Bibliografías temáticas / Fossil Geographical distribution

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Literatura académica sobre el tema "Fossil Geographical distribution"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 19 de febrero de 2022

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Artículos de revistas sobre el tema "Fossil Geographical distribution"

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PINTO, IRAJÁ DAMIANI. "The Fossil Blattoid Genus Amozonina. Taxonomy and Geographical Distribution." Pesquisas em Geociências 18, no. 1 (June 30, 1991): 88. http://dx.doi.org/10.22456/1807-9806.21370.

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É descrito um novo blatóide fóssil (Insecta) Amazonina purperae Pinto, sp. nov., do Estado de Minas Gerais, encontrado em argilito arrocheado associado a uma tafoflora atribuída ao Pleistoceno. O material é proveniente do km 30,25 da Rodovia BR-262, Belo Horizonte – Uberaba. A amostra contém um único élitro. Trata-se do primeiro blatídeo fóssil de Amazonina, Hebard, 1929, gênero de ampla distribuição na América do Sul e América Central. O élitro apresenta extraordinária semelhança com os élitros de Amazonina rehni Albuquerque, 1964, dos quais se diferencia pelo número de ramos e pela bifurcaçã
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Wani, Ryoji. "Geological duration of ammonoids controlled their geographical range of fossil distribution." PeerJ 5 (November 28, 2017): e4108. http://dx.doi.org/10.7717/peerj.4108.

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The latitudinal distributions in Devonian–Cretaceous ammonoids were analyzed at the genus level, and were compared with the hatchling sizes (i.e., ammonitella diameters) and the geological durations. The results show that (1) length of temporal ranges of ammonoids effected broader ranges of fossil distribution and paleobiogeography of ammonoids, and (2) the hatchling size was not related to the geographical range of fossil distribution of ammonoids. Reducing the influence of geological duration in this analysis implies that hatchling size was one of the controlling factors that determined the
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Brizuela, Santiago, and Adriana María Albino. "Tupinambine teiids from the middle Miocene of north-western Patagonia (Argentina)." Amphibia-Reptilia 29, no. 3 (2008): 425–31. http://dx.doi.org/10.1163/156853808785112110.

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Abstract Remains of teiids assignable to the Tupinambinae (Tupinambis sp. or Crocodilurus sp.) are here described from the middle Miocene Collón Curá Formation at Cañadón del Tordillo, in Neuquén province, Argentina. No tupinambine species presently inhabits the region of the fossil locality. The fossils represent the westernmost distribution of fossil tupinambine teiids in Patagonia, enlarging the known geographical distribution of the teiids through the Miocene in a longitudinal range. Also, they constitute the first record of lizards from the Colloncuran SALMA, partially filling the record
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Tell, Guillermo. "Recent and fossil species of the genus Pediastrum Meyen (Chlorococcales) from Argentina and their geographical distribution." Algological Studies/Archiv für Hydrobiologie, Supplement Volumes 112 (May 1, 2004): 49–71. http://dx.doi.org/10.1127/1864-1318/2004/0112-0049.

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Pan, Y. R., and N. G. Jablonski. "The age and geographical distribution of fossil cercopithecids in China." Human Evolution 2, no. 1 (February 1987): 59–69. http://dx.doi.org/10.1007/bf02436531.

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Terrill, David F., Charles M. Henderson, and Jason S. Anderson. "New application of strontium isotopes reveals evidence of limited migratory behaviour in Late Cretaceous hadrosaurs." Biology Letters 16, no. 3 (March 2020): 20190930. http://dx.doi.org/10.1098/rsbl.2019.0930.

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Dinosaur migration patterns are very difficult to determine, often relying solely on the geographical distribution of fossils. Unfortunately, it is generally not possible to determine if a fossil taxon's geographical distribution is the result of migration or simply a wide distribution. Whereas some attempts have been made to use isotopic systems to determine migratory patterns in dinosaurs, these methods have yet to achieve wider usage in the study of dinosaur ecology. Here, we have used strontium isotope ratios from fossil enamel to reconstruct the movements of an individual hadrosaur from D
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Hayashi, Ryota. "A checklist of turtle and whale barnacles (Cirripedia: Thoracica: Coronuloidea)." Journal of the Marine Biological Association of the United Kingdom 93, no. 1 (August 10, 2012): 143–82. http://dx.doi.org/10.1017/s0025315412000847.

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A checklist of published records of coronuloid barnacles (Cirripedia: Thoracica: Coronuloidea) attached to marine vertebrates is presented, with 44 species (including 15 fossil species) belonging to 14 genera (including 3 fossil genera) and 3 families recorded. Also included is information on their geographical distribution and the hosts with which they occur.
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TAN, JING J., DONG REN, and CHUNG K. SHIH. "First record of fossil Priacma (Coleoptera: Archostemata: Cupedidae) from the Jehol Biota of western Liaoning, China." Zootaxa 1326, no. 1 (October 2, 2006): 55. http://dx.doi.org/10.11646/zootaxa.1326.1.6.

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Four new fossil species of the genus Priacma, P. latidentata sp. nov., P. tuberculosa sp. nov., P. clavata sp. nov. and P. renaria sp. nov., are described from the Yixian Formation of western Liaoning, China. This finding documents the first record of fossil Priacma in China and extends the geographical distribution of this genus.
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Santos, Rodolfo Otávio, Michel Laurin, and Hussam Zaher. "A review of the fossil record of caecilians (Lissamphibia: Gymnophionomorpha) with comments on its use to calibrate molecular timetrees." Biological Journal of the Linnean Society 131, no. 4 (November 3, 2020): 737–55. http://dx.doi.org/10.1093/biolinnean/blaa148.

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Abstract Gymnophiona, popularly known as caecilians, the most poorly known major taxon of extant amphibians, are elongate and limbless tetrapods, with compact ossified skulls and reduced eyes, mainly adapted to fossorial life as adults. Caecilians are poorly represented in the fossil record, but despite the scarcity of fossil specimens described (only four named taxa, in addition to indeterminate fragmentary material), their fossils play a key role in our knowledge of the origin and evolution of Lissamphibia, as well as contribute directly to a better understanding of the phylogeny, taxonomy a
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Murienne, Jerome, Savel R. Daniels, Thomas R. Buckley, Georg Mayer, and Gonzalo Giribet. "A living fossil tale of Pangaean biogeography." Proceedings of the Royal Society B: Biological Sciences 281, no. 1775 (January 22, 2014): 20132648. http://dx.doi.org/10.1098/rspb.2013.2648.

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The current distributions of widespread groups of terrestrial animals and plants are supposedly the result of a mixture of either vicariance owing to continental split or more recent trans-oceanic dispersal. For organisms exhibiting a vicariant biogeographic pattern—achieving their current distribution by riding on the plates of former supercontinents—this view is largely inspired by the belief that Pangaea lacked geographical or ecological barriers, or that extinctions and dispersal would have erased any biogeographic signal since the early Mesozoic. We here present a time-calibrated molecula
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Tesis sobre el tema "Fossil Geographical distribution"

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Welling, Leigh A. "Environmental control of radiolarian abundance in the Central Equatorial Pacific and implications for paleoceanographic reconstructions." Thesis, 1996. http://hdl.handle.net/1957/28239.

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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 wel
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Chen, Jianye. "Evolution and biogeography of frogs and salamanders, inferred from fossils, morphology and molecules." Thesis, 2016. https://doi.org/10.7916/D8GX4BSN.

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Classified in the Lissamphibia, modern amphibians are the only non-amniote tetrapods living today. They consist of three morphologically distinct groups: the tailless frogs and toads (Anura), the limbless caecilians (Gymnophiona), and the tailed salamanders and newts (Urodela). With 205 species, the caecilians are highly specialized worm-like forms that live a fossorial lifestyle, with a relatively narrow distribution in the tropic rainforests of South America, Africa and Asia (Duellman and Trueb, 1994; Amphibiaweb, 2015). Salamanders, with 683 species, are widely distributed in the North Amer
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Hamm, Shawn A. "Systematic, stratigraphic, geographic and paleoecological distribution of the late cretaceous shark genus ptychodus within the Western Interior Seaway /." 2008. http://proquest.umi.com/pqdweb?did=1654491301&sid=3&Fmt=2&clientId=10361&RQT=309&VName=PQD.

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Libros sobre el tema "Fossil Geographical distribution"

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Purdue, James R. Dynamics of mammalian distribution in the Holocene of Illinois. Edited by Styles Bonnie Whatley 1950-. Springfield, Ill: Illinois State Museum, 1986.

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Smith, Gerald Ray. Fishes of the Mio-Pliocene Ringold Formation, Washington: Pliocene capture of the Snake River by the Columbia River. Ann Arbor, Mich: Museum of Paleontology, the University of Michigan, 2000.

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Smith, Gerald Ray. Fishes of the Mio-Pliocene Ringold Formation, Washington: Pliocene capture of the Snake River by the Columbia River. Ann Arbor, Mich: Museum of Paleontology, University of Michigan, 2000.

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Puckett, T. Markham. Systematics and paleobiogeography of brachycytherine Ostracoda. New York: Micropaleontology Press, American Museum of Natural History, 2002.

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Petuch, Edward J. Neogene history of tropical American mollusks: Biogeography & evolutionary patterns of tropical Western Atlantic Mollusca. Charlottesville, Va: Coastal Education & Research Foundation, 1988.

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Haller-Probst, Melitta S. Die Verbreitung der Reptilia in den Klimazonen der Erde: Unter Berücksichtigung Känozoischer Vorkommen Europas. Frankfurt am Main: Senckenbergische Naturforschende Gesellschaft, 1997.

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R. J. W. van Leeuwen. Sea-floor distribution and Late Quaternary faunal patterns of planktonic and benthic Foraminifers in the Angola Basin. Utrecht, Netherlands: Dept. of Stratigraphy and Paleontology, State University of Utrecht, 1989.

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Whiteaves, Joseph Frederick. On the land and fresh-water molluska of Lower Canada. [S.l: s.n., 1985.

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Whiteaves, Joseph Frederick. On the land and fresh-water molluska of Lower Canada. [S.l: s.n., 1985.

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10

Palaeobiogeography of marine fossil invertebrates: Concepts and methods. London: Taylor & Francis, 2002.

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Capítulos de libros sobre el tema "Fossil Geographical distribution"

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Stephenson, Steven L., Martin Schnittler, and Yuri K. Novozhilov. "Myxomycete diversity and distribution from the fossil record to the present." In Protist Diversity and Geographical Distribution, 51–67. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-90-481-2801-3_5.

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Jellad, Tarek, Khaled Taouil, and Zied Chtourou. "Power Management in Microgrids." In Handbook of Research on Novel Soft Computing Intelligent Algorithms, 141–64. IGI Global, 2014. http://dx.doi.org/10.4018/978-1-4666-4450-2.ch005.

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Conventional power generation stations used to be centralized and located far from customers. The transport and distribution infrastructure incur power losses that are mainly due to cabling resistance. Distributed power generation resources located close to customers are sought as a solution to minimize transport power losses. They are also good alternatives in situations where connection to the grid is not possible due to geographical or economical reasons. Furthermore, the adoption of renewable energies as alternatives for the scarce fossil energy sources paves the way to more distributed energy production. These Distributed energy resources, when located in a limited region, can be interconnected with loads and eventually storages to form a microgrid. A microgrid can operate in off-grid, on-grid, or alternate between these modes while optimizing power quality and cost. Multi-Agent Systems (MAS) and Petri nets could be put into contribution for high level planning of energy exchanges within a microgrid. This strategy has been validated on the basis of a dynamic model for the simulation and optimization of power exchanges between different DERs.
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Meadowcroft, James. "Governing the transition to a new energy economy." In Energy... beyond oil. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780199209965.003.0015.

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Over the next two or three decades a new energy economy should begin to take shape in the developed industrial countries. This will not be a post-fossil fuel economy. But it could be an economy in which non-fossil sources play a more important role; where efficiency in the production, distribution, and use of energy is significantly enhanced; where new storage and carrier technologies are being adopted; and where the fossil sector is being transformed by the imperative of carbon sequestration. Such an energy economy would represent a critical staging post in a much longer transition towards a carbon neutral, low-environmental impact, energy system. The extent to which a new energy economy actually materializes will depend on many factors including the pace and orientation of international economic development, the rate and direction of technological innovation and diffusion, as well as patterns of geo-strategic cooperation and conflict. But there is no doubt the trajectory will be significantly influenced by political decisions and government action on the energy file. This is the issue with which this chapter is concerned. At the moment there are two main political drivers for the move to look beyond oil. First, there are supply concerns. Increasing global demand, production bottlenecks, and political instability have pushed oil prices towards historic highs. Although the oil intensity (oil consumption per unit of GDP) of the OECD economies is less than during the oil crises of the 1970s (IMF, 2005), there is no doubt that the long term economic impact of high oil prices would be considerable. There are also critical issues associated with the geographic distribution of reserves. Production from areas opened up following the turbulence of the early 1970s (such as the North Sea) is peaking. In coming years the United States will be more heavily dependent on imported oil, with an increasing percentage of these imports destined to come from politically volatile areas in the Middle East and Asia. And this presents a serious risk of supply disruption.
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Actas de conferencias sobre el tema "Fossil Geographical distribution"

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Nyborg, Torrey, Brant Nyborg, Hal Fairfield, and Birgitta Jansen. "FOSSIL FISHES OF DEATH VALLEY NATIONAL PARK, CALIFORNIA: RECONSTRUCTING THE ORIGINS AND GEOGRAPHICAL DISTRIBUTION OF THE INDIGENOUS ICHTHYOFAUNA OF SOUTHEASTERN CALIFORNIA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302235.

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Nemati Mehr, Seyyed Mahdi, and Hossein Afshin. "Numerical Simulation of NOx Pollutant Formation in a Natural Gas Fired Power Generation Boiler, by Using Burner’s Parameters." In ASME 2012 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/imece2012-85277.

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The major source of energy is fossil fuels, known as hydrocarbon containing C and H as the main elements. The heat generated from combustion of these fuels is used in power generation cycles to generate electricity. Main products of a hydrocarbon combustion reaction are water and carbon dioxide, but due to some reasons such as excessive temperature and inappropriate air-fuel mixing, always some pollutants are formed. One of the major concerns of recent years are NOx pollutants, which is mostly generated in the high temperature combustions. According to the geographical and economic issues, mos
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van de Ketterij, R. G. "Emissions reduction at the Netherlands ministry of defence: potential, possibilities and impact." In 14th International Naval Engineering Conference and Exhibition. IMarEST, 2018. http://dx.doi.org/10.24868/issn.2515-818x.2018.065.

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To limit the global temperature rise to 1.5°C in 2100 compared to mid nineteenth century, net post 2015 emissions should amount maximum 200 Gigaton Carbon (GTC) or 734 GT CO2 emissions [Millar, 2017]. Annual world CO2 emission rate was 36.2GT, and CO2_eq (the combined impact of all emissions on global warming, translated to the equivalent impact of CO2 emissions) emission rate was 49 GT in 2016, [Carbonatlas, 2017]. Currently only 685 GT CO2 emission quota is left, or 14 years of emitting at the current emission rate. Estimates vary widely: IPCC thinks we only have 485 GT CO2 emission quota le
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Rodriguez, Stephanie C., Matthew P. Garb, and Jone Naujokaityte. "PREDICTING GEOGRAPHIC DISTRIBUTION OF BEDFORMS AND TRACE FOSSILS IN STRATA USING INDICATOR KRIGING IN EMIGRANT PASS, CALIFORNIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284107.

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