Relevant bibliographies by topics / Ostracoda, Fossil

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Academic literature on the topic 'Ostracoda, Fossil'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 March 2023

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Journal articles on the topic "Ostracoda, Fossil"

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Smith, Robin James. "Possible fossil ostracod (Crustacea) eggs from the Cretaceous of Brazil." Journal of Micropalaeontology 18, no. 1 (June 1, 1999): 81–87. http://dx.doi.org/10.1144/jm.18.1.81.

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Abstract. Spherical objects recovered from the acetic acid preparation residues of vertebrate fossils from the Santana Formation (Lower Cretaceous) of northeast Brazil are postulated as the eggs of the ostracod Pattersoncypris micropapillosa Bate, 1972 (Ostracoda). These spheres are phosphatized and range from 85 to 110 μm in diameter, and are comparable in many respects to the eggs of several Recent ostracod species.
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Szwarc, Agata, and Tadeusz Namiotko. "Biodiversity of Non-Marine Ostracoda (Crustacea) of Botswana: An Annotated Checklist with Notes on Distribution." Water 14, no. 9 (April 30, 2022): 1441. http://dx.doi.org/10.3390/w14091441.

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Botswana constitutes a major gap in our knowledge of the distribution of Ostracoda in the region of Southern Africa, restraining thorough biogeographic interpretations. We combine records from previously published surveys along with our own field collections to provide a collation of living and fossil (Late Pleistocene to Holocene) Ostracoda recorded in Botswana. Our survey yielded 17 species, of which nine species have not been recorded before in the country. Including the present update, 54 species (45 living and nine fossil or subfossil) belonging to 22 genera of five families (with 76% species belonging to the family Cyprididae) are currently reported from Botswana. Yet, 23 taxa are left in open nomenclature, indicating the urgent need for sound systematic studies on harmonizing taxonomy of Southern African ostracods, especially of those inhabiting small temporary waterbodies, considered as threatened with extinction before being properly described or discovered. This updated checklist provides detailed information about the distribution and habitat of each recorded species. Species richness, distribution patterns, and diversity of ostracod species regionally and in different freshwater ecoregions are also discussed. We found low alpha (site) diversity (mean 3.3 species per site) and a significant difference in species composition and beta diversity of the Okavango ecoregion versus the Kalahari and Zambezian Lowveld ecoregions.
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Lawrence, James R., Kiseong Hyeong, Rosalie F. Maddocks, and Kwang-Sik Lee. "Passage of Tropical Storm Allison (2001) over southeast Texas recorded in δ18O values of Ostracoda." Quaternary Research 70, no. 2 (September 2008): 339–42. http://dx.doi.org/10.1016/j.yqres.2008.04.004.

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AbstractFreshwater Ostracoda collected in ephemeral pond-waters derived from Tropical Storm Allison (2001, Texas) recorded the unusually low oxygen-isotope values of that storm. Therefore, the potential clearly exists, in locations where tropical cyclones make landfall, to obtain a long-term record of tropical cyclone activity from fossil ostracode calcite.
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Antonietto, Lucas S., Lisa E. Park Boush, Celina A. Suarez, Andrew R. C. Milner, and James I. Kirkland. "The ‘Last Hurrah of the Reigning Darwinulocopines’? Ostracoda (Arthropoda, Crustacea) from the Lower Jurassic Moenave Formation, Arizona and Utah, USA." Journal of Paleontology 92, no. 4 (April 26, 2018): 648–60. http://dx.doi.org/10.1017/jpa.2017.150.

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AbstractAn ostracode fauna is described from lacustrine sediments of the Hettangian, Lower Jurassic, Whitmore Point Member of the Moenave Formation. The Moenave is well known for its rich, Late Triassic?–Early Jurassic fossil record, which includes fossil fishes, stromatolites, ostracodes, spinicaudatans, and a diverse ichnofauna of invertebrates and vertebrates. Four ostracode species, all belonging to the suborder Darwinulocopina, were recovered from these sediments:Suchonellina globosa,S. stricta,Whipplella? sp. 1, andW.? sp. 2. The diversity and composition of the Whitmore Point Member ostracode fauna agree with previous interpretations about Lake Dixie and nearby paleoenvironments as shallow lakes inhabited by darwinulocopine species that survived the effects of the Central Atlantic Magmatic Province and the subsequent end-Triassic extinction and quickly recolonized these areas, thanks to asexual reproduction by parthenogenesis. The Lake Dixie region, in its geographical isolation, could represent the last episode of darwinulocopine dominance in nonmarine environments before the Late Jurassic diversification of the cypridocopine/cytherocopine modern ostracodes.
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Barbieri, Giulia, and Stefano Claudio Vaiani. "Benthic foraminifera or Ostracoda? Comparing the accuracy of palaeoenvironmental indicators from a Pleistocene lagoon of the Romagna coastal plain (Italy)." Journal of Micropalaeontology 37, no. 1 (January 29, 2018): 203–30. http://dx.doi.org/10.5194/jm-37-203-2018.

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Abstract. Integrated analyses of multiple groups of microfossils are frequently performed to unravel the palaeoenvironmental evolution of subsurface coastal successions, where the complex interaction among several palaeoecological factors can be detected with benthic assemblages. This work investigates the palaeoenvironmental resolution potential provided by benthic foraminifera and ostracoda within a Pleistocene lagoonal succession of the Romagna coastal plain (northern Italy). Quantitative approaches and statistical techniques have been applied to both groups in order to understand the main factors that controlled the composition of assemblages and compare the palaeoecological record provided by single fossil groups. The two faunal groups are characterized by the high dominance of opportunistic species (Ammonia tepida–Ammonia parkinsoniana and Cyprideis torosa); however, detailed palaeoecological information is inferred from less common taxa. Benthic foraminiferal assemblages are mainly determined by the frequencies of abnormal individuals and species related to high concentrations of organic matter, showing two assemblages: a stressed assemblage, consistent with a brackish-water environment subject to salinity and oxygen fluctuations, and an unstressed assemblage, which indicates more stable conditions. Despite the lower number of species, ostracoda show more significant differences in terms of species composition and ecological structure between their three assemblages, formed in response to a salinity gradient and indicative of inner, central, and outer lagoon conditions. The stratigraphic distribution of ostracod assemblages shows a general transgressive–regressive trend with minor fluctuations, whereas benthic foraminifera highlight the presence of a significant palaeoenvironmental stress. In this case, the higher abundance along the stratigraphic succession, the higher differentiation of the assemblages, and the well-defined relationship between taxa and ecological parameters determine Ostracoda as the most reliable fossil group for precise palaeoenvironmental reconstructions. Nevertheless, benthic foraminifera indicate palaeoenvironmental stress and can be used to refine the environmental interpretation in the presence of monospecific ostracod assemblages.
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Whittaker, J. E. "Fossil Nonmarine Ostracoda of the United States." Marine and Petroleum Geology 17, no. 4 (April 2000): 560. http://dx.doi.org/10.1016/s0264-8172(99)00065-3.

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Park, Lisa E., and R. Douglas Ricketts. "Evolutionary History of the Ostracoda and the Origin of Nonmarine Faunas." Paleontological Society Papers 9 (November 2003): 11–36. http://dx.doi.org/10.1017/s1089332600002138.

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The Ostracoda are one of the most diverse arthropod groups alive today; they also have a tremendous fossil record. Because of their widespread environmental distributions, small size and carbonate shell, they have become extremely useful biostratigraphic and paleoenvironmental proxy indicators, particularly in nonmarine environments. Despite this utility, little is known about the phylogenetic history of this important group. We reconstructed a phylogenetic history of the major orders and suborders of Ostracoda in order to test the legitimacy of current classification schemes, determine if it is possible for ostracodes to have a Precambrian origin, and test the fidelity of some of the major morphological characters that have documented trends of either increased complexity, such as the hinge and marginal pore canals, or reduction in segments, such as the adductor muscle scar.In our phylogenetic analysis to test taxonomic fidelity, we coded seven morphological hard part characters for nine taxa from the orders Archaeocopida, Leperditicopida, Palaeocopida, Podocopida, and Myodocopida. A parsimony analysis was performed using PAUP (v. 4.0) yielding 4 trees of 17 steps with low levels of homoplasy and a strong phylogenetic signal. A majority rule consensus tree indicates there is not complete agreement between the standard classification scheme and the phylogeny produced by the characters used to establish the classification. In our complete analysis of Ostracoda, we coded 28 morphological characters that included 14 hard part and 14 soft part characters for twelve taxa that include the Archaeocopida, Leperditicopida, Podocopida, and Myodocopida. A parsimony analysis was completed using PAUP (v. 4.0) yielding 1 tree of 125 steps with low levels of homoplasy and a strong phylogenetic signal. An unrooted analysis of this character set has the Cambrian Archaeopodocopida and the Ordovician-Devonian Leperditicopida in an unresolved polytomy with much younger groups such as the Myodocopina, suggesting a much deeper split in the lineage and a possible Precambrian origin for the Ostracoda. Testing the various character state acquisitions over the tree indicates that the hinge does not show an increase in complexity within a phylogenetic context, while the adductor muscle scars do show a significant trend of decrease in complexity across the tree topology. The marginal pore canals, which are functionally tied to osmoregulation as well as carapace secretion, are extremely homoplastic, indicating that this character, which is related to nonmarine invasions and tolerances, was acquired many times throughout the evolutionary history of Ostracoda.By creating an evolutionary framework for the Ostracoda such as is presented here, we can further assess character state acquisition, and how it functionally and evolutionarily relates to ostracode paleoenvironmental tolerances. The framework will not only allow us to understand the overall evolution ofthis group but will also allow us to compare the history of the ostracode clade with other groups that also have a history ofmarine and nonmarine transitions.
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Dykan, Natalia. "Some theoretical aspects of the systematic study of fossil ostracods (Arthropoda, Crustacea, Ostracoda) in the context of species problems in palaeontology." Novitates Theriologicae, no. 12 (June 16, 2021): 127–39. http://dx.doi.org/10.53452/nt1223.

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Theoretical contributions into the systematics and taxonomy of fossil ostracods conducted according to unified methodological stands have resolved some key problems of paleontology. For example, this is a problem of species and its derivatives, namely the identification of species, the estimation of the taxonomic weight of morphological characters, the determination of diagnostic characters of different taxonomic ranks, and taxa diagnoses. The unification of the terminology and the formalization of morphological description of fossil shells made it possible to estimate the taxonomic weight of morphological elements. A scheme to identify the rank of taxonomic characters (pyramid principle) has been developed. A unified terminological dictionary has been prepared to describe the morphological elements of ostracod shells in detail.
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Lord, Alan. "Towards objectivity in Ostracoda species definition." BSGF - Earth Sciences Bulletin 191 (2020): 27. http://dx.doi.org/10.1051/bsgf/2020029.

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The problem of consistent identification of unornamented fossil ostracod taxa, especially species, is reviewed in an historical context. The solution lies in modern imaging and image storage and handling technologies combined with a careful but pragmatic (heuristic) approach to identification and taxonomy.
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MAZZINI, ILARIA, FEDERICO MARRONE, MARCO ARCULEO, and GIAMPAOLO ROSSETTI. "Revision of Recent and fossil Mixtacandona Klie 1938 (Ostracoda, Candonidae) from Italy, with description of a new species." Zootaxa 4221, no. 3 (January 17, 2017): 323. http://dx.doi.org/10.11646/zootaxa.4221.3.3.

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Although studies on ostracods dwelling in inland subterranean habitats of Italy have increased in the last decades, highlighting a considerable taxonomic diversity, available information is still far from sufficient to understand phylogenetic and biogeographic relationships. Mixtacandona Klie 1938 is one of the most common and diverse genera of ostracods in subterranean waters. Of the 20 living recognized species in the genus, all stygobiontic and restricted to the Palearctic Region, four are known for the Italian peninsula and Sardinia, one of which exclusively as fossil. Several other Recent and fossil taxa attributable to Mixtacandona, but identified at supraspecific level, have been reported from various Italian regions. Here we report Mixtacandona idrisi n. sp., collected in a cave near Palermo, the first cavernicolous ostracod from the island of Sicily; in addition, the description of material recently collected in northern Italy, consisting of M. laisi and of a putative new species that has been tentatively allocated to the same genus, is given. Mixtacandona (Trapezicandona) italica Karanovic & Pesce, 2000 is tentatively treated as a junior synonym of M. talianae Gliozzi & Mazzini, 1998. The validity of species-groups within Mixtacandona is discussed. Relying on the results of this study, the authors argue for the need of a comprehensive revision of the genus.
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Dissertations / Theses on the topic "Ostracoda, Fossil"

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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.
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Syme, Anna. "A systematic revision of the cylindroleberididae (Crustacea Ostracoda Mydodocopa) /." Connect to thesis, 2007. http://eprints.unimelb.edu.au/archive/00002921.

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Conway-Physick, Jessica Ann. "The holocene ostracods of the Agulhas Bank, South Africa : their classification, distribution and ecology." Master's thesis, University of Cape Town, 1995. http://hdl.handle.net/11427/17467.

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Bibliography: pages 69-77.
An analysis of the Holocene ostracod fauna of the Agulhas Bank has been carried out on seventy-three surficial sediment samples. Sixty-six species of Ostracoda have been recorded, of which fifty-nine species are accounted for in forty genera and the remaining seven species are of indeterminate classification. The species are described and their distribution and ecology is given. An. analysis of the sedimentology, as well as an oceanographic analysis of the bottom water on the Agulhas Bank, has provided environmental parameters for each sediment sample location, enabling relationships to be described between ostracod faunas and environmental conditions. Quantitative factor analysis has been carried out on the twenty-four most abundant species, generating seven factor associations relating ostracod assemblages to a set of environmental parameters. The independent variables analyzed were the temperature, salinity and dissolved-oxygen content of the bottom water, as well as the sand content of the sediment. Contour maps of these variables have been drawn up using SADCO data for the oceanographic variables, and the sediment samples to calculate the sand content. The overall oceanography of the Agulhas Bank has been analyzed by relating the environmental parameters generated at each location to the water masses present on the shelf, and to the oceanic currents affecting them. Finally, the seven factor associations generated have been related directly to the substrate types, the water masses, and the currents present on the Agulhas Bank.
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White, Tom Samuel. "Late middle Pleistocene molluscan and ostracod successions and their relevance to the British Paleolithic record." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648393.

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Abke, Rodney Alan. "A fossil assemblage of ostracoda, foraminifera, and gastropoda of the West Texas salt flats." Virtual Press, 1994. http://liblink.bsu.edu/uhtbin/catkey/897497.

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The salt flats of west Texas are large ephemeral lakes, Pleistocene to Holocene in age. The evaporite material in these lakes represents the sedimentary history of the lake and the surrounding area. Recently, a fossil assemblage was found in the sediments of this deposit. This assemblage includes four species of ostracoda (Limnocvthere staplini, Candona rawsoni, Candona thomasi, and Cvprideis salbrosa), two species of gastropoda, (Amnicola decepta, and Amnicola pilsbrvi), and discovery is significant because this assemblage has not been previously reported, and it provides an opportunity to reconstruct part of the physical and chemical environment of the salt flats during a portion of its history. Autecological comparison of these species indicate that they lived in a shallow, alkaline, brackish water environment. The known paleoclimate of the area, and the sedimentology support this interpretation.
Department of Geology
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Frewin, J. "Palaeogene ostracods from the South African continental shelf." Master's thesis, University of Cape Town, 1987. http://hdl.handle.net/11427/17003.

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Bibliography: pages 147-155.
92 cytheracean species, representing 44 genera are recorded from the Palaeogene Agulhas Bank and west coast margin of South Africa. 11 genera and 3 species are common with the Upper Cretaceous faunas. 12 genera (18 species) are left in open nomenclature. The following genera are represented:- Bythoceratina, Incongruellina, Ruggieria, Eucythere, Krithe, Parakrithe, Eucytherura, Cytheropteron, Ambostracon, Urocythereis, Muellerina, Leguminocythereis, Loxoconcha, Schlerochilus, Poseidonamicus, Bradleya, Agrenocythere, Australileberis, Chrysocythere, Costa, Echinocythereis, Haughtonileberis, Henryhowella, Parvacythereis, Phacorhabdotus, Soudanella, Stigmatocythere, Togoina, Trachyleberis, Veenia, Atlanticythere, Xestoleberis. Data on South African Cretaceous and Palaeogene ostracod faunas are discussed in terms of: faunal associations for the South African Palaeogene JC-1, Agulhas Bank and west coast provinces; characteristic species of Upper Eocene and Upper Eocene to Oligocene strata; generic variations across the Cretaceous/Tertiary boundary. Palaeo-environmental trends from a Cytheracea, Cypridacea + Bairdiacea, Cytherellidae (CCBC) plot indicate a sea level change from <100m (Palaeocene- Eocene), to shallower water with restricted circulation (Upper Eocene) to moderate depth, 100 - 200m (Lower Oligocene). South African faunas are compared with those from adjacent Palaeogene ostracod faunal provinces. Strong generic links occur with West Africa (8 genera in common) and Pakistan (9 genera in common) with only 3 genera in common with Australia and 3 with Argentina.
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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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McFarland, Andrew J. "Using Ostracode Dynamics to Track Ecosystem Response to Climatically and Tectonically Induced Lake-Level Fluctuations in Fossil Basin, Green River Basin, Wyoming, USA." University of Akron / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=akron1348242706.

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Sipahioglu, Sara M. "Tracking storms through time event deposition and biologic response in Storr's Lake, San Salvador Island, Bahamas /." Akron, OH : University of Akron, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=akron1227031927.

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Thesis (M.S.)--University of Akron, Dept. of Geology, 2008.
"December, 2008." Title from electronic thesis title page (viewed 12/13/2009) Advisor, Lisa E. Park; Faculty Readers, Ira D. Sasowsky, John Peck; Department Chair, John P. Szabo; Dean of the College, Ronald F. Levant; Dean of the Graduate School, George R. Newkome. Includes bibliographical references.
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Tölderer-Farmer, Martine. "Causalité des variations morphologiques de la carapace chez les Ostracodes : essai d'interprétation sur des populations actuelles et fossiles." Bordeaux 1, 1985. http://www.theses.fr/1985BOR10539.

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Les variations architecturales de quatre types d'ornementation des carapaces sont etudiees, chez plusieurs especes actuelles d'ostracodes, dans des environnements et paleoenvironnements marins et lacustres. Une approche qualitative et quantitative est adoptee, avec la distinction des differents variants morphologiques dans les populations et l'analyse de la composition chimique de leurs valves a la microsonde electronique. Les variations morphologiques et chimiques sont mises en parallele avec les modifications des parametres du milieu. La relation ornementation des valves composition chimique des eaux n'est pas directe mais passe par l'intermediaire des equilibres chimiques et des associations chimiques. Le role de la matiere organique apparait primordial. Son controle vis-a-vis de la reticulation et de la costulation des carapaces passe par celui de l'equilibre de saturation des carbonates dissous dans l'eau. La spinosite des carapaces est interpretee comme une structure de protection des pores et des soies sensorielles envers les depots, sedimentaires et organiques, fins et le developpement des voiles bacteriens. La nodation des carapaces apparait comme une reaction physiologique de l'animal envers des composes terrigenes matiere humique silice. Les modifications intraspecifiques de l'ornementation des carapaces d'ostracodes sont en etroite relation avec l'environnement. Les parametres determinants et leur mode d'influence sur les populations sont particuliers a chaque type architectural. L'utilisation de ces modifications en paleoecologie renseigne sur les conditions physicochimiques a l'interface eau-sediment, et au-dela sur l'origine et la quantite des apports nutritifs, les circulations oceaniques, la nature des bassins versants et le type de climat en milieu continental
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Books on the topic "Ostracoda, Fossil"

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Fossil nonmarine ostracoda of the United States. Amsterdam: Elsevier, 1999.

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Geological Survey (U.S.) and New Jersey Geological Survey, eds. Distribution of selected Campanian and Maastrichtian ostracoda in stratigraphic test holes of the New Jersey Coastal Plain. [Reston, VA]: U.S. Geological Survey, 1992.

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Maddocks, Rosalie F. Living and fossil Macrocyprididae (Ostracoda). Lawrence, Kan: University of Kansas Paleontological Institute, 1990.

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International, Symposium on Ostracoda (12th 1994 Prague Czech Republic). Ostracoda and biostratigraphy: Proceedings of the twelfth International Symposium on Ostracoda, Prague, Czech Republic, 26-30 July 1994. Rotterdam: A.A. Balkema, 1995.

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European Ostracodologists' Meeting (3rd 1996 Paris, France). What about ostracoda!: 3e Congrès européen des ostracodologistes, 3rd European Ostracodologists Meeting : Paris-Bierville, France, 8-12 juillet 1996 : recuil des communications. Pau, France: Elf ep-Editions, 1998.

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Griffiths, Huw I. Non-marine ostracods & Quaternary palaeoenvironments. London: Quaternary Research Association, 2000.

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Majoran, Stefan. Mid-Cretaceous Ostracoda of northeastern Algeria. Oslo: Universitetsforlaget, 1989.

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Majoran, Stefan. Mid-Cretaceous Ostracoda of northeastern Algeria. Oslo: Universitetsforlaget, 1989.

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International Symposium on Ostracoda (9th 1985 Shizuoka-shi, Japan). Evolutionary biology of Ostracoda: Its fundamentals and applications : proceedings of the Ninth International Symposium on Ostracoda, held in Shizuoka, Japan, 29 July-2 August 1985. Tokyo: Kodansha, 1988.

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Bassiouni, M. A. A. Middle Eocene Ostracoda from northern Somalia. Frankfurt a.M: Senckenbergische Naturforschende Gesellschaft, 1996.

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Book chapters on the topic "Ostracoda, Fossil"

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Reyment, Richard A., and Ashraf M. T. Elewa. "Predation by Drills on Ostracoda." In Predator—Prey Interactions in the Fossil Record, 93–111. Boston, MA: Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0161-9_5.

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Frogley, M. R., H. I. Griffiths, and K. Martens. "Modern and fossil ostracods from ancient lakes." In The Ostracoda: Applications in Quaternary Research, 167–84. Washington, D. C.: American Geophysical Union, 2002. http://dx.doi.org/10.1029/131gm09.

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Huw, I., and Michael R. Frogley. "Fossil Ostracods, Faunistics and the Evolution of Regional Biodiversity." In Balkan Biodiversity, 261–72. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-1-4020-2854-0_15.

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Damotte, Par Renée. "Ostracodes du Crétacé moyen et supérieur Téthysien Etat des connaissances — paléogéographie." In New Aspects on Tethyan Cretaceous Fossil Assemblages, 171–84. Vienna: Springer Vienna, 1992. http://dx.doi.org/10.1007/978-3-7091-5644-5_10.

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Belis, Claudio A. "Palaeoenvironmental Reconstruction of Lago di Albano (Central Italy) During the Late Pleistocene Using Fossil Ostracod Assemblages." In The Interactions Between Sediments and Water, 593–600. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5552-6_60.

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De Deckker, P., and M. A. J. Williams. "Lacustrine Paleoenvironments of the Area of Bir Tarfawi-Bir Sahara East Reconstructed from Fossil Ostracods and the Chemistry of their Shells." In Egypt During the Last Interglacial, 115–19. Boston, MA: Springer US, 1993. http://dx.doi.org/10.1007/978-1-4615-2908-8_6.

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Park Boush, Lisa E., Christine M. S. Hall, Lucas S. Antonietto, and Andrew J. McFarland. "Ecological Response of Ostracodes (Arthropoda, Crustacea) to Lake-Level Fluctuations in the Eocene Green River Formation, Fossil Basin, Wyoming, USA." In Limnogeology: Progress, Challenges and Opportunities, 207–31. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-66576-0_7.

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"Fossil and Recent meet Kempf Database." In The Recent and Fossil meet Kempf Database Ostracoda, 1–4. BRILL, 2015. http://dx.doi.org/10.1163/9789004287600_002.

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"New methods for collecting Ostracoda (Crustacea) in stony sediments with methodological remarks on the separation of ostracods from sediment." In The Recent and Fossil meet Kempf Database Ostracoda, 240–51. BRILL, 2015. http://dx.doi.org/10.1163/9789004287600_013.

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"The ostracod springtail — camera recordings of a previously undescribed high-speed escape jump in the genus Tanycypris (Ostracoda, Cypridoidea)." In The Recent and Fossil meet Kempf Database Ostracoda, 176–98. BRILL, 2015. http://dx.doi.org/10.1163/9789004287600_010.

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Conference papers on the topic "Ostracoda, Fossil"

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Desai, Dipa, Paris M. Morgan, and Jorge W. Moreno-Bernal. "OSTRACODA FROM A NEW FOSSIL LOCALITY IN THE PANAMA CANAL ZONE: A PRELIMINARY REPORT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285600.

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Hunt, Gene, Maria João Fernandes Martins, T. Markham Puckett, Jack O. Shaw, Rowan Lockwood, and John P. Swaddle. "SEXUAL DIMORPHISM IS GENERALLY STABLE OVER THE LIFETIME OF FOSSIL OSTRACODE SPECIES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306412.

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Park Boush, Lisa, Christine Hall, Lucas S. Antonietto, and Andrew Mcfarland. "OSTRACODE (ARTHROPODA, CRUSTACEA) DISTRIBUTION IN RESPONSE TO LAKE LEVEL FLUCTUATIONS IN THE EOCENE GREEN RIVER FORMATION, FOSSIL BASIN, WYOMING, USA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356843.

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Reports on the topic "Ostracoda, Fossil"

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Chriscoe, Mackenzie, Rowan Lockwood, Justin Tweet, and Vincent Santucci. Colonial National Historical Park: Paleontological resource inventory (public version). National Park Service, February 2022. http://dx.doi.org/10.36967/nrr-2291851.

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Abstract:
Colonial National Historical Park (COLO) in eastern Virginia was established for its historical significance, but significant paleontological resources are also found within its boundaries. The bluffs around Yorktown are composed of sedimentary rocks and deposits of the Yorktown Formation, a marine unit deposited approximately 4.9 to 2.8 million years ago. When the Yorktown Formation was being deposited, the shallow seas were populated by many species of invertebrates, vertebrates, and micro-organisms which have left body fossils and trace fossils behind. Corals, bryozoans, bivalves, gastropods, scaphopods, worms, crabs, ostracodes, echinoids, sharks, bony fishes, whales, and others were abundant. People have long known about the fossils of the Yorktown area. Beginning in the British colonial era, fossiliferous deposits were used to make lime and construct roads, while more consolidated intervals furnished building stone. Large shells were used as plates and dippers. Collection of specimens for study began in the late 17th century, before they were even recognized as fossils. The oldest image of a fossil from North America is of a typical Yorktown Formation shell now known as Chesapecten jeffersonius, probably collected from the Yorktown area and very likely from within what is now COLO. Fossil shells were observed by participants of the 1781 siege of Yorktown, and the landmark known as “Cornwallis Cave” is carved into rock made of shell fragments. Scientific description of Yorktown Formation fossils began in the early 19th century. At least 25 fossil species have been named from specimens known to have been discovered within COLO boundaries, and at least another 96 have been named from specimens potentially discovered within COLO, but with insufficient locality information to be certain. At least a dozen external repositories and probably many more have fossils collected from lands now within COLO, but again limited locality information makes it difficult to be sure. This paleontological resource inventory is the first of its kind for Colonial National Historical Park (COLO). Although COLO fossils have been studied as part of the Northeast Coastal Barrier Network (NCBN; Tweet et al. 2014) and, to a lesser extent, as part of a thematic inventory of caves (Santucci et al. 2001), the park had not received a comprehensive paleontological inventory before this report. This inventory allows for a deeper understanding of the park’s paleontological resources and compiles information from historical papers as well as recently completed field work. In summer 2020, researchers went into the field and collected eight bulk samples from three different localities within COLO. These samples will be added to COLO’s museum collections, making their overall collection more robust. In the future, these samples may be used for educational purposes, both for the general public and for employees of the park.
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