Thematische Bibliographien / Paleontology Cambrian

Auswahl der wissenschaftlichen Literatur zum Thema „Paleontology Cambrian“

Autor: Grafiati
Veröffentlicht am 4. Juni 2021
Zuletzt aktualisiert am 25. Januar 2023

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Inhaltsverzeichnis

  1. Zeitschriftenartikel
  2. Dissertationen
  3. Bücher
  4. Buchteile
  5. Konferenzberichte
  6. Berichte der Organisationen

Zeitschriftenartikel zum Thema "Paleontology Cambrian":

1

Vidal, Gonzalo. „Proterozoic and Cambrian bioevents“. Spanish Journal of Palaeontology 13, Nr. 3 (27.02.2022): 11. http://dx.doi.org/10.7203/sjp.23973.

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2

Fortey, Richard A. „Late Cambrian trilobites from the Sultanate of Oman“. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 194, Nr. 1 (28.11.1994): 25–53. http://dx.doi.org/10.1127/njgpa/194/1994/25.

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3

Jago, James B., und Peter W. Haines. „Recent radiometric dating of some Cambrian rocks in southern Australia: relevance to the Cambrian time scale.“ Spanish Journal of Palaeontology 13, Nr. 3 (27.02.2022): 115. http://dx.doi.org/10.7203/sjp.23984.

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4

Landing, Ed, und Guy M. Narbonne. „Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”“. Journal of Paleontology 66, Nr. 2 (März 1992): 338. http://dx.doi.org/10.1017/s0022336000033837.

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In a recent article, Narbonne et al. (1991) documented that the stratigraphic range of the chondrophorine Kullingia delicata continues above the the uppermost Precambrian (Vendian) into the lowermost Cambrian (Placentian Series) of the Avalonian faunal province. The revised text published in the Journal of Paleontology includes several references to Scenella Billings, 1872, as a Cambrian chondrophorine. This classification is in error and unfortunately serves to reinforce several recent reports that conclude that Scenella is a chondrophorine rather than a helcionacean mollusk.
5

Waggoner, Ben, und James W. Hagadorn. „An unmineralized alga from the Lower Cambrian of California, USA“. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 231, Nr. 1 (02.02.2004): 67–83. http://dx.doi.org/10.1127/njgpa/231/2004/67.

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6

Chang, Wen T. „Cambrian biogeography of the Perigondwana Faunal Realm“. Spanish Journal of Palaeontology 13, Nr. 3 (27.02.2022): 35. http://dx.doi.org/10.7203/sjp.23977.

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Chang, Wen T. „Cambrian correlation within the Perigondwana Faunal Realm“. Spanish Journal of Palaeontology 13, Nr. 3 (27.02.2022): 23. http://dx.doi.org/10.7203/sjp.23976.

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8

Kuzmina, T. V., A. A. Ratnovskaya und A. A. Madison. „Lophophore Evolution from the Cambrian to the Present“. Paleontological Journal 55, Nr. 10 (Dezember 2021): 1109–40. http://dx.doi.org/10.1134/s0031030121100051.

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9

Geyer, Gerd, und Michael Streng. „Middle Cambrian pelecypods from the Anti-Atlas, Morocco“. Spanish Journal of Palaeontology 13, Nr. 3 (27.02.2022): 83. http://dx.doi.org/10.7203/sjp.23980.

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10

Bordonaro, Osvaldo Luis, und Eladio Liñán Guijarro. „Some middle Cambrian agnostoids from the Precordillera Argentina.“ Spanish Journal of Palaeontology 9, Nr. 1 (10.08.2022): 105. http://dx.doi.org/10.7203/sjp.24355.

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Die Auswahlen zum Thema "Paleontology Cambrian" für konkrete Quellenarten können Sie auch interessieren:
Zeitschriftenartikel Dissertationen Bücher

Dissertationen zum Thema "Paleontology Cambrian":

1

Skinner, Ethan S. „Taphonomy of exceptionally perserved fossils from the Kinzers Formation (Cambrian), southeastern Pennsylvania“. Connect to this title online, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1090592371.

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Thesis (Ph. D.)--Ohio State University, 2004.
Title from first page of PDF file. Document formatted into pages; contains xiv, 167 p.; also includes graphics. Includes bibliographical references (p. 127-143).
2

Fuller, Margaret. „Early Cambrian corals from the Moorowie Formation, Eastern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SM/09smf967.pdf.

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3

Ahn, Soo Yeun. „Ediacaran-Cambrian Stratigraphy and Paleontology of Western Nevada and Eastern California“. The Ohio State University, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=osu1275489532.

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Bohach, Lisa Lynn. „Systematics and biostratigraphy of Lower Cambrian trilobites of western Laurentia“. Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ32705.pdf.

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5

Hegna, Thomas Arthur. „Systematics of late Cambrian (Sunwaptian) trilobites from the St. Charles Formation, southeastern Idaho“. Thesis, University of Iowa, 2006. http://ir.uiowa.edu/etd/45.

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6

Baghiyan-Yazd, Mohammad Hassan. „Palaeoichnology of the terminal Proterozoic-Early Cambrian transition in central Australia : interregional correlation and palaeoecology“. Title page, table of contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phb1445.pdf.

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7

Tremblay, James Vincent. „Trilobites and strata of the Lower and Middle Cambrian Peyto, Mount Whyte and Naiset Formations, Alberta and British Columbia /“. *McMaster only, 1996.

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8

Skinner, Ethan S. „Taphonomy of exceptionally preserved fossils from the Kinzers Formation (Cambrian), southeastern Pennsylvania“. The Ohio State University, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=osu1090592371.

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9

Kastigar, Jessica M. „Application of X-ray Computed Tomography to Interpreting the Origin and Fossil Content of Siliceous Concretions from the Conasauga Formation (Cambrian) of Georgia and Alabama, USA“. The Ohio State University, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=osu1461271051.

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10

Peteya, Jennifer Anita. „Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed Tomographic Imaging Techniques“. The Ohio State University, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=osu1366025146.

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Bücher zum Thema "Paleontology Cambrian":

1

W, Cowie J., und Brasier M. D, Hrsg. The Precambrian-Cambrian boundary. Oxford: Clarendon Press, 1989.

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2

E, Logan William. Remarks on the fauna of the Quebec group of rocks and the primordial zone of Canada: Addressed to Mr. Joachim Barrande. [Montreal: s.n.], 1986.

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3

Kruse, P. D. Cambrian palaeontology of the Daly Basin. Darwin: Govt. Printer of the Northern Territory, 1990.

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4

Bengtson, Stefan. Early Cambrian fossils from South Australia. Brisbane: Association of Australasian Palaeontologists, 1990.

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5

Chlupáč, Ivo. Palaeozoic of the Barrandian: Cambrian to Devonian. Prague: Czech Geological Survey, 1998.

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6

Moczydłowska, Małgorzata. Acritarch biostratigraphy of the Lower Cambrian and the Precambrian--Cambrian boundary in southeastern Poland. Oslo: Universitetsforlaget, 1991.

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Moczydlowska, Malgorzata. Acritarch biostratigraphy of the Lower Cambrian and the Precambrian--Cambrian boundary in southeastern Poland. Oslo: Universitetsforlaget, 1991.

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8

McMenamin, Mark A. S. The emergence of animals: The Cambrian breakthrough. New York: Columbia University Press, 1990.

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9

McMenamin, Mark. The emergence of animals: The Cambrian breakthrough. New York: Columbia University Press, 1989.

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10

Tsuchiya, Ken. Ediakara-ki, kanburia-ki no seibutsu: Ediacaran & Cambrian creatures. 8. Aufl. Tōkyō-to Shinjuku-ku: Gijutsu Hyōronsha, 2013.

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Buchteile zum Thema "Paleontology Cambrian":

1

McMenamin, Mark A. S. „Cambrian Cannibals“. In Dynamic Paleontology, 181–89. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-22777-1_11.

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2

Palmer, A. R., und Stephen M. Rowland. „Day 1: Early Cambrian stratigraphy and paleontology, southern Great Basin, California-Nevada“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 17–27. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0017.

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3

Signor, Philip W., und Jeffrey F. Mount. „Paleontology of the Lower Cambrian Waucoban Series in eastern California and western Nevada“. In Late Proterozoic and Cambrian Tectonics, Sedimentation, and Record of Metazoan Radiation in the Western United States: Pocatello, Idaho, to Reno, Nevada 20–29 July, 1989, 47–53. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft331p0047.

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4

Rees, Margaret N., und Richard A. Robison. „Days 5 and 6: Cambrian stratigraphy and paleontology of the central House Range and Drum Mountains, Utah“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 59–72. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0059.

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5

Palmer, A. R. „Day 0: Early and Middle Cambrian stratigraphy of Frenchman Mountain, Nevada“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 14–16. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0014.

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6

Cook, Harry E., Michael E. Taylor und James F. Miller. „Day 2: Late Cambrian and Early Ordovician stratigraphy, biostratigraphy and depositional environments, Hot Creek Range, Nevada“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 28–36. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0028.

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7

Miller, James F., und Michael E. Taylor. „Day 4: Late Cambrian and Early Ordovician stratigraphy and biostratigraphy, southern House Range (“Ibex area”), Utah“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 45–58. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0045.

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8

Taylor, Michael E., Harry E. Cook und James F. Miller. „Day 3: Late Cambrian and Early Ordovician biostratigraphy and depositional environments of the Whipple Cave Formation and House Limestone, central Egan Range, Nevada“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 37–44. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0037.

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9

Taylor, Michael E. „Introduction and background for Field Trip T125“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 1–5. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0001.

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10

Cook, Harry E. „Geology of the Basin and Range Province, western United States: An overview“. In Cambrian and Early Ordovician Stratigraphy and Paleontology of the Basin and Range Province, Western United States: Las Vegas, Nevada to Salt Lake City, Utah, July 1–7, 1989, 6–13. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft125p0006.

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Konferenzberichte zum Thema "Paleontology Cambrian":

1

Collantes Ruiz, Mayoral Alfaro und Gozalo Gutiérrez. „The genus Serrodiscus (Trilobita) in the upper Marianian (early Cambrian) from nothern Huelva province, SW Spain“. In XVIII Encuentro de Jóvenes Investigadores en Paleontologia. Nova.id.fct, 2021. http://dx.doi.org/10.21695/cterraproc.v1i0.394.

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Berichte der Organisationen zum Thema "Paleontology Cambrian":

1

Tweet, Justin, Holley Flora, Summer Weeks, Eathan McIntyre und Vincent Santucci. Grand Canyon-Parashant National Monument: Paleontological resource inventory (public version). National Park Service, Dezember 2021. http://dx.doi.org/10.36967/nrr-2289972.

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Annotation:
Grand Canyon-Parashant National Monument (PARA) in northwestern Arizona has significant paleontological resources, which are recognized in the establishing presidential proclamation. Because of the challenges of working in this remote area, there has been little documentation of these resources over the years. PARA also has an unusual management situation which complicates resource management. The majority of PARA is administered by the Bureau of Land Management (BLM; this land is described here as PARA-BLM), while about 20% of the monument is administered by the National Park Service (NPS; this land is described here as PARA-NPS) in conjunction with Lake Mead National Recreation Area (LAKE). Parcels of state and private land are scattered throughout the monument. Reports of fossils within what is now PARA go back to at least 1914. Geologic and paleontologic reports have been sporadic over the past century. Much of what was known of the paleontology before the 2020 field inventory was documented by geologists focused on nearby Grand Canyon National Park (GRCA) and LAKE, or by students working on graduate projects; in either case, paleontology was a secondary topic of interest. The historical record of fossil discoveries in PARA is dominated by Edwin McKee, who reported fossils from localities in PARA-NPS and PARA-BLM as part of larger regional projects published from the 1930s to the 1980s. The U.S. Geological Survey (USGS) has mapped the geology of PARA in a series of publications since the early 1980s. Unpublished reports by researchers from regional institutions have documented paleontological resources in Quaternary caves and rock shelters. From September to December 2020, a field inventory was conducted to better understand the scope and distribution of paleontological resources at PARA. Thirty-eight localities distributed across the monument and throughout its numerous geologic units were documented extensively, including more than 420 GPS points and 1,300 photos, and a small number of fossil specimens were collected and catalogued under 38 numbers. In addition, interviews were conducted with staff to document the status of paleontology at PARA, and potential directions for future management, research, protection, and interpretation. In geologic terms, PARA is located on the boundary of the Colorado Plateau and the Basin and Range provinces. Before the uplift of the Colorado Plateau near the end of the Cretaceous 66 million years ago, this area was much lower in elevation and subject to flooding by shallow continental seas. This led to prolonged episodes of marine deposition as well as complex stratigraphic intervals of alternating terrestrial and marine strata. Most of the rock formations that are exposed in the monument belong to the Paleozoic part of the Grand Canyon section, deposited between approximately 510 and 270 million years ago in mostly shallow marine settings. These rocks have abundant fossils of marine invertebrates such as sponges, corals, bryozoans, brachiopods, bivalves, gastropods, crinoids, and echinoids. The Cambrian–Devonian portion of the Grand Canyon Paleozoic section is represented in only a few areas of PARA. The bulk of the Paleozoic rocks at PARA are Mississippian to Permian in age, approximately 360 to 270 million years old, and belong to the Redwall Limestone through the Kaibab Formation. While the Grand Canyon section has only small remnants of younger Mesozoic rocks, several Mesozoic formations are exposed within PARA, mostly ranging in age from the Early Triassic to the Early Jurassic (approximately 252 to 175 million years ago), as well as some middle Cretaceous rocks deposited approximately 100 million years ago. Mesozoic fossils in PARA include marine fossils in the Moenkopi Formation and petrified wood and invertebrate trace fossils in the Chinle Formation and undivided Moenave and Kayenta Formations.

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