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Статті в журналах з теми "Paleontology Oligocene"
Gladenkov, Yu B. "The Oligocene of Sakhalin." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 234, no. 1-3 (December 22, 2004): 433–40. http://dx.doi.org/10.1127/njgpa/234/2004/433.
Повний текст джерелаAbdelghany, Osman, and Mahmoud Faris. "Early Oligocene calcareous nannofossils, planktonic and larger foraminifera from the United Arab Emirates, Oman Mountains." Micropaleontology 63, no. 6 (2018): 445–56. http://dx.doi.org/10.47894/mpal.63.6.06.
Повний текст джерелаFreudenthal, Matias, José Ignacio Lacomba, and Maria Angeles Sacristán. "Classification of european oligocene cricetids." Spanish Journal of Palaeontology 7, no. 3 (August 10, 2022): 49. http://dx.doi.org/10.7203/sjp.25014.
Повний текст джерелаBenedetti, Andrea. "Benthic foraminiferal turnover at the Eocene-Oligocene transition in the Caltavuturo Formation cropping out near Santa Cristina Gela (Sicily)." Micropaleontology 65, no. 5 (2019): 425–34. http://dx.doi.org/10.47894/mpal.65.5.03.
Повний текст джерелаKochhann, Karlos Guilherme Diemer, Simone Baecker-Fauth, and Gerson Fauth. "Systematic paleontology and biostratigraphy of Paleocene to late Oligocene Radiolaria from DSDP Site 329, Falkland Plateau, South Atlantic Ocean." Micropaleontology 59, no. 6 (2013): 529–54. http://dx.doi.org/10.47894/mpal.59.6.02.
Повний текст джерелаFraass, Andrew J., and R. Mark Leckie. "Oligocene Planktic Foraminiferal Taxonomy and Evolution: An Illustrated Revision of Ocean Drilling Program Site 803." Journal of Foraminiferal Research 51, no. 3 (July 31, 2021): 139–64. http://dx.doi.org/10.2113/gsjfr.51.3.139.
Повний текст джерелаDingle, Richard V. "Review of the history of the deep-sea ostracod genera Abyssocythere Benson and Dutoitella Dingle, and their responses to Cretaceous - Cenozoic oceanic water-mass changes." Micropaleontology 68, no. 3 (2022): 243–55. http://dx.doi.org/10.47894/mpal.68.3.04.
Повний текст джерелаMachalskij, D. V. "BACTERIAL PALEONTOLOGY OF THE OLIGOCENE OF THE UKRAINIAN CARPATHIANS." Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine 2 (April 30, 2009): 277–81. http://dx.doi.org/10.30836/igs.2522-9753.2009.148113.
Повний текст джерелаBenedetti, Andrea. "Biometric study of Planorbulina (Foraminiferida) from the Late Eocene-early Oligocene of Portella Colla (Madonie Mountains, Sicily)." Micropaleontology 63, no. 6 (2018): 403–12. http://dx.doi.org/10.47894/mpal.63.6.03.
Повний текст джерелаVerdenius, Jacob G., and Michael A. Kaminski. "Hyperammina grosserugosa, nom. nov., a replacement name for Hyperammina rugosa Verdenius and Van Hinte 1983." Micropaleontology 66, no. 6 (2020): 572. http://dx.doi.org/10.47894/mpal.66.6.07.
Повний текст джерелаДисертації з теми "Paleontology Oligocene"
Peleo-Alampay, Alyssa M. "Miocene and oligocene calcareous nannofossils : biochronology and paleoceanography /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1997. http://wwwlib.umi.com/cr/ucsd/fullcit?p9823695.
Повний текст джерелаMay, Geoffrey. "Oligocene to recent evolution of the Calama Basin, northern Chile." Thesis, University of Aberdeen, 1997. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=191900.
Повний текст джерелаEpa, Yuwan Ranjeev. "Paleoecology of the Freshwater Ampullariidae from the Late Oligocene Nsungwe Formation of Tanzania." Ohio University / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou149250551093219.
Повний текст джерелаShackelton, Allison Lee. "REGIONAL AND STRATIGRAPHIC VARIABILITY OF MICROWEAR ON THE MOLARS OF LEPTOMERYX FROM EOCENE-OLIGOCENE STRATA OF WYOMING AND NEBRASKA." Master's thesis, Temple University Libraries, 2016. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/402261.
Повний текст джерелаM.S.
Climate change across the terrestrial Eocene-Oligocene boundary of the Great Plains is recorded by shifts in sediments, facies, paleosols, and isotopic records, and is interpreted as a shift to overall cooler and drier conditions. As an independent test of paleoenvironmental shifts caused by climatic change, I compared microwear on M2 molars of Leptomeryx from the White River Group (WR) at Toadstool Park, Nebraska (n = 9) and Flagstaff Rim, Wyoming (n = 11). Comparisons of microwear were made through time at each section. Various measurements of microwear were quantified on original, uncoated specimens using environmental scanning electron microscopy and Microware 4.0 software, and evaluated with ANOVA and Kruskal-Wallis statistical tests. Values of the scratch:pit ratio, scratch number, feature major:minor axis ratio, feature vector length, major axis standard deviation, major:minor axis standard deviation, and feature orientation standard deviation for Leptomeryx M2 molars are significantly different (p<0.05) between Wyoming and Nebraska. Microwear patterns suggest paleoecological differences between the two locations, possibly related to differences in Leptomeryx diet or in amount or character of sediment adhering to ingested vegetation. Little fossil evidence of vegetation type is preserved at either locality, other than clay-filled root traces or occasional rhizoliths or silicified fragments. However, sediments of the WR are a mixture of volcaniclastic enriched mudstone, siltstone, and sandstone, with generally coarser overall particle sizes in Wyoming that reflect proximity to siliciclastic sources. The degree of overall volcaniclastic enrichment and number of airfall tuffs is also higher at Flagstaff Rim. Paleosols suggest a shift from closed canopy forest to progressively open conditions at each locality and, although microwear differences could result from differences in vegetation or particle sizes of adhered sediments on plants, no or very low correlations between microwear features and stratigraphic level were detected at either locality, indicating that any changes in paleoecology over time did not significantly alter the diets of Leptomeryx, although diet may have been geographically different.
Temple University--Theses
Sancay, Recep Hayrettin. "Palynostratigraphic And Palynofacies Investigation Of The Oligocene-miocene Units In The Kars-erzurum-mus Sub-basins (eastern Anatolia)." Phd thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12606637/index.pdf.
Повний текст джерела#8217
s of Compositae (tubuliflorae type), Slowakipollenites hipophä
eoides, Mediocolpopollis compactus, Monoporopollenites gramineoides and Umbelliferae at the base of Rupelian, FAD of Wetzeliella gochtii in the middle Rupelian, LAD of Ascostomocystis potane in the late Rupelian, LAD of Wetzeliella gochtii in the latest Rupelian, LAD of Deflandrea spp. in the latest Chattian, peak occurrences of Chriptoredium spp. in the early and late Aquitanian, FAD of Hystrichosphaeropsis obscura, followed by FAD of Membranilarnacea ?picena in the late Aquitanian should have particular emphasis for palynostratigraphic divisions in regional correlations and indicate that a continuous deposition took place in Eastern Anatolia from Late Eocene to the end of the Early Miocene. A relatively deeper marine deposition prevailed during the Late Eocene, which was followed by a shallowing-upward deposition during the Oligocene in MuS, Tekman, Tercan-ASkale, and Pasinler-Horasan basins. These basins were also characterized by an Early Miocene regional transgression, and terrestrial (lacustrine and fluvial) deposition during the Late Miocene-Pliocene whereas terrestrial conditions have been predominating since Late Eocene in the Bayburt-Kars Plateau. Paleoclimatological reconstructions of Eastern Anatolian Oligocene-Miocene sediments suggest temperate to subtropical climates in which mean annual temperatures vary between 15,6 to 21,3 °
C, mean temperatures of the coldest and the warmest month are 5.0 to 13.3 °
C and 24.7 to 28.1 °
C, respectively, and mean annual precipitation is 1122.0 to 1522.0 mm.
Chovanec, Kevin. "Non-anguimorph Lizards of the Late Oligocene and Early Miocene of Florida and Implications for the Reorganization of the North American Herpetofauna." Digital Commons @ East Tennessee State University, 2014. https://dc.etsu.edu/etd/2384.
Повний текст джерелаSanjuan, i. Girbau Josep. "Els caròfits del límit Eocè-Oligocè de la Conca de l’Ebre." Doctoral thesis, Universitat de Barcelona, 2013. http://hdl.handle.net/10803/133718.
Повний текст джерелаQuaglio, Fernanda. "Taxonomia de invertebrados fósseis (Oligoceno-Mioceno) da ilha Rei George (Antártica ocidental) e paleobiogeografia dos Bivalvia cenozóicos da Antártica." Universidade de São Paulo, 2007. http://www.teses.usp.br/teses/disponiveis/44/44139/tde-25042008-153222/.
Повний текст джерелаThe research presented in this dissertation comprised part of the CNPq - PROANTAR Project 550352/02-3 \"Mudanças paleoclimáticas na Antártica durante o Cenozóico: o registro geológico terrestre\", which studies Cenozoic deposits from King George Island in order to elucidate the environmental and climatic Cenozoic histories of this Antarctic region. Cenozoic evolution of marine and atmospheric circulation in the Southern Hemisphere occurred in response to the geographic and thermal isolation of Antarctica, which resulted from the separation of Antarctica from Australia, around Eocene/Oligocene boundary, and from South America, during the late Oligocene. Thus, study of fossil organisms from Antarctic Cenozoic deposits contributes to the understanding of biological and environmental evolutions that accompanied paleogeographic, oceanographic and climatic changes during the Cenozoic. As a result of the difficult access, logistic demand and extensive ice cover, only a small part of the Cenozoic Antarctic record is available for study. King George Island records climatic and environmental changes from the Oligocene to the Miocene, including evidence of the first full-scale glaciation (Oligocene) of West Antarctica. Despite the abundance of fossils in Cenozoic deposits of the island, taxonomic studies with detailed systematic descriptions of bivalves are very rare. The first section of this work consists of taxonomic descriptions of invertebrates from Cenozoic deposits cropping out in two localities of King George Island, West Antarctica. Seven taxa of bivalves, including six new species were described from the Cape Melville Formation (Miocene), at Melville Peninsula. Seven taxa of invertebrates (bivalves, brachiopods, serpulid tubes, bryozoans, and echinoderm fragments) were described from the Polonez Cove Formation (Oligocene), at Vauréal Peak, a site previously unexplored paleontologically. The second section presents the results of a survey of the Cenozoic fossil record of Antarctic bivalves. The analysis of the fossil record confirmed that the current knowledge about the Cenozoic diversity of the group is very scarce. Moreover, comparison of Cenozoic bivalve genera from Antarctica and New Zealand showed that the greatest number of shared taxa is recorded in Eocene deposits. This finding supports the geographic isolation of Antarctic and the drop in faunal interchange between Antarctica and periphery after the Oligocene. Analysis of the fossil record suggested an intensive dispersal event during the Eocene, and restricted pulses of dispersal from the Oligocene onwards. The distribution pattern of taxa provides partial support for available reconstructions of marine currents. Eocene dispersal would have occurred from Antarctica to New Zealand in Atlantic-Pacific direction. This dispersal event is consistent with the hypothesis of shallow marine connections between West and East Antarctica (\"Shackleton Seaway\"), as well of the existence of the Weddellian Province from the Late Cretaceous to the Eocene. Dispersal events following the Oligocene would have occurred during and after the establishment of the Circum-Antarctic Current, along the West-Atlantic and East margins of Antarctica towards New Zealand, and no longer through \"Shackleton Seaway\". These analyses also support the hypothesis of full-scale glaciation in West Antarctica from the early Oligocene onwards, and in East Antarctica since the mid-Oligocene, with warmer temperatures than today.
Engelman, Russell K. "New Specimens of Sparassodonta (Mammalia, Metatheria) from Chile and Bolivia." Case Western Reserve University School of Graduate Studies / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=case1536337238964166.
Повний текст джерелаBlaj, Teodora. "Late Eocene through Oligocene calcareous nannofossils from the paleo-equatorial Pacific Ocean – taxonomy, preservation history, biochronology and evolution." Doctoral thesis, Stockholm : Department of geology and geochemistry, Stockholm university, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-27600.
Повний текст джерелаКниги з теми "Paleontology Oligocene"
Laagland, H. Cycloclypeus in the Mediterranean Oligocene. Utrecht, Netherlands: U.M.B., 1990.
Знайти повний текст джерелаLambe, Lawrence M. The vertebrata of the Oligocene of the Cypress Hills, Saskatchewan. Ottawa: Govt. Print. Bureau, 1997.
Знайти повний текст джерелаKacharava, M. V. Geologicheskie sobytii͡a︡ na granit͡s︡e ėot͡s︡ena i oligot͡s︡ena Gruzii. Tbilisi: "Met͡n︡iereba", 1991.
Знайти повний текст джерелаOligocene Echinoids of North Carolina. Washington, D.C: Smithsonian Institution Press, 1997.
Знайти повний текст джерелаLaGarry, Hannan E. Taphonomic evidence of bone processing from the Oligocene of northwestern Nebraska. Lincoln: School of Natural Resources, Institute of Agriculture and Natural Resources, University of Nebraska-Lincoln, 2004.
Знайти повний текст джерелаThe Eocene-Oligocene transition: Paradise lost. New York: Columbia University Press, 1994.
Знайти повний текст джерелаHolmes, Thom. The age of mammals: The Oligocene and Miocene epochs. New York: Chelsea House, 2009.
Знайти повний текст джерелаRasmussen, D. Tab. Fossil birds from the Oligocene Jebel Qatrani Formation, Fayum Province, Egypt. Washington, D.C: Smithsonian Institution Press, 1987.
Знайти повний текст джерелаKatz, Mirian E. Oligocene bathyal to abyssal benthic foraminifera of the Atlantic Ocean. New York: Micropaleontology Project, 2004.
Знайти повний текст джерелаSzyndlar, Zbigniew. Non-ercine Booidea from the Oligocene and Miocene of Europe. Kraków: Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, 2003.
Знайти повний текст джерелаЧастини книг з теми "Paleontology Oligocene"
Prothero, Donald R. "Magnetic stratigraphy of the Eocene-Oligocene floral transition in western North America." In Paleontology of the Upper Eocene Florissant Formation, Colorado. Geological Society of America, 2008. http://dx.doi.org/10.1130/2008.2435(05).
Повний текст джерелаNyborg*, Torrey, and E. Bruce Lander*. "Vertebrate paleontology and Cenozoic depositional environments of Death Valley National Park, California, USA." In Field Excursions from Las Vegas, Nevada: Guides to the 2022 GSA Cordilleran and Rocky Mountain Joint Section Meeting, 1–22. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.0063(01).
Повний текст джерелаТези доповідей конференцій з теми "Paleontology Oligocene"
Cruz Vega, Eduardo. "RECENT ADVANCES IN CARIBBEAN PALEONTOLOGY: A CASE STUDY OF OLIGOCENE FAUNA FROM THE SAN SEBASTIÁN FORMATION, PUERTO RICO." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-368853.
Повний текст джерела