The Bluff Downs fossil site is a paleontological site of Pliocene age in northern Queensland, Australia. It is one of the most significant fossil sites of Pliocene age in Australia due to its unique fauna and specific dating. [1] [2] The fossil site lies on the banks of the Allingham Creek on the pastoral property of Bluff Downs Station, northwest of Charters Towers on the Cape York Peninsula [3]
Precise dating of vertebrate fossil sites in Australia is rare, and many Cenozoic-age sediments remain undated. [2] As of 2000, only two Pliocene vertebrate-bearing fossil faunas were specifically dated, Bluff Downs Local Fauna and the Hamilton Local Fauna in Victoria. [4] 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; [2] 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, [2] 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 [5]
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. [6] 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. [7] There was significant volcanic activity in the region 4.5-4.0, 2.3, 1.3 and 1.1 million years ago. [7] Four million years ago, the landscape of northern Queensland would have been similar to Hawaii, with frequent lava flows, [8] 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. [6] 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. [7]
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 [7] ., 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. [6] Bluff Downs Fossil Site is located within the Nulla Basalt Province.
The Nulla Basalt Province covers approximately 4200 square kilometres and is dated to the late Pliocene or early Pleistocene [6] 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. [2] The dating of these flows matches the ordering suggested by analysis of aerial photographs. [7] 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. [7]
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. [2] [7] The flow is associated with the eruption that occurred between 4.5 and 4.0 million years ago.
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. [2] Its position directly above the fossiliferous sediment helped to protect the fossils from erosion, thus ensuring their survival. [8]
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 [9] and analysis of the sediments suggests that during the early Pliocene, a stream widened to form a shallow lake. [10] 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. [2]
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. [10] Fossils were first discovered, collected and reported to the Queensland Museum in 1973. [10] The Bluff Downs Local Fauna is derived from the vertebrate species found in the Allingham Formation.
The Bluff Downs Local Fauna, named and described by Archer in 1976, includes numerous vertebrate species found at the Bluff Downs Fossil Site, [2] 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. [10] This assemblage was noted to be considerably biodiverse by Archer, [10] 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 originally identified by Archer featured 22 taxa with 12 mammals, [10] but this has since been expanded by further discoveries at the site. The fauna includes a wide range of marsupials from families that are still alive today (extant) as well as extinct families, and is typical of Australian Pliocene-era faunas. [5] Several large reptilian predators, such as crocodiles and a giant varanid (monitor lizard), have been found, which has long puzzled palaeontologists as no large predatory terrestrial mammals have been found at the site. [8]
Below is a table of the taxa that were identified by Archer in 1976 and formed the Bluff Downs Local Fauna at that time. Various species within this table have since been confirmed and additional finds of fossils have led to greater biodiversity identified at the site.
| Phylum | Subphylum | Fossil Finds | Species |
| Arthropoda | Crustacea | Gastroliths | Unidentified species
|
| Superclass | Infraclass | Fossil Finds |
| Osteichthys | Teleostei | Spines and vertebra |
| Class | Family | Fossil Finds | Species and additional information |
| Reptilia | Chelidae | Most common fossils found at the site are fragments of shells | Chelodina sp.
|
| Crododilidae | Crocodile teeth second most common fossils, likely multiple species, large vertebrae, limb bones, scutes, skull fragments | Palimnarchus sp. (megafaunal crodidilian)
| |
| Agamidae | Small dentary fragment with seven teeth | Unidentified species
| |
| Varanidae | Two vertebrae, a tooth that is twice as large as teeth of a seven foot Varanus salvadorii | Megalania sp. (giant goanna) | |
| Boidae | Three vertebrae, very large | Bluff Downs Giant Python (Liasis dubudingala) | |
| Elapidae | Two small vertebrae | Unidentified species
| |
| Aves | Circoniidae | Tarsometatarsus | Xenorhyncus asiaticus (Blackheaded Stork) |
| Mammalia | Peramelidae | Isolated molar | Perameles allinghamensis (Bluff Downs Bandicoot) |
| Vombatidae | Left dentary with four molars | Phascolonus lemley (megafaunal wombat) | |
| Phascolarctidae | Isolated molar | Koobor jimbarrati (small koala) | |
| Thylacoleonidae | Dentary fragment | Thylacoleo sp. (very small marsupial lion) | |
| Macopodidae | Partial jaw, several teeth | Protemnodon sp. (short-faced kangaroo) | |
| Fragmented dentaries and jaw | Macropus sp.
| ||
| Isolated molar | Macropus sp.
| ||
| Two isolated molars | Thylogale (pademelon) | ||
| Isolated molar | Small macropodine | ||
| Diprotodontidae | Isolated premolar | Zygomaturus sp. | |
| One complete, two partial skulls, several dentaries, isolated teeth | Euryzygoma sp. | ||
| Dentary fragments | Nototheriine, indeterminate genus | ||
| Unidentified Families | Tooth fragments | Numbigilga ernielundeliusi
| |
| Unidentified Class | Unidentified Families | Coprolites | Unidentified species
|
Other taxa of note include;
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, [12] [15] [14] 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, [15] [9] [12] and many species are similar across these two locations. [8]
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. [13]
The order Peramelemorphia includes the bandicoots and bilbies; it equates approximately to the mainstream of marsupial omnivores. All members of the order are endemic to the twin land masses of Australia-New Guinea and most have the characteristic bandicoot shape: a plump, arch-backed body with a long, delicately tapering snout, very large upright ears, relatively long, thin legs, and a thin tail. Their size varies from about 140 grams up to 4 kilograms, but most species are about one kilogram, or the weight of a half-grown kitten.
Liasis is a genus of pythons found in Indonesia, New Guinea and Australia. Currently, three extant species are recognized and one giant fossil species L. dubudingala, estimated to have been around 10 m (33 ft) in length.
Perameles is a genus of marsupials of the order Peramelemorphia. They are referred to as long-nosed bandicoots or barred bandicoots.
Quinkana is an extinct genus of crocodylians that lived in Australia from about 24 million to about 40,000 years ago. Most attributed specimens have been found in Queensland. It is speculated to have been one of the top predators of Pleistocene Australia.
Palorchestes is an extinct genus of terrestrial, herbivorous marsupials of the family Palorchestidae. The genus was endemic to Australia, living from the Miocene through to the Pleistocene epochs.
The Rattlesnake Formation is a Miocene to late Pliocene geologic formation found along the John Day River Valley of Oregon, in the Western United States.
Elseya is a genus of large side-necked turtles, commonly known as Australian snapping turtles, in the family Chelidae. Species in the genus Elseya are found in river systems in northern and northeastern Australia and throughout the river systems of New Guinea. They are identified by the presence of alveolar ridges on the triturating surfaces of the mouth and the presence of a complex bridge strut.
Perameles allinghamensis, the Bluff Downs bandicoot, is a small extinct bandicoot that lived in Australia 4 million years ago in the Pliocene period. It was discovered at the Bluff Downs fossil site in northern Queensland. Its diet probably consisted of insects and soft roots dug for with its front claws.
The Tingamarra Fauna is associated with the early Eocene Murgon fossil site, and contains the earliest known non-flying eutherian, passerine, trionychidae turtles, mekosuchine crocodiles along with frogs, lungfish and teleost fish in Australia. The Murgon fossil site is located near Kingaroy in south-east Queensland.
Thylacoleo hilli lived during the Pliocene and was half the size of Thylacoleo crassidentatus.
Elseya nadibajagu is a Pliocene species of extinct Australian snapping turtle, described from the Bluff Downs region of Queensland, Australia.
Paleontology in Louisiana refers to paleontological research occurring within or conducted by people from the U.S. state of Louisiana. Outcrops of fossil-bearing sediments and sedimentary rocks within Louisiana are quite rare. In part, this is because Louisiana’s semi-humid climate results in the rapid weathering and erosion of any exposures and the growth of thick vegetation that conceal any fossil-bearing strata. In addition, Holocene alluvial sediments left behind by rivers like the Mississippi, Red, and Ouachita, as well as marsh deposits, cover about 55% of Louisiana and deeply bury local fossiliferous strata.
The Ringold Formation is a geologic formation in Eastern Washington, United States. The formation consists of sediment laid down by the Columbia River following the flood basalt eruptions of the Columbia River Basalt Group reaching up to 1,000 feet (300 m) thick in places. It preserves fossils dating back to the Neogene period.
Kanapoi is a paleontological site in the Kenyan Rift Valley, to the southwest of Lake Turkana. Fossils were first found at Kanapoi in the 1960s by a Harvard expedition, and later by expeditions from the National Museums of Kenya.
Tubul Formation is an Early Pleistocene sedimentary formation located in Arauco Province in south–central Chile. Its sediments were deposited in marine conditions. It overlies unconformably the folded sedimentary formations of Ranquil (Miocene–Pliocene), Quiriquina and the Lebu Group (Paleocene-Eocene).
Hipposideros winsburyorum is a hipposiderid species of bat known by fossil specimens, one of the many new taxa of chiropterans discovered in the Riversleigh World Heritage Area. The species existed during the Pliocene.
Macropus pan is a species of marsupial that existed during the Pliocene in Australia, known only from fossils located at several sites across Australia. The species is recognised as allied to the modern grey kangaroos, the western Macropus fuliginosus and eastern Macropus giganteus, in a clade initially named as subgenus Macropus (Macropus) Dawson & Flannery. The first description was provided by Charles W. De Vis in 1895, emerging from the author's examination of fossil material held at the Queensland Museum. Fossil specimens of Quanbun local fauna, named for a site in Western Australia, were also identified as this species. The origin of the type specimen was not recorded, although based on comparisons to material with a known provenance it is assumed to have excavated at Chinchilla, Queensland. A larger macropod than any modern species, the standing height was estimated to be over two metres.
Crash bandicoot is an extinct bandicoot, known from fossils located at the Riversleigh World Heritage Area in northeast Australia.
Palorchestes selestiae is a fossil species of Diprotodontidae, ancient mammals that existed in Australia.
Koobor was a genus of extinct phascolarctid marsupials. It has two sub-species and they are Koobor jimbarratti and Koobor notabillis. And it has seven sister-species, they are Invictokaola, Madakoala, Litokoala, Nimiokoala, Perikoala, Phascolarcto, and Priscakoala with only Phascolarctos having an extant species.