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Articoli di riviste sul tema "Fossil South Australia St"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 29 gennaio 2023

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1

Cann, John H., Antonio P. Belperio, Victor A. Gostin, and Colin V. Murray-Wallace. "Sea-Level History, 45,000 to 30,000 yr B.P., Inferred from Benthic Foraminifera, Gulf St. Vincent, South Australia." Quaternary Research 29, no. 2 (March 1988): 153–75. http://dx.doi.org/10.1016/0033-5894(88)90058-0.

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Surficial sediments of Gulf St. Vincent, South Australia, are predominantly bioclastic, cool-temperate carbonates. Benthic foraminifera are abundant and distribution of species is closely related to water depth. For example, Massilina milletti is most common at depths ca. 40 m, while Discorbis dimidiatus is characteristics of shallow, subtidal environments. Elphidium crispum, a shallow-water species, and E. macelliforme, favoring deeper water, provide a useful numerical ratio. Their logarithmic relative abundance, in the sediment size fraction 0.50–0.25 mm, correlates strongly with water depth

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2

Conran, John G., and David C. Christophel. "A Fossil Byblidaceae Seed from Eocene South Australia." International Journal of Plant Sciences 165, no. 4 (July 2004): 691–94. http://dx.doi.org/10.1086/386555.

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3

Easton, L. C. "Pleistocene Grey Kangaroos from the Fossil Chamber of Victoria Fossil Cave, Naracoorte, South Australia." Transactions of the Royal Society of South Australia 130, no. 1 (January 2006): 17–28. http://dx.doi.org/10.1080/3721426.2006.10887045.

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4

Itzstein-Davey, Freea. "The representation of Proteaceae in modern pollen rain in species-rich vegetation communities in south-western Australia." Australian Journal of Botany 51, no. 2 (2003): 135. http://dx.doi.org/10.1071/bt02048.

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The Proteaceae family is a large Gondwanan plant family with a major centre of richness in south-western Australia. Modern pollen–vegetation relationships in the two areas of species richness in the northern and southern sandplains of south-western Australia were investigated to calibrate fossil-pollen studies concurrently conducted on Eocene, Pliocene and Quaternary sediment. Results indicated that the Proteaceae component in modern pollen rain can be quite high, contributing up to 50% of the count. Some sites showed a dominant type (such as Banksia–Dryandra), whilst others had up to six diff

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5

Harris, Jamie M. "Fossil Occurrences of Cercartetus Nanus (Marsupialia: Burramyidae) in South Australia." Transactions of the Royal Society of South Australia 130, no. 2 (January 2006): 239–44. http://dx.doi.org/10.1080/3721426.2006.10887063.

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6

Betts, Marissa J., John R. Paterson, James B. Jago, Sarah M. Jacquet, Christian B. Skovsted, Timothy P. Topper, and Glenn A. Brock. "A new lower Cambrian shelly fossil biostratigraphy for South Australia." Gondwana Research 36 (August 2016): 176–208. http://dx.doi.org/10.1016/j.gr.2016.05.005.

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7

Reed, E. H., and S. J. Bourne. "Pleistocene Fossil vertebrate Sites of the South East Region of South Australia II." Transactions of the Royal Society of South Australia 133, no. 1 (January 2009): 30–40. http://dx.doi.org/10.1080/03721426.2009.10887108.

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8

Betts, Marissa J., John R. Paterson, James B. Jago, Sarah M. Jacquet, Christian B. Skovsted, Timothy P. Topper, and Glenn A. Brock. "A new lower Cambrian shelly fossil biostratigraphy for South Australia: Reply." Gondwana Research 44 (April 2017): 262–64. http://dx.doi.org/10.1016/j.gr.2016.11.004.

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9

Turner, S. "Australia's first discovered fossil fish is still missing!" Geological Curator 9, no. 5 (May 2011): 285–90. http://dx.doi.org/10.55468/gc83.

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Seeking Australian specimens collected in the 19th century always needs detective work. Fossils collected by one colourful collector, the Polish 'Count' Paul Strzelecki, from early travels in the colony of New South Wales are being sought. A 30-year search has still not brought to light in Australia or Britain the first fossil fish found from the Lower Carboniferous of New South Wales.

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10

Field, Judith, and John Dodson. "Late Pleistocene Megafauna and Archaeology from Cuddie Springs, South-eastern Australia." Proceedings of the Prehistoric Society 65 (1999): 275–301. http://dx.doi.org/10.1017/s0079497x00002024.

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The Cuddie Springs site in south-eastern Australia provides the first evidence of an unequivocal association of megafauna with humans for this continent. Cuddie Springs has been known as a fossil megafauna locality for over a century, but its archaeological record has only recently been identified. Cuddie Springs is an open site, with the fossil deposits preserved in a claypan on the floor of an ancient ephemeral lake. Investigations revealed a stratified deposit of human occupation and fossil megafauna, suggesting a temporal overlap and an active association of megafauna with people in the le

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11

Thorn, Kailah M., Robin Roe, Alexander Baynes, Raymond P. Hart, Kenneth A. Lance, Duncan Merrilees, Jennifer K. Poorter, and Sandra Sofoulis. "Fossil mammals of Caladenia Cave, northern Swan Coastal Plain, south-western Australia." Records of the Western Australian Museum 32, no. 2 (2017): 217. http://dx.doi.org/10.18195/10.18195/issn.0312-3162.32(2).2017.217-236.

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12

Thorn, Kailah M., Robin Roe, Alexander Baynes, Raymond P. Hart, Kenneth A. Lance, Duncan Merrilees, Jennifer K. Poorter, and Sandra Sofoulis. "Fossil mammals of Caladenia Cave, northern Swan Coastal Plain, south-western Australia." Records of the Western Australian Museum 32, no. 2 (2017): 217. http://dx.doi.org/10.18195/issn.0312-3162.32(2).2017.217-236.

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13

Gell, P., J. Tibby, J. Fluin, P. Leahy, M. Reid, K. Adamson, S. Bulpin, et al. "Accessing limnological change and variability using fossil diatom assemblages, south-east Australia." River Research and Applications 21, no. 2-3 (2005): 257–69. http://dx.doi.org/10.1002/rra.845.

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14

Macphail, Mike, and Andrew H. Thornhill. "How old are the eucalypts? A review of the microfossil and phylogenetic evidence." Australian Journal of Botany 64, no. 8 (2016): 579. http://dx.doi.org/10.1071/bt16124.

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Molecular age estimates for the Eucalypteae (family Myrtaceae) suggest that the eucalypts, possibly associated with fire, have been present for ~65 million years. In contrast, macrofossils and fossil pollen attributable to three important eucalypt genera (Angophora, Corymbia and Eucalyptus) in the Eucalypteae date to ~51–53 million years ago (mid-Early Eocene) in Patagonia, eastern Antarctica and south-eastern Australia. At present, there is no fossil evidence to show that eucalypts had evolved before this epoch, i.e. when Australia was part of eastern Gondwana, although this seems probable on

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15

Greenwood, DR. "Eocene monsoon forests in central Australia?" Australian Systematic Botany 9, no. 2 (1996): 95. http://dx.doi.org/10.1071/sb9960095.

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The Australian Tertiary plant fossil record documents rainforests of a tropical to temperate character in south-eastern and south-western Australia for much of the Early Tertiary, and also shows the climatically mediated contraction of these rainforests in the mid to Late Tertiary. The fossil record of Australian monsoon forests, that is semi-evergreen to deciduous vine forests and woodlands of the wet-dry tropics, however, is poorly known. Phytogeographic analyses have suggested an immigrant origin for some floral elements of present day monsoon forests in northern Australia, while other elem

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16

Martin, Helene A. "History of the family Malpighiaceae in Australia and its biogeographic implications: evidence from pollen." Australian Journal of Botany 50, no. 2 (2002): 171. http://dx.doi.org/10.1071/bt01039.

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Three pollen types of the family Malpighiaceae have been identified in the Tertiary fossil record of south-eastern Australia. There are two species of the family native to Australia and they have the same pollen type. There was thus a greater diversity of malpighiaceous taxa during the Tertiary than there is today. The family is found mainly in tropical regions and it is thought that northern South America was the centre of origin. The restriction of the two species to coastal north-eastern Australia suggests recent migration into the area and gives no hint of the long history of the family in

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17

Hill, Robert S., Tom Lewis, Raymond J. Carpenter, and Sung Soo Whang. "Agathis (Araucariaceae) macrofossils from Cainozoic sediments in south-eastern Australia." Australian Systematic Botany 21, no. 3 (2008): 162. http://dx.doi.org/10.1071/sb08006.

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Organically preserved Cainozoic leaf fossils previously referred to Agathis are re-examined, and in all cases their affinity with that genus is confirmed. Previously undescribed organically preserved leaf fossils from several Cainozoic sites in south-eastern Australia are compared with Agathis and Wollemia and two new species of Agathis are described. Intraspecific variation in leaf cuticle morphology is examined in extant A. macrophylla in particular, and is found to be much higher than previously recorded. This makes assignment of fossil Agathis leaves to species difficult, especially when o

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18

Droser, Mary L., Lidya G. Tarhan, Scott D. Evans, Rachel L. Surprenant, and James G. Gehling. "Biostratinomy of the Ediacara Member (Rawnsley Quartzite, South Australia): implications for depositional environments, ecology and biology of Ediacara organisms." Interface Focus 10, no. 4 (June 12, 2020): 20190100. http://dx.doi.org/10.1098/rsfs.2019.0100.

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The Precambrian Ediacara Biota—Earth's earliest fossil record of communities of macroscopic, multicellular organisms—provides critical insights into the emergence of complex life on our planet. Excavation and reconstruction of nearly 300 m 2 of fossiliferous bedding planes in the Ediacara Member of the Rawnsley Quartzite, at the National Heritage Ediacara fossil site Nilpena in South Australia, have permitted detailed study of the sedimentology, taphonomy and palaeoecology of Ediacara fossil assemblages. Characterization of Ediacara macrofossils and textured organic surfaces at the scale of fa

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19

SCHMIDT, ROLF, and YVONNE BONE. "Biogeography of Eocene bryozoans from the St Vincent Basin, South Australia." Lethaia 36, no. 4 (December 2003): 345–56. http://dx.doi.org/10.1080/00241160310006394.

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20

Sprigg, Reg. "On the 1946 Discovery of the Precambrian Ediacabian Fossil Fauna in South Australia." Earth Sciences History 7, no. 1 (January 1, 1988): 46–51. http://dx.doi.org/10.17704/eshi.7.1.p13447q2753jr055.

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The discovery of the Ediacarian metazoan fossil fauna in South Australia on March 27, 1946, by the author represented the culmination of a decade of widespread and diligent search. It was not, as one authority has recorded,…"basically fortuitous." The find was made in the course of widespread mapping of the late Proterozoic-Cambrian succession and followed Sprigg's remapping, remeasurement and redefinition of Howchin's "Adelaide Series" through to the base of the fossiliferous Cambrian succession.

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21

Basinger, J. F., D. R. Greenwood, P. G. Wilson, and D. C. Christophel. "Fossil flowers and fruits of capsular Myrtaceae from the Eocene of South Australia." Canadian Journal of Botany 85, no. 2 (January 2007): 204–15. http://dx.doi.org/10.1139/b07-001.

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Flowers and fruits of the Myrtaceae are described from the Middle Eocene Golden Grove locality of South Australia, and the taxon is here named Tristaniandra alleyi gen. et sp.nov. Flowers are pentamerous and perigynous, with sepals, petals, and stamens inserted on the rim of a hypanthium. Filaments are basally fused to form antepetalous stamen bundles, each consisting of about 6–8 stamens. The tricarpellate ovary becomes exserted on maturation, forming a partly exserted, dry fruit with loculicidal dehiscence. These features are typical of capsular-fruited members of the Myrtaceae; in particula

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22

Wilson, George D. F. "Gondwanan groundwater: subterranean connections of Australian phreatoicidean isopods (Crustacea) to India and New Zealand." Invertebrate Systematics 22, no. 2 (2008): 301. http://dx.doi.org/10.1071/is07030.

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Phreatoicidea Stebbing, 1893 live in freshwaters of Gondwana: Australia, South Africa, India and New Zealand. Many of these isopods have a subterranean lifestyle. Parsimony analysis of morphological data of generic exemplars and a Triassic fossil was used to explore the timing of this habitat adaption. The monophyly of the Hypsimetopidae Nicholls, 1943, including blind taxa Hyperoedesipus Nicholls & Milner, 1923 (Western Australia), Nichollsia Chopra and Tiwari, 1950 (Ganges Plain, India) and Phreatoicoides Sayce, 1900 (Tasmania and Victoria) was strongly supported. Crenisopus Wilson and K

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23

Gehling, James G., Bruce N. Runnegar, and Mary L. Droser. "Scratch Traces of Large Ediacara Bilaterian Animals." Journal of Paleontology 88, no. 2 (March 2014): 284–98. http://dx.doi.org/10.1666/13-054.

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Ediacara fan-shaped sets of paired scratchesKimberichnus teruzziifrom the Ediacara Member of the Rawnsley Quartzite, South Australia, and the White Sea region of Russia, represent the earliest known evidence in the fossil record of feeding traces associated with the responsible bilaterian organism. These feeding patterns exclude arthropod makers and point to the systematic feeding excavation of seafloor microbial mats by large bilaterians of molluscan grade. Since the scratch traces were made into microbial mats, animals could crawl over previous traces without disturbing them. The trace maker

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24

Bell, Phil R., Russell D. C. Bicknell, and Elizabeth T. Smith. "Crayfish bio-gastroliths from eastern Australia and the middle Cretaceous distribution of Parastacidae." Geological Magazine 157, no. 7 (October 30, 2019): 1023–30. http://dx.doi.org/10.1017/s0016756819001092.

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AbstractFossil crayfish are typically rare, worldwide. In Australia, the strictly Southern Hemisphere clade Parastacidae, while ubiquitous in modern freshwater systems, is known only from sparse fossil occurrences from the Aptian–Albian of Victoria. We expand this record to the Cenomanian of northern New South Wales, where opalized bio-gastroliths (temporary calcium storage bodies found in the foregut of pre-moult crayfish) form a significant proportion of the fauna of the Griman Creek Formation. Crayfish bio-gastroliths are exceedingly rare in the fossil record but here form a remarkable supp

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25

Hill, RS. "Araucaria (Araucariaceae) species from Australian tertiary sediments — a micromorphological study." Australian Systematic Botany 3, no. 2 (1990): 203. http://dx.doi.org/10.1071/sb9900203.

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The cuticular micromorphology of four existing and four new species of Araucaria from Australian Tertiary sediments is examined using scanning electron microscopy. Scanning electron microscopy is very useful for distinguishing species, but less successful for determining the affinities of the fossil species within the genus. Two fossil species, A. balcombensis Selling and A. hastiensis Bigwood & Hill, are closely related to the extant South American species A. araucana (Molina) K. Koch (section Columbea). Five fossil species, A. lignitici Cookson & Duigan, A. planus R. Hill, sp. nov.,

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26

SURPRENANT, RACHEL L., JAMES G. GEHLING, and MARY L. DROSER. "BIOLOGICAL AND ECOLOGICAL INSIGHTS FROM THE PRESERVATIONAL VARIABILITY OF FUNISIA DOROTHEA, EDIACARA MEMBER, SOUTH AUSTRALIA." PALAIOS 35, no. 9 (September 1, 2020): 359–76. http://dx.doi.org/10.2110/palo.2020.014.

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ABSTRACT The Ediacara Biota represents a turning point in the evolution of life on Earth, signifying the transition from single celled organisms to complex, community-forming macrobiota. The exceptional fossil record of the soft-bodied Ediacara Biota provides critical insight into the nature of this transition and into ecosystem dynamics leading up to the so-called “Cambrian Explosion”. However, the preservation of non-biomineralizing organisms in a diversity of lithologies goes hand-in-hand with considerable taphonomic complexity that often shrouds true paleoecological and paleobiological sig

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27

Li, Yifan, Luliang Huang, Cheng Quan, Jianhua Jin, and Alexei A. Oskolski. "Fossil wood of Syzygium from the Miocene of Guangxi, South China: the earliest fossil evidence of the genus in eastern Asia." IAWA Journal 42, no. 4 (September 17, 2021): 435–41. http://dx.doi.org/10.1163/22941932-bja10069.

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Abstract A new species, Syzygium guipingensis sp. nov. (Myrtaceae), is described based on mummified fossil wood from the Miocene Erzitang Formation of Guiping Basin, Guangxi, South China. This species represents the most ancient reliable fossil record of the genus Syzygium in eastern Asia, showing the greatest similarity to the extant species S. buxifolium Hook. et Arnott. Its occurrence in the Miocene is consistent with the diversification age of the Asian lineage within Syzygium as estimated by molecular dating (11.4 Ma). The fossil record of Syzygium suggests that this genus migrated from A

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28

Bennett, C. Verity, Paul Upchurch, Francisco J. Goin, and Anjali Goswami. "Deep time diversity of metatherian mammals: implications for evolutionary history and fossil-record quality." Paleobiology 44, no. 2 (February 6, 2018): 171–98. http://dx.doi.org/10.1017/pab.2017.34.

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AbstractDespite a global fossil record, Metatheria are now largely restricted to Australasia and South America. Most metatherian paleodiversity studies to date are limited to particular subclades, time intervals, and/or regions, and few consider uneven sampling. Here, we present a comprehensive new data set on metatherian fossil occurrences (Barremian to end Pliocene). These data are analyzed using standard rarefaction and shareholder quorum subsampling (including a new protocol for handling Lagerstätte-like localities).Global metatherian diversity was lowest during the Cretaceous, and increas

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29

Maher, W. A. "Trace metal concentrations in marine organisms from St. Vincent Gulf, South Australia." Water, Air, and Soil Pollution 29, no. 1 (May 1986): 77–84. http://dx.doi.org/10.1007/bf00149330.

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30

Antos, Mark, and William Steele. "A likely breeding record of Brown Quail Synoicus ypsilophorus at St Peter Island, Nuyts Archipelago, South Australia." Australian Field Ornithology 38 (2021): 107–12. http://dx.doi.org/10.20938/afo38107112.

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This note reports observations of birds and other vertebrates during a short stay at St Peter Island, Nuyts Archipelago, South Australia, during November 2019. Of most interest was a sighting of juvenile Brown Quail Synoicus ypsilophorus, outside the generally reported range of this species and representing the first breeding record of which we are aware for this species at St Peter Island. This is one of a series of relatively recent sightings in the west of South Australia, which indicates an ongoing range expansion for this species. Further fauna surveys on the Nuyts Archipelago, with docum

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31

Sappenfield, Aaron, Mary L. Droser, and James G. Gehling. "Problematica, trace fossils, and tubes within the Ediacara Member (South Australia): redefining the ediacaran trace fossil record one tube at a time." Journal of Paleontology 85, no. 2 (March 2011): 256–65. http://dx.doi.org/10.1666/10-068.1.

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Ediacaran trace fossils are becoming an increasingly less common component of the total Precambrian fossil record as structures previously interpreted as trace fossils are reinterpreted as body fossils by utilizing qualitative criteria. Two morphotypes, Form E and Form F of Glaessner (1969), interpreted as trace fossils from the Ediacara Member of the Rawnsley Quartzite in South Australia are shown here to be body fossils of a single, previously unidentified tubular constructional morphology formally described herein as Somatohelix sinuosus n. gen. n. sp. S. sinuosus is 2-7 mm wide and 3-14 cm

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32

PERRI, E., M. E. TUCKER, and A. SPADAFORA. "Carbonate organo-mineral micro- and ultrastructures in sub-fossil stromatolites: Marion lake, South Australia." Geobiology 10, no. 2 (October 31, 2011): 105–17. http://dx.doi.org/10.1111/j.1472-4669.2011.00304.x.

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Murray, Andrew P., Dianne Padley, David M. McKirdy, Webber E. Booth, and Roger E. Summons. "Oceanic transport of fossil dammar resin: The chemistry of coastal resinites from South Australia." Geochimica et Cosmochimica Acta 58, no. 14 (July 1994): 3049–59. http://dx.doi.org/10.1016/0016-7037(94)90178-3.

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34

Gehling, J. G. "Earliest known echinoderm — a new Ediacaran fossil from the Pound Subgroup of South Australia." Alcheringa: An Australasian Journal of Palaeontology 11, no. 4 (January 1987): 337–45. http://dx.doi.org/10.1080/03115518708619143.

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35

Gr�n, Rainer, Kevin Moriarty, and Rod Wells. "Electron spin resonance dating of the fossil deposits in the Naracoorte Caves, South Australia." Journal of Quaternary Science 16, no. 1 (January 2001): 49–59. http://dx.doi.org/10.1002/1099-1417(200101)16:1<49::aid-jqs570>3.0.co;2-#.

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36

Fraser, Rebecca, and Roderick Wells. "Palaeontological excavation and taphonomic investigation of the late Pleistocene fossil deposit in Grant Hall, Victoria Fossil Cave, Naracoorte, South Australia." Alcheringa: An Australasian Journal of Palaeontology 31 (2006): 147–61. http://dx.doi.org/10.1080/03115510608619579.

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FRASER, REBECCA A., and RODERICK T. WELLS. "Palaeontological excavation and taphonomic investigation of the late Pleistocene fossil deposit in Grant Hall, Victoria Fossil Cave, Naracoorte, South Australia." Alcheringa: An Australasian Journal of Palaeontology 30, sup1 (January 2006): 147–61. http://dx.doi.org/10.1080/03115510609506860.

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38

Liddle, Nerida R., Matthew C. McDowell, and Gavin J. Prideaux. "Insights into the pre-European mammalian fauna of the southern Flinders Ranges, South Australia." Australian Mammalogy 40, no. 2 (2018): 262. http://dx.doi.org/10.1071/am17035.

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Many Australian mammal species have suffered significant declines since European colonisation. During the first century of settlement, information on species distribution was rarely recorded. However, fossil accumulations can assist the reconstruction of historical distributions. We examine a fossil vertebrate assemblage from Mair’s Cave, one of few known from the southern Flinders Ranges, South Australia. The Mair’s Cave assemblage was dominated by mammals but also included birds and reptiles. Of the 18 mammals recovered, two have not previously been recorded from the southern Flinders Ranges

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39

Evans, Scott D., Ian V. Hughes, James G. Gehling, and Mary L. Droser. "Discovery of the oldest bilaterian from the Ediacaran of South Australia." Proceedings of the National Academy of Sciences 117, no. 14 (March 23, 2020): 7845–50. http://dx.doi.org/10.1073/pnas.2001045117.

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Analysis of modern animals and Ediacaran trace fossils predicts that the oldest bilaterians were simple and small. Such organisms would be difficult to recognize in the fossil record, but should have been part of the Ediacara Biota, the earliest preserved macroscopic, complex animal communities. Here, we describeIkaria wariootiagen. et sp. nov. from the Ediacara Member, South Australia, a small, simple organism with anterior/posterior differentiation. We find that the size and morphology ofIkariamatch predictions for the progenitor of the trace fossilHelminthoidichnites—indicative of mobility

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40

Hill, RS. "Leaves of Eucryphia (Eucryphiaceae) from tertiary sediments in south-eastern Australia." Australian Systematic Botany 4, no. 3 (1991): 481. http://dx.doi.org/10.1071/sb9910481.

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Eucryphia leaves recovered from Tertiary sediments in south-eastern Australia are assigned to three new species, E. falcata (Late Palaeocene, Lake Bungarby), E. microstoma (Early Eocene, Regatta Point) and E. aberensis (Middle to Late Eocene, Loch Aber). Leaves from Early Pleistocene sediments at Regatta Point are re-examined and are considered to be closely related to the extant species, E. lucida and E. milliganii. An examination of the leaf morphology of the fossil and extant species suggests that evolution has taken place, resulting in smaller leaves at higher latitudes and/or altitudes pr

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Haby, Nerissa, and Darren Herpich. "Search for cryptic Pseudomys shortridgei in suitable habitat in the south-east of South Australia." Australian Mammalogy 32, no. 1 (2010): 47. http://dx.doi.org/10.1071/am09022.

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Abstract (sommario):

Pseudomys shortridgei has been recorded from a restricted and fragmented distribution across southern Australia. Fossil deposits represented the species in mainland South Australia. However, the discovery of an extant population of P. shortridgei in the lower south-east of South Australia, and its morphological similarity to the more common Rattus fuscipes and R. lutreolus highlighted the need to verify the current distribution of the species. Existing vegetation community and systematic baseline biological survey data were used in a fast, cost-effective and systematic desktop assessment to id

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42

Bean, Lynne B. "Reappraisal of Mesozoic fishes and associated invertebrates and flora from Talbragar and Koonwarra, eastern Australia." Proceedings of the Royal Society of Victoria 129, no. 1 (2017): 7. http://dx.doi.org/10.1071/rs17001.

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Abstract (sommario):

Eastern Australia has two major Mesozoic fossil localities. The Talbragar Fish Bed in central west New South Wales contains an assemblage of Upper Jurassic fishes, plants and insects. The Koonwarra Fossil Bed, in South Gippsland, Victoria, has an assemblage of Lower Cretaceous fishes, plants and insects. The geological settings of these localities are described. Each locality has a common genus of fish that was originally described as Leptolepis. The names of both these fish have been changed, the Talbragar one to Cavenderichthys talbragarensis and the Koonwarra one to Waldmanichthys koonwarri

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43

McDowell, Matthew C., Alexander Baynes, Graham C. Medlin, and Gavin J. Prideaux. "The impact of European colonization on the late-Holocene non-volant mammals of Yorke Peninsula, South Australia." Holocene 22, no. 12 (September 24, 2012): 1441–50. http://dx.doi.org/10.1177/0959683612455542.

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Abstract (sommario):

Over the last 200 years Australia has suffered the greatest rate of mammal species extinction of any continent. This demands extensive biodiversity research, but unfortunately has been hampered by poor documentation of Australia’s native species at the time of European colonization. Late-Holocene fossil mammal assemblages preserved in caves, rockshelters and surface lag deposits from deflated sand dunes can provide a more complete understanding of pre-European ecological conditions than can be developed from our knowledge of present biodiversity. In South Australia, few regions have experience

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44

Brown, Lauren. "The enigmatic palaeoecology and palaeobiogeography of the giant, horned, fossil turtles of Australasia: a review and reanalysis of the data." Herpetological Journal, Volume 29, Number 4 (October 1, 2018): 252–63. http://dx.doi.org/10.33256/29.4.252263.

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Abstract (sommario):

The distribution pattern of the bizarre Australasian giant, horned, fossil turtles of the clade Meiolaniidae has puzzled biogeographers since their discovery late in the nineteenth century. While their distribution suggests a Gondwanan origin, the lack of fossil evidence from key times and places has inhibited a better understanding of their dispersal pathways to Australia and the south-west Pacific islands in which their fossils have been found. Much palaeoecological speculation related to their dispersal capabilities, ranging from purely terrestrial to freshwater, estuarine, and saltwater li

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45

Triantafillos, Lianos, Stephen Donnellan, and Alan J. Butler. "Population genetic structure of the muricid gastropodLepsiella vinosain Gulf St Vincent, South Australia." Molluscan Research 19, no. 2 (January 1998): 31–42. http://dx.doi.org/10.1080/13235818.1998.10673716.

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46

de Silva Samarasinghe, J. R., L. Bode, and L. B. Mason. "Modelled response of Gulf St Vincent (South Australia) to evaporation, heating and winds." Continental Shelf Research 23, no. 14-15 (September 2003): 1285–313. http://dx.doi.org/10.1016/s0278-4343(03)00129-8.

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47

James, Noel P., and Yvonne Bone. "Eocene cool-water carbonate and biosiliceous sedimentation dynamics, St Vincent Basin, South Australia." Sedimentology 47, no. 4 (August 2000): 761–86. http://dx.doi.org/10.1046/j.1365-3091.2000.00315.x.

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48

Butler, A. J. "Recruitment of sessile invertebrates at five sites in Gulf St. Vincent, South Australia." Journal of Experimental Marine Biology and Ecology 97, no. 1 (June 1986): 13–36. http://dx.doi.org/10.1016/0022-0981(86)90065-1.

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49

Pledge, Neville S. "The Curramulka local fauna: A new late Tertiary fossil assemblage from Yorke Peninsula, South Australia." Beagle : Records of the Museums and Art Galleries of the Northern Territory 9, no. 1 (December 1992): 115–42. http://dx.doi.org/10.5962/p.263122.

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50

Beattie, Robert G., and Steven Avery. "Palaeoecology and palaeoenvironment of the Jurassic Talbragar Fossil Fish Bed, Gulgong, New South Wales, Australia." Alcheringa: An Australasian Journal of Palaeontology 36, no. 4 (December 2012): 453–68. http://dx.doi.org/10.1080/03115518.2012.671675.

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