Agraulos

• A. ceticephalus (= Arionellus longicephalus Hicks, 1872) ^[6] occurs in the Middle Cambrian Jince Formation of the Czech Republic.^[7] The species was first described from the Skryje Member of the Buchava Formation (Chlupáč et al. 1998; Fatka et al. 2011) ^[8][9] on the slopes of the Berounka River in the Týřovice-Luh-Skryje area between Prague and Plzeň in the Skryje-Týřovice Basin. The species has been recovered also from the Menevia Formation of St. David's, South Wales (Fletcher, 2017, Fig. 8, I, J, K and Fig. 9, A-C) and, as its junior subjective synonym "Agraulos longicephalus" (Hicks, 1872), from the Nant-y-big Formation (Hypagnostus parvifrons Biozone) of Porth Ceiriad, North Wales (Young et al., 2002; Young et al., 1994, p. 343),^[10][11] the Manuels river formation of Eastern Newfoundland (Martin and Dean, 1988, p. 21, pl.3, figs. 9, 11, 12; non figs. 10 & 13),^[12] and Spain (Sdzuy, 1961, pl.23, ?figs. 8–11, 15).^[13] Fletcher (2017, p. 26) observed that specimens described by Weidner and Nielsen (2015, pl. 41A–F; Fig. 22B) as Agraulos longicephalus ^[14] (from the Middle Cambrian Paradoxides paradoxissimus Superzone of the Alum Shale Formation and within the lower and upper parts of the Ptychagnostus s.l. atavus Zone as well as in the Ptychagnostus punctuosus Zone), are in fact "marked by a conspicuous small median projection on the occipital ring, quite different from any species recorded elsewhere".
• A. socialis (Billings, 1872) occurs in the Manuels River Formation (Drumian Stage) of Eastern Newfoundland where localities include the eastern side of chapel arm in Trinity Bay, Deep Cove in St Mary's Bay, and the Manuels River Section near St John's (Fletcher, 2017, p. 25). Fletcher also observed (op. cit. pp. 25, 26) that "of all the specimens referred to longicephalus, the exoskeleton from the Montagne Noire figured by Courtessole (1973, pl. 10, fig. 5; Fig. 22P) ^[15] appears to be very close to A. socialis, as are Sdzuy's 1961 illustrations of associated Spanish cranidia and a thoracic axis without notable nodes or spines".
• A. affinis (Billings, 1872) derives from the Big Gulley Member green mudstone of the Chamberlain's Brook Formation in the coastal cliffs of the greater Branch Cove on both sides of the Branch River estuary, St Mary's Bay, Newfoundland, originally as part of the Geological Survey of Newfoundland Collection (Fletcher, op. cit, p. 21). The species occurs in association with the Scandinavian taxa Condylopyge carinata Westergärd, 1936 and Parasolenopleura gregaria [Solenopleura cristata Linnarsson, 1877] ^[16] indicating a zonal position about that of Ptychagnostus praecurrens (Fletcher, op.cit.) and Eccaparadoxides oelandicus.
• A. lewisi Fletcher, 2017 (p. 19, fig. 9D-I) is recorded from the Menevia Formation of Porth-y-rhaw, St. David's, Wales and derives from the Hypagnostus parvifrons Biozone (Localities PR-4 and PR-16 of Rees et al., 2014).^[17] The species is also recorded from the parvifrons Zone in the Harlech Dome of North Wales, Clogau Formation, above Rhaiadr Bridge (Fletcher, op. cit. Fig. 8, F & G).

Arionellus quadrangularis Whitfield (1884), originally collected from the mid-Cambrian Braintree Formation at Old Hayward Quarry, Quincy, Massachusetts, US, had previously been assigned to Agraulos by Walcott and others.^[18] McMenamin (2002), however, erected Skehanos to accommodate the species as Skehanos quadrangularis.^[19]

Scandinavian species attributed by Westergård (1953)^[20] to Agraulos [i.e. A. difformis, A. aculeatus, A. acuminatus (all Angelin, 1851), and A. anceps] were transferred by Ahlberg & Bergström (1978)^[21] to Proampyx^[22] although several Lower Cambrian forms they also assigned to Proampyx would later be allocated to various other genera.