Eurypterids from the Price Formation of Virginia: First Eurypterids from the Mississippian of North America

Abstract. A new hibbertopterid eurypterid, Cyrtoctenus bambachi n. sp., is described from the Early Mississippian (Tournaisian) Price Formation of western Virginia. The same unit yields an unidentifiable stylonurine eurypterid. These are the first eurypterids documented from the Mississippian of North America, and only the fourth locality of this age anywhere in the world to yield eurypterids.


Introduction
Eurypterids are rare components of Mississippian faunal assemblages.Only three families are known, although they belong to both suborders, the Eurypterina and the Stylonurina (Table 1).These same higher taxa persist until the final extinction of the eurypterids during the Permian, with overall diversity remaining low (Lamsdell et al., 2010;Lamsdell and Selden, 2017).In late Paleozoic strata, eurypterids are found only in freshwater environments (Lamsdell and Selden, 2017).
The geographic range of Mississippian eurypterids is also limited (Tetlie, 2007).More than half of the Mississippian eurypterids come from Visean and Serpukhovian units in Scotland and were described in detail by Charles Waterston (Waterston, 1957(Waterston, , 1968;;Størmer and Waterston, 1968).Additional early Carboniferous eurypterid localities in Scotland were mentioned but not described by Smithson et al. (2012).Outside of Scotland, only Cyrtoctenus wittebergensis Waterston, Oelofsen, and Oosthuizen, 1985, from the Tournaisian of South Africa is well known.Here, we describe the first Mississippian eurypterids from North America and only the fourth eurypterid occurrence known from the Tournaisian.

Geological setting
The Price Formation is a Lower Mississippian unit exposed in a narrow outcrop belt in the Appalachians from Virginia northeast into Pennsylvania (Kammer and Bjerstedt, 1986;Bjerstedt and Kammer, 1988;Nolde, 1994).It is interpreted as a southwestprograding deltaic complex, comprising a complex of marine, delta front, and coastal alluvial facies, including coal-producing swamp deposits (Kreisa and Bambach, 1973;Bjerstedt and Kammer, 1988).In Virginia, the upper part of the Price, which contains the deltaic sequence, is dated as Kinderhookian to lower Osagean (Kammer and Bjerstedt, 1986;Bjerstedt and Kammer, 1988;Gensel, 1988;Gensel and Pigg, 2010) or solely Osagean (Nolde, 1994), which corresponds to Tournaisian.Two localities in the Virginia portion of the outcrop belt (Brush Mountain-Little Walker Mountain outcrop belt; Bjerstedt and Kammer, 1998, fig.2) have yielded specimens of eurypterids from shales.
Locality 1: Coal Bank Hollow.-About 100 m of the Price Formation is exposed along U.S. 460, between Coal Bank Hollow Road and County Route 648 (Brown, 1983), Brush Mountain, 3.2 km north of Blacksburg, Montgomery County, Virginia (37.27571°N, 80.418900°W; WGS84).This is locality 11 of Kreisa and Bambach (1973).A detailed section of this site (with lithologies including sandstone, siltstone, claystone, and mudstone) was given by Brown (1983), who placed it in the upper part of the Price Formation.The fine-grained intervals are near the base of the section; a coal layer is near the top.Plants from the site listed by Jennings (1975) and Scheckler (1978, cited in Brown, 1983) consist of: Lepidodendropsis scobiniformes (Meek, 1880); L. vandergrachtii Jongmans, Gothan, and Darrah, 1937;Lepidophylloides sp., Protostigmaria eggertiana Jennings, 1975(miscopied by Brown, 1983, as Protostigmaria essetiema); and Rhodea sp.The exact horizons yielding the eurypterid specimens are not known.The eurypterids from Coal Bank Hollow were briefly discussed in Briggs and Rolfe (1983), based on preliminary observations by Plotnick.near to locality 6 of Kreisa and Bambach (1973) and is probably section C of Brown (1983, p. 54).This is also a coarsening upward sequence, with claystone at base and sandstone at the top.The specimens come from a gray/mottled white finegrained shale with abundant iron stains, with a diverse associated flora including Triphyllopteris, Rhodeopteridium (Rhodea), Neuropteris, Lagenospermum, and Gnetopsis (P.Gensel, personal communication, 1981).Neuropteris antiqua (Stur, 1877) and Rhodeopteridium sp.occur on the slab (P.Gensel, personal communication, 2018) that includes the eurypterid (Gensel, 1988).Again, the exact horizon of the eurypterid specimen is not known.
The two localities are non-marine strata, associated directly with the Price Formation delta complex.They are either delta plain (Facies 7 of Kreisa and Bambach, 1973) or swamp (Facies 8 of Kreisa and Bambach, 1973).Gensel (personal communication, 1981) favored either a levee or channel area of a delta plain deposit for the Pond Lick Hollow Road specimen.

Materials and methods
Specimens from Coal Bank Hollow were collected by faculty and students at Virginia Polytechnic Institute and State University, including Chauncey G. Tillman, Frank Whitten, and David Goodman, and deposited in the collections of the Department of Geological Sciences.In 2021 they were transferred to the Virginia Museum of Natural History and given specimen numbers.The specimen from Pond Lick Hollow was collected by Patricia Gensel.
Specimens were photographed with a Canon PowerShot Pro Series S5 IS digital camera.Figure 1.1 was drawn with a camera lucida attached to a Wild M5 binocular microscope.
Repositories and institutional abbreviations.-Type and figured specimens examined in this study are deposited in the following institutions: Virginia Museum of Natural History (VMNH), Martinsville, Virginia, USA, and the paleontology collections of the University of North Carolina (NCUPC), Chapel Hill, North Carolina, USA.

Cyrtoctenus bambachi new species
Figure 1 Holotype Description.-Eachtype specimen is described individually below.Holotype VMNH 129168.-Specimencomprises a moveable finger or blade with a length of 60 mm and a width of 10 mm proximally, expanding to 13 mm wide distally.The anterior (or dorsal) margin is straight, demarcated by a thickened ridge of imbricate scales.The posterior (or ventral margin) is slightly curved and is also ornamented with a ridge of imbricate scales.The distal termination of the finger is rounded, with four scales from the posterior margin projecting out to form blunt spines.
Paratype VMNH 129166.-Fragment of opisthosomal tergite in part and counterpart, preserved width 92 mm, preserved length 53 mm.No natural edge of the tergite is preserved except for the posterior margin, which is crenulated.Tergite strongly ornamented.Ornamentation grades from dense, small acicular scales anteriorly to larger, increasingly spread-out lunate scales posteriorly.The crenulation along the posterior margin is formed from a dense accumulation massively enlarged lunate scales that show significant relief, forming longitudinal ridges and furrows.
Paratype VMNH 129169.-Fragment of cuticle, most likely part of a prosomal appendage.The specimen has a length of 91 mm and is 21 mm wide proximally, expanding to 50 mm wide distally, with a recurved distal margin.The podomere is densely ornamented with acicular and semilunate scales that increase in size distally.An indentation running down the center of the podomere for 66 mm may represent a ventral groove.
Etymology.-Named for Richard K. Bambach, in honor of his many contributions to paleontology and the education of generations of paleontologists.2022) synonymized the hibbertopterid genera Hibbertopterus, Dunsopterus, and Vernonopterus, but considered Cyrtoctenus to be distinct due to the presence of combs on the prosomal appendages.The Coal Bank Hollow material exhibits a tergite ornamentation more typical of Hibbertopterus (illustrated as Campylocephalus by Waterston, 1957) with dense acicular scales, and the enlarged acicular scales forming crenulations along the tergite posterior in VMNH 129166 specimens are also observed in specimens of Hibbertopterus formerly assigned to Dunsopterus (Waterston, 1968).The morphology of the podomere preserved at Coal Bank Hollow, VMNH 129169, closely matches podomeres of Hibbertopterus stevensoni (Etheridge, 1877) in ornamentation and overall morphology (Waterston, 1968).However, the moveable finger (VMNH 129168) is a clear indicator that the new species possessed combs and therefore is assignable to Cyrtoctenus (Størmer and Waterston, 1968;Waterston et al., 1985).The combination of traits in the new species further suggests that the genera Hibbertopterus and Cyrtoctenus may be synonyms (Jeram and Selden, 1994;Lamsdell et al., 2010;Lamsdell, 2013), although the current material is too sparse to warrant a full reassessment of the genera.
Despite being known from only a handful of fragmentary specimens, Cyrtoctenus bambachi n. sp.can be differentiated from other currently known Cyrtoctenus species based on the morphology of the moveable finger.The moveable fingers of Cyrtoctenus peachi and Cyrtoctenus dewalqui (Fraipont, 1889) are curved, narrow distally, and have pointed terminations (Størmer and Waterston, 1968), quite unlike those of Cyrtoctenus bambachi n. sp.Cyrtoctenus wittebergensis possesses moveable fingers that are straight, as in Cyrtoctenus bambachi n. sp., but narrow distally and terminate in a point.The moveable finger of Cyrtoctenus
Description.-Seven,possibly eight, opisthosomal segments preserved with some relief.Anterior and posterior broken and incomplete.A large crack runs through the posterior of the specimen; the portion posterior to this can be removed.No discernable ornamentation, trilobation, or division into preabdomen and postabdomen.Segment 1 is short.Indication of a marginal rim on some segments (left side segments 3-5; Fig. 2).Total length is 67 mm, maximum width is 29 mm. Material.-NCUPC135A.
Remarks.-The specimen lacks sufficient characters to confidently assign it to a taxon within the eurypterids.The lack of ornamentation on the segments, as well as no clear indication of a division into pre-and postabdomen, argues against inclusion within the Adelophthalmidae, the surviving clade of the Eurypterina (Lamsdell and Selden, 2017).The overall shape, smooth texture, and marginal rim resemble members of the Stylonurina, such as the Upper Devonian Stylonurella(?) beecheri Hall and Clarke, 1888 (Plotnick, 2022, fig. 8).Pending additional specimens, we place it as incertae sedis within the Stylonurina.

Discussion
Although eurypterids are relatively common in both Late Devonian and Pennsylvanian terrestrial settings, they are by comparison extraordinarily rare in the Mississippian (Tetlie, 2007;Lamsdell and Selden, 2017).No members of the clade have been documented previously from North America.These specimens thus fill a key break in our understanding of the later history of this group.Ward et al. (2006) suggested that terrestrial arthropods showed a chronological gap during the Visean equivalent to Romer's gap for vertebrates, which they attributed to low atmospheric oxygen levels.On the face of it, the record of Carboniferous eurypterids supports the existence of an arthropod gap.The forms reported here support the contention by Smithson et al. (2012) that the gap is an artifact of collection failure, with additional eurypterid material from this interval awaiting future discoveries.