Bluff Downs fossil site

The Bluff Downs fossil site is a paleontological site of Pliocene age in northern Queensland, Australia, and is one of the most significant fossil sites of Pliocene age in Australia due to its unique fauna and specific dating. The fossil site lies on the banks of Allingham Creek on the pastoral property of Bluff Downs Station, northwest of Charters Towers on the Cape York Peninsula

Dating

Precise dating of vertebrate fossil sites in Australia is rare, and many Cenozoic-age sediments remain undated. As of 2000, only two Pliocene vertebrate-bearing fossil faunas were specifically dated, Bluff Downs Local Fauna and the Hamilton Local Fauna in Victoria. Unusually, the Bluff Downs Local Fauna have been specifically dated. This is because there is a minimum age control in the form of a basalt layer (the Bluff Downs Flow) directly overlies the fossiliferous deposit. According to stratigraphy, the fossils must have been deposited before the basalt and thus, since the Bluff Downs Flow has been dated to 3.62 ±0.5 million years old; the fossils were deposited prior to this. The fossils were also deposited directly above another basalt flow, the Allensleigh Flow, allowing a maximum age control. The fossils were likely deposited between 5.2 and 3.6 million years ago during the late Pliocene period, which matches dates estimated through biocorrelation. The Allingham Formation has been radiometrically dated to no less than 4 ±0.12 million years old, placing it in the early Pliocene

Geology

Volcanic Activity and Basalt Flows

Bluff Downs fossil site describes a layer of fossiliferous sediment dating to the late Pliocene era that is sandwiched between basalt flows within the Nulla Basalt Province. Late Cenozoic basalts cover more than 28, 000 square kilometres in northern Queensland, and were divided into four physiographic provinces and given relative ages by Twidale in 1956; the McBride, Chudleigh, Sturgeon and Nulla Basalt provinces. This basalt is present due to volcanic activity from at least four separate periods, the most recent of which was approximately 13, 000 years ago, based on radiocarbon dating of sediment under the youngest of the flows, the Toomba flow. There was significant volcanic activity in the region 4.5-4.0, 2.3, 1.3 and 1.1 million years ago. Four million years ago, the landscape of northern Queensland would have been similar to Hawaii, with frequent lava flows , especially since the basalts were related to a central type of eruption not to fissures, and therefore were similar to those which can be observed today at Mauna Loa. The vents which the lavas came from appear to follow existing lineaments following a north-east direction in the valley, which lies on the eastern flank of the Great Dividing Range, and were at the head of this valley.

The lavas themselves are relatively thin, at a thickness of 30 metres to the east of Allensleigh but only 4 metres near Bluff Downs Station., this likely being due to the underlying topography. They form large plateaux which were noted by Twidale as peripherally dissected, and of a vesicular amygdaloidal nature with vivianite, zeolites and chalcedonic silica commonly found within amygdales. Bluff Downs Fossil Site is located within the Nulla Basalt Province.

Nulla Basalt Province

The Nulla Basalt Province covers approximately 4200 square kilometres and is dated to the late Pliocene or early Pleistocene and consists of multiple olivine basalt flows as the result of lava flows associated with volcanic activity 4.5-4.0, 2.3, 1.3 and 1.1 million years ago, according to radiogenic argon determination dating. The dating of these flows matches the ordering suggested by analysis of aerial photographs. The flows, which include the Allensleigh Flow and Bluff Downs Flow, overlie uneven Palaeozoic sedimentary, igneous and metamorphic rocks as well as sediments from the early Cenozoic, all of which have been weathered (lateritised) due to a humid and tropical palaeoenvironment.

Allensleigh Flow

The Allensleigh flow is the oldest and most widespread basalt flow in the Nulla Province, and responsible for the deposition of the Allingham Formation and thus, the presence of fossils, as it obliterated a channel, damming and causing drainage of the ancestral Burdekin River at the time of deposition. The flow is associated with the eruption that occurred between 4.5 and 4.0 million years ago.

Bluff Downs Flow

The Bluff Downs Flow is a basalt flow that directly overlies the Allingham Formation, and is dated to 3.62 ± 0.5 million years ago. It’s position directly above the fossiliferous sediment helped to protect the fossils from erosion, thus ensuring their survival.

The Allingham Formation

The Allingham Formation, named by Archer and Wade in 1976, is a lake and stream deposit within the Nulla Basalt Province, containing the fossils which the Bluff Downs Local Fauna are attributed to. It consists of a mixture of sediment that originated on land and was washed away after eroding into nearby waterbodies (terrigenous sediment), clays, silts, sands (including calcareous sands), and Chara limestones (calcareous nodules that were deposited directly over the fossiliferous sediment and consequently overlain by basalt). These sediments were formed in lakes and rivers (i.e. are lacustrine and fluviatile), indicating the presence of various water bodies such as lakes, rivers and streams in the palaeoenvironment at the time of deposition. There were several different depositional events and analysis of the sediments suggests that during the early Pliocene, a stream widened to form a shallow lake. The formation could be as young as 4.0 to 3.6 million years old, with the fossils were likely deposited at the lower end of the period between 5.2 and 3.6 million years ago.

The Allingham Formation, named by Archer and Wade in 1976, is the section of the Nulla Basalt Province which contains the fossils which the Bluff Downs Local Fauna are attributed to. It consists of a mixture of sediment that originated on land and was washed away after eroding into nearby waterbodies (terrigenous sediment), clays, silts, sands (including calcareous sands), and Chara limestones (calcareous nodules that were deposited directly over the fossiliferous sediment and consequently overlain by basalt). These sediments were formed in lakes and rivers (i.e. are lacustrine and fluviatile), indicating the presence of various water bodies such as lakes, rivers and streams in the palaeoenvironment at the time of deposition. There were several different depositional events and analysis of the sediments suggests that during the early Pliocene, a stream widened to form a shallow lake.

Fossils

The fossils found at Bluff Downs fossil site consist of a diverse range of vertebrates dating to the Pliocene, found in the terrigenous sediments of the Allingham Formation. These include both broken and complete bones and skulls, though articulated skeletons (with the bones in the same position as upon the organism’s death) are rare, and most organisms are found as isolated floats. Fossils were first discovered, collected and reported to the Queensland Museum in 1973. The Bluff Downs Local Fauna is derived from the vertebrate species found in the Allingham Formation.

Bluff Downs Local Fauna

The Bluff Downs Local Fauna, named and described by Archer in 1976, includes numerous vertebrate species found at the Bluff Downs Fossil Site, many of which are similar to but slightly older than the Chinchilla fauna (associated with Chinchilla Fossil Site, also in Queensland), according to more ancestral physical features. This collection of vertebrate species was noted to be considerably biodiverse by Archer, and features many ancestors of the species we now recognise as uniquely Australian, as well as unusual extinct species of megafauna, such as Diprotodonts and Thylacoleonids.

The Bluff Downs Local Fauna includes several large reptilian predators, such as crocodiles and a giant varanid (monitor lizard), which has long puzzled palaeontologists as no large predatory terrestrial mammals have been found at the site.

The fauna include species such as the:

• Bluff Downs giant python (Liasis dubudingala), which grew up to 10 m in length
• Bluff Downs giant goanna (Megalania sp.)
• Bluff Downs bandicoot (Perameles allinghamensis)

Palaeoenvironment

The palaeoenvironment of Bluff Downs during the Pliocene featured large water bodies and riparian forests. This is inferred from the presence of certain species which have specialised habitats, as well as the nature of the sediments within the Allingham Formation. The presence of fluviatile and lacustrine sedimentary deposits as well as presence of certain species such as pygmy geese and darters confirms the presence of extensive permanent water bodies, and short-necked chelids and long-necked tortoises suggest shallow, turbid lagoon were a feature of the prehistoric landscape. There was persistent freshwater in the region as fossils of Chara flora, crusteaceans and fish have been found and short-necked chelids also indicate presence of well developed rivers, creeks and lagoons with abundant aquatic fauna. The area experienced a high level of precipitation and humidity, and the palaeoenvironment was similar to present-day Kakadu, and many species are similar across these two locations.

Mammals associated with terrestrial and arboreal habitats, such as ringtail possums, indicate that there was some closed forest habitat present. This forest would have been river-based (riparian) rainforest, and formed a minor component of the palaeoenvironment, as the paucity of possum fossils despite the use of screen washing of sediments suggests.

References

Sources

• Rich, T.H.; Archer, M.; Plane, M.; Flannery, T.F.; Pledge, N.S.; Hand, S. & Rich, P.V. (1982). Australian Tertiary mammal localities. In: "The Fossil Vertebrate Record of Australasia", (ed P.V. Rich & E.M. Thompson). Melbourne: Monash University. pp. 525–572. ISBN 0-86746-153-5.
• "Bluff Downs". Fossil sites of Australia. Australian Museum. 11 August 2009. Retrieved 6 March 2011.
• Archer, M, & Wade, M, 1976. ‘Results of the Ray E. Lemley Expeditions. I. The Allingham Formation and a New Pliocene Vertebrate Fauna from Northern Queensland’. Memoirs of the Queensland Museum, vol.17, no. 3, pp. 379–97.
• Beck, R, Archer, M, Godthelp, H, Mackness, BS, Hand, SJ, & Muirhead, J, 2008, ‘A Bizarre New Family of Marsupialia (Incertae sedis) from the Early Pliocene of Northeastern Australia: Implications for the Phylogeny of Bunodont Marsupials’ Journal of Paleontology, vol. 82, no. 4, pp. 749–762, doi: 10.1666/06-124.1.
• Boles, WE and Mackness B, 1994. ‘Birds from the bluff downs local fauna, Allingham formation, Queensland’. Records of the South Australian Museum, 27, pp. 139–149.
• Hand, SJ, Archer, M, Gilkeson, CF, Godthelp, H, & Cifelli, R, 1992, ‘Earliest known Australian Tertiary mammal fauna’, Nature (London), vol. 356, no. 6369, pp. 514–516, doi: 10.1038/356514a0.
• Mackness, BS, Whitehead, PW, & McNamara, GC, 2000, ‘New potassium-argon basalt date in relation to the Pliocene Bluff Downs Local Fauna, northern Australia’, Australian Journal of Earth Sciences, vol. 47, no. 4, pp. 807–811, doi: 10.1046/j.1440-0952.2000.00812.x.
• Mackness, BS, Wroe, S, Muirhead, J, Wilkinson, C & Wilkinson, D, 2000. ‘First Fossil Bandicoots from the Pliocene’, Australian Mammalogy, vol. 22, no.2, pp. 133–136.
• Scanlon, JD & Mackness, BS 2001, ‘A new giant python from the Pliocene Bluff Downs Local Fauna of northeastern Queensland’, Alcheringa (Sydney), vol. 25, no. 4, pp. 425–437, doi: 10.1080/03115510108619232.
• Thomson, S and Mackness, B, 1999. ‘Fossil turtles from the early Pliocene Bluff Downs Local Fauna, with a description of a new species of Elseya’, Transactions of the Royal Society of South Australia, vol. 123, no. 3, pp. 101–105.
• Twidale, CR, 1956, ‘A physiographic reconnaissance of some Volcanic Provinces in North Queensland, Australia’, Bulletin of Volcanology, vol. 18, no. 1, pp. 3–23, doi: 10.1007/BF02596610.
• Wyatt, DH & Webb, AW, 1970. ‘Potassium‐argon ages of some northern Queensland basalts and an interpretation of late Cainozoic history’, Journal of the Geological Society of Australia, 17(1), pp. 39–51.