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Academic literature on the topic 'Cenozoic Era'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Cenozoic Era"

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Jurdy, Donna M., and Michael Stefanick. "Plate-driving forces over the Cenozoic Era." Journal of Geophysical Research 93, B10 (1988): 11833. http://dx.doi.org/10.1029/jb093ib10p11833.

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Bibaeva, A. Y. "Transformation of Priolhonye Geosystems in Later Cenozoic Era." Bulletin of Irkutsk State University. Series Earth Sciences 23 (2018): 28–42. http://dx.doi.org/10.26516/2073-3402.2018.23.28.

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Zeebe, Richard E., and Lucas J. Lourens. "Geologically constrained astronomical solutions for the Cenozoic era." Earth and Planetary Science Letters 592 (August 2022): 117595. http://dx.doi.org/10.1016/j.epsl.2022.117595.

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Berry, Thomas. "Transition from the cenozoic to the ecozoic era." Environmental Carcinogenesis Reviews 8, no. 2 (January 1990): 391–400. http://dx.doi.org/10.1080/10590509009373394.

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MURRAY, D. F. "Papers from Khabarovsk: Beringia in the Cenozoic Era." Science 232, no. 4749 (April 25, 1986): 533. http://dx.doi.org/10.1126/science.232.4749.533.

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Bai, Ying, Hong Liang Wang, Qian Ru Li, and Peng Wu. "Cenozoic Tectonic Evolution and Controlling Factor on Hydrocarbon Accumulation in the Southern East China Sea Shelf Basin." Applied Mechanics and Materials 416-417 (September 2013): 1908–13. http://dx.doi.org/10.4028/www.scientific.net/amm.416-417.1908.

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The East China Sea shelf basin, which is a fault subsidence during the Cenozoic Era, locates in the East China Sea continental shelf. In this paper, balanced section technique has been applied to analyzing the differential evolution in the East China Sea shelf basin south of Cenozoic tectonic and summarizing the control factors of tectonic activities on the petroleum accumulation. Our study results will provide essential data and basis for the distribution of the Cenozoic oil and gas and promote the development of the petroleum exploration in the East China Sea shelf basin.
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Kagale, Sateesh, Stephen J. Robinson, John Nixon, Rong Xiao, Terry Huebert, Janet Condie, Dallas Kessler, et al. "Polyploid Evolution of the Brassicaceae during the Cenozoic Era." Plant Cell 26, no. 7 (July 2014): 2777–91. http://dx.doi.org/10.1105/tpc.114.126391.

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Davies, Bethan J., Michael J. Hambrey, John L. Smellie, Jonathan L. Carrivick, and Neil F. Glasser. "Antarctic Peninsula Ice Sheet evolution during the Cenozoic Era." Quaternary Science Reviews 31 (January 2012): 30–66. http://dx.doi.org/10.1016/j.quascirev.2011.10.012.

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Maevskaya, Anna, Nikolay Sheshko, Natalia Shpendik, and Maksim Bogdasarov. "Structural geological mapping of the Cenozoic sediments of the Brest region using GIS technologies." E3S Web of Conferences 212 (2020): 01010. http://dx.doi.org/10.1051/e3sconf/202021201010.

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Cenozoic sediments of the territory of the Brest region is the object of research in this work. The aim of this work is to detail the structure of the Cenozoic stratigraphic deposits by creating a set of structural geological maps. The process of creating maps included several sequential stages implemented using the ArcGIS 10.5 software product. In general, a set of maps for each period of the Cenozoic era was made according to the implemented method. As a result of mapping, the features of the geological structure of the Cenozoic sediments were detailed (based on the use of the most complete materials on the drilling exploration of the territory during the construction). The use of geoinformation systems in the process of building will allow for quick updating of cartographic materials in the future.
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Head, Martin J., Marie-Pierre Aubry, Mike Walker, Kenneth G. Miller, and Brian R. Pratt. "A case for formalizing subseries (subepochs) of the Cenozoic Era(a)." Episodes 40, no. 1 (March 1, 2017): 22–27. http://dx.doi.org/10.18814/epiiugs/2017/v40i1/017004.

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Books on the topic "Cenozoic Era"

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Vsesojuznyj simpozium Beringijskaja susna i ee znacenie dlja razvitija golarkticesrih flor i faun v kajnozoe (1973 Khabarovsk, Russie). Beringia in the Cenozoic era. Edited by Kontrimavicus Vitautas Leonovic. Rotterdam: Balkema, 1986.

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Vsesoi︠u︡znyĭ simpozium Beringiĭskai︠a︡ susha i ee znachenie dli︠a︡ razvitii︠a︡ golarkticheskikh flor i faun v kaĭnozoe (1973 Khabarovsk, R.S.F.S.R.). Beringia in the Cenozoic era. Edited by Kontrimavichus Vitautas Leonovich. Rotterdam: A.A. Balkema, 1985.

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Rafferty, John P. The Cenozoic era: Age of mammals. New York, NY: Britannica Educational pub. In association with Rosen Educational Services, 2011.

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Blashfield, Jean F. When giant mammals thundered: The cenozoic era. Chicago: Heinemann Library, 2006.

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Staff, Britannica Educational Publishing, and John P. Rafferty. Cenozoic Era: Age of Mammals. Rosen Publishing Group, 2010.

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Howard, Abby. Mammal Takeover!: Journey Through the Cenozoic Era. Abrams, Inc., 2019.

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Blashfield, Jean F. When Giant Mammals Thundered: The Cenozoic Era. Raintree, 2005.

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Howard, Abby. Mammal Takeover!: Journey through the Cenozoic Era. Amulet Paperbacks, 2021.

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(Editor), V. L. Kontrimavichus, and R. Chakravarty (Translator), eds. BERINGIA IN CENOZOIC ERA (Russian Translations Series, 28). Routledge, 1985.

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Burn Learn Or Memoirs Of The Cenozoic Era. Leaping Dog Press, 2009.

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Book chapters on the topic "Cenozoic Era"

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David, Anisha, and Akash Gautam. "Cenozoic Era." In Encyclopedia of Animal Cognition and Behavior, 1133–47. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-319-55065-7_1954.

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David, Anisha, and Akash Gautam. "Cenozoic Era." In Encyclopedia of Animal Cognition and Behavior, 1–15. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-319-47829-6_1954-1.

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"Cenozoic Era." In Dictionary of Geotourism, 68. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-2538-0_266.

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Ervin-Blankenheim, Elisabeth. "Biography of the Earth." In Song of the Earth, 214–28. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197502464.003.0012.

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The last era in the Phanerozoic Eon, the Cenozoic Era, is detailed in this chapter. The rise and radiation of the mammals occurred during Cenozoic after the devastation wrought by the Chicxulub Asteroid impact at the end of the Mesozoic Era. Ecological resources and niches vacated by the dinosaurs because of the mass extinction were filled by the mammals with concurrent developments in plants. Changes in climate and the mid-Miocene warming happened mid-era, then drying out and opening of grasslands followed by a plunge into ice ages and the Pleistocene extinction event. The late Cenozoic witnessed the development of humankind as the great ice sheets from the Pleistocene started to melt and the climate warm. The planet started to look similar to how it appears to humans today, and the current age of the Earth is the Cenozoic Era, Quaternary Period, Holocene Epoch, Meghalayan Age.
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Zalasiewicz, Jan. "9. A very brief history of the Earth." In Geology: A Very Short Introduction, 121–38. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198804451.003.0009.

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Our planet is ancient—at 4.6 billion years—and over that time it has changed enormously. ‘A very brief history of the Earth’ describes how the Earth and Moon were created in the Chaotian Eon from the collision of two planets: Tellus and Theia. It outlines the heavy meteorite bombardment of the Hadean Eon; the Archean Eon (c.3.8 billion years ago) when rocks were first preserved; the arrival of oxygen in Earth’s atmosphere and explosion of organic life in the Proterozoic Eon; and the Phanerozoic Eon, in which we still live. The various eras of this eon are described: the Palaeozoic Era, the Mesozoic Era, and the Cenozoic Era.
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Schierenbeck, Kristina A. "The Cenozoic Era: Paleogene and Neogene Periods (65–2.6 Ma)." In Phylogeography of California, 37–54. University of California Press, 2014. http://dx.doi.org/10.1525/california/9780520278875.003.0003.

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"6. The Age of Birds and Mammals: The Cenozoic Era." In Dinosaur Tracks and Other Fossil Footprints of the Western United States, 243–84. New York Chichester, West Sussex: Columbia University Press, 1995. http://dx.doi.org/10.7312/lock90868-009.

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"3. The Cenozoic Era: Paleogene and Neogene Periods (65–2.6 Ma)." In Phylogeography of California, 37–54. Berkeley: University of California Press, 2019. http://dx.doi.org/10.1525/9780520959248-004.

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Holman, J. Alan. "The European Herpetofauna: Paleocene Through Pliocene." In Pleistocene Amphibians and Reptiles in Britain and Europe. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195112320.003.0007.

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In both Europe and North America, modern herpetological families and genera became established quite early in the Cenozoic, and modern species occurred as early as the Miocene. Because of deteriorating climates that began late in the Eocene, a marked decrease in herpetological diversity occurred in the Oligocene in both continents. However, both areas became herpetologically enriched in the Miocene. In post-Miocene times Europe was isolated from Africa and warm areas in the east by the Mediterranean Sea and eastern mountain ranges, and a depauperate herpetofauna developed there that continued into recent times. In North America, however, with its vast, accessible southern land mass, the richness of the Miocene herpetofauna (with the exception of several archaic colubrid genera [Parmley and Holman, 1995] that became extinct in the the Miocene) persisted into modern times. The following discussion of changes in the European herpetofauna in the Cenozoic era has been synthesized from Auge (1986), Ballón (1991a), Bailon ct al. (1988), Barbadillo et al. (1997), Crochet et al. (1981), Estes (1981, 1982, 1983), Fritz (1995), Holman (1995c), Milncr (1986), Milner et al. (1982), Mlynarski (1976), Rage (1984a, 1984c, 1986, 1993), Rage and Auge (1993), Rage and Ford (1980), Roček (1994), Sanchiz. (1977b, in press), Sanchiz and Mlynarski (1979), Sanchiz and Roček (1996), Spinar (1972), Szyndlar (1984, 1991b, 1991c), and Szyndlar and Bohme (1993). Because of the high probability that herpetological fossils have been identified correctly at the family level, herpetological families arc used here to reflect the taxonomic diversity of the European herpetofauna from the Paleocene through the Pliocene. In a following section, the earliest appearance of herpetological genera and species in the European Tertiary arc discussed. Extinct families are prefixed with an asterisk (*). Families that became extinct in Europe in the Cenozoic but presently occur elsewhere are prefixed with a number sign (#). Two primitive, extinct, presumably permanently aquatic salamander families, me *Albanerpetontidae and *Batrachosauroididae (the latter also known from the Tertiary of North America) made limited appearances in the Cenozoic of Europe. The *Albanerpetontidae occurred only in the Middle Miocene (having reappeared from the Cretaceous), and the *Batrachosauroididae occurred from the Upper Paleocene to the Lower Eocene.
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Ervin-Blankenheim, Elisabeth. "Life on the Earth." In Song of the Earth, 137–62. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197502464.003.0008.

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Change in life forms over the long span of the Earth’s history, and the theory of evolution are discussed in chapter 7. Along with the tenets of geologic time (chapters 3 and 4) and plate tectonics (chapters 5 and 6), evolution encompasses another foundational idea in geology. This chapter examines the history of evolutionary thought and theory, starting with Charles Darwin and his work on natural selection. The historic “Bone Wars” that occurred with the discovery of the dinosaur fossils is an example of how fossils are used and sometimes misused to unravel the evolution of a significant branch in the Earth’s history of life. So too, the story of horses and their ancestors is portrayed in the Cenozoic era, as early equine ancestor species responded in their body size and tooth and foot structure to changes in climate and the opening of grasslands. The number and variety of life forms waxes and wanes over geologic time, through evolution and sometimes extinction events, only to re-emerge over eons, eras, periods, and epochs, leading to pulses of biodiversity in the fossil record. The theory of evolution was forged after the work by Darwin and others by later developments in molecular biology and DNA research which support modern evolutionary theory.
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Conference papers on the topic "Cenozoic Era"

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Pisarev, Denis Yurievich, Ildar Fanurovich Sharipov, Artur Michailovich Aslanyan, Danila Nikolaevich Gulyaev, and Anastasiya Nikolaevna Nikonorova. "Oil Production Enhancement by EOR Candidates Optimization." In SPE Russian Petroleum Technology Conference. SPE, 2021. http://dx.doi.org/10.2118/206498-ms.

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The study field is located in the Nizhnevartovsk district of the Khanty-Mansi autonomous region. The deposit is located in the Nizhnevartovsk crest zone. The geological section of this deposit features a thick layer (2740-2870 meters) of Meso-Cenozoic era sedimentary rocks starting from the Jurassic period up to and including the Quaternary period, and rests unconformably on the surface of the deposits of the folded Paleozoic basement. The pay zones of study oil and gas fields features mainly sandstone-siltstone reservoirs. The study formation XX11-2 features interleaved rocks with a high clay content. In the west and south-west of the field, the oil-saturated thicknesses vary on average from 5-10 m, and in the north, the thickness increases to 10-20 m. This field has a long-lasting production history as a result of drilling vertical and horizontal wells but is currently at production decline stage. The existing reservoir pressure support system assumes that the water-cut trend at the wells will increase. In recent years, there has been advanced flooding in some areas, resulting in a drop in oil production, while the reasons for the advanced flooding are not always clear. This is often due to the progressing spontaneous fracturing in the injector wells (Aslanyan, Akimov et al., 2020).
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Elobaid, Elnaiem Ali, Fadhil Sadooni, and Hamad Al Saad. "Tectonic and Geologic Settings of Halul and Al-Alyia Offshore Islands, Examples of Different Evolution Models, Within the Emergence of the Arabian Gulf Geosyncline: A Review." In Qatar University Annual Research Forum & Exhibition. Qatar University Press, 2020. http://dx.doi.org/10.29117/quarfe.2020.0044.

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The Arabian Gulf represents a significant water body and strategic pathway, which has pronounced regional and international benefits. This research investigated the evolution of the Arabian Gulf geosyncline. Furthermore, it explored the formation, geologic and tectonic settings of Halul and Al-Alyia offshore Islands, as examples of two different evolution models, within the emergence framework. The Arabian Gulf geosyncline has been emerged during the Cenozoic Era (Late Miocene-Pliocene Epoch), situated in the northeastern collisional marginal part of the Arabian Plate, as a foredeep geosyncline or basin, squeezed or crammed between the stable Arabian Plate and the mobile Euro-Asian Plate, along the subduction zone, within Zagros Mountain Fold Thrust Belt. Halul Island is situated to the northeast of the Greater Doha City and has great national economic value. It has a unique shape, elongated domal structure, oriented from South-West to North-East. The tectonic setting of Halul Island is classified as salt diapirism. The surface geology of this Island is dominated by carbonate rocks, mainly limestone and dolomitic limestone, and some igneous rock, such as basalt and Tholeiite. Al-Alyia Island is an integral part of the mainland. It is situated within the Greater Doha City's vicinity, in the eastern coastal zone. The Island is oriented from south-east to north-west. It is characterized by a gentle slope and low relief topography. The main rocks forming the island is the limestone and dolomitic limestone of the Simsima /Umm Bab Member of the Upper Dammam Formation of Tertiary age. This fact suggests that the island has a similar geologic setting to the mainland. This study revealed that the Halul Island evolution model is completely different from the evolution model of Al-Alyia Island, as Halul Island is a typical example model of salt dome Island, and remnants of the infracambrian salt basin, while Al-Alyia Island represents a different sedimentation model. This research has been carried out as part of the Environmental Science Center (ESC), Qatar University research agenda.
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