Erik Norman Kjellesvig-Waering

Summary

Erik Norman Kjellesvig-Waering Eurypterids of the Devonian Holland Quarry Shale of Ohio (1961)

In contrast to these active swimmers, the associated eurypterids, namely, Dolichopterus asperatus and Syntomopterus richardsoni, had simple, small chelicerae not serviceable as weapons of either defense or predation; both were probably benthonic forms, crawling on the mud but perhaps capable of swimming to a limited extent. These could well have been prey to the fishes and, indeed, to the large pterygotids. However, in this shale the fishes are the only animals with a covering rigid and hard enough to abrade the tough pincer-teeth of the pterygotids.
Source: Wikisource

Erik Norman Kjellesvig-Waering Eurypterids of the Devonian Holland Quarry Shale of Ohio (1961)

Besides the common fishes and eurypterids, no animal remains are present. It is difficult to explain the intimate association of fishes and eurypterids not only in this black shale but also throughout the Silurian and Devonian sections other than by the conclusion that one served as prey for the other. In the Ohio Devonian, the pterygotids surpassed five feet in length (from the anterior of the carapace to the end of the telson) and were armed with stout and formidable chelicerae which, with their strong teeth, served as excellent grasping organs.
Source: Wikisource

Erik Norman Kjellesvig-Waering Eurypterids of the Devonian Holland Quarry Shale of Ohio (1961)

However, part of the general stout aspect is inherent. The majority of the teeth are small, with several large, thick teeth interspersed. The central, or principal, tooth of the free ramus (no. 1 in figs. 35–38) is the largest, and is represented by a curved, thick structure. Nearly opposite this tooth is a similar but smaller tooth (no. 3) . In front of this tooth is another one, half as large (no. 4) . This combination is present on all chelicerae of this species.
Source: Wikisource

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