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Thematische Bibliographien / Ostracoda Australia

Auswahl der wissenschaftlichen Literatur zum Thema „Ostracoda Australia“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 28. Januar 2023

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Buchteile

Zeitschriftenartikel zum Thema "Ostracoda Australia":

1

Salas, María José, Jean Vannier und Mark Williams. „Early Ordovician ostracods from Argentina: their bearing on the origin of binodicope and palaeocope clades“. Journal of Paleontology 81, Nr. 6 (November 2007): 1384–95. http://dx.doi.org/10.1666/05-134.1.

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New species of ostracods are described from the Tremadoc of the Cordillera Oriental (Argentina). These are among the earliest well-documented records of Ostracoda sensu stricto. The ostracod assemblages are sourced from shallow marine clastics and are dominated by palaeocopes (Eopilla waisfeldaen. sp.,Nanopsis coquenan. sp.), and the binodicopeKimsella luciaen. gen. and sp.EopillaandKimsellashow affinities with species from paleocontinental Gondwana (e.g., Ibero-Armorica, Turkey, Australia, Carnic Alps), butNanopsisis previously known only from paleocontinental Baltica. This study confirms that two of the major clades of Ordovician ostracods, namely the Binodicopa and the Palaeocopa, were already geographically widespread during the late Tremadoc, suggesting a still earlier origin for these groups, possibly from within the Cambrian to Early Ordovician Bradoriida. Evidence from soft-part anatomy indicates that phosphatocopids, the other group hypothesized to be ancestral ostracods, have apomorphies that preclude them as direct ancestors. The origin of ostracods is more likely to be found within the Bradoriida, a probable polyphyletic group that resembles Early Ordovician ostracods in the external sculpture of their bivalved carapace. Evidence from carapace morphology suggests that the ancestors of true ostracods might lie within the bradoriid groups Beyrichonidae and Hipponicharionidae, a hypothesis that can only truly be tested when more evidence from fossilized soft tissues becomes available.

2

Schön, Isa, Stuart Halse und Koen Martens. „Cyprideis(Crustacea, Ostracoda) in Australia“. Journal of Micropalaeontology 36, Nr. 1 (Januar 2017): 31–37. http://dx.doi.org/10.1144/jmpaleo2016-032.

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3

Mckenzie, Kenneth G., Richard A. Reyment und Eva R. Reyment. „ocene-Oligocene ostracoda from south Australia and Victoria, Australia.“ Spanish Journal of Palaeontology 6, Nr. 2 (11.08.2022): 135. http://dx.doi.org/10.7203/sjp.25056.

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4

SYME, ANNA E., und GARY C. B. POORE. „Three new ostracod species from coastal Australian waters (Crustacea: Ostracoda: Myodocopa: Cylindroleberididae)“. Zootaxa 1305, Nr. 1 (31.08.2006): 51. http://dx.doi.org/10.11646/zootaxa.1305.1.5.

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Three new species of Cylindroleberididae are described: Parasterope gamurru from Lizard Island (Queensland), Diasterope wirraka from Bass Strait (Victoria), and Cylindroleberis marranyin from Sandy Point (Victoria). This is the first record of species of Cylindroleberis and Diasterope from Australia, and the first record of a species of Parasterope from Queensland. Juvenile instars of species of Cylindroleberis are compared in order to assign appropriate stages to those of Cylindroleberis marranyin.

5

Martens, Koen, und Giampaolo Rossetti. „On the Darwinulidae (Crustacea : Ostracoda) from Oceania“. Invertebrate Systematics 16, Nr. 2 (2002): 195. http://dx.doi.org/10.1071/it01022.

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This paper reviews the darwinulid ostracods from Australia and Oceanian islands. Eleven species in three genera have thus far been found in Australia, only the genera Microdarwinula and Alicenula are absent. Vestalenula matildae, sp. nov. is here described from Western Australia. Some taxonomic notes on other species, as well as a preliminary discussion on the distribution of the group on this continent, are also offered.

6

Karanovic, Ivana. „Three interesting Cyprididae (Ostracoda) from Western Australia“. Records of the Western Australian Museum 24, Nr. 3 (2008): 267. http://dx.doi.org/10.18195/issn.0312-3162.24(3).2008.267-287.

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7

Finston, Terrie. „Morphology and molecules conflict to confound species boundaries in salt lake ostracodes of the genus Mytilocypris (Crustacea : Ostracoda)“. Australian Journal of Zoology 48, Nr. 4 (2000): 393. http://dx.doi.org/10.1071/zo00046.

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The ostracode genus Mytilocypris comprises eight species, and has a widespread distribution in saline habitats of semi-arid Australia. Fifteen populations, representing all eight species in the genus, were analysed at 19 enzyme loci to identify markers to delineate species boundaries. Only five distinct genetic groups were found: M. mytiloides, M. ambiguosa, M. splendida, M. praenuncia, and M. henricae. Three presumptive species, M. mytiloides, M. tasmanica chapmani, and M. minuta have sympatric distributions in Western Australia. The three show similar internal morphology, lack any diagnostic features of colour, pattern or setation of the shell, but differ in the size and shape of the shell. They also show microhabitat divisions along a salinity gradient. There were no genetic markers to distinguish the three Western Australian species from one another, and they showed high genetic similarity to a population of M. mytiloides from near its type locality in South Australia. Furthermore, seven populations containing more than one species in the mytiloides complex failed to show evidence of reproductive isolation between species, when tested for genetic differentiation. In contrast, a multivariate analysis, used to quantify and evaluate patterns of variation within and among the three species in the mytiloides complex, revealed differences in size, shape and allometry among species, but also showed overlap of body shapes and sizes of individuals. Two explanations are plausible for the lack of congruence between morphological and allozyme data: the three may be closely related species with undetected genetic differentiation, or the three taxa may be conspecific, and shell size, shape and allometry may be plastic characters. The role of fluctuating environmental conditions on crustacean morphology and life history variation is discussed.

8

Eagar, Stephen H. „Freshwater Ostracoda from Tarawa, Kiribati: their implications for dispersal mechanisms“. Journal of Micropalaeontology 19, Nr. 1 (01.05.2000): 68. http://dx.doi.org/10.1144/jm.19.1.68.

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Abstract. Tarawa Atoll, Gilbert Islands (1° 30′N, 173° 00′E) is an isolated place, comparatively recently emergent – 2500 years bp and 2 – 3 m above present sea-level (Marshall & Jacobson, 1985). During the course of a study of the marine ostracods (Eagar, in press) it was noted that there are relatively few places where freshwater is visible on the surface of the atoll. This is not unusual, given the low precipitation (154 mm a−1) and the daytime temperatures of Tarawa (27–30°C). Five freshwater ponds on South Tarawa (Fig. 1) were examined and two species of Ostracoda were found: Cyprinotus cingalensis Brady, 1886 and Limnocythere notodonta Vávra, 1906. At Bairiki (locality A), a pond adjacent to the causeway linking Bairiki with Betio was sampled and yielded abundant Cyprinotus cingalensis. Other ponds were found at Ambo (Locality B) and Temaiku Bight (Localities C and D with two ponds). Only the pond (Locality B), an established babai pit (taro; Cyrtosperma chamissonis), adjacent to the roadside at Ambo yielded further specimens of the ostracod Limnocythere notodonta, although in low numbers.The question of how these species were introduced onto Tarawa Atoll is intriguing. C. cingalensis is known from Ceylon (Brady, 1886), Hawaii and the Sandwich Islands. The record by Vávra (1906) from Australia may be incorrect. Limnocythere notodonta was previously recorded only from Java (Vávra, 1906). Both species may have been distributed in the same way that Sars (e.g., Sars, 1896) transported species from different parts of the world to Norway to describe . . .

9

Kornicker, L. S. „Codonocera cuspidata, a new species of pelagic ostracode from off Queensland, Australia (Crustacea: Ostracoda: Cypridinidae)“. Records of the Australian Museum 38, Nr. 3 (01.12.1986): 119–34. http://dx.doi.org/10.3853/j.0067-1975.38.1986.178.

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10

Siveter, David J., Jean M. C. Vannier und Douglas Palmer. „Silurian Myodocopes: Pioneer pelagic ostracods and the chronology of an ecological shift“. Journal of Micropalaeontology 10, Nr. 2 (01.12.1991): 151–73. http://dx.doi.org/10.1144/jm.10.2.151.

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Abstract. Analysis of all relevant palaeontological and global geological data strongly supports the notion that representatives of Silurian myodocope ostracods had pelagic lifestyles and habitats and that they may well be, within the Ostracoda, pioneer colonisers of such environments. Morphological evidence (from fossil and Recent myodocopes) combined with facies distributional and concomitant faunal evidence (from the Silurian of, for example, Britain, France, Czechoslovakia, Sardinia, Australia and China) endorses the idea that myodocope ostracods may have undergone a benthic to pelagic ecological shift during mid Silurian times.Lower Silurian myodocopes lived, with benthic associates, on well oxygenated shelves. Upper Silurian ostracods lived, typically with low diversity, largely pelagic faunas in outer shelf topographic lows or off-shelf basin slopes, and are characteristically associated with deposits which are in part suggestive of lowered oxygen levels or even anoxic conditions. A pre-adaptation for swimming may have allowed Silurian myodocopes to respond to environmental forcing (negative oxygen levels; positive trophic and nutrient incentives; rises in sea levels) by migrating, through time, up the water column.

Mehr Quellen

Dissertationen zum Thema "Ostracoda Australia":

1

Reeves, Jessica Marie. „The use of ostracoda in the palaeoenvironmental reconstruction of the Gulf of Carpentaria, Australia, from the last interglacial to present“. Access electronically, 2004. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20050111.153534/index.html.

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2

Ferdinando, Darren. „Ostracode and foraminiferal taxonomy and palaeoecology of the Fossil Cliff Member of the Holmwood Shale, northern Perth Basin, Western Australia“. University of Western Australia. Dept. of Geology and Geophysics, 2001. http://theses.library.uwa.edu.au/adt-WU2003.0019.

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The Sakmarian (Cisuralian, Permian) Fossil Cliff Member of the Holmwood Shale is situated in the northern Perth Basin, Western Australia, and consists of alternating beds of shale and silty calcarenite forming three parasequences. Within this member a diverse fauna of ostracodes and foraminifera are present. During the Cisuralian the northern Perth Basin formed part of the Gondwanan supercontinent and was linked to Greater India via an epeiric sea that opened to the north. The ostracode fauna is restricted to the calcareous beds of the member and consists of a diverse benthic fauna comprising 31 new species and 13 previously recorded species. Species from the Healdioidea, Bairdioidea, Youngielloidea, and Thlipsuroidea dominate the assemblage and suggest a normal-marine environment during the period represented by the calcareous beds, with an overall shallowing trend up the sequence. The fauna shows some similarity to faunas from the Tethyan deposits of North America and the Boreal deposits of Russia during the Late Carboniferous and Cisuralian. Twenty-eight species of foraminifera were recorded from the Fossil Cliff Member and underlying Holmwood Shale and comprise two distinct faunas, an agglutinated benthic foraminiferal fauna found within the shale beds and a calcareous benthic foraminiferal fauna present in the calcarenite units. The agglutinated foraminifera are inferred to represent deposition in dysoxic to suboxic (0.1-1.5 mL/LO2;), poorly circulated bottom waters below wave base. The calcareous foraminifera are inferred to represent deposition in normal-marine conditions. Both foraminiferal assemblages show a shallowing trend in their distribution that matches the trend identified in the ostracode fauna. Based upon the palaeoecology of the ostracode and foraminiferal faunas, the depositional environment for the Fossil Cliff Member is inferred to have been within shallow water in an epeiric basin during an overall marine regression that is overprinted by eustatic and isostatic oscillations resulting from deglaciation that occurred during the early Sakmarian (Cisuralian). These sea-level oscillations raised and lowered the oxic surface waters of the epeiric sea above and below the substrate resulting in a sparse agglutinated foraminiferal fauna or an abundant and diverse ostracode and calcareous foraminiferal fauna respectively.

3

De, Deckker P. „Australian Quaternary studies : a compilation of papers and documents submitted for the degree of Doctor of Science in the Faculty of Science, University of Adelaide /“. Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SD/09sdd299.pdf.

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4

Davies, Miles. „Ostracod assemblages and paloeoenvironments of a purported cold water section of the Mannum Formation, Devon Downs, South Australia /“. Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bd2561.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1996.
Australian National Grid reference S1/54 Renmark sheet 1:250000. Includes bibliographical references (leaves 37-43).

5

Gouramanis, Chris. „High-resolution holocene paleoenvironmental and paleoclimatic changes recorded in Southern Australian lakes based on ostracods and their chemical composition“. Phd thesis, 2009. http://hdl.handle.net/1885/150571.

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6

De, Deckker P. (Patrick). „Australian Quaternary studies : a compilation of papers and documents submitted for the degree of Doctor of Science in the Faculty of Science, University of Adelaide“. 2002. http://web4.library.adelaide.edu.au/theses/09SD/09sdd299.pdf.

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"April 2002" Includes bibliographical references and list of the publications and papers submitted. Pt. 1: section 1. Ostracod taxonomy and ecology -- section 2. Limnology of salt lakes -- section 3. Ostracod palaoecology - Quaternary environments -- section 4. Palaolimnology - Quaternary paleoenvironments and geology -- pt. 2: section 5. Geochemistry of ostracod shells -- section 6. Palaeoceanography Contains the majority of the author's scientific publications. Aims at reconstructing Quaternary paleoenvironments, mostly from the Australian region, using the fossil remains of organisms as well as new geochemical techniques.

7

Passlow, Victoria. „Late Quaternary history of the Southern Ocean offshore Southeastern Australia, based on deep-sea Ostracoda“. Phd thesis, 1994. http://hdl.handle.net/1885/140921.

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8

Radke, Lynda C. „Solute divides and chemical facies in southeastern Australian salt lakes and the response of ostracods in time (holocene) and space“. Phd thesis, 2000. http://hdl.handle.net/1885/147146.

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Bücher zum Thema "Ostracoda Australia":

1

Kornicker, Louis S. Ostracoda (Myodocopina) from shallow waters of the Northern Territory and Queensland, Australia. Washington, D.C: Smithsonian Institution Press, 1996.

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2

International Symposium on Ostracoda. (11th 1991 Warrnambool, Victoria). Ostracoda in the earth and life sciences: Proceedings of the 11th International Symposium on Ostracoda : Warrnambook, Victoria, Australia, 8-12, July 1991. Rotterdam: A.A. Balkema, 1993.

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3

Jones, P. J. Lower Carboniferous Ostracoda (Beyrichicopida and Kirkbyocopa) from the Bonaparte Basin, northwestern Australia. Canberra: Australian Govt. Pub. Service, 1989.

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4

S, Kornicker Louis. Ostracoda (Myodocopina) of the SE Australian continental slope. Washington, D.C: Smithsonian Institution Press, 1996.

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5

S, Kornicker Louis. Ostracoda (Myodocopina) of the SE Australian continental slope. Washington, D.C: Smithsonian Institution Press, 1996.

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6

S, Kornicker Louis. Ostracoda (Myodocopina) of the SE Australian continental slope. Washington, D.C: Smithsonian Institution Press, 1994.

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7

Kornicker, Louis S. Ostracoda (Myodocopina) of the SE Australian continental slope, part 2. Washington, D.C: Smithsonian Institution Press, 1995.

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8

S, Kornicker Louis. Ostracoda (Myodocopina) of the SE Australian continental slope, part 2. Washington, D.C: Smithsonian Institution Press, 1995.

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9

Karanovic, Ivana. Candoninae (Ostracoda) from the Pilbara Region in Western Australia. BRILL, 2007.

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10

Karanovic, Ivana. Candoninae (Ostracoda) from the Pilbara Region in Western Australia (Crustaceana Monographs). BRILL, 2007.

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Buchteile zum Thema "Ostracoda Australia":

1

Neil, John V. „Factors influencing intraspecific variation and polymorphism in marine podocopid Ostracoda, with particular reference to Tertiary species from southeastern Australia“. In Evolutionary Biology and Ecology of Ostracoda, 161–80. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-1508-9_13.

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2

Reeves, Jessica M., Patrick De Deckker und Stuart A. Halse. „Groundwater Ostracods from the arid Pilbara region of northwestern Australia: distribution and water chemistry“. In Ostracodology — Linking Bio- and Geosciences, 99–118. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6418-0_9.

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3

Guzel, Michelle. „Jurassic and Early Cretaceous Ostracods from Western Australia: What They Reveal About Evolution of the Indian Ocean“. In Earth and Life, 849–82. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-90-481-3428-1_30.

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4

„Tribe Humphreyscandonini Karanovic, 2005“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 151–368. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.13.

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5

„Preliminary Material“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, i—2. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.2.

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6

„Key To The Species Of Candoninae Of The Pilbara Region“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 369–74. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.22.

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7

„Phylogenetic Analysis Of The Pilbara Candoninae“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 375–82. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.23.

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8

„Phylogenetic Analysis Of The Genera Of The Recent Candoninae“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 383–87. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.24.

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9

„Key To The Genera Of Recent Candoninae Of The World“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 388–89. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.27.

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10

„General Discussion“. In Candoninae (Ostracoda) from the Pilbara Region in Western Australia, 390–95. BRILL, 2010. http://dx.doi.org/10.1163/ej.9789004156937.i-434.28.

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