Academic literature on the topic 'Burgess, Schiste de (Canada)'

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Journal articles on the topic "Burgess, Schiste de (Canada)"

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Conway Morris, Simon, and John S. Peel. "A new helcionelloid mollusk from the middle Cambrian Burgess Shale, Canada." Journal of Paleontology 87, no. 6 (2013): 1067–70. http://dx.doi.org/10.1666/13-050.

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Burgess Shale-type faunas provide unique insights into the Cambrian “explosion”. Their degree of representativeness of Cambrian marine life in general is, however, less easy to establish. One line of evidence is to consider only the skeletal component of a Burgess Shale-type fauna and compare that with a typical Cambrian assemblage. This paper describes a new species of helcionelloid mollusk (Totoralia reticulata n. sp.) from the middle Cambrian Burgess Shale of British Columbia. Whilst much rarer than the co-occurring smooth shelled helcionelloid Scenella amii, the strongly costate morphology
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DALEY, ALLISON C., and GRAHAM E. BUDD. "New anomalocaridid appendages from the Burgess Shale, Canada." Palaeontology 53, no. 4 (2010): 721–38. http://dx.doi.org/10.1111/j.1475-4983.2010.00955.x.

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Sprinkle, James, and Desmond Collins. "New eocrinoids from the Burgess Shale, southern British Columbia, Canada, and the Spence Shale, northern Utah, USA." Canadian Journal of Earth Sciences 43, no. 3 (2006): 303–22. http://dx.doi.org/10.1139/e05-107.

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The family Lyracystidae n.fam. and genus Lyracystis n.gen. are proposed for the holotype and one paratype of the Middle Cambrian eocrinoid Gogia? radiata Sprinkle, the Burgess Shale "Arms" from the same unit, and many additional partial and more complete specimens of this eocrinoid collected from the Burgess Shale since 1975. A second species, Lyracystis reesei n.gen. and n.sp. is described from a single partly complete specimen from the similar-aged Spence Shale of northern Utah. Lyracystis has three wide V-shaped arms bearing numerous long straight brachioles in the notch, a partly organized
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Sun, Zhixin, Han Zeng, and Fangchen Zhao. "First occurrence of the Cambrian arthropod Sidneyia Walcott, 1911 outside of Laurentia." Geological Magazine 157, no. 3 (2019): 405–10. http://dx.doi.org/10.1017/s0016756819000864.

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AbstractThe arthropod Sidneyia Walcott, 1911 is a remarkable animal of the Burgess Shale biota (Cambrian Miaolingian, Wuliuan; British Columbia, Canada), which has not been confidently reported from other Cambrian Konservat-Lagerstätten. Here we report the discovery of Sidneyia cf. inexpectans from the Wuliuan Mantou Formation of North China, which substantially expands the known palaeogeographical distribution of this genus. Our discovery suggests that Sidneyia had much greater dispersal ability than hitherto thought. It also confirms the presence of exceptionally preserved fossils in the Wul
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Petrie, Meredith Blair, Jane A. Gilotti, William C. McClelland, Cees Van Staal, and Sierra J. Isard. "Geologic Setting of Eclogite-facies Assemblages in the St. Cyr Klippe, Yukon–Tanana Terrane, Yukon, Canada." Geoscience Canada 42, no. 3 (2015): 327. http://dx.doi.org/10.12789/geocanj.2015.42.073.

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The St. Cyr area near Quiet Lake hosts well preserved to variably retrogressed eclogite found as sub-metre to hundreds of metre-long lenses within quartzofeldspathic schist in south-central Yukon, Canada. The St. Cyr klippe consists of structurally imbricated, polydeformed and polymetamorphosed units of continental arc crust and ultramafic–mafic rocks. Eclogite-bearing quartzofeldspathic schist forms thrust slices in a 30 km long by 6 km wide, northwest-striking outcrop belt. The schist unit comprises metasedimentary and felsic intrusive rocks that are intercalated on the metre to tens of metr
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Minter, Nicholas J., M. Gabriela Mángano, and Jean-Bernard Caron. "Skimming the surface with Burgess Shale arthropod locomotion." Proceedings of the Royal Society B: Biological Sciences 279, no. 1733 (2011): 1613–20. http://dx.doi.org/10.1098/rspb.2011.1986.

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The first arthropod trackways are described from the Middle Cambrian Burgess Shale Formation of Canada. Trace fossils, including trackways, provide a rich source of biological and ecological information, including direct evidence of behaviour not commonly available from body fossils alone. The discovery of large arthropod trackways is unique for Burgess Shale-type deposits. Trackway dimensions and the requisite number of limbs are matched with the body plan of a tegopeltid arthropod. Tegopelte , one of the rarest Burgess Shale animals, is over twice the size of all other benthic arthropods kno
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Ausich, William I., and Loren E. Babcock. "Phylogenetic Affinities of Echmatocrinus Brachiatus (Middle Cambrian Burgess Shale, Canada)." Paleontological Society Special Publications 8 (1996): 16. http://dx.doi.org/10.1017/s2475262200000186.

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García-Bellido, Diego C., Jean Vannier, and Desmond Collins. "Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada." Acta Palaeontologica Polonica 54, no. 4 (2009): 699–712. https://doi.org/10.4202/app.2009.0024.

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García-Bellido, Diego C., Vannier, Jean, Collins, Desmond (2009): Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada. Acta Palaeontologica Polonica 54 (4): 699-712, DOI: 10.4202/app.2009.0024, URL: http://dx.doi.org/10.4202/app.2009.0024
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Verdun, Amy. "The Federal Features of the EU: Lessons from Canada." Politics and Governance 4, no. 3 (2016): 100–110. http://dx.doi.org/10.17645/pag.v4i3.598.

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There has been a rise and fall in interest in federalism in the context of European integration. This article assesses the federal nature of the EU. It draws in particular on the work of Michael Burgess who has been one of the key thinkers on this issue. Because there are many types of ‘federalisms’ available across the globe, it is helpful to make a comparison with another political system to offer a base line. In this article I explore to what extent the EU already has federal features. With the help of the work of Burgess I seek to look beyond the specific characteristics of the EU and refl
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Rigby, J. Keith, Lloyd F. Gunther, and Freida Gunther. "The first occurrence of the Burgess Shale demosponge Hazelia palmata Walcott, 1920, in the Cambrian of Utah." Journal of Paleontology 71, no. 6 (1997): 994–97. http://dx.doi.org/10.1017/s0022336000035976.

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A single specimen of Hazelia palmata Walcott, 1920, was collected from the Middle Cambrian Marjum Formation near Marjum Pass, in the central House Range, western Utah. This is a first occurrence of the species outside the Burgess shale region of British Columbia, Canada. The flattened oval impression of the monaxonid demosponge shows characteristic tufts and spicule structures of the species.
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Dissertations / Theses on the topic "Burgess, Schiste de (Canada)"

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Thorette, Jacques. "Contribution à l'étude de l'hydrothermalisme océanique : exemple du district minéralisé de York-Harbour (massif ophiolitique de Blow-Me-Down, Bay-of-Islands, Terre-Neuve)." Brest, 1986. http://www.theses.fr/1986BRES2002.

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Les mineralisations a cu-fe-zn de york-harbour sont encaissees dans l'unite volcanique situee au sommet de l'ophiolite cambrienne de blow-me-down. Celle-ci s'est formee a l'axe d'une dorsale oceanique a proximite d'une faille transformante. L'organisation en synclinal du secteur mineralise resulte du rejet des failles synvolcaniques en direction nord 135 et nord 45
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Ramírez-Guerrero, Greta M. "The systematics and evolution of Cambrian graptolites from the Burgess Shale of Canada." Thèse, 2019. http://hdl.handle.net/1866/22745.

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"Paleoecology of the burgess shale formation at The Monarch, Southern Rocky Mountains, Canada." Thesis, 2003. http://hdl.handle.net/10388/6561.

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The Middle Cambrian Burgess Shale Formation 1S a unique deposit hosting a remarkable diversity of soft-bodied and skeletal organisms. This unit onlaps the shallow-water dolomites of the Cathedral Formation which have been cut by a near vertical truncation surface known as the Cathedral Escarpment, a feature continuous for nearly 100 km. An abundant and diverse fauna is known from the classic quarries on Fossil Ridge between Mount Field and Mount Wapta, but other fossiliferous localities are present along the strike of the Cathedral Escarpment. In order to understand the ecological and paleonto
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"TAXONOMY, TAPHONOMY AND PALEOECOLOGY OF A NEW BURGESS SHALE-TYPE LAGERSTÄTTE FROM THE MACKENZIE MOUNTAINS, NORTHWEST TERRITORIES, CANADA." Thesis, 2014. http://hdl.handle.net/10388/ETD-2014-09-1719.

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The middle Cambrian (Drumian) Rockslide Formation is a deeper-water succession of mixed carbonates and siliciclastics. At the Ravens Throat River location it hosts a Burgess Shale-type (BST) deposit. The BST units are found in two separate 1m thick horizons of green-coloured calcareous mudstone and contain a biota similar to that of the Wheeler and Marjum formations of Utah, and to some extent the Burgess Shale itself. The biota is low in diversity and preserves mainly robust soft-tissue parts. The lithologically heterogeneous composition of the formation (shale, dolomite, lime mudstone, sands
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Books on the topic "Burgess, Schiste de (Canada)"

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Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. W.W. Norton, 1989.

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Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. Hutchinson Radius, 1990.

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Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. W.W. Norton, 1989.

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Gould, Stephen Jay. Wonderful life: The Burgess shale and the nature of history. Penguin, 1991.

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Briggs, D. E. G. The fossils of the Burgess Shale. Smithsonian Institution Press, 1994.

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Burgess, Alexander Mackinnon. Immigration: Evidence of A.M. Burgess, Esq., Deputy Minister of the Interior before the Select Committee of the House of Commons of Canada on Agriculture and Colonization, session 1896. Govt. Print. Bureau, 2004.

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Wonderful Life: Burgess Shale. Books on Tape, 1989.

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Gould, Stephen Jay. Wonderful Life: Burgess Shale and the Nature of History. Radius, 1990.

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Gould, Stephen Jay. Wonderful Life: Burgess Shale and the Nature of History. Radius, 1990.

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Wonderful Life - The Burgess Shale and the Nature of History. Norton, 1989.

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Book chapters on the topic "Burgess, Schiste de (Canada)"

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"Burgess Shale, British Columbia, Canada: Cradle of Early Life." In Travels with Trilobites. Columbia University Press, 2022. http://dx.doi.org/10.7312/sech20096-017.

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Ervin-Blankenheim, Elisabeth. "The Biography of the Earth." In Song of the Earth. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197502464.003.0010.

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This chapter focuses on the first era of the Phanerozoic Eon (“visible life”), the Paleozoic Era, when life burgeoned after a rapid shift from a frozen setting during Snowball Earth times to dramatic warming related to greenhouse conditions. The chapter includes stories, such as that of the finding of the unique creatures of the Burgess Shale in Canada, that represent the diversity of life in the early part of the Paleozoic, the Cambrian Period. Several climatic shifts happened in the Paleozoic with resulting extinction events, the first occurring at the end of the Ordovician Period, the secon
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Conference papers on the topic "Burgess, Schiste de (Canada)"

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Anderson, Thomas, Matthew James, and Paul McNeil. "THE BURGESS SHALE LAGERSTATTEN AT THE WALCOTT QUARRY, YOHO NATIONAL PARK, CANADA." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370219.

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Ramirez, Greta, and Christopher B. Cameron. "SYSTEMATICS OF PTEROBRANCHS FROM THE BURGESS SHALES OF CANADA AND THE EARLY EVOLUTION OF GRAPTOLITES." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-395905.

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Reports on the topic "Burgess, Schiste de (Canada)"

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Kottachchi, N. Fossils of the Middle Cambrian Burgess Shale, British Columbia, Canada: distribution and biostratinomic change through time. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212976.

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Fossils: fossils of the Burgess Shale, a national treasure in Yoho National Park, B.C., Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/226111.

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