ZooKeys 255: 103–132, doi: 10.3897/zookeys.255.3774
Twentieth century occurrence of the Long-Beaked Echidna Zaglossus bruijnii in the Kimberley region of Australia
Kristofer M. Helgen 1, Roberto Portela Miguez 2, James L. Kohen 3,  Lauren E. Helgen 1
1 Division of Mammals, Department of Vertebrate Zoology, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, MRC 108, Washington, D.C. 20013-7012, USA
2 Mammal Section, Department of Life Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK
3 Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia

Academic editor: W. Bogdanowicz

received 5 August 2012 | accepted 31 October 2012 | Published 28 December 2012

(C) 2012 Kristofer M. Helgen. This is an open access article distributed under the terms of the Creative Commons Attribution License 3.0 (CC-BY), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

For reference, use of the paginated PDF or printed version of this article is recommended.


The monotreme genus Zaglossus, the largest egg-laying mammal, comprises several endangered taxa today known only from New Guinea. Zaglossus is considered to be extinct in Australia, where its apparent occurrence (in addition to the large echidna genus Megalibgwilia) is recorded by Pleistocene fossil remains, as well as from convincing representations in Aboriginal rock art from Arnhem Land (Northern Territory). Here we report on the existence and history of a well documented but previously overlooked museum specimen (skin and skull) of the Western Long-Beaked Echidna (Zaglossus bruijnii) collected by John T. Tunney at Mount Anderson in the West Kimberley region of northern Western Australia in 1901, now deposited in the Natural History Museum, London. Possible accounts from living memory of Zaglossus are provided by Aboriginal inhabitants from Kununurra in the East Kimberley. We conclude that, like Tachyglossus, Zaglossus is part of the modern fauna of the Kimberley region of Western Australia, where it apparently survived as a rare element into the twentieth century, and may still survive.


Extinction, Kimberley, monotreme, Pleistocene survival, rock art, Zaglossus


The egg-laying mammals, or monotremes (Monotremata), are the sister group to all other extant mammals and are known as living animals only from the Australian continent, incorporating the modern landmasses of Tasmania, Australia, and New Guinea, which share a continental shelf that is periodically united during times of lowered sea levels as a single continuous landmass (“Sahul” or “Meganesia”). There are two extant monotreme families. The platypus, Ornithorhynchidae, is represented by a single living genus and species, Ornithorhynchus anatinus (Shaw, 1799), a semi-aquatic monotreme distributed throughout eastern Australia from tropical Queensland south to Tasmania and Kangaroo Island. The echidnas, Tachyglossidae, are classified in two living genera, the smaller short-beaked echidna (genus Tachyglossus), represented by one species, Tachyglossus aculeatus (Shaw, 1792), and the larger long-beaked echidnas (genus Zaglossus), with three living species currently recognized (Flannery and Groves 1998). Tachyglossus aculeatus is one of the most widely distributed Meganesian mammals, occurring in a wide range of habitats throughout Tasmania, Australia, and much of New Guinea. The long-beaked echidnas, today known only from New Guinea, are inhabitants of rainforests and subalpine meadows—Zaglossus bruijnii (Peters and Doria, 1876), distributed in western New Guinea, Zaglossus bartoni (Thomas, 1907a), distributed in central and eastern New Guinea, mainly at higher elevations, and Zaglossus attenboroughi Flannery and Groves, 1998, reported to date only from the Cyclops Mountains (Flannery and Groves 1998, Groves 2005, Baillie et al. 2009), an outlying mountain range along the north coast of New Guinea (Figure 1).

Though Tachyglossus is regarded as the only extant echidna in Australia, until the late Pleistocene several additional tachyglossids, all larger than Tachyglossus, occurred in Australia. Megalibgwilia owenii (Krefft, 1868) (often called Megalibgwilia ramsayi, a junior synonym, in current literature) was a Zaglossus-sized echidna (estimated mass circa 10 kg, but more robust than Zaglossus and with a less elongate or downcurved rostrum) known from Pleistocene localities in New South Wales (Wellington Caves), South Australia (Naracoorte), Tasmania (Montagu Caves and King Island), and south-western Western Australia (Tight Entrance Cave) (Murray 1978b, Griffiths et al. 1991, Turney et al. 2008, Prideaux et al. 2010), indicating a distribution centered on more temperate regions of the continent. “Zaglossushacketti Glauert, 1914, the largest monotreme yet discovered (estimated mass circa 20 kg), is documented only from Pleistocene postcranial remains from south-western Western Australia (Mammoth Cave); its generic placement has always been provisional pending the discovery of cranial material or detailed comparative taxonomic study of tachyglossid postcrania (Griffiths et al. 1991, Long et al. 2002). Postcranial remains of a relatively gracile Zaglossus-sized echidna, provisionally referred to the living Zaglossus bruijnii, have been reported from the Pleistocene of South Australia (Henschke’s Quarry Cave at Naracoorte) (Murray 1978a [but see Pledge (1980), who considered this more likely a “giant Tachyglossus”]), and Aboriginal rock art corresponding to Zaglossus (Zaglossus cf. bruijnii) is compellingly recorded from Arnhem Land, Northern Territory (Murray and Chaloupka 1984, Lewis 1986, Chaloupka and Murray 1986) (Figure 2). Thus, at least four echidna species, Tachyglossus aculeatus, Megalibgwilia oweni, “Z.” hacketti, and Zaglossus cf. bruijnii, constitute the known Quaternary tachyglossid fauna of the Australian continent south of New Guinea.

Here we report an overlooked modern museum specimen (skin, skull, and forelimb skeleton) of Zaglossus that was apparently collected in 1901 in the West Kimberley region of north-western Australia by the Australian naturalist and collector John T. Tunney (Figure 3). Based on an agreement between Lord L. Walter Rothschild, the eccentric naturalist who built up an astonishingly large personal collection of natural history specimens in his private museum in Tring (in the county Hertfordshire outside of London), and Bernard Henry Woodward, the London-born director of the Western Australian Museum in Perth, Tunney was commissioned by Rothschild to travel through some of the most remote areas of northern Australia in the first years of the twentieth century in order to collect butterflies, moths, mammals, and birds for Tring, and Aboriginal cultural artifacts for the museum at Perth. From April 1901 to November 1903, in a pioneering effort, Tunney collected natural history specimens and cultural artifacts along a transect that extended from the Pilbara Region in Western Australia to the South Alligator River in Northern Territory, before returning to Perth (Thomas 1904a, Hartert 1905, Whittell 1954, Storr 1966, Gray 2003, Chadwick 2008). On this northern Australian expedition, Tunney obtained the first specimens of various mammals previously unknown to science, including the small dasyurid marsupial Antechinus bellus (Thomas, 1904a), the rats Rattus tunneyi (Thomas, 1904a) and Rattus colletti (Thomas, 1904c), and two larger mammals, both kangaroos—the Black Wallaroo Macropus bernardus (Rothschild 1904) and Rothschild’s Rock-Wallaby Petrogale rothschildi (Thomas, 1904b). Tunney also collected what were to become the type specimens of several other then-undescribed mammal taxa known by a few other museum specimens at the time, including the small dasyurid marsupial Phascogale pirata Thomas, 1904a; the West Kimberley and Northern Territory subspecies of the wallaroo (Macropus robustus woodwardi Thomas, 1901, and Macropus robustus alligatoris Thomas, 1904a, respectively); and the Arnhem Land subspecies of the Nabarlek or Pygmy Rock-Wallaby, Petrogale concinna canescens Thomas, 1909.

Despite the importance of Tunney’s mammalogical collections, no full report on these materials has ever been published. The most important account is M.R. Oldfield Thomas’ (1904a) preliminary discussion written after receipt and early review of Tunney’s material received at the Tring Museum. (The Tunney collection was transferred, along with the rest of Rothschild’s mammal collections, from Tring to the Natural History Museum, London, in 1939 following Rothschild’s death in 1937.) One of the most important Tunney specimens that was never critically reported is what appears to be a north-western Australian specimen of Zaglossus collected in 1901, which we discuss here. This specimenchallenges current thinking about the timing of extinction of the genus in Australia and offers new insight into northern Australian biogeography and the ecology of this critically endangered monotreme lineage.

Figure 1.

Map of the Greater Australian continent. Map includes an outline of the larger land mass know as “Sahul” or “Meganesia” that forms when the continental shelf (dark grey) is exposed during glaciation. Overlaid is the modern distribution of the three recognized species of Zaglossus: Zaglossus bartoni (red), Zaglossus bruijnii (yellow), and Zaglossus attenboroughi (blue diamond), with the Kimberley record of Zaglossus bruijnii highlighted by a yellow star. Other possible Australian records of Zaglossus cf. bruijnii are numbered by general locality: 1 Pleistocene fossil remains from Naracoorte, South Australia, referred to Zaglossus cf. bruijnii by Murray (1978a)2 Aboriginal rock art (probably late Pleistocene in age) from Arnhem Land, Northern Territory (see Figure 2) 3 Aboriginal reports of a second, larger echidna taxon, in addition to Tachyglossus, present in the East Kimberley (Kununurra, Western Australia) in recent (20th century) memory (see text).

Figure 2.

Australian rock art of Zaglossus. Photograph of an Aboriginal rock art illustration from Arnhem Land depicting the characteristic long and down-curved beak (and whitish head of some specimens) of Zaglossus (see Murray and Chaloupka 1984). Photograph by G. Chaloupka.

Figure 3.

Dramatis personae. Clockwise from top: Australian natural history collector John T. Tunney (1871–1929), preparing specimens on the northern Australian expeditionary efforts during which his Zaglossus specimen was collected; M.R. (Michael Rogers) Oldfield Thomas (1858–1929), mammal taxonomist at the British Museum (Natural History), London, who studied the Tunney Zaglossus specimen; Lord L. (Lionel) Walter Rothschild (1868–1937), eccentric collector and naturalist who used his family fortune to amass a very large personal scientific collection, which became the Zoological Museum at Tring and included the Tunney Zaglossus specimen. Tunney portrait courtesy of the Western Australian Museum, Perth; Rothschild and Thomas portraits courtesy of the Natural History Museum, London.


Specimens discussed in this paper are stored in the collections of the American Museum of Natural History, New York , USA (AMNH); the Natural History Museum, London, UK (BMNH); the Museum of Comparative Zoology, Harvard University, Cambridge, Massachusetts, USA (MCZ); the Museum Zoologicum Bogor, Cibinong, Indonesia (MZB); the National Museum of Natural History, Smithsonian Institution, Washington, D.C., USA (USNM); and the Western Australian Museum, Perth, Australia (WAM).

The Kimberley Zaglossus specimen

During a visit to the Natural History Museum, London, in 2009, the first author studied a museum skin of Zaglossus bruijnii (BMNH 1939.3315; Figures 49), bearing original tags from John T. Tunney, stored among supposedly unprovenanced specimens of Zaglossus. This skin also has an associated cranium, mandibles, and distal right forelimb elements, which were extracted from the study skin early in the twentieth century (see below). The tags record the collection of this specimen from Mount Anderson, an inland locality in the West Kimberley region of north-western Western Australia, on 20 November 1901 (Figure 7).

Tunney’s typical tags (used by Tunney and some other collectors from the Western Australian Museum in Perth) were strong card tags preprinted with the following categories (see figure in Chadwick [2008]): (on one side of the card) “No.” (i.e., field number), “Date” (i.e., date of collection), “Sex” (i.e., male or female), “Colour of Iris” (i.e., eye color, used by Tunney for birds, but generally not for mammals), “Colour of Leg” (used by Tunney for birds, but not for mammals), “Name” (given by Tunney either as the scientific or common name of the species), “Loc.” (i.e., the collection locality); and (on the other side of the card) “Nature of Place where caught” (i.e., habitat), “Rare or Common” (i.e., an indication of abundance), “H + B.” (i.e., length of head and body), “T.” (i.e., length of tail), and “H. F.” (i.e., length of hind foot).

Tunney’s tag, written in his characteristic handwriting, and tied with thick sturdy string to the right hindfoot of the specimen (Figures 4 and 7), bears an original field number (347), a date (“20 Nov. 1901”), reports the specimen’s collection from “conglomerate hills” (“Nature of Place where caught”) at “Mt Anderson (W Kimberley)” (locality), and indicates that it was “Rare” (a classification only occasionally reported on his mammal tags). Tunney originally marked the sex of the animal as female (“♀”), which was later corrected in pen on the tag to “young ♂” (reflecting a mammal difficult to sex, as echidnas can be). Tunney left the “Name” field blank on his tag, which is somewhat unusual—he usually reported a scientific or common name on his mammal tags. This may indicate that Tunney was uncertain exactly what species he had before him. Tunney also usually reported standard length measurements on tags for his mammal and bird specimens (i.e., head-body, tail, and hind foot lengths), but in this case he gave the measurements of the specimen only as “21 inches over back from tip to tip” and “under measurement 20 inches”, indicating a mammal for which the head-body and tail lengths were unusually difficult to measure. Thetotal study skin, as now prepared, still measures about 21 inches measured over the dorsum and 20 inches measured along the underside. The specimen also bears a smaller field tag, worn and dirty, that is made of cloth-like paper, attached to the right hindleg with wire, and bearing only the field number, “N 347” (Figure 7).

The specimen is a well-made study skin, with the hindlegs directed posteriorly and the forelegs folded back against the underside (Figure 4). It was originally prepared with the skull and parts of the limbs retained intact inside the skin (the skull and right forelimb were apparently later removed from the skin and prepared in England—see below). The pelage is quite pale brown, and the specimen is rather sparsely furred, with mostly white spines, and has spines invading the sides of the belly, claws only on the middle three digits of both forefeet and both hindfeet, and hindleg spurs.

This specimen was misidentified as a Short-beaked echidna before its skull was extracted and studied. Identified by field number (347), it was listed as “Echidna aculeata” (i.e., Tachyglossus aculeatus) when it was sent from Australia to Rothschild at Tring, and identified as such in a letter dated 25 April 1904 sent by Bernard Woodward to Oldfield Thomas in London, discussing details of the mammal specimens collected by Tunney (Figure 8). Soon after its arrival at Tring, ectoparasite specimens taken from this skin formed the basis for the description of a new species of tick, Amblyomma australiense, by Neumann (1905), and a new species of flea, Echidnophaga liopus, by Jordan and Rothschild (1906). Both of these publications still listed the identity of the host as “Echidna aculeata” (these parasitological discoveries are discussed further below).

Though the identification of this specimen as Zaglossus has gone unreported in the literature until now, we are not the first researchers to notice that this specimen provides a modern record for Zaglossus from Western Australia. Oldfield Thomas, arguably the greatest mammalogical taxonomist of all time, examined Tunney’s specimens when they arrived in England, and made notes that indicate he understood Tunney’s specimen was a Kimberley Zaglossus. Thomas would have known that the Tunney skin in question was a Zaglossus rather than a Tachyglossus the moment he saw it, even if Rothschild was unaware of this. Thomas apparently removed the skull (the skull, by its lack of sutural ossifications, shows the animal to be a nearly mature subadult) and the bones of the right forelimb (articulated radius, ulna, and forefoot) from the study skin. The skull is intact apart from some missing basicranial fragments and is labelled “Kimberley” in Thomas’ handwriting on the palate (Figure 5); it also bears two labels in Thomas’ handwriting, one identifying the specimen as an “imm[ature]. Zaglossus, coll[ected by]. Tunney” and the other noting that the skull compares favorably to an immature specimen of Zaglossus bruijnii from Fakfak (western New Guinea) preserved in the Zoological Museum in Amsterdam. The dentary is also marked in ink with the word “Kimberley” in Thomas’ handwriting (Figure 5). Thomas labeled the forelimb “Zaglossus Kimberley N.W.A. (Tunney)” (i.e., N.W.A. = north-western Australia) (Figure 6). These labels indicate to us that Thomas recognized that the specimen was indeed a Zaglossus, and that he was satisfied that it had been collected by Tunney in the Kimberley region of Australia. We suspect that Thomas extracted the right forelimb elements from the skin of the specimen to see if its humerus was preserved. He would have wanted to compare it to the humeri of the large fossil echidnas that had previously been described from Australia; the holotypes of two large echidna taxa described from the Australian Pleistocene (Echidna owenii Krefft, 1868, Echidna ramsayi Owen, 1884, now classified in the genus Megalibgwilia) are right humeri (Mahoney and Ride 1975). Only the radius, ulna, and distal elements of the manus were present in the skin, however. An x-ray of the skin confirms that the right forelimb and skull of this specimen were indeed extracted from the skin, with their impressions, still evident inside the skin, closely matching the osteological elements.

It is not clear on what date Thomas extracted the skull and forelimb of the Tunney specimen, but he may have written the accompanying labels after 1907 (or replaced them with newer labels if he had written them earlier), because until at least 1907 Thomas was apparently under the impression that Acanthoglossus (rather than Zaglossus) was the correct generic name for the long-beaked echidnas (Thomas 1907a, 1907b), though usage of this name wavered at the time. Universally accepted usage of Zaglossus Gill 1877, which predates the generic synonyms Acanthoglossus Gervais 1877a and Proechidna Gervais 1877b(names which had previously enjoyed wide usage), followed from Allen’s (1912) influential monograph on the genus, though earlier authors, including Rothschild, had regularly pointed out that Zaglossus was the earliest generic name (e.g., Gill 1885, Palmer 1895, Coues 1895, Rothschild 1905a). In any case, Thomas died in 1929 (Thomas and Tunney both passed away in June 1929) without discussing Tunney’s Zaglossus specimen in any publication, which is surprising considering that Thomas was such a prolific author of papers on mammals (he produced approximately 1100 publications on mammal taxonomy, naming 2900 mammal taxa [Hill 1990]). We can identify several reasons why Thomas may not have prioritized publishing a note about this specimen. The most important might be Rothschild’s eccentric penchant for echidnas (along with kangaroos—similar to his personal interest in ratites amongst his ornithological collections [M. Rothschild 1983]), which may have excluded Thomas from freely publishing on these holdings at Tring. Rothschild permitted Thomas to publish many papers based on Tring mammals, but Rothschild was very fond of kangaroos and echidnas, keeping various kinds alive at his family’s estate (M. Rothschild 1983), and it seems he preferred to publish reviews of Tring’s kangaroos and echidnas on his own, except perhaps where Thomas chose to name them in Rothschild’s honor (as in the case of Petrogale rothschildi Thomas, 1904b). This may have suited Thomas fine, as Rothschild’s publications on kangaroos and echidnas were often premature and incompletely prepared and reasoned (e.g., Rothschild 1903, 1904, 1905b, 1905c, 1907) (with some important exceptions, such as the tree kangaroo monograph published by Rothschild and Dollman 1936), in general falling far short of Thomas’ authoritative command of these groups, which was established early in Thomas’ career (Thomas 1888). Another reason that Thomas did not publish on the specimen could be that it was not clearly describable as a new taxon (the Thomasian special focus), the single specimen available being indistinguishable from specimens of Zaglossus bruijnii from western New Guinea. With the wealth of clearly new mammal taxa Thomas had available to describe, he may have set this echidna specimen to the side, hoping that additional Australian specimens, especially a mature specimen or a series, might become available so that he could better understand the characteristics of the Kimberley Zaglossus.

While Thomas’ impressions as to the identity of the Tunney Zaglossus specimen seem clear, it is not clear whether Rothschild was aware that the specimen was a Zaglossus, or if so, whether he accepted its authenticity. Rothschild published several observations on echidna taxonomy (Rothschild 1892, 1905a, 1913), including one co-authored with Thomas (Thomas and Rothschild 1922), and one in which Thomas abstained or was excluded from authorship (Rothschild, in Thomas and Rothschild 1922). Like Thomas, Rothschild never mentioned Tunney’s Zaglossus specimen in a publication before he died in 1937. In 1939, the Tring mammal collection was transferred to the BMNH, and most of it is now housed at South Kensington. This is when the echidna specimen was given the BMNH accession number 1939.3315. The BMNH Mammalogy accession register only mentions a skin for this specimen, raising the possibility that the skull (which confirmed the identity of the specimen beyond doubt to Thomas) had been retained on loan by Thomas at South Kensington, perhaps to be described one day, and was only reunited with the skin on its permanent arrival to the BMNH in 1939. Importantly, the Tunney Zaglossus specimen bears a third tag, added to the right hind leg either at the Tring Museum or when the specimen arrived with the Rothschild Bequest (Figure 9). This tag disputes the Tunney association of the specimen, noting, “other label apparently does not belong to this specimen” on one side, and “Zaglossus bruijni goodfellowi see Nov. Zoologicae vol 20, 1913” on the other side. The author of this label has been identified as Fred Young, who was a taxidermist at the Tring Zoological Museum, by Effie Ward, Tring librarian. The 1913 paper mentioned on this tag (Rothschild 1913) discusses Zaglossus specimens at BMNH and Tring that Rothschild was aware of in 1913, and lists them by taxon, age, sex, and preparation. The Tunney Zaglossus specimen, being an immature male skin (and, possibly, extracted skull) is not clearly associable with any specimens identified in this paper. The paper in question provides a taxonomic key for Zaglossus identification, and we take the tag’s reference to this Novitates Zoologicae paper to refer to this key. In effect, our understanding is that the person who wrote the message on this third tag resorted to using Rothschild’s key, and discovered that the Tunney specimen keys out to Rothschild’s concept of “Zaglossus bruijnii goodfellowi”, a taxon then considered endemic to the island of Salawati (= Salwaty, a continental island off the coast of western New Guinea)in Rothschild’s taxonomic scheme. We suggest that, on account of this specimen’s keyed identification, the writer of this last skin tag seems to have discounted the possibility that Tunney’s original tag details could be correct, and that this was done without any critical examination of the background and data associated with this specimen or consideration of Thomas’ extraction and examination of the skull and forelimb.

From the beginning of our investigations regarding this specimen, we have of course considered whether its original Tunney field tags truly belong to it, or whether they might have been transferred to it by mistake, as the latest tag associated with the specimen implies. However, several lines of evidence point to the fact that Tunney’s tags were always associated with an echidna, and that this tag was not likely to have been transferred by mistake from a Tachyglossus specimen to a Zaglossus specimen.

In addition to Tunney’s original tag, two sources—correspondence between Perth and London/Tring, and several parasitological publications—establish that Tunney’s specimen (his field number 347) was definitely an echidna, such that we are certain that its original tags were not transferred by mistake from a specimen of some other kind of animal. The specimen was mentioned in the original export paperwork, and discussed in parasitological literature, as Tachyglossus aculeatus (originally as Echidna aculeata), and its tag data, including the difficulty of sexing and the style of measurement, suggest an echidna. Thus the only conceivable mix-up could involve a Tachyglossus specimen collected by Tunney, with tags that became disassociated from the original specimen, and later erroneously attached to a specimen of Zaglossus bruijnii that came from New Guinea. However, we believe that Tunney’s original tags from Mt. Anderson are authentically associated with this Zaglossus specimen for several reasons. First, the nature and timing of any putative specimen switch is difficult to understand. Tunney collected only a few Tachyglossus during his expeditions in northern Australia, and these seem to be accounted for in the WAM and BMNH collections, and we note with interest that these tags were written somewhat differently. For example, on the tag of the only Tunney-collected Tachyglossus at BMNH, Tunney provided the name of the species as “Echidna” (left blank on the Zaglossus tag), and stated its abundance as “numerous” (“Rare” in the case of the Zaglossus specimen). Second, such a switch would have to have taken place after the echidna specimen arrived at Tring (in 1903-1904), not earlier in Perth, because no Zaglossus specimen was available in Perth—Tunney never collected in New Guinea, and the WAM has apparently never had a modern Zaglossus specimen in their mammal collection (as judged by details from the WAM accession register). But any switch must have already happened by the time that Thomas first inspected the Tunney specimens sent to Tring, as it seems clear that Thomas accepted that Tunney’s specimen number 347 was a Zaglossus collected in the Kimberley region once he was able to make confirming examinations of its skull and forelimb. Thomas had already published one report on Tunney’s 1903-1904 shipment to Tring by 1904 (Thomas 1904a), indicating that any switch that was unbeknownst to Thomas must have occurred at the very point of arrival at Tring. This is not impossible, but it is very difficult to imagine, especially in light of Rothschild’s clearly very active interest in all incoming echidnas. The Tunney skin came with two original tags, a small tag with field number wired to the leg, and a heavier card tag tied to a leg with strong twine. Both tags would need to have been removed from a Tachyglossus specimen, and reattached by mistake to one of Rothschild’s few and precious Zaglossus skins at Tring, which is unlikely. A decade later, there were still only 13 Zaglossus specimens identified in the Tring collection, and it is clear from Rothschild’s publications that these were highly valued and carefully curated by Rothschild (Rothschild 1913). In summary, it is highly implausible to envision a switch-up in Perth or in Tring that could explain how tags from an Australian Tachyglossus specimen would have become mistakenly associated with a specimen of Zaglossus that originated from New Guinea.

Another important consideration is the size of the animal measured by Tunney. Tunney’s tag gives the specimen’s total length measurement as 21 inches (= 533 mm), and this value matches very well the size of the study skin to which it is currently attached, as measured with a flexible measuring tape. This body size measurement is consistent with either a subadult Zaglossus (i.e., like the specimen to which it is attached) or an unusually large adult Tachyglossus. Total length measurements of 539-1000 mm have been reported for adult Zaglossus bruijnii (Allen 1912, Rothschild 1913). Extremely large Tachyglossus specimens only rarely reach the lower limit of this size range. Typical lengths for adult Tachyglossus are in the range of 300-450 mm (Wood Jones 1923, Menkhorst and Knight 2001, Augee 2005). An unusually large and aged male Tachyglossus aculeatus (USNM 283961) from Groote Eylandt, Northern Territory, measuring 555 mm in total length (original field measurements), approximates a maximum body size for the genus. This specimen is by far the largest Tachyglossus in the USNM collection (of about 40 specimens), and is among the very largest and most robust of Tachyglossus specimens in world museums by skin and skull size (K. Helgen and G. Perri, in litt, 2012). In summary, only the largest Tachyglossus outliers on record could match the size of the echidna reported on Tunney’s tag, Tunney’s measurements are consistent with the dimensions of a Zaglossus nearing cranial maturity, and Tunney’s measurements are a match for the actual dimensions of the specimen to which his tags are attached.

Figure 4.

Study skin of the Kimberley Zaglossus (BMNH 1939.3315), bearing the original field tags of John T. Tunney. From top: dorsal, ventral, right lateral, and left lateral views. Scale bar = 5 cm.

Figure 5.

Cranium and dentaries of the Kimberley Zaglossus (BMNH 1939.3315). From top: dorsal view of the cranium, dorsal view of the dentaries, ventral view of the cranium, ventral view of the dentaries, and, at bottom, close-up views of Thomas’ labeling of “Kimberley” on the specimen’s palate (left) and dentary (right). Scale bar = 20 cm.

Figure 6.

Articulated right forelimb elements of the Kimberley Zaglossus (BMNH 1939.3315). Associated label notes “Zaglossus Kimberley N.W.A. (Tunney)” in Thomas’ handwriting. Ventral view above, dorsal view below. Scale bar = 5 cm.

Figure 7.

John Tunney’s original field labels attached to the skin of BMNH 1939.3315. A front of card skin tag (attached with sturdy twine to right ankle of study skin) bearing original data, providing the specimen’s field number, date of collection, age and sex, and locality B back of same card skin tag bearing original data, detailing the specimen’s measurements, context of collection, and abundance C cloth tag bearing original field number (“N 347”), wired tightly to right ankle of study skin. See text for details.

Figure 8.

Specimen export list. A list of specimens shipped from Perth to Tring included in a letter, dated 25 April 1904, from Bernard Woodward at the Western Australian Museum to Oldfield Thomas, detailing the transfer of Tunney specimens to Rothschild at Tring. The list includes his number 347 (now BMNH 1939.3315), an echidna identified as “Echidna aculeata” (i.e. Tachyglossus aculeatus) prior to Thomas’ examination of the specimen in London, where he realized it is a Zaglossus; we have circled and highlighted this entry in the list.

Figure 9.

Non-original tag (views of front and back) added at Tring or BMNH, and apparently bearing the handwriting of Tring taxidermist Fred Young. The tag bears a note suggesting that the original labels must be incorrect because the specimen corresponds to Rothschild’s concept of Zaglossus bruijni goodfellowi, then considered endemic to the Indonesian island of Salawati, following his 1913 key (Rothschild 1913). The note seems to indicate that knowledge of the importance of this specimen has been obscured since or before the specimen’s transfer from Tring to BMNH, as it was assumed by Young to be a mistake.

The specimen’s locality

The tag locality provided by Tunney for the Zaglossus specimen is “Mt. Anderson, W Kimberley.” First named in 1879 by Alexander Forrest in his “North-West Expedition” from DeGrey to Darwin (Forrest 1880), Mount Anderson is situated near the Grant Ranges, along the Fitzroy River about 90 km southeast of Derby at approximately 18o02'S, 123o56'E (Storr 1966). In early October, Tunney sailed from Port Hedland to Derby, where he arrived about October 11, and he collected at and in the vicinity of Mount Anderson from the end of October to late November (Storr 1966), during which time (20 November 1901) the echidna was collected.

Inland areas of the West Kimberley were settled by white Australians for sheep and cattle pastoralism in the aftermath of Forrest’s surveys (since 1881) but the region has historically been very sparsely inhabited by both European and Aboriginal communities (Bolton 1952, Speck 1964) and remains so today. Tunney’s visit to the area took place in the early decades of the region’s utilization for livestock. It was the first reconnaissance for mammals in this region, and the immediate area remains zoologically little known today. On its tag, Tunney characterized the habitat of the Zaglossus specimen as “conglomerate hills”, suggesting that the animal was found in a rocky area, where echidnas would surely make their burrows. The only other mammals obtained by Tunney at Mount Anderson were specimens of the large macropodids Megalibgwilia antilopinus and Megalibgwilia robustus (specimens at BMNH). Birds collected by Tunney at Mount Anderson included the Varied Lorikeet (Psitteuteles versicolor), Red-backed Fairywren (Malurus melanocephalus cruentatus), and Brown Goshawk (Accipiter fasciatus cruentus) (specimens in the AMNH ornithological collections).

The distribution of Zaglossus in New Guinea is today centered on montane tropical rainforests (but open areas of subalpine grassland are also prime habitat, and some areas of lowland forest and limestone country are also utilized). It might thus be expected that the last areas of survival for Zaglossus populations in the Kimberley would be in the region’s many tiny and scattered evergreen rainforest fragments, which are largely distributed to the north of the Fitzroy River (McKenzie et al. 1991). However, the Mount Anderson area is reasonably well watered (Registrar et al. 1902), and its inaccessibility, sparse human population, and the availability of rugged, steep, rocky areas may explain its importance in hosting a late-surviving remnant population of Zaglossus in Australia. Six decades after Tunney’s visit, in their review of “Lands of the West Kimberley Area”, Speck et al. (1964: 191) discussed the Grant Ranges-Mt. Anderson area under their classification of “inaccessible country” and “inaccessible pasture land”, describing it thus:

"Environment. The rugged mountain ranges, elevated plateaux, steep hills, and associated valleys have a complex geological pattern with quartzites, sandstones, shales, slates, schists, basalt, dolerite, and limestone. It is mostly rough, inaccessible, unproductive, and undeveloped. Soils are varied but characteristically skeletal with extensive outcrop.

Composition. Most of the lands are within the higher-rainfall area and the vegetation of these parts is an open woodland with moderate shrub layer and grassy ground storey of curly spinifex pasture type…. In the lower-rainfall parts the vegetation is more stunted and open and the grass layer is hard spinifex… Grasses other than spinifex are poorly represented. Edible top feed is also scanty.

Pastoral Value. Only where these lands are adjacent to better country is utilization possible. They are more likely to have a nuisance value. They are generally well watered and therefore provide a hideout for scrub bulls, increasing the difficulty of herd management and mustering. At best it will remain extremely poor pastoral country.

Reaction to Grazing, and Management. Much of the area is unstocked and there is little or no evidence of pasture degradation or denudation except in isolated, restricted areas adjacent to watering points."

A visual representation of the vegetation currently present around Mount Anderson today can be seen with mapping resources available in the online resource Atlas of Living Australia (http://spatial.ala.org.au/), which indicates that present vegetation is dominated by “Acacia open woodlands” but also includes some small areas of “Rainforest and vine thickets.” We suggest that these latter habitats (rainforest, vine thickets) would be relevant remnant habitat for Zaglossus, and that these habitats were likely more expansive at the time of Tunney’s visit to the region well over a century ago in 1901.

Relatively inaccessible and sparsely inhabited rocky areas provide some of the most important remaining areas of occurrence for Zaglossus in New Guinea, on the southern and northern slopes of the Central Cordillera, and in limestone country throughout the “Bird’s Neck” region in the west of the island. That similarly remote and sparsely inhabited areas of northern Australia apparently sheltered at least one remnant population of Zaglossus into the twentieth century is an astonishing realization, and serves as strong encouragement for wildlife researchers to undertake surveys of remote candidate areas of northern Australia with the goal of establishing whether Zaglossus may still exist in any rainforest fragments or rugged gorges across the Kimberley.

Taxonomy, biogeography, and the Kimberley Zaglossus

We confidently identify the Kimberley specimen of Zaglossus as the Western Long-Beaked Echidna, Zaglossus bruijnii, otherwise known only from the western portion of the island of New Guinea, which it matches in size, cranial features, claw number, and pelage features. Zaglossus bruijnii is the only echidna taxon that typically lacks claws on the first and fifth digits of all feet (the claw conformation seen in the Kimberleyspecimen), and always lacks a claw on the first digit of the hindfeet (a claw is always present on the first digit of the hindfoot in Zaglossus bartoni) (Flannery and Groves 1998). As Oldfield Thomas noted, the subadult skull of the Kimberley specimen is a good match in overall size and shape for specimens of Zaglossus bruijnii that are of equivalent age (as judged by cranial development, in terms of robustness and sutural ossification). The relatively short and modest (rather than long and heavy) growth of fur in between the spines on the dorsum, relatively pale brown (rather than blackish brown) pelage, presence of some black-tipped spines on the dorsum, and presence of visible spines on the underside, are external features that in combination are typical only of lowland populations of Zaglossus bruijnii, such as those recorded from the land-bridge island of Salawati, the adjacent Vogelkop coast at Sorong, and the Fakfak and Charles Louis Ranges in the Bird’s Neck region (skins especially at the BMNH, MCZ, and MZB).

The Western Long-beaked echidna, Zaglossus bruijnii, occurs in western New Guinea in habitats from as low as sea level up to the top of the highest peaks in the Vogelkop Peninsula—in the Tamrau and Arfak Ranges (to 2900 m)—and from the land-bridge island of Salawati in the west, to the “Bird’s Neck region” of New Guinea in the east, extending as far east as the Fakfak Range and possibly the Charles Louis Ranges on the western edge of the Central Cordillera (in the south) and possibly to the eastern shores of Geelvink (= Cenderawasih) Bay (in the north) (Rothschild in Thomas and Rothschild 1922, Van Deusen and George 1969, Flannery 1995a, 1995b, Flannery and Groves 1998, Aplin et al. 1999, Helgen 2007). The Eastern long-beaked echidna, Zaglossus bartoni, does not usually occur in habitats below about 1000 m, with low-elevation records known only in far south-eastern New Guinea at Collingwood Bay (down to 0–200 m) and in the vicinity of Haia on the south side of the Central Cordillera in east-central New Guinea (down to about 500–600 m).

Though previously recorded only from western New Guinea, Zaglossus bruijnii is the Zaglossus taxon occurring in closest geographical proximity to the Kimberley region, and is the only Zaglossus regularly documented in lowland contexts. Given that similar relevant habitats, including sparsely inhabitated limestone country and remnant rainforests, are to be found across the Kimberley region, it does not surprise us that the modern Kimberley representative of the genusshould be Zaglossus bruijnii. We envision a late Pleistocene distribution of Zaglossus bruijnii that extended across rugged, rocky country and rainforests along the western parts of the Sahul Shelf, comprising much of the area between Australia and New Guinea that has been inundated by the Arafura Sea since the terminal Pleistocene, thus connecting the restricted Recent range from the Vogelkop Peninsula in the north to the Kimberley region and Arnhem Land in the south.

Ectoparasites from the Kimberley Zaglossus

The Kimberley Zaglossus specimen, while overlooked in mammalogical literature, has been referenced with surprising regularity in parasitological papers. It is the “symbiotype” (i.e., host to the type series; Frey et al. [1992]) for two ectoparasite taxa, the flea Echidnophaga liopus Jordan and Rothschild, 1906; and the ixodid tick Amblyomma australiense Neumann, 1905. In all of the parasitological literature in which Tunney’s specimen is referenced, the specimen is mistakenly referred to as a Tachyglossus (e.g., Neumann 1905, Jordan and Rothschild 1906, Robinson 1926, Roberts 1953, Dunnet and Mardon 1974, Keirans 1982), obscuring until now the correct host association of these parasites.

The flea Echidnophaga liopus is so far documented firmly only from Tunney’s Zaglossus specimen and is unknown to date in Tachyglossus. Other Echidnophaga specimens attributed to Echidnophaga liopus in literature, which come from Indian rodents (Rothschild and Jordan 1906), seem more likely to represent a distinct Asian species (Dunnet and Mardon 1974). Out of interest, we note that two of the most commonly recorded and host-specific fleas of Tachyglossus aculeatusEchidnophaga ambulans and Bradiopsyllae echidnae (Dunnet and Mardon 1974)—have not been recovered from Tunney’s specimen.

Neumann (1905) originally described the Australian tick Amblyomma australiense based on examplars in the N.C. Rothschild collection taken from Tunney’s Zaglossus specimen (Robinson 1926, Roberts 1964, Keirans 1982). Apart from this original record from Tunney’s Zaglossus, a few other records of occurrence are available for this apparently northern Australian tick; Taylor (1913) and Roberts (1964) recorded it from Tachyglossus at Townsville in Queensland, Robinson (1926) recorded it from a unidentified large lizard at Darwin in Northern Territory, and Roberts (1964) recorded it from an “unspecified snake”, also at Darwin. The closely related tick Amblyomma echidnae Roberts, 1953, considered by some to be conspecific with Amblyomma australiense (but held as distinct, pending critical study, by Guglielmone et al. [2009]) is apparently known to date only from Australian Tachyglossus (Roberts 1953, 1964, 1970).

So far, none of the ectoparasites recorded from Tunney’s Zaglossus have been reported from New Guinea Zaglossus, but very little is known about the parasites of Long-beaked echidnas. We are aware of only two ectoparasites definitively recorded from New Guinea Zaglossus. The tick Bothriocroton oudemansi (Neumann, 1910) has been reported from Zaglossus bruijnii at Fakfak, and from Zaglossus bartoni in the Central Cordillera (Beati et al. 2008). The tick Ixodes zaglossi Kohls, 1960, was described from a specimen of Zaglossus bartoni from the Wissel Lakes at the western end of New Guinea’s Central Cordillera. Whether either of these ticks is the same taxon as Ixodes acanthoglossi Lucas, 1878 (regarded as an indeterminable nomen dubium by Beati et al. [2008]), originally described as a parasite of Zaglossus bruijnii in the Arfak Mountains, has not been determined.

Possible Aboriginal familiarity with Zaglossus in the Kimberley

The Late Quaternary occurrence of Long-beaked echidnasin northern Australia is widely accepted on the basis of a compelling Aboriginal rock art illustration (Figure 2), from an undisclosed Arnhem Land locality, that accurately depicts Zaglossus (Murray and Chaloupka 1984). This illustration, usually considered Late Pleistocene in age, has been often reproduced in reference books on Australian mammals (e.g. Johnson 2006, Tyndale-Biscoe 2005), and demonstrates Australian Aboriginal familiarity and interaction with Long-beaked echidnas.

It is possible that Aboriginal Australians also interacted with Zaglossus much more recently. In 2001, years before we became aware of the Australian provenance of the Zaglossus specimen reported here, one of us (Kohen) recorded a potential example of living memory of Zaglossus while engaged in field work in the East Kimberley. His account of the experience is as follows:

While conducting faunalsurveys at Faraway Bay, I was accompanied by an Aboriginal woman in her fifties who belonged to the Miriwoong Gadjerong tribe. Their territory extends from the coast inland in the region close to the Western Australia-Northern Territory border. In this part of Australia, tribal affiliation is passed down through the female line. However, Faraway Bay is on her father’s country, and he belonged to the Kwini tribe.

While walking close to the coast, we found a scat. On asking my informant what she thought it was, she correctly identified it as an echidna scat, which she referred to as “porcupine”. As only one echidna is traditionally known from Australia, I assumed that it belonged to Tachyglossus. A few hours later we had returned to the camp and were sharing tea when she commented about the echidna scat we had found. She said that her grandmothers “used to hunt the other one”. I asked her what other one, and she said that she meant a much larger echidna. She indicated its height which I estimated to be around 40 cm.

I was intrigued, as both of her grandmothers were still alive and in their nineties. However, one had recently suffered a stroke and the other lived some distance away. When we returned to Kununurra, I had an opportunity to speak to my informant’s mother. As it happened, I had a copy of Tim Flannery’s 1990 paper [Flannery 1990] on the extinct megafauna of Australia, which included a series of shadow illustrations of large Australian mammals. When I showed this to her, and asked her if she knew any of these animals, she identified the Zaglossus. My impression was that the animal had not been seen for a long time.

We readily acknowledge that these kinds of informant accounts are fraught with difficulty of interpretation. However, we mention these interactions, because, like the Tunney specimen, this information from Kohen’s informants could be relevant to the survival of Zaglossus in the Kimberley region into the twentieth century. We suggest that future efforts to investigate the recent survival of Zaglossus in remote northern Australia take into account evidence that may be derived from cultural sources such as rock art, living memories from Aboriginal cultures, and examination of vocabularies relevant to animal names in Aboriginal languages.

Specimen-based evidence of recent survival of Zaglossus in Australia

We are sufficiently convinced by the tags and information associated with the Tunney Zaglossus specimen to regard it as evidence for the survival of the long-beaked echidna in the Kimberley region into the early twentieth century. We accordingly recommend that the Western Long-beaked echidna, Zaglossus bruijnii, be included in future faunal compilations of the modern mammal fauna of Australia (e.g., Walton 1988, Walton and Richardson 1989, Menkhorst and Knight 2001, Van Dyck and Strahan 2005), and on the long list of mammal species that have declined to extirpation, extinction, or near extinction in Australia over the past two centuries (Johnson 2006).

We realize that, despite our conclusions, summarized here, others may remain skeptical of this Zaglossus specimen’s association with Tunney’s tags. Additional studies of this remarkable specimen might include analyses of ancient DNA, stable isotopes, and trace elements to test its origins and the context of its collection. Further targeted studies of relevant Kimberley Pleistocene and Holocene subfossil assemblages (e.g. O’Connor et al. [2008], Start et al. [2012]) may also shed useful light on the late survival of Zaglossus in northern Australia.

Quaternary and recent extinctions

Most of Australia’s remarkable Pleistocene megafauna (gigantic marsupials, reptiles, and birds) became extinct after about 50, 000 years before the present (Flannery 1994, Roberts et al. 2001, Miller et al. 2005, Rule et al. 2012) following the arrival of humans to the continent. Many other mammal species declined broadly, many to the point of extinction, across their mainland Australian distributions during the Holocene (e.g., thylacine, Thylacinus; Tasmanian devil, Sarcophilus) or since the onset of European impacts in the mid-1800s (Flannery 1994, Johnson 2006). The Tunney specimen adds Zaglossus bruijnii to the list of mammal species that underwent dramatic declines in Australia during recent times.

Anotherrather unexpected recent addition to the list of Quaternary extinctions in the Kimberley region is a fruit-bat of the genus Styloctenium, identified by Pettigrew et al. (2008) from definitive illustrations in (Late Pleistocene?) rock art from near Kalumburu. Species of Styloctenium are today known only from the large Indonesian island of Sulawesi (and some of its satellites) and the Philippine island of Mindoro (Bergmans and Rozendaal 1988, Esselstyn 2007). We also note with interest that compelling rock art images of the large, extinct carnivorous marsupial Thylacaleo have also recently come to light in the Kimberley (Akerman 2009, Akerman and Willing 2009). These discoveries point to the importance of rock art as a source of information about the past distributions in time and space of animals in northern Australian contexts.

Both Styloctenium and Zaglossus are largely rainforest-associated lineages that today are known only from tropical islands north of Australia. Their presence in the late Quaternary fauna of the Kimberley region doubtless reflects the former presence of extensive mesic forested habitats across much of northern Australia, with fragmentation and extinction of forest-reliant species driven by a combination of climate-change and prehistoric human impacts in recent millennia (McKenzie et al. 1991)—a topic that so far has received much greater attention in the Wet Tropics of Queensland than in the tropical rainforests of the Kimberley region (Joseph et al. 1995, Williams 1997, Schneider and Moritz 1999, Bowman et al. 2010). Today, none of the mammal species known to occur in Kimberley rainforests are entirely dependent on rainforest habitats (Friend et al. 1991). However, we suggest that further critical examination of rock art depictions, and of fossil and subfossil assemblages, will likely illuminate the former presence in the Kimberley rainforests of additional taxa typical of modern Indo-Malayan or Australo-Papuan rainforest habitats.

We hold out a small optimism that Long-beaked echidnasmight yet dig burrows and hunt invertebrates in at least one hidden corner of Australia’s north-west. Such hopes are founded on the remoteness of this little-studied expanse of the Australian continent, and on the relatively late discovery of other medium-sized Kimberley mammals including the Monjon, Petrogale burbidgei (Kitchener and Sanson 1978), a small rock wallaby endemic to the north-west Kimberley, and the recent rediscovery of the Scaly-tailed Possum (Wyulda squamicaudata) in the eastern Kimberley (Doody et al. 2012), where it had not been recorded since 1917.

All living Zaglossus taxa in New Guinea are considered to be critically endangered (Isaac et al. 2007, Leary et al. 2008a, 2008b, 2008c), with primary threats being subsistence hunting and habitat loss. While it is vitally and urgently important to explore whether Zaglossus still survives in remote areas of the Kimberley, it is also important to learn more about its recent distribution and history of decline. Such studies may identify hitherto unsuspected dimensions to the adaptive breadth of Zaglossus species, reveal the existing or former presence of populations with genetic diversity unrepresented in New Guinea, and possibly assist with long term conservation of Zaglossus in New Guinea by illuminating important patterns of habitat occurrence and historical decline in Australia. If Zaglossus bruijnii is extinct in the Kimberley region, it might also warrant consideration as a candidate for reintroduction, once more is learned of its former distribution and ecological role.

Ecology of Zaglossus bruijnii in western New Guinea and Australia

Little is definitively recorded about diet in Long-beaked echidnas. Most information is based on anecdotes or extremely limited studies of Zaglossus bartoni, which is thought to be a specialist earthworm feeder that also feeds on subterranean arthropods including centipedes and large insect larvae (Griffiths 1978, Griffiths et al. 1991, Flannery 1995a, Opiang 2009), with no evidence for feeding on social insects such as ants and termites, the principal diet of Tachyglossus (e.g. Abensperg-Traun and De Boer 1992). Because of the intimate cranial resemblance between Zaglossus bartoni and other Zaglossus taxa, it can be expected that the diets of these congeners are similar. However, it is possible that Zaglossus bruijnii eats more social insects than Zaglossus bartoni, perhaps especially in lowland environments. One of only two comments about diet in an individual of Zaglossus bruijnii is the firsthand account of naturalist Thomas Barbour, recounted by Allen (1912:302):

This specimen was kept alive for about a month and a few observations on its habits were made. It was absolutely nocturnal and spent the day partially buried in the deep layer of sand which was kept in its cage… At night it moved about sluggishly, often digging with motions that strongly recalled those of a turtle. It fed on ants only, which were procured by placing in a dish a considerable amount of shredded cocoanut. The ants soon swarmed in this and the whole was then placed in the Proechidna’s cage. It ate the insects by thrusting its long tongue down into the cocoanut. It took a little water or water with condensed milk, but seemed to drink very little.

It may of course be the case that this animal only ate ants because other, more favored foods were not offered to it. Ripley (1942: 256-259), provided the only other (conflicting) account that references the diet of Zaglossus bruijnii, based on a captive animalat Sansapor (a settlement adjacent to the Tamrau Range), noting “The echidna is supposed to live on ants, although this one would never touch them, much preferring papaya and raw eggs.” Studies of the anatomy of the salivary glands of Zaglossus bruijnii (not available for Zaglossus bartoni) show these glands to be greatly developed, as in various ant-eating animals, and very similar to those of Tachyglossus (Viallanes 1880, Allen 1912). Ants and termites would presumably constitute a reliable source of food for a large echidna in northern Australian contexts (Andersen and Majer 1991, Milewski et al. 1994, Barrow et al. 2006, 2007), though earthworms might remain key resources especially in remnant rainforest areas (McKenzie and Dyne 1991). If Zaglossus bruijnii is more dependent on ants in lowland New Guinea (and Australian) habitats than other Zaglossus populations arein montane New Guinea habitats, its presence across northern Australia until recent times may shed new light on the riddle, posed by Milewski et al. (1994), of why, unlike other southern continents, Australia seems to have had no species larger than Tachyglossus exploiting social insects as a major food resource. Griffiths et al. (1991) similarly suggested that Megalibgwilia, the other (and more southerly distributed) large echidna genus present in the Australian Quaternary, may also have been an insect-eater rather than an earthworm-eating specialist.


We thank P. Jenkins, L. Tomsett, J. Maclaine, R. How, E. Westwig, P. Sweet, D. Lunde, L. Gordon, S. Ingleby, J. Chupasko, Maharadatunkamsi, and M. Sinaga for assistance with specimens in museum collections around the world. We thank K. Aplin, G. Perri, M. Opiang, T. Flannery, M. Eldridge, C. Groves, M. Copley, E. Ward, R. How, J. Hatton, R. Roberts, R. Robbins, P. Engelbrektsson and O. Crimmen for helpful discussion. We acknowledge the very helpful assistance of M. Triffitt of the Western Australian Museum Library. We thank the Smithsonian Institution, the Natural History Museum (London), and the Australian Biological Resources Study for funding support.

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