Relevant bibliographies by topics / Oligocene-Miocene

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Oligocene-Miocene'

Author: Grafiati
Published: 4 June 2021
Last updated: 18 February 2022

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Journal articles on the topic "Oligocene-Miocene"

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del Río, Claudia Julia. "Tertiary marine molluscan assemblages of eastern Patagonia (Argentina): A biostratigraphic analysis." Journal of Paleontology 78, no. 6 (2004): 1097–122. http://dx.doi.org/10.1017/s0022336000043912.

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Pectinids are the most abundant and widely distributed taxa in the Tertiary marine beds of Patagonia. Along with other very common molluscan species, they characterize five assemblages, from oldest to youngest: 1) the Oligocene Panopea sierrana-Parinomya patagonensis Assemblage; 2) the Late Oligocene–Early Miocene Jorgechlamys centralis–Reticulochlamys borjasensis Assemblage; 3) the Early Miocene Reticulochlamys zinsmeisteri–Struthiolarella patagoniensis–Pleuromeris cruzensis Assemblage; 4) the Early Miocene Pseudoportlandia glabra–Antimelatoma quemadensis Assemblage; and 5) the latest Early M
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Baskin, Jon, Edwin Dickinson, John DuBois, Henry Galiano, and Adam Hartstone-Rose. "?Amphictis (Carnivora, Ailuridae) from the Belgrade Formation of North Carolina, USA." PeerJ 8 (July 8, 2020): e9284. http://dx.doi.org/10.7717/peerj.9284.

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Miocene terrestrial mammals are poorly known from the Atlantic Coastal Plain. Fossils of the Order Carnivora from this time and region are especially rare. We describe a carnivoran mandible with a p4 from the late Oligocene or early early Miocene Belgrade Formation in Jones County, North Carolina. Comparisons are made with carnivoran jaws with similar premolar and molar lengths from the late Oligocene and Miocene of North America and Eurasia. These indicate that the North Carolina jaw is assignable to the Ailuridae, a family whose only living member is the red panda. The jaw is tentatively ref
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Ladant, J. B., Y. Donnadieu, and C. Dumas. "Links between CO<sub>2</sub>, glaciation and water flow: reconciling the Cenozoic history of the Antarctic Circumpolar Current." Climate of the Past Discussions 10, no. 3 (2014): 2397–416. http://dx.doi.org/10.5194/cpd-10-2397-2014.

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Abstract. The timing of the onset of the Antarctic Circumpolar Current (ACC) is a crucial event of the Cenozoic because of its cooling and isolating effect over Antarctica. It is intimately related to the glaciations occurring throughout the Cenozoic from the Eocene–Oligocene (EO) transition (≈34 Ma) to the middle Miocene glaciations (≈13.9 Ma). However, the exact timing of the onset remains debated with evidence for a late Eocene set up contradicting others data pointing to an occurrence closer to the Oligocene–Miocene (OM) boundary. In this study, we show the potential impact of the Antarcti
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Archer, M., R. Arena, M. Bassarova, et al. "The Evolutionary History and Diversity of Australian Mammals." Australian Mammalogy 21, no. 1 (1999): 1. http://dx.doi.org/10.1071/am99001.

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Palaeodiversity and relationships of all groups of Australian mammals are reviewed. The fossil record spanning this time is of variable quality. &amp;apos;Dark Ages&amp;apos; about which nothing is known in terms of Australian mammal evolution include the late Triassic to late Jurassic, late Cretaceous to late Paleocene and middle Eocene to middle Oligocene. Very little is known about the early Cretaceous and late Miocene. The late Oligocene to middle Miocene record documents the highest levels of biodiversity known for the continent, comparable to that which characterises the lowland rainfore
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Pashko, Pandeli. "Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin." Bulletin of the Geological Society of Greece 52, no. 1 (2018): 1. http://dx.doi.org/10.12681/bgsg.15837.

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The Morava Mountain Oligocene-Middle Miocene molasse deposits take part in the Albanian-Thessalian Basin, which developed NW-SE from eastern Albania to Thessaly in Greece, where it is called as Mesohellenic Basin. The 4.5 km thick basin infill is subdivided into three molasse cycles separated by two regional unconformities at the Eocene/Oligocene and Aquitanian/Burdigalian boundaries. The Morava Mountain Oligocene-Middle Miocene molase, ~ 3500 m thick, represents an exposed continuous, rich in fossil fauna succession. Six stratigraphic sections were studied and measured.
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Johnson, Kenneth G. "Middle Miocene recovery of Caribbean reef corals: New data from the Tamana Formation, Trinidad." Journal of Paleontology 75, no. 3 (2001): 513–26. http://dx.doi.org/10.1017/s0022336000039639.

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Caribbean coral reef communities were restructured by episodes of accelerated biotic change during the late Oligocene/early Miocene and the late Pliocene/early Pleistocene. However, rigorous description of the effects of rapid biotic change is problematic because preservation and exposure of coral-bearing deposits is not consistent in all stratigraphic intervals. In the Caribbean, early and middle Miocene exposures are more rare than late Miocene and Pliocene exposures. One exception is the late early to early middle Miocene Tamana Formation of Trinidad, and old and new collections from this u
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Ladant, J. B., Y. Donnadieu, and C. Dumas. "Links between CO<sub>2</sub>, glaciation and water flow: reconciling the Cenozoic history of the Antarctic Circumpolar Current." Climate of the Past 10, no. 6 (2014): 1957–66. http://dx.doi.org/10.5194/cp-10-1957-2014.

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Abstract. The timing of the onset of the Antarctic Circumpolar Current (ACC) is a crucial event of the Cenozoic because of its cooling and isolating effect over Antarctica. It is intimately related to the glaciations occurring throughout the Cenozoic from the Eocene–Oligocene (EO) transition (&amp;amp;approx; 34 Ma) to the middle Miocene glaciations (&amp;amp;approx; 13.9 Ma). However, the exact timing of the onset remains debated, with evidence for a late Eocene setup contradicting other data pointing to an occurrence closer to the Oligocene–Miocene (OM) boundary. In this study, we show the p
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Shackleton, N. J., S. J. Crowhurst, G. P. Weedon, and J. Laskar. "Astronomical calibration of Oligocene--Miocene time." Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences 357, no. 1757 (1999): 1907–29. http://dx.doi.org/10.1098/rsta.1999.0407.

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Wallace, M. W., E. Condilis, A. Powell, et al. "GEOLOGICAL CONTROLS ON SONIC VELOCITY IN THE CENOZOIC CARBONATES OF THE NORTHERN CARNARVON BASIN, NORTH WEST SHELF, WESTERN AUSTRALIA." APPEA Journal 43, no. 1 (2003): 385. http://dx.doi.org/10.1071/aj02020.

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The Cenozoic carbonates of the Bounty-Talisman region can be divided into five major facies. From oldest to youngest, these are: Paleocene to Eocene basinal facies, Oligocene to Miocene slope-canyon facies, Oligocene to Miocene shelf facies, Oligocene to Miocene near-shore facies, and Pliocene-Quaternary shelf facies. This represents a shallowing-upwards cycle up to the late Miocene, followed by a significant transgression and a return to more open marine conditions in the Pliocene- Quaternary. The dominant geological processes controlling sonic velocity in the Cenozoic carbonates are physical
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de Santana dos Anjos Zerfass, Geise, Dmitry A. Ruban, Farid Chemale Jr., and Henrique Zerfass. "Cenozoic synthem stratigraphic architecture of the SE Brazilian shelf and its global eustatic context: evidence from the Pelotas Basin (offshore Brazil)." Geologos 19, no. 4 (2013): 273–90. http://dx.doi.org/10.2478/logos-2013-0018.

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Abstract The Pelotas Basin, located on the SE Brazilian shelf, has evolved since the Aptian. Stratigraphical data from the basin can be used for delineation of the unconformity-bounded units (synthems) on the shelf, which is a first step towards a full understanding of its stratigraphic architecture, evolution, and hydrocarbon potential. Hiatuses in the Cenozoic succession of the Pelotas Basin are established with both biostratigraphic (planktonic foraminifers and calcareous nannofossils) and isotopic (87Sr/86Sr) data. The seven recognised hiatuses are dated respectively as (1) Palaeocene (Dan
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Dissertations / Theses on the topic "Oligocene-Miocene"

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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.

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Smith, Richard Edward. "The Oligocene-Miocene Transition : new insights from the Newfoundland Margin." Thesis, University of Southampton, 2017. https://eprints.soton.ac.uk/421152/.

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As a major site of deep water formation, the North Atlantic plays a critical role in global climate. To understand better how Earth’s climate system works it should therefore be a priority for geologists to study the record of past climate change encoded in the sedimentary archives that accumulate in the deep Atlantic. Here, sediment drilled in several cores on the Newfoundland Margin by International Ocean Discovery Program (IODP) Expedition 342 is utilized to provide fresh insights into palaeoclimate history, focusing on one of the more enigmatic events of the Cenozoic: the Oligocene-Miocene
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Zahid, Khandaker Uddin Ashraf. "Provenance and basin tectonics of Oligocene-Miocene sequences of the Bengal Basin, Bangladesh." Auburn, Ala., 2005. http://repo.lib.auburn.edu/2005%20Fall/Thesis/ZAHID_KHANDAKER_14.pdf.

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Irvine, Janelle Rose Mae. "Sedimentology, stratigraphy and palaeogeography of Oligocene to Miocene rocks of North Canterbury-Marlborough." Thesis, University of Canterbury. Geological Sciences, 2012. http://hdl.handle.net/10092/6826.

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The Cenozoic was a time of climatic, tectonic and eustatic change in the Southern Hemisphere. Cooling at the pole, glaciation and substantial sea ice formation occurred as latitudinal temperature gradients increased and tectonics altered Southern Hemisphere circulation patterns. During this same time frame, the tectonic regime of the New Zealand continental block transitioned from a passive margin to an active plate boundary, resulting in the reversal of a long-standing transgression and an influx of terrigenous sediment to marine basins. In this transition, depositional basins in the South Is
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Ngah, Khalid Bin. "Deposition and diagenesis of Oligocene-Lower Miocene sandstones in the southern Malay Basin." Thesis, Imperial College London, 1990. http://hdl.handle.net/10044/1/46470.

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Hayes, Frederick Glynn. "Paleomagnetics and biostratigraphy of the Pine Ridge Arikaree Group (late Oligocene-early Miocene), Nebraska." [Lincoln, Neb. : University of Nebraska-Lincoln], 2004. http://www.unl.edu/libr/Dissertations/2004/HayesDis.pdf.

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Ramli, N. "Oligocene and Miocene sedimentology in the southeastern part of the Malay Basin, offshore west Malaysia." Thesis, University of Oxford, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.376944.

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Kender, Sev. "Foraminiferal characterisation and taxonomy of Oligocene-Miocene Congo Fan deep sea sub-environments, offshore Angola." Thesis, University College London (University of London), 2007. http://discovery.ucl.ac.uk/1444769/.

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The Congo Fan has been accumulating sediment since the mid-Oligocene, and is of particular interest to the oil industry due to abundant large reservoirs contained within the meandering sandy palaeochannels from largely Miocene and Oligocene deposits. The high sedimentation rates and rich benthic foraminiferal faunas also provide an interesting record of Miocene and Oligocene palaeoceanographic change in the southeast Atlantic, a stratigraphic time interval that has had no recovery from proximal ODP and DSDP Sites. Three oil wells spanning the Upper Oligocene to Middle Miocene from the distal p
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Ghafur, Ala. "Sedimentology and reservoir characteristics of the oligocene-early miocene carbonates (Kirkuk group) of southern Kurdistan." Thesis, Cardiff University, 2012. http://orca.cf.ac.uk/43598/.

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Kirkuk Group Formations (in addition to Avanah and Jaddala Formations) of southern Kurdistan were studied in order to determine biostratigraphy, chronostratigraphy and sequence stratigraphic relationships, in addition to major sediment producing environments and type of platform configuration. As well as to determine the paragenetic sequences with special attention to micrite diagenesis and its effect on microporosity. Five biozones were identified in the study area in which two of them from Middle- Late Eocene: Alveolina biozone (AL) and Discocyclina biozone (DI) with three biozones from the
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Stewart, Joseph A. "Variation in silicate weathering across the Oligocene-Miocene boundary : evidence from lithium and neodymium isotopes." Thesis, University of Southampton, 2012. https://eprints.soton.ac.uk/351811/.

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Books on the topic "Oligocene-Miocene"

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Piller, Werner E., Fritz F. Steininger, and Fred Rögl. Oligocene/Miocene transitions in the eastern Mediterranean. Schweizerbart'sche Verlagsbuchhandlung, 2004.

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Mutti, M., Werner E. Piller, and Christian Betzler. Carbonate systems during the Oligocene-Miocene climatic transition. Blackwell Pub., 2010.

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Mutti, Maria, Werner Piller, and Christian Betzler, eds. Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.

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Rasmussen, Erik Skovbjerg. Lithostratigraphy of the Upper Oligocene-Miocene succession of Denmark. Geological Survey of Denmark and Greenland, Ministry of Climate and Energy, 2010.

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Holmes, Thom. The age of mammals: The Oligocene and Miocene epochs. Chelsea House, 2009.

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Szyndlar, Zbigniew. Non-ercine Booidea from the Oligocene and Miocene of Europe. Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, 2003.

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Weems, R. E. Geology of Oligocene, Miocene, and younger deposits in the coastal area of Georgia. Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 2001.

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Foronda, V. Joseph. Sequence stratigraphy of an Oligocene-Miocene mixed siliciclastic-carbonate system, Visayan Basin, central Cebu (Philippines). Holos, 1994.

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Schröder-Adams, C. J. Oligocene to Miocene agglutinated foraminifers in deltaic and deep-water facies of the Beaufort-Mackenzie Basin. Geological Survey of Canada, 1994.

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Bray, E. A. Du. Geochemistry and petrology of Oligocene and Miocene ash-flow tuffs of the southeastern Great Basin, Nevada. U.S. G.P.O., 1995.

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Book chapters on the topic "Oligocene-Miocene"

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Billups, Katharina, and Kathleen Scheiderich. "A Synthesis of Late Oligocene through Miocene Deep Sea Temperatures as Inferred from Foraminiferal Mg/Ca Ratios." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch1.

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Braga, Juan C., Davide Bassi, and Werner E. Piller. "Palaeoenvironmental Significance of Oligocene-Miocene Coralline Red Algae - a Review." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch10.

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Harzhauser, Mathias, and Werner E. Piller. "Molluscs as a Major Part of Subtropical Shallow-Water Carbonate Production - an Example from a Middle Miocene Oolite Shoal (Upper Serravallian, Austria)." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch11.

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Kroh, Andreas, and James H. Nebelsick. "Echinoderms and Oligo-Miocene Carbonate Systems: Potential Applications in Sedimentology and Environmental Reconstruction." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch12.

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Bosellini, Francesca R., and Christine Perrin. "Coral Diversity and Temperature: a Palaeoclimatic Perspective for the Oligo-Miocene of the Mediterranean Region." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch13.

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Iryu, Y., S. Inagaki, Y. Suzuki, and K. Yamamoto. "Late Oligocene to Miocene Reef Formation on Kita-Daito-Jima, Northern Philippine Sea." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch14.

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Vigorito, Mario, Marco Murru, and Lucia Simone. "Carbonate Production in Rift Basins: Models for Platform Inception, Growth and Dismantling, and for Shelf to Basin Sediment Transport, Miocene Sardinia Rift Basin, Italy." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch15.

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Perrin, Christine, and Wolfgang Kiessling. "Latitudinal Trends in Cenozoic Reef Patterns and their Relationship to Climate." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch2.

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Kindler, Pascal, and Moyra E. J. Wilson. "Carbonate Grain Associations: their Use and Environmental Significance, a Brief Review." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch3.

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Martín, José M., Juan C. Braga, Isabel M. Sánchez-Almazo, and Julio Aguirre. "Temperate and Tropical Carbonatesedimentation Episodes in the Neogene Betic Basins (Southern Spain) Linked to cLimatic Oscillations and Changes in Atlantic-Mediterranean Connections: Constraints from Isotopic Data." In Carbonate Systems during the Oligocene-Miocene Climatic Transition. Wiley-Blackwell, 2012. http://dx.doi.org/10.1002/9781118398364.ch4.

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Conference papers on the topic "Oligocene-Miocene"

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Beasley, Charlotte, Kate Littler, Sev Kender, et al. "The Oligocene–Miocene Transition in the Tropical Low Latitudes." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.151.

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Ismaylova, G. H. "Reservoir Rock Properties of the Oligocene-Miocene Sediments in the SCB." In 76th EAGE Conference and Exhibition 2014. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20141646.

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Posamentier, Henry W., and Priscilla Laurin. "Seismic geomorphology of oligocene to miocene carbonate buildups offshore Madura, Indonesia." In SEG Technical Program Expanded Abstracts 2005. Society of Exploration Geophysicists, 2005. http://dx.doi.org/10.1190/1.2142233.

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Kudryashov, A., V. Kerimov, and N. Yandarbiev. "Shale Strata of The Azov-Kuban Oligocene-Miocene Generation-Accumulation Hydrocarbon System." In EAGE/SPE Workshop on Shale Science 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202151012.

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Kosyanov, V. A., V. Y. Kerimov, D. D. Ismailov, R. N. Mustaev, and A. O. Koval. "Assessment of the Generation Potential of the Oligocene-Miocene Deposits of the Caucasus." In Third International Conference on Geology of the Caspian Sea and Adjacent Areas. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201952011.

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Brink, G., J. Hernandez, J. Bencomo, et al. "OLIGOCENE AND MIOCENE SEQUENCE STRATIGRAPHY OF THE NORTH MALAY BASIN, MALAYSIA AND THAILAND." In APGCE 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201903363.

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S. Jeddi, R., and H. B. Kilani. "Hydrocarbon Potential of Oligocene Miocene Reservoirs in the Gulf of Hammamet Basins, Tunisia." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406059.

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Green, Donald, Keith Seanard, and Anthony Neil Martin. "Hydraulic Fracturing of Miocene and Oligocene Sandstones in the Taranaki Basin, New Zealand." In SPE Asia Pacific Oil & Gas Conference and Exhibition. Society of Petroleum Engineers, 2006. http://dx.doi.org/10.2118/101121-ms.

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Nana Yobo, Lucien, and Juan Carlos Silva-Tamayo. "REGIONAL EFFECT ON OLIGOCENE-MIOCENE SHALLOW MARINE CARBONATE ALONG THE SE CIRCUM - CARIBBEAN." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287340.

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Grabowski, George J., Po C. Tai, Chengjie Liu, and Augustus O. Wilson. "Upper Oligocene-Lower Miocene Carbonate and Evaporite Depositional Systems of the Northern Arabian Plate." In International Petroleum Technology Conference. International Petroleum Technology Conference, 2014. http://dx.doi.org/10.2523/iptc-17531-ms.

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Reports on the topic "Oligocene-Miocene"

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Schröder-Adams, C. J., and D. H. McNeil. Oligocene to Miocene agglutinated foraminifers in deltaic and deep-water facies of the Beaufort-Mackenzie Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/195162.

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LePain, D. L., R. B. Blodgett, and J. G. Clough. Sedimentology and hydrocarbon source rock potential of Miocene-Oligocene strata, McGrath Quadrangle: An outcrop analog for the Holitna Basin. Alaska Division of Geological & Geophysical Surveys, 2003. http://dx.doi.org/10.14509/2870.

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Schroder-Adams, C. J., and D. H. McNeil. Biostratigraphic Distribution of Agglutinated Foraminifera in Oligocene and Miocene Shallow To Deep Water Facies of the Beaufort-Mackenzie Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128195.

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Geologic map of Oligocene and Miocene volcanic rocks, Paradise Peak and western part of the Ione quadrangles, Nye County, Nevada. US Geological Survey, 1988. http://dx.doi.org/10.3133/mf2025.

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Stratigraphy, regional distribution, and reconnaissance geochemistry of Oligocene and Miocene volcanic rocks in the Paradise Range and northern Pactolus hills, Nye County, Nevada. US Geological Survey, 1992. http://dx.doi.org/10.3133/b1974.

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Map showing Late Eocene erosion surface, Oligocene-Miocene paleovalleys, and Tertiary deposits in the Pueblo, Denver, and Greeley 1 degree by 2 degrees quadrangles, Colorado. US Geological Survey, 1986. http://dx.doi.org/10.3133/i1626.

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Properties and chemical constituents in ground water from the permeable zone E (lower Miocene-upper Oligocene deposits), coastal lowlands aquifer system, south-central United States. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri924103.

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Structure contour map of the top of the Oligocene to Middle Miocene Temblor Formation in the Kettleman Hills and Lost Hills areas, Fresno, Kings, and Kern counties, California. US Geological Survey, 1987. http://dx.doi.org/10.3133/mf1896.

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Paleogeography of the western Transverse Range province, California; new evidence from the late Oligocene and early Miocene Vaqueros Formation; Stratigraphy of the fine-grained facies of the Sisquoc Formation, Santa Maria Basin, California; paleoceanographic and tectonic implications; The Sisquoc Formation-Foxen Mudstone boundary in the Santa Maria Basin, California; sedimentary response to the new tectonic regime. US Geological Survey, 1998. http://dx.doi.org/10.3133/b1995tuv.

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