Ellis William Shuler

Summary

Ellis William Shuler A New Ordovician Eurypterid (1915)

The bed is an argillaceous sandstone which has a pronounced brick red color. It seems worthy of note that the bed carrying marine fossils is distinctly redder than the non-fossiliferous part of the sandstone. The southwestern section of the Bays sandstone along Walker Mountain, carrying the fossiliferous horizon, is also, on the whole, a deeper red than the section along the mountain to the northeast, which is practically barren of fossils.
Source: Wikisource

Ellis William Shuler A New Ordovician Eurypterid (1915)

This species possesses elongated joints fringed with spines along the posterior margin. While there is a difference in the general shape of the joints the chief distinction between the species multispinosus and alveolatus is in the prominent development of the alveolar process and the unusual size of the distal spine in the specimen from the Bays sandstone.
Source: Wikisource

Ellis William Shuler A New Ordovician Eurypterid (1915)

All spines have been lost from the third segment but five alveolar processes are seen, the distal one being the larger. The alveolar processes in all the segments have a distinct serial arrangement along a median line. The pronounced flattening of the bristles or spines gave a much enlarged paddle-like surface to the whole endognathite.
The anterior margins of the segments show a smooth arcuate curve without dentition. The joints show the expected thickening around the articulating surfaces.
Source: Wikisource

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