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Relevant bibliographies by topics / Eocene

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Academic literature on the topic 'Eocene'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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Journal articles on the topic "Eocene"

1

Айрапетян, Ф. А. "ЗОНАЛЬНОЕ ДЕЛЕНИЕ ЭОЦЕНОВЫХ ОТЛОЖЕНИЙ ПО МЕЛКИМ ФОРАМИНИФЕРАМ ПО МАТЕРИАЛАМ ИЗ СКВАЖИНЫ «ЛАНДЖАР-2»". Proceedings of the YSU C: Geological and Geographical Sciences 43, № 2 (219) (2009): 28–36. http://dx.doi.org/10.46991/pysu:c/2009.43.2.028.

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The present study is focused on the zonal distribution of Eocene deposits from the borehole materials of «Langjar 2» (South-East Armenia). Studying the area and analyzing 35 plankton Foraminifera species several zones have been revealed. Morozovella aragonesis and Acarinina pentacamerata (Lower Eocene), Acarinina bullbrooki, Ac. rotundimarginata, Hantkenina alabamensis, Orb. beckmanii and Truncorotaloides rohri (Middle Eocene), Globigerapsis semiinvoluta and Globorotalia cocoaensis (Upper Eocene). By benthonic Foraminifera the following zones have been revealed: Heterolepa eocaena, Uvigerina c

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Hou, Lianhai, and Per G. P. Ericson. "A Middle Eocene Shorebird from China." Condor 104, no. 4 (2002): 896–99. http://dx.doi.org/10.1093/condor/104.4.896.

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Abstract We describe a new species of shorebird, tentatively referred to the family Charadriidae, from the Huadian Formation (Middle Eocene) in Jilin Province, China. In general morphology the specimen closely matches that of an extant charadriid, and corresponds in size to the Killdeer (Charadrius vociferus). If correctly identified this is the oldest record of the Charadriidae. The Middle Eocene paleoenvironment of the Huadian region is thought to have resembled a subtropical swamp. Un Ave Playera de China del Eoceno Medio Resumen. Describimos una nueva especie de ave playera, tentativamente

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Trubin, Y. S. "Family Naticidae of the Tavda formation (Eocene, Western Siberia)." Ruthenica, Russian Malacological Journal 28, no. 1 (2018): 11–17. http://dx.doi.org/10.35885/10.35885/ruthenica.2018.28(1).2.

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The present work is one of several planned articles on updating information on the biodiversity of malacofauna and palaeogeography of the Middle-Late Eocen Tavda Sea, which existed in the Western Siberia. Paper contains data on fossil species diversity of the family Naticidae of the Middle and Late Eocene West Siberian Sea and on drill holes. The drill holes indicate predator activity, prey of Naticidae and influence of abiotic factors on their behavior. Previously the invertebrate macroauna of the Eocene of Western Siberia was not studied. As a result, the biodiversity, paleogeography and pal

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Strougo, Amin. "The Middle Eocene/Upper Eocene transition in Egypt reconsidered." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 186, no. 1-2 (1992): 71–89. http://dx.doi.org/10.1127/njgpa/186/1992/71.

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Lygina, E. A., N. V. Pravikova, E. R. Chizhova, et al. "Eocene seismicity and paleogeography of the Central Crimea." Moscow University Bulletin. Series 4. Geology, no. 5 (December 17, 2022): 68–77. http://dx.doi.org/10.33623/0579-9406-2022-5-68-77.

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The article considers the results of a comprehensive study of the Cretaceous-Eocene deposits of the Central Crimea (Ak-Kaya mount.). The temperature and salinity of the formation of Maastrichtian and Eocene rocks have been determined, and a correlation has been made with the global climatic event EЕСO (Early Eocene Climate Optimum). The synchronicity of the formation of steep submeridional fractures and the basal horizon of the Eocene has been proved. Three major stages of deformation have been identified: pre-Eocene, Eocene, and post-Eocene. It is shown that the Eocene stage corresponds to th

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Averianov, Alexander O. "Paleogene Sea Snakes from the Eastern Part of Tethys." Russian Journal of Herpetology 4, no. 2 (2011): 128–42. http://dx.doi.org/10.30906/1026-2296-1997-4-2-128-142.

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Nessovophis tamdy gen. et sp. nov. (Nigerophiidae, middle Eocene, Bartonian), Nessovophis zhylga sp. nov. (early Eocene, Ypresian), Palaeophis ferganicus sp. nov. (early Eocene, Ypresian), Palaeophis udovichenkoi sp. nov. (middle – ?late Eocene, Bartonian – ?Priabonian), Palaeophis nessovi sp. nov. (late Eocene, Priabonian), Palaeophis sp. (middle Eocene, Bartonian), and Pterosphenus muruntau sp. nov. (middle Eocene, Bartonian) are described and Vialovophis zhylan Nessov, 1984 (?latest Paleocene) is redescribed on the basis of 45 isolated vertebrae from 8 localities in Kazakhstan, Tajikistan,

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Liliegraven, J. A. "Eocene Revelations." Science 264, no. 5161 (1994): 1004–5. http://dx.doi.org/10.1126/science.264.5161.1004.

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Huber, Matthew, and Aaron Goldner. "Eocene monsoons." Journal of Asian Earth Sciences 44 (January 2012): 3–23. http://dx.doi.org/10.1016/j.jseaes.2011.09.014.

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Browning, James V., Kenneth G. Miller, W. John Schmelz, and Peter J. Sugarman. "Eocene sequences and forward modeling of the New Jersey coastal plain, U.S.A.: changing depositional styles in response to climate and sea level." Journal of Sedimentary Research 95, no. 2 (2025): 383–404. https://doi.org/10.2110/jsr.2024.069.

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ABSTRACT We map the spatial and temporal distribution and depositional environments of Eocene sequences and formations in the New Jersey Coastal Plain, USA, using an array of coreholes and gamma logs. On this passive margin, Eocene depositional systems reflect a change from prograding earliest Eocene mud lobes, to early to middle Eocene hemipelagic ramp, and finally to late middle Eocene prograding sandy sequences. The Marlboro Clay, containing the Paleocene–Eocene Thermal Maximum (PETM), was deposited as prograding fluid mud during times of high global temperatures; it is found in northern an

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Aubry, Marie-Pierre, and Rehab Salem. "The Dababiya Quarry Core: Coccolith biostratigraphy." Stratigraphy 9, no. 3-4 (2012): 241–59. http://dx.doi.org/10.29041/strat.09.3.08.

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We establish the coccolith stratigraphy of the Maastrichtian through lower Eocene section recovered from the Dababiya Core taken ~200 m from the GSSP for the Paleocene/Eocene boundary, and correlate coccolith biozones with lithostratigraphic units in the core. The section extends from Maestrichtian Subzone CC25a to lowermost Eocene Subzone NP9c. The composite Paleocene-lower Eocene Dababiya section recovered in the core and accessible in outcrop in the DababiyaQuarry exhibits an unexpected contrast in thickness between the Lower Eocene succession (~Esna Shales) and the Paleocene one (~Dakhla S

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Dissertations / Theses on the topic "Eocene"

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Williams, David J. "The provenance of middle Eocene to late Eocene sands, Willunga Embayment, South Australia /." Title page, table of contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bw722.pdf.

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Rivero, Cuesta Lucía. "Response of Phytoplankton to Climatic Changes during the Eocene-Oligocene Transition at the North Atlantic ODP Site 612." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-256769.

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The development of modern glacial climates occurred during the Eocene-Oligocene transition (34 to 35.5 Ma) when a decrease of atmospheric CO2 led to a global temperature fall. The ocean was deeply affected, both in the surface and the deep-sea, suffering a strong reorganization including currents and phytoplankton distribution. Spanning that time, 35 samples from the North Atlantic Ocean Drilling Program Site 612 have been analyzed by counting coccoliths abundance in different size groups (< 4 µm, 4 to 8 µm and > 8 µm) and silica fragments abundance. Absolute coccoliths abundance were es

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Kordesch, Wendy E. C. "Middle Eocene greenhouse climate instability." Thesis, University of Southampton, 2016. https://eprints.soton.ac.uk/402327/.

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Understanding warm climate states is increasingly important as projections of anthropogenic climate change indicate atmospheric carbon dioxide concentrations in the coming century not previously seen on Earth for tens of millions of years. The Eocene (~56-34 Ma) is a critical period in the long-term Cenozoic climate evolution, encompassing the transition from widespread greenhouse warmth and high atmospheric carbon dioxide levels pervasive during the early Eocene to an icehouse world with major Antarctic ice sheets and cooler temperatures. Increasingly, it has become apparent that global clima

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Murray, Alison M. "The Eocene cichlids (Perciformes:Labroidei) of Mahenge, Tanzania /." Thesis, McGill University, 2000. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=37794.

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A new genus and five new species of fossil cichlid fishes (Perciformes: Labroidei) are described from Mahenge, Tanzania. These cichlids represent the oldest confirmed fossils of the family, dating from the middle of the Eocene. The specimens share many lepidological characters, and, from comparison with other members of the family, are identified as being a monophyletic group. Therefore, they are described as belonging to a single genus, Mahengechromis gen. nov., named for the type locality. Detailed anatomical study of the well-preserved specimens allows five species to be identified, M. plet

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Adams, D. P. M. "Cretaceous and Eocene geology of South Westland." Thesis, University of Canterbury. Geology, 1987. http://hdl.handle.net/10092/7117.

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The Cretaceous and Eocene sequence of South Westland crops out within a 6km wide coastal area from Ship Creek to the Mahitahi River. The oldest unit, the Otumotu Formation (Motuan-Arowhanan), lies with angular unconformity on the Paleozoic Greenland Group. It is divided into two members, an older Tauweritiki Member (new) overlain by the Topsy Member. Both are entirely clastic but the lower unit is significantly coarser ranging from boulder conglomerate to mudstone, while granule conglomerate, sandstone analysis of sedimentary features to pebble breccia and the upper member comprises and mudst

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Coxall, Helen Katherine. "Hantkeninid planktonic foraminifera and Eocene palaeoceanographic change." Thesis, University of Bristol, 2000. http://hdl.handle.net/1983/8efa1d22-0ff8-45a3-9a5c-bd5ea90e266f.

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The morphological and ecologicalevolution of middle-upper Eocene planktonic foraminiferal family Hantkeninidae is investigated in the context of the dramatic palaeoceanographic and climatic changes that marked the transition from Paleogene "greenhouse" to Neogene "icehouse" climatic conditions. Morphometric analysis proves that evolution in family Hantkeninidae was gradual but complex in detail with periods of relative stasis. Multiple lines of evidence demonstrate that Hantkenina evolved from planispiral clavate genus Clavigerinella and not, as was previously believed, from Pseudohastigerina

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Baky, Alaaeldin Mohamed Abdel. "Maastrichtian to early Eocene calcareous nannofossils from Egypt." Thesis, University College London (University of London), 1988. http://discovery.ucl.ac.uk/1317747/.

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A study of calcareous nannofossils from the Maastrichtian-Early Eocene from Egypt has resulted in the recognition of four Maastrichtian and seven Early Tertiary biostratigraphic zones. These nannoplankton zones are based upon local ranges and compared with the zones proposed by Martini (1971), Sissingh (1977), Verbeek (1977) and Romein (1979). A new zone, the Fasciculithus ragaae Zone is described and the E1lipsolithus macellus Zone and the Fasciculithus tympaniformis Zone are emended. Study of the vertical ranges of the species provided many markers (including the zonal markers) with distinct

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Sexton, Philip. "Foraminiferal taphonomy, palaeoecology and palaeoceanography of the Eocene." Thesis, University of Southampton, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.416473.

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Sahy, Claudia Diana. "Geochronology and chronostratigraphy of the Eocene-Oligocene transition." Thesis, University of Leicester, 2014. http://hdl.handle.net/2381/28952.

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This thesis integrates high-precision (<0.2%, 2σ) [superscript 206]Pb/[superscript 238]U dating of zircons from volcanic tuffs intercalated in key Late Eocene-Oligocene marine and terrestrial sedimentary successions, with high-resolution biostratigraphic and magnetostratigraphic data sets in order to critically examine the accuracy and precision of the numerical age calibration of the Eocene – Oligocene transition (EOT). Weighted mean [superscript 206]Pb/[superscript 238]U ages from the Italian Umbria-Marche and North American White River Group (WRG) sedimentary successions are 0.4-1.0 Myr you

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Cameron, Adele Jane. "Ocean circulation during Eocene extreme "greenhouse" climatic warmth." Thesis, Open University, 2016. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.699820.

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The Early Eocene (47-56 Ma) 'greenhouse' climate represented the warmest climatic conditions witnessed in the last 90 million years, with peak Eocene warmth (the Early Eocene Climatic optimum, EECO) occurring around 50-52 Ma (Sexton et al. 2006; Bijl et al. 2009; Zachos et al. 2008; Littler et al. 2014) with subsequent global cooling thereafter (Sexton et al. 2006; Zachos et al. 2008). Ocean circulation plays a critical role in redistributing thermal energy across the planet and providing ventilation to the deepest parts of the ocean. Understanding how it may have operated in a globally warm w

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Books on the topic "Eocene"

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Gunnell, Gregg F., ed. Eocene Biodiversity. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1271-4.

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Charles, Pomerol, Premoli-Silva I, and International Geological Correlation Programme. Project no. 174 on "Geological Events at the Eocene-Oligocene Boundary.", eds. Terminal Eocene events. Elsevier, 1986.

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Zágoršek, Kamil. Eocene bryozoa from Hungary. Senckenbirgische Naturforschende Gesellschaft, 2001.

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R, Prothero Donald, and Berggren William A, eds. Eocene-Oligocene climatic and biotic evolution. Princeton University Press, 1992.

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Bassiouni, M. A. A. Middle Eocene Ostracoda from northern Somalia. Senckenbergische Naturforschende Gesellschaft, 1996.

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6

Kacharava, M. V. Geologicheskie sobytii͡a︡ na granit͡s︡e ėot͡s︡ena i oligot͡s︡ena Gruzii. "Met͡n︡iereba", 1991.

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1957-, Bestland Erick A., and Fremd Theodore J. 1952-, eds. Eocene and Oligocene paleosols of central Oregon. Geological Society of America, 1999.

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8

Rose, Kenneth David. Earliest Eocene mammalian fauna from the Paleocene-Eocene Thermal Maximum at Sand Creek Divide, southern Bighorn Basin, Wyoming. Museum of Paleontology, University of Michigan, 2012.

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Thewissen, J. G. M. Ambulocetus natans, an Eocene cetacean (Mammalia) from Pakistan. Senckenbergische Naturforschende Gesellschaft, 1996.

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Axelrod, Daniel I. The Eocene Thunder Mountain flora of central Idaho. University of California Press, 1998.

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Book chapters on the topic "Eocene"

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Shaltami, Osama Rahil, Fares F. Fares, Hwedi Errishi, and Farag M. EL Oshebi. "Eocene Deposits." In Isotope Geochronology of the Exposed Rocks in the Cyrenaica Basin, NE Libya. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-63010-2_3.

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Rull, Valentí. "Eocene Origin." In Ecological Studies. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-57612-6_3.

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Kellhammer, Oliver. "Neo-Eocene." In Making the Geologic Now. punctum books, 2012. https://doi.org/10.21983/p3.0014.1.35.

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Back in the mid-1960s, I was a feral sort of a child who loved scampering around construc-tion sites, climbing the huge, grey piles of excavated shale that were popping up all over my rapidly developing Toronto suburb. I might have been six or so when I first really noticed the slabs of muddy smelling rock often contained the imprints of scallop shells, snails, and fragments of coral, things I recognized from picture books but hadn’t yet seen in real life as we lived hundreds of miles from the near-est ocean. Yet 450 million years before, during the Ordovician era, where I was playing would ha

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Oberhänsli, Hedi, and Kenneth J. Hsü. "Paleocene - Eocene Paleoceanography." In Mesozoic and Cenozoic Oceans. American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd015p0085.

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Corliss, Bruce H., and Lloyd D. Keigwin. "Eocene-Oligocene paleoceanography." In Mesozoic and Cenozoic Oceans. American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd015p0101.

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Long, Douglas J. "Paleoecology of Eocene Antarctic sharks." In The Antarctic Paleoenvironment: A Perspective on Global Change: Part One. American Geophysical Union, 1992. http://dx.doi.org/10.1029/ar056p0131.

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Simons, Elwyn L., D. Tab Rasmussen, Thomas M. Bown, and Prithijit S. Chatrath. "The Eocene Origin of Anthropoid Primates." In Anthropoid Origins. Springer US, 1994. http://dx.doi.org/10.1007/978-1-4757-9197-6_8.

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Gebo, Daniel L., Elwyn L. Simons, D. Tab Rasmussen, and Marian Dagosto. "Eocene Anthropoid Postcrania from the Eayum, Egypt." In Anthropoid Origins. Springer US, 1994. http://dx.doi.org/10.1007/978-1-4757-9197-6_9.

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Uhen, Mark D. "Middle to Late Eocene Basilosaurines and Dorudontines." In The Emergence of Whales. Springer US, 1998. http://dx.doi.org/10.1007/978-1-4899-0159-0_2.

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Hardyman, Richard F. "Eocene magmatism, Challis volcanic field, central Idaho." In Cordilleran Volcanism, Plutonism, and Magma Generation at Various Crustal Levels, Montana and Idaho Western Montana and Central Idaho. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft337p0032.

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Conference papers on the topic "Eocene"

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Wade, Bridget S., James O'Neill, Chawisa Phujareanchaiwon, Imran Ali, Mitchell Lyle, and Jakub Witkowski. "DEEP-SEA SEDIMENT EVOLUTION ACROSS THE PALEOCENE-EOCENE AND EOCENE-OLIGOCENE BOUNDARIES." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357116.

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Yunus, F. A. M. "Palinspastic Reconstruction of X Block, Anggursi Sub-Basin." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-sg-135.

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North Anggursi Sub-basin is one of the sub-basins in the North West Java Basin, located on northern of North West Java Basin. North Anggursi Sub-basin regionally was a sinistral pull-apart basin with northeast-southwest orientation which the direction of the extension was east west at Eocene. This subbasin is a back-arc basin during the Eocene to Oligocene. The dynamics of the North Anggursi Sub-basin were analysed using the palinspastic reconstruction method using 2D seismic lines which have east-west direction and biostratigraphy data. This analysis was carried out to determine the tectonic

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Legalov, A. A. "COMPOSITION OF WEEVIL AMBER FAUNAS (CURCULIONOIDEA) IN THE EOCENE OF EUROPE." In V International Scientific Conference CONCEPTUAL AND APPLIED ASPECTS OF INVERTEBRATE SCIENTIFIC RESEARCH AND BIOLOGICAL EDUCATION. Tomsk State University Press, 2020. http://dx.doi.org/10.17223/978-5-94621-931-0-2020-22.

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The analysis of the structure of the weevil fauna from the Eocene amber of Europe is given. 143 species from eight families are discovered. The differences between the faunas of the early and the middle Eocene amber are shown.

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Guan, Dayong, Geng Qian, Junpei Yue, Wenjing Pan, and Weiyan Lu. "Influence of the Tan-Lu Strike-Slip Fault Zone on Depositional Facies Distribution within the Fault Terrace Zone of the Yellow River Estuary Depression, Southern Bohai Sea, Eastern China." In International Petroleum Technology Conference. IPTC, 2025. https://doi.org/10.2523/iptc-24880-ms.

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Abstract The Bohai area is China's largest offshore crude oil production base, with proven reserves of Paleogene clastic rocks accounting for less than 30%. This positions it as a crucial production field for the future. Currently, accurately predicting the spatial distribution of these Paleogene clastic rock reservoirs remains a significant challenge. Located in the southern Bohai Sea, the fault terrace zone of the Yellow River estuary depression is bounded by the Tan-Lu strike-slip fault zone, which traverses eastern China. Recent drilling has revealed considerable variations in the spatial

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Vanderlip, Christopher, and Randel T. Cox. "NEWLY IDENTIFIED EOCENE THRUST FAULT, TIPTON COUNTY, TN, AND IMPLICATIONS FOR EARLY-EOCENE STRESS FIELD." In 50th Annual GSA South-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016sc-273583.

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Ressel, Michael W. "EOCENE GOLD METALLOGENY OF NORTHERN NEVADA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281995.

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Sousa, Francis J. "EOCENE ORIGIN OF OWENS VALLEY, CALIFORNIA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-337792.

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Saraswati, Pratul Kumar, Sonal Khanolkar, D. S. N. Raju, and Santanu Banerjee. "An Updated Eocene Stratigraphy of Kutch." In Recent Studies on the Geology of Kachchh. Geological Society of India, 2016. http://dx.doi.org/10.17491/cgsi/2016/105406.

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Radwan, A., A. Kassem, A. Atef, A. Uchman, and R. Jach. "Contribution to the Eocene Sediments in Egypt: A New Formation Name for the Earlymiddle Eocene Sediment." In 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202011446.

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Lee, Keehwan, Lucien Nana Yobo, Franco Marcantonio, Howard Scher, and Michael Bizimis. "Spread of Ice Sheet during Late Eocene Event Before Major Ice Growth at the Eocene-Oligocene Transition." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.23449.

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Reports on the topic "Eocene"

1

Miller, P. E. Paleogeography, III, Labrador sea, Earliest early Eocene and middle Eocene Paleoenvironments. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127194.

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Dafoe, L. T., K. Dickie, G. L. Williams, and T. McCartney. Stratigraphy of the Labrador margin: a synthesis and new perspectives. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321829.

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The Labrador Sea formed during rifting between North America and Greenland beginning in the Early Cretaceous, with subsequent seafloor spreading from the Maastrichtian (chron C31) to Early Paleocene (chron C27n) that ended by chron C13 (earliest Oligocene). Early Cretaceous rifting resulted in accumulation of Alexis Formation basalt units and Bjarni Formation nonmarine and marginal marine clastic rocks. In the Late Cretaceous, extension focused further offshore as sag basin conditions formed across the shelf, with a basinwide transgression of Markland Formation shale and localized Freydis Memb

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Parrish, R. R., R. M. Friedman, and R. L. Armstrong. Part G: Eocene Extension Faults [Chapter 17: Structural Styles]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134121.

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Miller, P. E., and J. S. Bell. Paleogeography, IV, Labrador sea, Late Eocene and early Oligocene Paleoenvironments. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127195.

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Irving, E., and P. J. Wynne. The paleolatitude of the eocene fossil forests of Arctic Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131957.

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Bell, J. S., and P. N. Moir. Isopach / Net Sandstone, IV, Labrador sea, Kenamu formation [Early to late Eocene]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127191.

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Ross, G. M., J. Mariano, R. Dumont, B. Kjarsgaard, and D. Teskey. Eocene magmatism in southern Alberta: magnetic expression and implications for petroleum exploration. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209401.

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Villeneuve, M. E., and R. Mathewes. An Early Eocene age for the Quilchena fossil locality, southern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/221300.

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Byrnes, Mark. Provenance study of late Eocene arkosic sandstones in southwest and central Washington. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.5290.

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McClincy, Matthew. Tephrostratigraphy of the middle Eocene Chumstick Formation, Cascade Range, Douglas County, Washington. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.5501.

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