AKTASTINIAN (EARLY ARTINSKIAN, EARLY PERMIAN) BRACHIOPODS FROM THE JIMBA JIMBA CALCARENITE, WOORAMEL GROUP, CARNARVON BASIN, WESTERN AUSTRALIA N. W. G. R. Archbold and Shi School of Aquatic Science and Natural Resources Management, Deakin University, Rusden Campus, 662 Blackburn Road, Clayton, Victoria 3168 Archbold, N. W. & Shi, G. R., 1993:11:01. Aktastinian (Early Artinskian, Early Permian) brachiopods from the Jimba Jimba Calcarenite, Wooramcl Group, Carnarvon Basin, Western Australia. Proceedings of the Royal Society of Victoria 105 (2): 187-202. ISSN 0035-9211. The brachiopod fauna of the Jimba Jimba Calcarenite, Carnarvon Basin, Western Australia is reviewed and described. New species named are Neochonetes (Sommeriella) cockbaini. Cleiothyridina ovalis and Crassispirifer condoni. The fauna is assigned to the Strophalosia jimbaensis Zone and an Aktastinian (Early Permian) age is preferred for the fauna. THE CARNARVON Basin contains the best above’. This calcarenite was also treated as a for- preserved Early Permian marine succession of mational unit by Playford et al. (1975), but van all the Western Australian intracratonic basins de GraafTet al. (1977) and Hocking et al. (1987) and one of the richest sequences of Permian considered the Jimba Jimba Calcarenite to be a Gondwanan marine faunas. Brachiopod faunas member at the base of the Billidee Formation. from the Wooramel Group have received rela¬ We retain the unit as a formation because, tively minor attention until recently, apart from although limited in outcrop, it is clearly a few species from the Jimba Jimba Calcarenite mappable as shown by Condon (1967). described by Waterhouse (1970), Archbold At its type section 15 km west of the Jimba (1983, 1986) and Archbold & Thomas (1986a), Jimba Homestead the Jimba Jimba Calcarenite and small faunas from the One Gum and is 61 m thick. The unit is also recognised 14 km Billidee formations recently documented by east of the type section (Condon 1967). Archbold (1991). The present study describes the moderately diverse brachiopod fauna of the Jimba Jimba Calcarenite which is stratigraphic- PREVIOUS FAUNAL STUDIES ally below the Billidee Formation. This fauna No fossils were listed from the Jimba Jimba Cal¬ has been referred to in several reports (Condon carenite by Condon (1965) who considered its 1967, Thomas 1969, Playford et al. 1975) age to be Artinskian ‘by reference to its position although only a few specimens have been de¬ above the Callytharra Formation'. Later, Con¬ scribed and figured. Documentation of the don (1967: 88-91) provided a short list of fossil fauna confirms its biostratigraphical import¬ names and noted that the Jimba Jimba fauna ance as well as its faunal relationship with, and was ‘superficially very like that of the Cally¬ distinction from, the fauna of the Callytharra tharra Formation’. His list included Bryozoa, Formation, which is stratigraphically below the crinoid ossicles, Linoproductus spp., Neospirifer Wooramel Group. spp., Cleiothyridina, Phricodothyris, Dictyoclos- tus, 4Chonetes’ and Derby ia. Additional fossil STRATIGRAPHY collections from the Jimba Jimba Calcarenite The stratigraphy and structure of the Carnarvon were made by Dr A. E. Cockbain and Mr B. S. Basin have been reviewed by Playford et al. Ingram in 1966 from the Kennedy Range Dam (1975) and by Hocking et al. (1987). Only the site. Cockbain (1966) compared the fauna and pertinent stratigraphy concerning the Jimba lithology of the Jimba Jimba Calcarenite with Jimba Calcarenite is summarised below. those of the underlying Callytharra Formation The Jimba Jimba Calcarenite was originally and concluded that the gross faunal and litho¬ proposed by Condon (1965: 7) as a ‘formation of logical aspects of the two units were nearly ident¬ fossiliferous calcarenite with calcilutite and ical. In the same report, Cockbain listed for both sandstone conformably between the Moogooloo the Jimba Jimba Calcarenite and the Callytharra Sandstone below and the Billidee Formation Formation the following taxa: Neochonetes 187 188 N. W. ARCHBOLD AND G. R. SHI pratti (Davidson), Dictyoclostus callytharrensis to, the Wooramel Group include Strophalosia (Prendergast), Linoproductus cora foordi (Ether¬ jimbaensis Archbold (known from the Jimba idge) and Neospirifer spp. Waterhouse (1970) Jimba Calcarenite and from both the One described and figured Stepanoviella flexuosa Gum and Billidee formations), Neochonetes from the Jimba Jimba Calcarenite and also (Sommeriella) cockbain i sp. nov., Cleiothyridina favoured an Aktastinian age for the unit. ovalis sp. nov. and Globiella flexuosa Water- Dickins (1963) drew attention to the mol- house (all restricted to the Jimba Jimba Calcar¬ luscan faunas of the Wooramel Group, proposed enite). Characteristic species from the Cally¬ a faunal Stage C for the bulk of the unit, and tharra Formation such as Permorthotetes cally¬ pointed out the close relationship of the assem¬ tharrensis Thomas, Tornquistia occidentals blage with that of his Stage B (representing Archbold, Stictozoster senticosa (Hosking), faunas from the Callytharra Formation and Strophalosia irwinensis Coleman, Heteralosia equivalent units). He indicated an Early Artins- etheridgei (Prendergast), Elivina hoskingae kian (Aktastinian) for Stage C. Runncgar (1969) Archbold & Thomas, Tomiopsis woodwardi and Waterhouse (1970) questioned the validity Archbold & Thomas and Spirelytha Jredericksi of Dickins’s Stage C and suggested that it should Archbold & Thomas have not been discovered be combined with Stage B. As a result, Cockbain in the Wooramel Group. There are also differ¬ (1980) considered the combined Stage B and C ences between the Callytharra Formation and to be one biostratigraphical unit of‘a fairly long the Wooramel Group in the bivalve and gastro¬ time range occurring at a number of shelly hor¬ pod faunas (Dickins 1963: 10, also figs 3-5). izons, often of limited extent’, and considered Foraminifcra from the Jimba Jimba Calcarenite that it could not be used for detailed biostrati¬ are distinctive and represent a younger zone graphical correlation. than those of the Callytharra Formation (Palmieri 1990). In summary, in view of the distinctive and AGE OF THE JIMBA JIMBA abundant species confined to the Wooramel CALCARENITE FAUNAL ASSEMBLAGE Group and the many characteristic forms of the The Aktastinian age usually ascribed to the Callytharra Formation which are absent from Jimba Jimba Calcarenite was principally based the Wooramel Group, we consider that the on the stratigraphical position of the unit (over- fauna from the Wooramel Group represents lying the Callytharra Formation and underlying an important and separable biostratigraphical the Billidee Formation) and the close relation¬ horizon. An Aktastinian age was argued for the ship of the fauna with that of the Callytharra Wooramel Group by Archbold (1991). Formation. Ammonoids from the Callytharra Formation and the top of the Billidee Formation PRESERVATION, DEPOSITORIES AND are regarded as indicating late Sakmarian LOCALITIES (Sterlitamakian) and late Artinskian (Baigend- zhinian) ages respectively (Glenister & Furnish Material from the Jimba Jimba Calcarenite is 1961, Hocking et al. 1987). Alternative sug¬ moderately well preserved, generally as calcar¬ gestions that the Wooramel Group may be eous shells, but many specimens are incomplete Baigendzhinian in age (Cockbain 1980) have and frequently decorticated because of the diffi¬ been discussed by Archbold (1991). culty of extracting specimens from a limestone. Dickins (1963) and Archbold (1991) con¬ Specimens occur in a relatively homogeneous, in cluded that, although the Wooramel Group and some cases friable, grey to yellow fossiliferous the Callytharra Formation have some species calcarenite with minor calcilutite consisting in common, the two faunas have distinctive predominantly of brachiopod, bryozoan and , elements. Further data to support this view are crinoid fragments. ' presented in the present study. Several brachio- The described material is housed in the pod species from the Jimba Jimba Calcarenite Geological Survey of Western Australia, Perth occur in the Callytharra Formation, including (GSWA) and the Australian Geological Survey Callytharrella callytharrensis (Prendergast), Organisation, Canberra (AGSO). GSWA Neospirifer cf. N. hardmani (Foord), Trigono- material was collected by Dr A. E. Cockbain and treta neoaustralis Archbold & Thomas and Mr B. S. Ingram from a reference section of the Cleiothyridina cf. C. baracoodensis (Etheridge). Jimba Jimba Calcarenite at the Kennedy Range \ Species occurring abundantly in, and confined Dam site (GSWA field numbers F6243-F624S. EARLY PERMIAN BRACHIOPODS 189 F6251-F6254) and by Dr S. K. Skwarko from Subfamily Rugosochonetinae Muir-Wood, the type section of the Jimba Jimba Calcarenite 1962 (GSWA field number 94218). The Kennedy Range Dam site is across the Gascoyne River, Genus Neochonetes Muir-Wood, 1962 just north of the Jimba Jimba type locality. Subgenus Neochonetes (Sommeriella) AGSO material was also collected from the type Archbold, 1982 section of the Jimba Jimba Calcarenite (AGSO locality W03) and is registered in the Common¬ Type species. Chonetes prattii Davidson, 1859. wealth Palaeontological Collection (numbers Neochonetes (Sommeriella) cockbaini with CPC prefix). Archbold sp. nov. Fig. 1A-L SYSTEMATIC PALAEONTOLOGY Neochonetes (Sommeria) pratti.—Archbold 1981: The brachiopod fauna of the Jimba Jimba Cal¬ 114, fig. 5V, W (non cet.). carenite consists of the following species. All Etymology. For Dr A. E. Cockbain, geologist and species are illustrated but only new species and palaeontologist. material adding to the description of previously named species are described in this study. Holotype. CPC 19869, a complete shell, from the type section of the Jimba Jimba Calcarenite (AGSO locality Perrnorthotetes cf. P. lindneri Thomas, 1958 W03). (Fig. 8A) Paratypes. GSWA F43871-F43872, two juvenile dor¬ Neochonetes (Sotnmeriella) cockbaini Archbold sal valves, from GSWA locality F6244; GSWA sp. nov. (Fig. 1A-L) F43873, one mature dorsal valve, from GSWA locality Strophalosia jimbaensis Archbold, 1986 (Fig. F6252; CPC 31484-31488, CPC 19869, one incom¬ 2A-J) plete dorsal valve, four complete shells and one incom¬ Reedoconcho? sp. (Fig. 3A) plete shell, all from AGSO locality W03. Callytharrella callytharrensis (Prendergast, Size ranges. Maximum width: 14-40 mm; hinge 1943) (Fig. 3N, O) width: 14-36 mm; shell height: 8-24 mm; shell thick¬ Costatumulus cf. C. irwinensis (Archbold, 1983) ness: 5-9 mm. (Fig. 3C-G, L) Diagnosis. Very large Neochonetes (Sommer¬ Globiella flexuosa (Waterhouse, 1970) (Fig. 3B, iella) with deep, relatively narrow sulcus and H-K) robust dorsal septa at maturity. Productidina or Chonctidina indet. (Fig. 3M) Cleiothyridina ovalis Shi sp. nov. (Fig. 4A-P) Description. Convexity of ventral valve distinct Cleiothyridina cf. C. baracoodensis (Etheridge, with prominent sulcus arising close to umbo, 1903) (Fig. 5A-G) usually with deep median valley. Dorsal valve Cyrtellal sp. (Fig. 6A, B) planar to gently concave with narrow, distinct Neospirifer hardmani (Foord, 1890) (Fig. 6C-E, fold developed anterior to umbo, broadening to J) anterior valve margin. Greatest width of shell at Neospirifer cf. N. foordi Archbold & Thomas, midlength or anterior to midlength. Exterior 1986a (Fig. 6F-I, K) surface with weakly developed growth lines and Crassispirifer condoni Archbold & Shi sp. nov. fine capillae (about 3-4 per mm at 1 cm from (Fig. 7A-N) umbo), increasing in number by bifurcation. Trigonotreta neoaustralis Archbold & Thomas, Ventral interarea low, dorsal interarea very low. 1986a (Fig. 8B-E) Cardinal spines poorly known. Ventral umbo Tomiopsis cf. T. rams Archbold & Thomas, low, rounded. 1986b (Fig. 8G-I) Ventral interior poorly known. Teeth short, Spirelytha sp. (Fig. 8F) stout. Delthyrium broad, relatively small. Hoskingial sp. (Fig. 8J) Cardinal process low, robust at maturity. Chilidium not known. Alveolus deep, promi¬ nent at base of process at maturity. Socket ridges Order Chonetida Nalivkin, 1979 prominent, sockets distinct, deep, lateral septa Suborder Chonetidina Muir-Wood, 1955 and median septum prominent and thickened at Superfamily Chonetacea Bronn, 1862 maturity, weakly developed in submature indi¬ Family Rugosochonetidae Muir-Wood, viduals. Brachial ridges indistinct. Interior of 1962 submature valves with rows of radial papillae. 190 N. W. ARCHBOLD AND G. R. SHI EARLY PERMIAN BRACHIOPODS 191 Fig. I. Neochonetes (Sommeriella) cockbaini Archbold sp. nov. A-D, CPC 19869, holotype, complete shell in ventral, posteroventral, anterior and dorsal views, x 1.8. E, GSWA F43871-F43872, juvenile dorsal valves, interior views, x 3.5. F, CPC 31485, incomplete shell in dorsal view, x 1.8. G, CPC 31484, incomplete dorsal valve, interior view, x 2. H, GSWA F43873, dorsal valve exterior view, x 1.5.1-J, CPC 31486, shell in ventral and dorsal views, x 1.8. K, CPC 31487, shell in ventral view, x 2. L, CPC 31488, shell in ventral view, x 2.5. At full maturity papillae restricted to anterior specimens, rarely high and narrowly triangular, and lateral margins of valve interior. Posterior flat or very gently concave, finely striated paral¬ margin of valve smooth. lel to hinge line. Delthyrium relatively small and narrow, filled with small, gently convex pseudo- Discussion. This distinctive large species can be deltidium. Umbo small and broad, little ex¬ differentiated from N. (S). prattii (Davidson) tended, with broad umbonal angle varying from (see Archbold 1981 for description of species) by 93° to 130°, truncated by usually weakly devel¬ its large size, characteristic deep sulcus and ro¬ oped cicatrix which is relatively small (4 mm in bust dorsal septa at maturity. N. (S.) prattii from diameter in largest specimens). Ears very' small, the Sterlitamakian Callytharra Formation and ill-defined. Cardinal extremities broadly correlative units in Western Australia is prob¬ rounded. Umbonal slopes gently convex. Lateral ably ancestral to N. (S.) cockbaini. and anterior slopes high and steep. Gentle The younger species N. (S.) tenuicapillatus median sulcus is present in most ventral speci¬ Archbold, 1981 from the Late Baigendzhinian mens examined, commences from about pos¬ Wandagee Formation possesses a more deeply terior third of shell curvature length and persists concave dorsal valve and finer capillae than the until anterior margin of shell, always shallow new species. and broad, strongest over midlength of valve. Dorsal valve moderately and evenly concave. Order Productida Sarycheva & Sokolskaya, Dorsal interarea distinct, broad, usually slightly 1959 lower than ventral interarea, bisected by small, Suborder Strophalosiidina Waterhouse, triangular notothyrium filled by gently convex 1975 chilidium. Superfamily Strophalosiacea Schuchert, Ventral valve ornament consists of spines and 1913 broad, weakly developed concentric lamellae. Family Strophalosiidae Schuchert, 1913 Coarse, suberect spines appear in a row along Subfamily Strophalosiinae Schuchert, 1913 hinge line and in up to three rows on cars, 0.8 mm across spine base. Body spines numer¬ Genus Strophalosia King, 1844 ous and evenly scattered on venter, slightly Type species. Strophalosia gerardi King, 1846. smaller than spines on ears, suberect, with swollen bases about 0.6-1 mm across, quincun- Strophalosia jimbaensis Archbold, 1986 cially arranged, 2-2.5 mm apart. Concentric Fig. 2A-J lamellae ill-defined in most specimens; fine Strophalosia jimbaensis Archbold 1986: 102, fig. 2A- growth lamellae at times crowded together to G.—Archbold 1991: 60, fig. 3A-P (with synonymy). form broad steps 2-5 mm wide. Dorsal valve lacks spines but possesses strongly developed Holotype. CPC 24405, a conjoined shell from the type concentric lamellae, 5-8 in 5 mm, and quincun- section of Jimba Jimba Calcarenite, Carnarvon Basin, cially arranged subcircular to elongate dimples figured by Archbold (1986). which are 0.8-1 mm in diameter and numbering Size ranges. Maximum width: 26-43 mm; hinge 3-4 in 5 mm. width: 12-25 mm; shell height: 25-39 mm; shell thick¬ Cardinal process arises from strong median ness: 75-18 mm; ventral intcrarea height: 1.5-4 mm; septum and lateral ridges which surround small, dorsal interarea height: 1-2 mm. deep sockets. Cardinal process moderately high, Description. Juvenile or submature shells erect, inclined at up to 65° to plane of dorsal vis¬ slightly elongately oval in outline, mature speci¬ ceral disc, trilobed in external view with central mens transversely oval; maximum width at lobe being most prominent, quadrilobed in midlength. internal view because of development of fine Hinge width varies from about 0.43 of maxi¬ median depression on central lobe. Median mum width to 0.70 of maximum width. Ventral septum extends to about midlength of dorsal interarea broadly triangular in shape in most valve, with tapering anterior end. Adductors 192 N. W. ARCHBOLD AND G. R. SHI EARLY PERMIAN BRACHIOPODS 193 '*8- 2. Strophalosiajimbaensis Archbold, from GSWA locality F94218. A, F, GSWA F43874, shell in dorsal and ventral views, x 1.6. B, GSWA F43875, shell in ventral view, x 1.6. C, G, GSWA F43876, dorsal valve interior view and cardinal process external view, x 1.6 and x 3. D, H, GSWA F43877, shell in lateral and anteroventral v'iews, x 1.6. E, GSWA F43878, dorsal valve interior view, x 1.6.1, GSWA F43879, gerontic shell in dorsal view, x 1-3. J, GSWA F43880, shell in ventral view, x 1.6. elongately oval in shape, smooth, bisected by (immature)-0.84 (mature); width of ventral muscle Median septum, moderately differentiated with field: 0.7-0.9 mm; length of ventral muscle field: anterior adductors being most prominent. 11-15 mm. Brachial ridges narrow, slightly to moderately Diagnosis. Shells of small to medium size for elevated above disc floor, smooth. A distinct genus; slightly transversely oval at maturity, Marginal ridge present in one dorsal interior, gently plano-convex to gently concavo-convex surrounding visceral disc. Numerous fine papil¬ in lateral profile; anterior commissure unipli- lae present on floor of visceral disc with excep¬ cate; concentric growth lamellae pronounced, tion of brachial ridges and adductors, as well as numbering 8-14 in 5 mm at midlength of on anterior trail where papillae may be arranged mature specimens. ,n distinct rows. Slight anterior thickening of dorsal valve occurs in all specimens available Description. Most specimens crushed and com¬ but varies in degree of development. pressed to varying degrees but all appear to be gently plano-convex to gently concavo-convex Discussion. The species was defined by Archbold in lateral profile. Outline slightly elongately oval (1986) on the basis of only four poorly preserved in immature specimens, transversely oval at full specimens, no isolated dorsal valves being avail¬ maturity. Maximum width at midlength. able. The present study of topotypic material has Ventral valve flat or gently concave in overall confirmed characteristics of the species such as appearance although umbonal region usually the large size at maturity, the weak ventral gently swollen. Ventral umbo erect, moderately sulcus, and the strongly developed concentric extended, truncated by small foramen of 1- lamellae and dimples on the dorsal valve. 2 mm diameter. Immature specimens almost The species was compared with allied forms lack sulcus, with nearly rectimarginate anterior by Archbold (1986: 102; 1991: 62). commissure. Mature specimens with very gentle median depression which deepens particularly Order Athyridida Dagys, 1974 at anterior margin, giving rise to moderately Superfamily Athyridacea McCoy, 1844 strongly uniplicate anterior commissure. Dorsal Family Athyrididae McCoy, 1844 valve gently to moderately convex, fastigium weakly developed, median fold results in unipli¬ Genus Cleiothyridina Buckman, 1906 cate anterior commissure. Concentric growth lamellae pronounced on Type species. Atrypa pectinifera Sowerby, 1840. both valves, numbering 8 in 5 mm at 8 mm from Cleiothyridina ovalis Shi sp. nov. ventral umbo, 10 in 5 mm at midlength of shell, and 15 or more in 5 mm near anterior margin Fig. 4A-P where a geniculate band 5-7 mm wide with Etymology. In reference to the oval outline of the crowded growth lamellae is observed in all large species. (mature) specimens. Presence of this genicu- llolotype. GSWA F43896, a complete submature shell lated band probably indicates full maturity of from GSWA locality F94218, Jimba Jimba Calcare- shells. Shell surfaces too abraded to preserve nitc, Carnarvon Basin. radial spines in most specimens, but traces Paratypes. GSWA F43894, one ventral valve, from of radial lines on lamellae present on some GSWA locality F6252; GSWA F43895, a complete specimens. shell, from GSWA locality F6243; GSWA F43896- Teeth robust, rounded, supported by dental F43903, one complete shell and seven ventral valves, plates which are fused into umbonal wall. Ven¬ from GSWA locality 94218. tral muscle field relatively large, occupying third Size ranges. Maximum width: 21-46 mm; shell length: to almost half ventral valve floor, well differen¬ 21-32 mm; shell thickness: 8.2 mm (measured from tiated into adductor and diductor scars. Adduc¬ holotype, the only one that appears not to have been tor scars heart-shaped, located at posterior end crushed or distorted); ratio of shell length to width: 1 of muscle field just below teeth, well depressed, EARLY PERMIAN BRACHIOPODS 195 3- A, Reedoconcha? sp., GSWA F43881, from locality F6248, incomplete ventral valve in ventral view, x 2.2. ’ Globiellajlexuosa (Waterhouse). B, GSWA F43882, from locality F6247, ventral valve in ventral view, f 1 *5- H, GSWA 43883, from locality F6247, ventral valve in anterovcntral view, x 1.5.1, J, GSWA F43884, from °cality F6247, ventral valve in lateral and ventral views, x 1.5. K, GSWA 43885, from locality F6244, ventral P^Ive in ventral view, x 1.5. C-G, L, Costatumuluscf. C. irwinensis(Archbold). C, GSWA F43886, from locality 6248, ventral valve in lateral view, x 1.8, D, GSWA F43888, from locality F6247, ventral valve in ventral view, GSWA F43891, from locality F6244, dorsal valve interior view, x 2. F, GSWA F43889, from locality 6247, ventral valve in ventral view, x 1.6. G, GSWA F43887, from locality F6248, ventral valve in ventral view, H) ’ ^ GSWA F43890, from locality F6247, dorsal valve interior view, x 2. N, O, Callylharrella callytharrensis rcndergast). N, GSWA F43892, from locality F6246, ventral valve in ventral view, x 1.2. O, CPC 31489, ^corticated dorsal valve in dorsal view, x 1. M, Productidina or Chonetidina indet., GSWA F43893, from locality F6243, ventral valve in ventral view, x 2. smooth, anteriorly passing onto low but promi- Cleiothyridina seriata Grant (1976: 199, pi. nent median ridge bisecting diductors. Diductor 53, figs 1-30, pi. 54, figs 1-62, text-fig. 18) from scars large, deeply depressed, separated from the Baigendzhinian or Kungurian fauna of the rcst of valve floor by raised ridges, weakly Rat Buri Limestone in south Thailand is smaller striated. Remainder of valve floor marked by in size, more rounded in outline, and moderately f^dial, in places anastomosing, vascular mark- biconvex in profile in comparison with C. ova/is. ,n8s. Interior of dorsal valve unknown. Another species figured as Cleiothyridina sp. from the Sterlitamakian fauna of the Ka Yao Discussion. The material is characterised by the Noi Formation of south Thailand (Waterhouse Iow convexity, the ill-defined sulcus and the ab¬ et al. 1981) is also small and little inflated like sence of a fold, and by the distinct uniplicate the Jimba Jimba material. The Thai form was ahterior commissure at maturity. These charac¬ said to be immature and thus cannot be ident¬ teristics are also displayed by the specimens ified or compared with any named species with from the Callytharra Formation figured by certainty, but it differs from C. ovalis in being Foord (1890) and Etheridge (1903) as Cleio- rounded in outline rather than elongately oval or lhyris (= Cleiothyridina) macleayana (not transversely oval. Etheridge 1889), judged from their illustrations and descriptions. The type material of Cleiothy- ddina macleayana (Etheridge 1889: 208, pi. 17, Order Spiriferida Waagen, 1883 %s 1-5) from the Baigendzhinian Noonkanbah Superfamily Spiriferacea Waagen, 1883 Formation of the Canning Basin resembles the Family Spiriferidae King, 1846 new species in size, outline and the anterior Subfamily Neospiriferinae Waterhouse, commissure but is clearly distinguished by its 1968 much more convex dorsal valve. The same is Genus Crassispirifer Archbold & Thomas, true of the comparison with C. semiconcava 1985 Waagen (1884: 481, pi. 41, figs 4-6) from the Late Artinskian to Kungurian Amb Formation Type species. Spirifer rostalinus Hosking, 1931. °f the Salt Range, Pakistan. The Salt Range Crassispirifer condoni Archbold & Shi sp. nov. species is further distinguished by its more strongly folded anterior commissure. C. roysii Fig. 7A-N var. penta Prendergast (1935: 24, pi. 2, figs 13- Etymology. For Mr M. A. Condon, who first proposed }$) from the Luiluigui Station, Kimberley Div- and mapped the Jimba Jimba Calcarenite in the ISJon, approaches the new species in size and Carnarvon Basin. Particularly in its flat to gently concave ventral valve, but this species is pentagonal in outline Ilolotype. CPC 31493, a complete specimen with valves conjoined, from BMR locality W03. and has a high dorsal valve and a deep, well pro¬ nounced sulcus and strongly uniplicate anterior Paratypes. CPC 31493-31496, a complete shell, two commissure. C. baracoodensis (Etheridge 1903: dorsal valves and one ventral valve from BMR locality F7, pi. 3, figs 5-9) from the Callytharra Forma- W03. GSWA F43912-F439I7, four ventral valves lion of the Carnarvon Basin is distinguished and two dorsal valves, all incomplete, from GSWA locality F6243. from the new species by its gently to moderately convex ventral valve and more inflated dorsal Size ranges. Maximum width: usually 40-70 mm, valve. rarely up to 90 mm; height: 18-32 mm; thickness 196 N. W. ARCHBOLD AND G. R. SHI