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Journal of Paleontology 92(3):442–458 Genus Buenellus Blaker, 1988


Type species.—Buenellus higginsi Blaker, 1988 from the lower part of the Buen Formation, Peary Land, North Greenland, by original designation.


Other species.—Buenellus chilhoweensis n. sp. (see below).


Diagnosis.—(Emended from Babcock and Peel, 2007.) Prox- imal portion of posterior cephalic margin approximately trans- verse or weakly posterolaterally oriented when traced distally from axial furrow to adgenal angle; adgenal angle weak or absent so that base of genal spine lies slightly posterior to or opposite lateral margins of LO. Genal spine broad-based. Intergenal spine absent or reduced to small dorsal swelling on posterior cephalic border immediately distal to adgenal angle. Glabella slightly tapered anteriorly. SO deepest midway between sagittal line and axial furrow, extremely shallow or not incised adjacent to axial furrow. Cephalic border furrow, axial furrow, and glabellar furrows, especially those anterior to SO, very shallow. Short preglabellar field. Weak parafrontal band extends around lateral and anterior margins of LA. Ocular lobe narrow (tr.), anterior portion of more subdued relief than pos- terior portion, summit lower than LA and separated from it by break in slope; inner margin poorly defined from interocular area; posterior tip transversely opposite lateral margin of SO or L1. Interocular area slightly narrower to slightly wider (tr.) than width (tr.) of extraocular area opposite S1. Intergenal ridge and posterior ocular line converge at intergenal swelling. Fine granulations on external surface of exoskeleton. Thorax (only known from type species) of 17 or 18 segments, maintaining width or widening slightly backward to eighth segment, then tapering posteriorly. Pygidium simple; may bear one thoracic- like segment fused to anterior edge. Posterior margin of pleurae of first nine or ten segments sigmoidally curved. Pleural spines short (exsag.), tips opposite axial ring of next one or two segments.


Remarks.—Buenellus was previously only known with certainty from the type species in North Greenland (see Babcock and Peel, 2007, p. 404, for discussion of a supposed occurrence in Novaya Zemlya). Discovery of Buenellus chilhoweensis n. sp. demonstrates that the genus occupied both the Innuitian and Iapetan margins of Laurentia. The generic diagnosis is herein emended to accommodate Buenellus chilhoweensis n. sp. and expanded to include several previously unspecified features that distinguish Buenellus from similar taxa. Blaker and Peel (1997) discussed differences between


Buenellus and several other similar genera, including the nevadioids Nevadella and Nevadia, the possible nevadioid Limniphacos, the holmiid olenelloids Holmia Matthew, 1890 and Kjerulfia Kiaer, 1917, and the problematic Callavia Matthew, 1897, which has been variously considered a holmiid


(Palmer and Repina in Whittington et al., 1997; Jell and Adrain, 2003) or a judomioid (Lieberman, 2001). Buenellus also shares many features with Pseudojudomia egregia Egorova in Gorjansky et al., 1964, which is the type and only known species of Pseudojudomia, including details of the glabellar furrows, the nature of the contact between the ocular lobes and the anterior glabella, and a general cephalic effacement. Although it is possible that some of these shared features represent symplesiomorphies or homoplasies, it is likely that the two genera are closely related. (A formal hypothesis of their relationship will be presented in a forthcoming cladistic analysis [Webster, in preparation].) The two genera are most reliably distinguished by differences in the form of the posterior cephalic margin: in Pseudojudomia egregia the posterior cephalic margin arcs posterolaterally and uniformly curves into the inner margin of the genal spine so that the spine and the cephalic border are smoothly confluent; whereas in Buenellus the posterior cephalic margin is more transversely oriented (often with a slight anterior deflection at the adgenal angle) when traced abaxially and there is a more distinct (although certainly not sharply) curved geniculation marking where the genal spine contacts the posterior cephalic border. Other publications relevant to the diagnosis and validity of the genus Buenellus include: Blaker (1988, p. 34–35), Palmer and Repina (1993, p. 31), Blaker and Peel (1997, p. 50–52), Palmer and Repina in Whittington et al. (1997, p. 428), Jell and Adrain (2003, p. 353, 474), and Babcock and Peel (2007, p. 411–412).


Buenellus chilhoweensis new species Figure 4


1890 undetermined species of Olenellus; Walcott, p. 570.


1890 Olenellus thompsoni?; Walcott, table on p. 575 (eastern Tennessee occurrence).


1890 Olenellus, sp.?; Walcott, p. 583.


1891 species of Olenellus closely allied to Olenellus thompsoni and Olenellus asaphoides in that portion of the head preserved; Walcott, p. 154.


1895 trilobites; Keith, 1895, p. 3. 1933 olenellid trilobites; Resser, p. 746. 1936 olenellid trilobites; Grabau, p. 12. 1949 trilobites; King, p. 520. 1952 Olenellus; King et al., table 2 on p. 4. 1952 Olenellus sp.; King et al., p. 15. 1960 Olenellus; King and Ferguson, p. 36. 1965 Olenellus; Neuman and Nelson, p. D29. 2016 nevadiid trilobite; Hageman and Miller, p. 146, fig. 7d.


Holotype.—USNM 645831 (internal and external mold; Fig. 4.3, 4.4).


Figure 4. Buenellus chilhoweensis n. sp. from the Murray Shale, Chilhowee Mountain, Blount County, Tennessee, U.S.A. (1) Internal mold of cephalon from ICS-10567, USNM 633932; (2) internal mold of cephalon from ICS-10568, USNM 645832.; (3, 4) internal and external mold, respectively, of holotype cephalon from ICS-10567, USNM 645831; (5, 6) internal and external mold, respectively, of cephalon from ICS-10568, USNM 645833; (7) external mold of cephalon from ICS-10568, USNM 645834; (8) latex peel of external mold of incomplete cephalon found by Walcott in 1889 and mentioned by Walcott (1890, 1891), USNM 18446, dorsal view. (1–7) from upper part of Murray Shale, locality CM3; (8) from Little River Gap area (USNM Locality 17). Scale bars 5mm.


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