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Relevant bibliographies by topics / Trace fossils Australia, Central

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Academic literature on the topic 'Trace fossils Australia, Central'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 January 2023

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Journal articles on the topic "Trace fossils Australia, Central"

1

Walter, M. R., R. Elphinstone, and G. R. Heys. "Proterozoic and Early Cambrian trace fossils from the Amadeus and Georgina Basins, central Australia." Alcheringa: An Australasian Journal of Palaeontology 13, no. 3 (January 1989): 209–56. http://dx.doi.org/10.1080/03115518908527821.

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McMahon, William J., Alexander G. Liu, Benjamin H. Tindal, and Maarten G. Kleinhans. "Ediacaran life close to land: Coastal and shoreface habitats of the Ediacaran macrobiota, the Central Flinders Ranges, South Australia." Journal of Sedimentary Research 90, no. 11 (November 30, 2020): 1463–99. http://dx.doi.org/10.2110/jsr.2020.029.

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ABSTRACT The Rawnsley Quartzite of South Australia hosts some of the world's most diverse Ediacaran macrofossil assemblages, with many of the constituent taxa interpreted as early representatives of metazoan clades. Globally, a link has been recognized between the taxonomic composition of individual Ediacaran bedding-plane assemblages and specific sedimentary facies. Thorough characterization of fossil-bearing facies is thus of fundamental importance for reconstructing the precise environments and ecosystems in which early animals thrived and radiated, and distinguishing between environmental

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3

Barnes, Richard W., and Robert S. Hill. "Ceratopetalum fruits from Australian cainozoic sediments and their significance for petal evolution in the genus." Australian Systematic Botany 12, no. 5 (1999): 635. http://dx.doi.org/10.1071/sb98014.

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Ceratopetalum Sm. fruits are characterised by 4–6 enlarged woody sepals radiating from a central disk, a semi-inferior ovary, anthers between and above each sepal and three-trace sepal venation with a prominent intra-sepal vein. Two new species of Ceratopetalum are described from fruits extracted from Australian Cainozoic sediments, C. westermannii and C. maslinensis. The presence of Ceratopetalum in Middle Eocene Maslin Bay sediments, South Australia, indicates a more widespread geographic distribution for the genus during the Cenozoic. Petally is present in one extant and two fossil species

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4

Cramwinckel, Margot J., Lineke Woelders, Emiel P. Huurdeman, Francien Peterse, Stephen J. Gallagher, Jörg Pross, Catherine E. Burgess, Gert-Jan Reichart, Appy Sluijs, and Peter K. Bijl. "Surface-circulation change in the southwest Pacific Ocean across the Middle Eocene Climatic Optimum: inferences from dinoflagellate cysts and biomarker paleothermometry." Climate of the Past 16, no. 5 (September 1, 2020): 1667–89. http://dx.doi.org/10.5194/cp-16-1667-2020.

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Abstract. Global climate cooled from the early Eocene hothouse (∼52–50 Ma) to the latest Eocene (∼34 Ma). At the same time, the tectonic evolution of the Southern Ocean was characterized by the opening and deepening of circum-Antarctic gateways, which affected both surface- and deep-ocean circulation. The Tasmanian Gateway played a key role in regulating ocean throughflow between Australia and Antarctica. Southern Ocean surface currents through and around the Tasmanian Gateway have left recognizable tracers in the spatiotemporal distribution of plankton fossils, including organic-walled dinofl

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5

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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TRAVOUILLON, KENNY J., BRUNO F. SIMÕES, ROBERTO PORTELA MIGUEZ, SELINA BRACE, PHILIPPA BREWER, DAVID STEMMER, GILBERT J. PRICE, JONATHAN CRAMB, and JULIEN LOUYS. "Hidden in plain sight: reassessment of the pig-footed bandicoot, Chaeropus ecaudatus (Peramelemorphia, Chaeropodidae), with a description of a new species from central australia, and use of the fossil record to trace its past distribution." Zootaxa 4566, no. 1 (March 13, 2019): 1. http://dx.doi.org/10.11646/zootaxa.4566.1.1.

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The Pig-footed Bandicoot, Chaeropus ecaudatus, an extinct arid-adapted bandicoot, was named in 1838 based on a specimen without a tail from the Murray River in New South Wales. Two additional species were later named, C. castanotis and C. occidentalis, which have since been synonymised with C. ecaudatus. Taxonomic research on the genus is rather difficult because of the limited material available for study. Aside from the types of C. castanotis and C. occidentalis housed at the Natural History Museum in London, and the type of C. ecaudatus at the Australian Museum in Sydney, there are fewer th

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7

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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8

Kakuwa, Yoshitaka, and James D. Floyd. "Trace fossils in Ordovician radiolarian chert successions in the Southern Uplands, Scotland." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 107, no. 1 (March 2016): 13–22. http://dx.doi.org/10.1017/s1755691017000044.

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ABSTRACTRadiolarian chert and associated siliceous claystone in the Southern Uplands of Scotland are examined, in order to study the Great Ordovician Biodiversification Event of benthic animals on the pelagic ocean bottom. Trace fossils which are uncommon, but convincing, are found in the grey chert and siliceous claystone of Gripps Cleuch. These observations constitute firm evidence that large benthic animals which could leave visible trace fossils had colonised the Iapetan Ocean by the late Middle Ordovician, confirming previous studies from Australia for Panthalassa, the other huge ocean. R

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9

Wnuk, Christopher, and John O. Maberry. "Enigmatic eight-meter trace fossils in the Lower Pennsylvanian Lee Sandstone, central Appalachian Basin, Tennessee." Journal of Paleontology 64, no. 3 (May 1990): 440–50. http://dx.doi.org/10.1017/s0022336000018679.

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Enigmatic tubular trace fossils up to eight meters long occur in the Lower Pennsylvanian Middlesboro Member of the Lee Formation. Two morphotypes occur: type 1 trace fossils are plain, smooth, vertical, nonbranching, parallel-walled, tubular structures; type 2 trace fossils branch, have walls with faint vertical striations, regularly or irregularly spaced nodes, and funnel-shaped terminations. Sandstone casts filling type 2 structures have helical spiral morphology, and, in rare individuals, faint meniscate fills have been observed. Both trace-fossil morphotypes have poorly cemented wall linin

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Gibson, Gail G. "Trace fossils from Late Precambrian Carolina slate belt, south-central North Carolina." Journal of Paleontology 63, no. 1 (January 1989): 1–10. http://dx.doi.org/10.1017/s0022336000040889.

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The volcanosedimentary sequence of the Carolina slate belt in south-central North Carolina was long thought to be unfossiliferous; however, the 5,484–7,315 meters of dominantly evenly bedded siltstones and mudstones have recently yielded body fossils of the late Precambrian Ediacarian fauna and a Middle Cambrian trilobite assemblage. Ongoing stratigraphic studies in the Carolina slate belt of southern North Carolina have now revealed trace fossils representing the ichnotaxa Gordia arcuata?, ?Helminthopsis sp., Monocraterion sp., Neonerites biserialis, N. uniserialis, ?Neonerites sp., Planolite

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Dissertations / Theses on the topic "Trace fossils Australia, Central"

1

Thomson, A. J. "Lower Cambrian trace fossils of the Amadeus Basin, central Australia /." Title page, abstract and contents only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbt482.pdf.

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Baghiyan-Yazd, Mohammad Hassan. "Palaeoichnology of the terminal Proterozoic-Early Cambrian transition in central Australia : interregional correlation and palaeoecology." Title page, table of contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phb1445.pdf.

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Baghiyan-Yazd, Mohammad Hassan. "Palaeoichnology of the terminal Proterozoic-Early Cambrian transition in central Australia : interregional correlation and palaeoecology / Mohammad Hassan Baghiyan-Yazd." Thesis, 1998. http://hdl.handle.net/2440/21668.

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Books on the topic "Trace fossils Australia, Central"

1

Jensen, Sören. Trace fossils from the Lower Cambrian Mickwitzia sandstone, south-central Sweden. Oslo: Scandinavian University Press, 1997.

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2

Mikuláš, Radek. Trace fossils from the Middle Cambrian of the Barrandian area (central Bohemia, Czech Republic). Prague: Czech Geological Survey, 2000.

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Fritz, W. H. Lithology, trace fossils, and correlation of Precambrian-Cambrian boundary beds, Cassiar Mountains, North-Central British Columbia. Ottawa: Energy, Mines and Resources Canada, 1985.

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Jensen, S. Trace Fossils from the Lower Cambrian Mickwitzia Sandstone, South-Central Sweden, Number 42. Wiley-Blackwell, 2006.

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5

Johansen, Bruce, and Adebowale Akande, eds. Nationalism: Past as Prologue. Nova Science Publishers, Inc., 2021. http://dx.doi.org/10.52305/aief3847.

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Nationalism: Past as Prologue began as a single volume being compiled by Ad Akande, a scholar from South Africa, who proposed it to me as co-author about two years ago. The original idea was to examine how the damaging roots of nationalism have been corroding political systems around the world, and creating dangerous obstacles for necessary international cooperation. Since I (Bruce E. Johansen) has written profusely about climate change (global warming, a.k.a. infrared forcing), I suggested a concerted effort in that direction. This is a worldwide existential threat that affects every living t

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Book chapters on the topic "Trace fossils Australia, Central"

1

JORDAN, DOUGLAS W. "TRACE FOSSILS AND DEPOSITIONAL ENVIRONMENTS OF UPPER DEVONIAN BLACK SHALES, EAST-CENTRAL KENTUCKY, U.S.A." In Biogenic Structures, 279–98. SEPM (Society for Sedimentary Geology), 1985. http://dx.doi.org/10.2110/pec.85.35.0279.

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2

Kakuwa, Yoshitaka, and John Webb. "Trace Fossils of a Middle to Upper Ordovician Pelagic Deep-Ocean Bedded Chert in Southeastern Australia." In Sediment–Organism InteractionsA Multifaceted Ichnology. SEPM Society for Sedimentary Geology, 2007. http://dx.doi.org/10.2110/pec.07.88.0267.

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Conference papers on the topic "Trace fossils Australia, Central"

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Cribb, Alison, Simon A. F. Darroch, and Marc Laflamme. "INTERPRETING COMPLEXITY OF TRACE FOSSILS FROM THE LATEST NEOPROTEROZOIC NAMA GROUP, NAMIBIA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290835.

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2

Korf, Jason J., John Westgaard, H. Douglas Hanks, Alexander Hastings, and Steve Willging. "TRACE FOSSILS IN THE LATE CRETACEOUS COLERAINE FORMATION; HILL ANNEX MINE STATE PARK, CALUMET, MINNESOTA." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348187.

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Martin, Tony, Melissa Lowery, Michael Hall, Thomas H. Rich, Steven Morton, Lesley Kool, Peter Swinkels, and Patricia Vickers-Rich. "CRETACEOUS POLAR ARTHROPODS ON WALKABOUTS: NEWLY DISCOVERED ARTHROPOD TRACE FOSSILS FROM THE WONTHAGGI FORMATION (BARREMIAN), VICTORIA, AUSTRALIA." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-364259.

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4

Metz, Robert. "TRACE FOSSILS IN FLUVIAL DEPOSITS OF THE UPPERMOST STOCKTON FORMATION (LATE TRIASSIC), WEST-CENTRAL NEW JERSEY." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-342810.

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5

Metz, Robert. "TRACE FOSSILS IN FLUVIAL DEPOSITS OF THE UPPERMOST STOCKTON FORMATION (LATE TRIASSIC), WEST-CENTRAL NEW JERSEY." In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-373447.

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6

Korf, Jason J., John Westgaard, H. Douglas Hanks, and Steve Willging. "PRELIMINARY LOOK AT TRACE FOSSILS IN THE LATE CRETACEOUS COLERAINE FORMATION; HILL ANNEX STATE PARK, CALUMET, MINNESOTA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291026.

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7

Getty, Patrick. "THE RADIATION OF INSECTS INTO LAKES IN THE EARLY JURASSIC, AS RECORDED BY TRACE FOSSILS FROM THE HARTFORD AND DEERFIELD BASINS OF MASSACHUSETTS." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-342879.

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8

Chupik, Daniel T., Jennifer J. Scott, and William E. Lukens. "TERRESTRIAL TRACE FOSSILS AS A TOOL FOR THE SEQUENCE STRATIGRAPHIC INTERPRETATION OF THE PLIOCENE CHEMERON FORMATION, BARINGO, CENTRAL KENYA RIFT VALLEY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336809.

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9

Hasiotis, Stephen T. "ASSESSMENT OF CONTINENTAL TRACE FOSSILS IN THE FRASNIAN–FAMENNIAN CATSKILL FORMATION, NORTH-CENTRAL PENNSYLVANIA: INITIATION OF DEVONIAN ECOSYSTEM ENGINEERING BY SOIL BIOTAS." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311373.

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Reports on the topic "Trace fossils Australia, Central"

1

Romano, M. Lower To Middle Ordovician Trace Fossils From the Central Iberian Zone of Portugal and Spain. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132188.

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2

Fritz, W. H., and T. P. Crimes. Lithology, trace fossils and correlation of Precambrian-Cambrian boundary beds, Cassiar Mountains, north-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120142.

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