Thematische Bibliographien / Burgess, Schiste de (Canada)

Auswahl der wissenschaftlichen Literatur zum Thema „Burgess, Schiste de (Canada)“

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Veröffentlicht am 25. Juli 2024

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Zeitschriftenartikel zum Thema "Burgess, Schiste de (Canada)"

Conway Morris, Simon, und John S. Peel. „A new helcionelloid mollusk from the middle Cambrian Burgess Shale, Canada“. Journal of Paleontology 87, Nr. 6 (November 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 of Totoralia reinforces comparisons with Cambrian shelly faunas. The extension of the range of Totoralia from Argentina to Canada adds support to the proposed derivation of the Precordillera terrane of Mendoza from Laurentia.

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DALEY, ALLISON C., und GRAHAM E. BUDD. „New anomalocaridid appendages from the Burgess Shale, Canada“. Palaeontology 53, Nr. 4 (19.07.2010): 721–38. http://dx.doi.org/10.1111/j.1475-4983.2010.00955.x.

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Sprinkle, James, und 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, Nr. 3 (01.03.2006): 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 theca having larger and smaller ridged plates with epispires, and a very long multiplated stalk made up of rounded or spiny small plates. Lyracystis is the longest-stalked, suspension-feeding echinoderm known from the Middle Cambrian. The three remaining paratypes of Gogia? radiata and four new specimens with possible branched brachioles from the Burgess Shale are renamed Gogia stephenensis n.sp.

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Petrie, Meredith Blair, Jane A. Gilotti, William C. McClelland, Cees Van Staal und Sierra J. Isard. „Geologic Setting of Eclogite-facies Assemblages in the St. Cyr Klippe, Yukon–Tanana Terrane, Yukon, Canada“. Geoscience Canada 42, Nr. 3 (29.07.2015): 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 metres scale. Ultramafic rocks, serpentinite and associated greenschist-facies metagabbro form imbricated tectonic slices within the eclogite-bearing quartzofeldspathic unit, which led to a previously held hypothesis that eclogite was exhumed within a tectonic mélange. The presence of phengite and Permian zircon crystallized under eclogite-facies metamorphic conditions in the quartzofeldspathic host rocks indicate that the eclogite was metamorphosed in situ together with the schist as a coherent unit that was part of the continental arc crust of the Yukon–Tanana terrane, rather than a mélange associated with the subduction of oceanic crust of the Slide Mountain terrane. Petrological, geochemical, geochronological and structural similarities link St. Cyr eclogite to other high-pressure localities within Yukon, indicating the high-pressure assemblages form a larger lithotectonic unit within the Yukon–Tanana terrane.RÉSUMÉLa région de St-Cyr renferme des éclogites bien conservées à légèrement rétrogradées qui se présentent sous forme de lentilles allant de la fraction de mètre à quelques centaines de mètres de longueur, au sein d’un schiste quartzofeldspathique du centre-sud du Yukon au Canada. La klippe de St-Cyr est structurellement constituée d’unités imbriquées, polydéformées et polymétamorphisées de croûte d’arc continental et de roches ultramafiques à mafiques. Les schistes quartzofeldspathiques à lentilles d’éclogites forment des écailles de chevauchement d’une bande de 30 km de longueur par 6 km de largeur de direction nord-ouest. Les schistes sont constitués de roches métasédimentaires et de roches intrusives felsiques intercalées à des intervalles qui vont du mètre à quelques dizaines de mètres. Les roches ultramafiques, serpentinites et métagabbros au facies à schiste vert forment des écailles tectoniques imbriquées au sein de l’unité quartzofeldspathique à lentilles d’éclogite, d’où une précédente hypothèse voulant que les éclogites soient un produit d’exhumation à partir d’un mélange tectonique. La présence de phengite et de zircon permien cristallisé sous conditions métamorphiques du faciès à éclogite au sein de la roche hôte quartzofeldspathique indiquent que l’éclogite a été métamorphisée en place, avec le schiste comme unité cohérente du terrane de croûte d’arc continental de Yukon–Tanana, plutôt qu’un mélange associé à une subduction de croûte océanique du terrane de Slide Mountain. Des similarités pétrologiques, géochimiques, géochronologiques et structurales lient les éclogites de St-Cyr à d’autres lieux de hautes pressions au Yukon, ce qui indique que les assemblages de hautes pressions forment une unité lithotectonique plus grande au sein du terrane de Yukon–Tanana.

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Ausich, William I., und 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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Sun, Zhixin, Han Zeng und Fangchen Zhao. „First occurrence of the Cambrian arthropod Sidneyia Walcott, 1911 outside of Laurentia“. Geological Magazine 157, Nr. 3 (28.08.2019): 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 Wuliuan Mantou Formation, one of the rare Burgess Shale-type deposits of North China.

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Verdun, Amy. „The Federal Features of the EU: Lessons from Canada“. Politics and Governance 4, Nr. 3 (11.08.2016): 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 reflect on how a comparison with this other polity can offer us insights into what is going on within the EU political system. Drawing on the comparison with Canada, I seek to identify the characteristics of the EU that are already those of a federation. Therefore, the guiding question of this article is: compared to Canada, what particular features does the EU have that reminds us of a federation and what features is it still lacking? It finds that the EU has a considerable amount of federal features (federation), but that a federal tradition, a federal ideology and advocacy to a federal goal (federalism) are mostly absent.

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Minter, Nicholas J., M. Gabriela Mángano und Jean-Bernard Caron. „Skimming the surface with Burgess Shale arthropod locomotion“. Proceedings of the Royal Society B: Biological Sciences 279, Nr. 1733 (09.11.2011): 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 known from this locality, and only its sister taxon, Saperion , from the Lower Cambrian Chengjiang biota of China, approaches a similar size. Biomechanical trackway analysis demonstrates that tegopeltids were capable of rapidly skimming across the seafloor and, in conjunction with the identification of gut diverticulae in Tegopelte , supports previous hypotheses on the locomotory capabilities and carnivorous mode of life of such arthropods. The trackways occur in the oldest part (Kicking Horse Shale Member) of the Burgess Shale Formation, which is also known for its scarce assemblage of soft-bodied organisms, and indicate at least intermittent oxygenated bottom waters and low sedimentation rates.

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Kimmig, Julien, und Brian R. Pratt. „Soft-bodied biota from the middle Cambrian (Drumian) Rockslide Formation, Mackenzie Mountains, northwestern Canada“. Journal of Paleontology 89, Nr. 1 (Januar 2015): 51–71. http://dx.doi.org/10.1017/jpa.2014.5.

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AbstractA new Burgess Shale-type Lagerstätte is described from the middle Cambrian (Series 3, Drumian) Rockslide Formation of the Mackenzie Mountains, Northwest Territories, Canada. The Rockslide Formation is a unit of deeper water ramp to slope, mixed carbonate, and siliciclastic facies deposited on the northwestern margin of Laurentia. At the fossil-bearing locality, the unit onlaps a fault scarp cutting lower Cambrian sandstones. There it consists of a succession of shale and thick-laminated to thin-bedded lime mudstone, calcareous sandstone, and greenish-colored calcareous mudstone, overlain by shallower water dolostones of the Avalanche Formation, which is indicative of an overall progradational sequence. The Rockslide Formation is of similar age to the Wheeler and Marjum formations of Utah, belonging to theBolaspidellaBiozone. Only two 1 m thick units of greenish mudstone exhibit soft-bodied preservation, with most specimens coming from the lower interval. However, the biota is common but not as diverse as that of other Lagerstätten such as the Burgess Shale in its type area. The shelly fauna is dominated by the hyolithHaplophrentis carinatusMatthew, 1899 along with sparse linguliformean brachiopods, agnostoid arthropods, and ptychoparioid trilobites. The nonmineralized biota includes the macrophytic algaMargaretia dorusWalcott, 1911, priapulid worms, and the carapaces of a number of arthropods. The arthropods belong toIsoxys mackenziensisn. sp.,Tuzoiacf.T. guntheriRobison and Richards, 1981;Branchiocaris? sp.,Perspicaris?dilatusRobison and Richards, 1981; and bradoriids, along with fragments of arthropods of indeterminate affinities. The style of preservation indicates that most soft parts underwent complete biodegradation, leaving just the more resistant materials such as chitinous arthropod cuticles. The range of preservation and similarity to the coeval biotas preserved in Utah suggests that the composition of this Lagerstätte is probably representative of the community living on the relatively deep-water ramp or slope during middle Cambrian time in Laurentia. This would argue that the extraordinary diversity of the Burgess Shale at Mount Field is anomalous.

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Rigby, J. Keith, Lloyd F. Gunther und Freida Gunther. „The first occurrence of the Burgess Shale demosponge Hazelia palmata Walcott, 1920, in the Cambrian of Utah“. Journal of Paleontology 71, Nr. 6 (November 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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Dissertationen zum Thema "Burgess, Schiste de (Canada)"

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 paleontological basis for lateral variations in faunal composition within the Burgess Shale, exposures 60 km to the southeast of the type area were examined at The Monarch, a mountain straddling the British Columbia/Alberta border. In four closely spaced sections, faunal elements are present only in the basal 30 m of the silty shales immediately adjacent to the Cathedral Escarpment; fossil occurrence decreases dramatically barely tens of meters away. The fauna is dominated by priapulid worms, hyolithids, and phosphatic and calcareous brachiopods, which together constitute more than 75% of specimens counted. Trilobites (mainly Olenoides serratus), sponges (mainly Vauxia spp.) and phosphatic tubes (Byronia annulata) are also significant components of the fauna. The fauna at The Monarch is much less diverse than that of the classic Burgess Shale on Fossil Ridge. A prominent difference is the absence of non-trilobite arthropods (e.g. Marrella splendens and Anomalocaris canadensis) and most soft-bodied elements. While all four sections at The Monarch are equally fossiliferous, differences between localities are evident in the distribution of the rarer biotic elements. Specifically, the arthropod Sidneyia inexpectans, the sponge Takakkawia sp. nov., and the probable lepadomorph barnacle Priscansermarinus barnetti occur, albeit rarely, only on the southern exposures. Fault-related fluid seeps along the base of the Cathedral Escarpment are a possible explanation for the localized biota. Sporadic and variably active seeps could have generated localized and intermittent increases in biologic productivity, especially bacteria, which in tum would have resulted in patchy concentrations of fauna close to the escarpment, a pattern consistent with the contrast in assemblages between The Monarch and the type area.

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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, sandstone, mudstone) and absence of metamorphism offer an opportunity to analyze the depositional environment and taphonomy of this deeper water unit. Geochemical analysis including, trace elements, organic carbon, biomarker, and synchrotron were attempted and yielded varying results. Trace element ratios, particularly V/Sc, indicate low oxygenation of the bottom waters during the deposition of the fossil-bearing interval. These results differ from most other BST deposits, which suggest that oxygenated bottom waters were maintained throughout sedimentation. In addition, organic matter in the sediments and δ13Corg values suggest the presence of benthic microbial mats. Silver is concentrated mostly in nm to μm-sized particles in the fossilifereous calcareous mudstone, suggesting elevated levels in the depositional environment. Organic films and the evidence for hyoliths feeding on them suggest an in situ preservation of the biota, perhaps from sudden and short anoxic events and quick burial under either microbial mats or the muddy sediment. This is also supported by the presence of only very rare trace fossils.

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Bücher zum Thema "Burgess, Schiste de (Canada)"

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

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

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

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

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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. Ottawa: Govt. Print. Bureau, 2004.

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Gould, Stephen Jay. La Vie est belle : Les Surprises de l'évolution. Seuil, 1998.

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Gould, Stephen Jay. La Vie est belle : Les Surprises de l'évolution. Seuil, 1991.

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Gould, Stephen Jay. Wonderful Life: The Burgess Shale and the Nature of History. Replica Books, 1989.

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Gould, Stephen Jay. Wonderful Life: The Burgess Shale and the Nature of History by Stephen Jay Gould. W. W. Norton, 1990.

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

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Buchteile zum Thema "Burgess, Schiste de (Canada)"

„Burgess Shale, British Columbia, Canada: Cradle of Early Life“. In Travels with Trilobites, 50–58. 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, 181–99. 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 second at the end of the Devonian, and a third massive extinction at the end of the Permian Period. The latter was the largest extinction event ever recorded when 95 percent of all genera were killed as the supercontinent Pangea began to be split apart at the end of the Paleozoic.

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Konferenzberichte zum Thema "Burgess, Schiste de (Canada)"

Anderson, Thomas, Matthew James und 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, und 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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Berichte der Organisationen zum Thema "Burgess, Schiste de (Canada)"

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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