consist of parts of at least eight individuals, mostly
preserved in dorsal aspect. There is a portion of a ventral example
seen to the left side next not the specimen that displays the
swimming legs. This is a large shale matrix suitable for framing
or mounting on a mantelpiece.
Also
see single Eurypterus specimens here and
here. |
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