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200 SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY The range of body sizes in the megapodes varies from the extinct Progura gallinacea De Vis (1888) of Australia, which reached the size of a turkey {Meleagris), to Megapodius laperouse of Micronesia, the smallest described species (28-30 cm). Steadman (1993a) reported an extinct, as yet undescribed species of Megapodius from the late Quaternary of 'Eua, Tonga, which was smaller than any other known megapode. The earliest known fossil occurrence of the Megapodiidae is from the Pliocene (Boles and Mackness, 1994); most records are from the Pleistocene. Because of its age and diminutive size, a recently identified megapode from late Oligocene deposits of central Australia, outside the current distribution of this family, is of considerable interest. FOSSIL RECORD OF MEGAPODES Mourer-Chauvire (1982) initially indicated the presence of the Megapodiidae in the Eocene-Oligocene deposits of Quercy, France. Later she regarded these as belonging to a more primitive family of galliforms, the Quercymegapodiidae (Mourer- Chauvire, 1992), consisting of the single genus Quercymegapodius, which she created for Palaeocryptonyx depereti Gaillard (1908), and a new species, Q. brodkorbi Mourer-Chauvire (1992). This family was interpreted as being the sister group of all the living Galliformes. Excluding the Quercymegapodiidae, there are no known occurrences of fossil megapodes outside Australia and the islands of the southwest Pacific. The Pleistocene record of megapodes is dominated by the fossil genus Progura. Progura gallinacea was originally described by De Vis (1888) as a large pigeon. Van Tets (1974) recognized that the specimens belonged to a megapode larger than any living species. Additional material identified by De Vis as pigeons, as well as material he identified as storks or as bustards, also was included in this taxon (van Tets, 1974; van Tets and Rich, 1990). Specimens of a smaller but related form were described as P. naracoortensis by van Tets (1974), to which were referred fossils that previously had been attributed to Alectura lathami (Lydekker, 1891; Longman, 1945). It was later suggested (van Tets, 1984) that the two taxa of Progura actually represented a single, sexually dimorphic species. The only other Australian species in the fossil record is Leipoa ocellata, which has been recovered from late Pleistocene deposits in South Australia (van Tets, 1974). The only Tertiary records come from the Pliocene of Australia. De Vis (1889) described the fossil megapode Chosornis praeteritus from Chinchilla, Queensland, which van Tets (1974) later placed in the synonymy of the Pleistocene species Progura gallinacea. Boles and Mackness (1994) reported on the presence of P. cf. naracoortensis at Bluff Downs, Queensland. A variety of fossil species of Megapodius, mostly extinct forms, are known from South Pacific islands from New Caledonia (Balouet and Olson, 1989) eastward into Polynesia (Steadman, 1989, 1993a, 1993b, 1995; see also Jones et al., 1995). Most of these sites are of Holocene age, and most or all of the extinctions were anthropogenic. The enigmatic Sylviomis neocaledoniae of New Caledonia was first described as a ratite (Poplin, 1980) but later was considered to be a large, flightless megapode (Poplin and Mourer- Chauvire, 1985). Balouet and Olson (1989) and C. Mourer- Chauvire (pers. comm., 1996) believe that that Sylviomis belongs to the Galliformes but is best placed in its own family. METHODS.—Measurements mostly follow those of Steadman (1980) and were made with digital calipers and rounded to the nearest 0.1 mm. Osteological nomenclature follows Baumel and Witmer (1993); taxonomic nomenclature for the Megapodiidae follows Jones et al. (1995). Comparisons were made with representatives of all extant genera of megapodes {Macrocephalon maleo, Eulipoa wallacii, Alectura lathami, Leipoa ocellata, Talegalla jobiensis, T. fuscirostris, Aepypodius arfakianus, A. bruijni, Megapodius reinwardt, M. freycinet, M. eremita, M. pritchardi, M. cumingii, M. nicobarensis) as well as with Progura gallinacea. ACKNOWLEDGMENTS.—We thank T. Rich (Museum of Victoria) and P. Vickers-Rich (Monash University) for permitting us to work on this fossil; T. Rich for supplying information from his field notes on the discovery of this specimen; D. Steadman for discussion of this fossil and of his work with megapodes; S. Olson, D. Steadman, and C. Mourer-Chauvire for valuable criticisms of the manuscript; T. Wickey and C. Bento (Australian Museum) for taking the photographs; R. Schodde and W. Longmore (Australian National Wildlife Collection), M. LeCroy (American Museum of Natural History) and S. Olson and J. Dean (National Museum of Natural History, Smithsonian Institution) for access to comparative material; and the Australian Museum for providing a venue in which to carry out this study. Systematic Paleontology Order GALLIFORMES Family MEGAPODIIDAE Because of the gracility of the trochleae of the tarsometatarsus described herein compared with those of some other megapodes, the Pinpa fossil bears a superficial resemblance to the tarsometatarsus of a medium-sized pigeon, such as the Wonga Pigeon, Leucosarcia melanoleuca Latham. Rich et al. (1991) originally placed it in the Columbidae, which is understandable because there are superficial similarities between the tarsometatarsus in these two families, as shown by De Vis's (1888) original description of the fossil megapode Progura gallinacea as a relative of the crowned pigeons {Gourd). Van Tets (1974) discussed characters that differentiate the two groups. The tarsometatarsus in the Megapodiidae may be identified by the following combination of characters: three cristae hypotarsi (medialis large) and four sulci hypotarsi (medialis broad), only one of which is enclosed; distal extension of crista media-

NUMBER 89 201 lis hypotarsi along the shaft flat and virtually absent; shaft dorsoplantarly compressed; depression on plantar face; fossa metatarsi I distinct; and trochleae metatarsi II and IV with equal distal extension. This suite of features separates the Megapodiidae from other living and most extinct Galliformes. The fossil and other Megapodiidae differ from the Quercymegapodiidae by having the crista metatarsi medialis projecting further plantarly, trochlea metatarsi II not globular, and trochleae metatarsi II and IV with equal distal extension (characters from Mourer-Chauvire, 1992). In species of the Gallinuloididae the depression on the plantar surface is more extensive than in the Megapodiidae. The Megapodiidae also differ from the Columbidae by lacking an indentation on the medial border of the shaft distal to the fossa metatarsi I and by having the sulcus hypotarsi in the same dorsoplantar line as the eminentia intercondylaris (in proximal view) rather than offset laterally; also, the trochlea metatarsi II is more in the same lateromedial line as trochleae metatarsi III and IV (in distal view) instead of being recessed plantarly and rotated medially. The fossil exhibits a suite of characters unlike those found in other genera of the Megapodiidae, for which reason it is recognized as a new genus. Ngawupodius, new genus TYPE SPECIES.—Ngawupodius minya, new species, by original designation and monotypy. ETYMOLOGY.—Ngawu, in South Australia an Aboriginal name for the Malleefowl Leipoa ocellata (see Peter and Peter, 1993), and -podius, Latinized Greek, "footed," in allusion to the similarities between the tarsometarsi of these taxa. DIAGNOSIS.—The proximal end is medially flared less than in Megapodius or Progura but is more so than in Alectura. The shape and size of the cotyla medialis are about the same as the cotyla lateralis in proximal view; the dorsal rim is not produced as far dorsally, and the medial rim is thin, unlike the conditions in Leipoa or Alectura. The sulcus hypotarsi is proportionally small in proximal view compared with all the modern taxa. The robustness of the lateral side of the hypotarsus in proximal view is blocky, unlike that in Megapodius. The plantar extension of the crista medialis hypotarsi is greater than in Alectura, Talegalla, Aepypodius, or Macrocephalon but is less than in Megapodius, Eulipoa, or Leipoa. The relative plantar extension of the crista lateralis hypotarsi differs from that in Alectura, Talegalla, Aepypodius, or Progura in being about one-half that of the crista medialis. The distally projecting process on the distal end of the hypotarsus is smaller than that in Megapodius. The dorsoventral compression of the shaft is greater than in Talegalla or Aepypodius. The sides of the shaft are relatively parallel and do not widen toward the distal end, unlike Alectura, Leipoa, Aepypodius, Talegalla, Macrocephalon, or Progura. The relative development of the tuberositas M. tibialis cranialis is shorter in the fossil than in the modern forms. The fossa metatarsi I is not as distinct as in Megapodius, Leipoa, or Progura and has little medial extension. The trochleae are gracile and are not swollen as in the other genera, particularly Megapodius. The trochlea metatarsi II is at the same level as the trochlea metatarsi IV, rather than slightly above, when viewed either distally (unlike Megapodius, Leipoa, or Talegalla) or dorsally (unlike Megapodius, Leipoa, Aepypodius, or Progura). The trochlea metatarsi II is neither inflated nor globular as it is in Megapodius or Eulipoa, and it does not diverge strongly medially, unlike Alectura, Leipoa, Aepypodius, Talegalla, Macrocephalon, or Progura. The trochlea metatarsi IV does not project laterally, unlike Megapodius or Eulipoa. The articular groove of the trochlea metatarsi IV is moderately well developed, more so than in Alectura, Leipoa, Aepypodius, Talegalla, or Progura, but is less distinct than in Megapodius. Ngawupodius minya, new species FIGURE 1A-C HOLOTYPE.—Complete right tarsometatarsus, Paleontology Collection of the Museum of Victoria (MV), Melbourne, P160493. Collected by I. Parker on 12 May 1979. TYPE LOCALITY.—South end of Lake Pinpa, South Australia (31°08'31"S, 140°12'47"E; T.H. Rich, pers. comm., 1996). HORIZON.—Namba Formation, Ericmas Fauna, late Oligocene. ETYMOLOGY.—Minya, in South Australia an Aboriginal word for "small" (Reed, 1977); for the purposes of nomenclature, minya should be considered to be without gender. DIAGNOSIS.—As for the genus. DESCRIPTION.—The fossil is from an adult bird because the surface lacks porosity, the tarsal cap is completely fused to the proximal end of the metatarsals, the hypotarsus is fully formed, and the metatarsals are fully fused over their entire length. In immature Leipoa ocellata, the tarsometatarsi may approach the size in that of adult birds yet still be highly porous and incompletely fused. Total length 40.2 mm; proximal width 8.1 mm; distal width 9.5 mm; distal depth 5.7 mm. Eminentia intercondylaris low, about same height as rim of cotyla medialis; both higher than rim of cotyla lateralis. Depth of crista hypotarsi medialis about one-half that of proximal end of bone (proximal depth to hypotarsus 4.4 mm; proximal depth with hypotarsus 8.0 mm), with laterally directed projection at end. In proximal view, sulcus medialis hypotarsi slightly laterad of eminentia intercondylaris, three shallow sulci lateralis hypotarsi and two low cristae lateralis hypotarsi on rather square hypotarsus. In lateral view, hypotarsus short (5.1 mm). Ridge extending distally from hypotarsus on facies plantaris very low. Shaft broad (midshaft width, 4.3 mm; shaft width at proximal edge of fossa metatarsi I, 4.5 mm) but dorsoplantarly flattened (midshaft depth, 2.6 mm; shaft depth at proximal edge of fossa metatarsi I, 2.8 mm), markedly so on medial side; lateral margin straight, medial margin somewhat concave distally to fossa metatarsi I; distal to fossa produced more medially. Fossa metatarsi I elongate (5.8 mm). Fos-

NUMBER 89 201<br />

lis hypotarsi along the shaft flat and virtually absent; shaft dorsoplantarly<br />

compressed; depression on plantar face; fossa<br />

metatarsi I distinct; and trochleae metatarsi II and IV with<br />

equal distal extension. This suite of features separates the<br />

Megapodiidae from other living and most extinct Galliformes.<br />

The fossil and other Megapodiidae differ from the Quercymegapodiidae<br />

by having the crista metatarsi medialis projecting<br />

further plantarly, trochlea metatarsi II not globular, and<br />

trochleae metatarsi II and IV with equal distal extension (characters<br />

from Mourer-Chauvire, 1992). In species of the Gallinuloididae<br />

the depression on the plantar surface is more extensive<br />

than in the Megapodiidae.<br />

The Megapodiidae also differ from the Columbidae by lacking<br />

an indentation on the medial border of the shaft distal to the<br />

fossa metatarsi I and by having the sulcus hypotarsi in the same<br />

dorsoplantar line as the eminentia intercondylaris (in proximal<br />

view) rather than offset laterally; also, the trochlea metatarsi II<br />

is more in the same lateromedial line as trochleae metatarsi III<br />

and IV (in distal view) instead of being recessed plantarly and<br />

rotated medially.<br />

The fossil exhibits a suite of characters unlike those found in<br />

other genera of the Megapodiidae, for which reason it is recognized<br />

as a new genus.<br />

Ngawupodius, new genus<br />

TYPE SPECIES.—Ngawupodius minya, new species, by original<br />

designation and monotypy.<br />

ETYMOLOGY.—Ngawu, in South Australia an Aboriginal<br />

name for the Malleefowl Leipoa ocellata (see Peter and Peter,<br />

1993), and -podius, Latinized Greek, "footed," in allusion to<br />

the similarities between the tarsometarsi of these taxa.<br />

DIAGNOSIS.—The proximal end is medially flared less than<br />

in Megapodius or Progura but is more so than in Alectura. The<br />

shape and size of the cotyla medialis are about the same as the<br />

cotyla lateralis in proximal view; the dorsal rim is not produced<br />

as far dorsally, and the medial rim is thin, unlike the conditions<br />

in Leipoa or Alectura. The sulcus hypotarsi is proportionally<br />

small in proximal view compared with all the modern taxa. The<br />

robustness of the lateral side of the hypotarsus in proximal<br />

view is blocky, unlike that in Megapodius. The plantar extension<br />

of the crista medialis hypotarsi is greater than in Alectura,<br />

Talegalla, Aepypodius, or Macrocephalon but is less than in<br />

Megapodius, Eulipoa, or Leipoa. The relative plantar extension<br />

of the crista lateralis hypotarsi differs from that in Alectura,<br />

Talegalla, Aepypodius, or Progura in being about one-half that<br />

of the crista medialis. The distally projecting process on the<br />

distal end of the hypotarsus is smaller than that in Megapodius.<br />

The dorsoventral compression of the shaft is greater than in Talegalla<br />

or Aepypodius. The sides of the shaft are relatively parallel<br />

and do not widen toward the distal end, unlike Alectura,<br />

Leipoa, Aepypodius, Talegalla, Macrocephalon, or Progura.<br />

The relative development of the tuberositas M. tibialis cranialis<br />

is shorter in the fossil than in the modern forms. The fossa<br />

metatarsi I is not as distinct as in Megapodius, Leipoa, or<br />

Progura and has little medial extension. The trochleae are<br />

gracile and are not swollen as in the other genera, particularly<br />

Megapodius. The trochlea metatarsi II is at the same level as<br />

the trochlea metatarsi IV, rather than slightly above, when<br />

viewed either distally (unlike Megapodius, Leipoa, or Talegalla)<br />

or dorsally (unlike Megapodius, Leipoa, Aepypodius, or<br />

Progura). The trochlea metatarsi II is neither inflated nor globular<br />

as it is in Megapodius or Eulipoa, and it does not diverge<br />

strongly medially, unlike Alectura, Leipoa, Aepypodius, Talegalla,<br />

Macrocephalon, or Progura. The trochlea metatarsi IV<br />

does not project laterally, unlike Megapodius or Eulipoa. The<br />

articular groove of the trochlea metatarsi IV is moderately well<br />

developed, more so than in Alectura, Leipoa, Aepypodius, Talegalla,<br />

or Progura, but is less distinct than in Megapodius.<br />

Ngawupodius minya, new species<br />

FIGURE 1A-C<br />

HOLOTYPE.—Complete right tarsometatarsus, Paleontology<br />

Collection of the Museum of Victoria (MV), Melbourne,<br />

P160493. Collected by I. Parker on 12 May 1979.<br />

TYPE LOCALITY.—South end of Lake Pinpa, South Australia<br />

(31°08'31"S, 140°12'47"E; T.H. Rich, pers. comm., 1996).<br />

HORIZON.—Namba Formation, Ericmas Fauna, late Oligocene.<br />

ETYMOLOGY.—Minya, in South Australia an Aboriginal<br />

word for "small" (Reed, 1977); for the purposes of nomenclature,<br />

minya should be considered to be without gender.<br />

DIAGNOSIS.—As for the genus.<br />

DESCRIPTION.—The fossil is from an adult bird because the<br />

surface lacks porosity, the tarsal cap is completely fused to the<br />

proximal end of the metatarsals, the hypotarsus is fully formed,<br />

and the metatarsals are fully fused over their entire length. In<br />

immature Leipoa ocellata, the tarsometatarsi may approach the<br />

size in that of adult birds yet still be highly porous and incompletely<br />

fused.<br />

Total length 40.2 mm; proximal width 8.1 mm; distal width<br />

9.5 mm; distal depth 5.7 mm. Eminentia intercondylaris low,<br />

about same height as rim of cotyla medialis; both higher than<br />

rim of cotyla lateralis. Depth of crista hypotarsi medialis about<br />

one-half that of proximal end of bone (proximal depth to hypotarsus<br />

4.4 mm; proximal depth with hypotarsus 8.0 mm), with<br />

laterally directed projection at end. In proximal view, sulcus<br />

medialis hypotarsi slightly laterad of eminentia intercondylaris,<br />

three shallow sulci lateralis hypotarsi and two low cristae lateralis<br />

hypotarsi on rather square hypotarsus. In lateral view, hypotarsus<br />

short (5.1 mm). Ridge extending distally from hypotarsus<br />

on facies plantaris very low. Shaft broad (midshaft width, 4.3<br />

mm; shaft width at proximal edge of fossa metatarsi I, 4.5 mm)<br />

but dorsoplantarly flattened (midshaft depth, 2.6 mm; shaft<br />

depth at proximal edge of fossa metatarsi I, 2.8 mm), markedly<br />

so on medial side; lateral margin straight, medial margin somewhat<br />

concave distally to fossa metatarsi I; distal to fossa produced<br />

more medially. Fossa metatarsi I elongate (5.8 mm). Fos-

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