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Artykuły w czasopismach na temat „Palaeogene”

Autor: Grafiati

Data publikacji: 2 czerwca 2025

Data aktualizacji: 31 lipca 2025

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1

King, Adam R., and Malte C. Ebach. "A novel approach to time-slicing areas within biogeographic-area classifications: Wallacea as an example." Australian Systematic Botany 30, no. 6 (2017): 495. http://dx.doi.org/10.1071/sb17028.

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Time-slicing of areas is a novel biogeographic method that helps resolve conflicting area relationships and assess temporal overlap as an explanation for the conflict. The method differs from others currently popular in biogeography in that it does not date nodes before analysis (e.g. divergence dating) to infer area relationships and classification. Here, time-slicing is used as a proof of concept approach to interpret the inter-relationships of Neogene and Palaeogene biotic areas of Wallacea, a well-studied area of biogeographic overlap between South-East Asia and Australasia. We used 18 Pal

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2

Murray, J. W. "Palaeogene and Neogene." Geological Society, London, Memoirs 13, no. 1 (1992): 141–47. http://dx.doi.org/10.1144/gsl.mem.1992.013.01.14.

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AbstractMost of the British Isles has been a land area throughout the Tertiary and the basic shape of the coastline had been determined by the late Palaeocene. Only in southeast England are there marine Palaeogene and Neogene successions and these were deposited in embayments marginal to the North Sea and English Channel.Much of the key information for the interpretation of the Tertiary history of the British Isles lies offshore. Thousands of kilometres of seismic profiles have been run and hundreds of boreholes drilled, mainly in the search for oil. The only part of the Tertiary which has bee

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3

Suandhi, P. A., M. Rozalli, W. Utomo, A. Budiman, and A. Bachtiar. "Paleogene Sediment Character of Mountain Front Central Sumatra Basin." Indonesian Journal on Geoscience 8, no. 3 (2013): 143–49. http://dx.doi.org/10.17014/ijog.8.3.143-149.

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DOI: 10.17014/ijog.v8i3.164The SE-NW trending Mountain Front of Central Sumatra Basin is located in the southern part of the basin. The Mountain Front is elongated parallel to the Bukit Barisan Mountain, extending from the Regencies of North Padang Lawas (Gunung Tua in the northwest), Rokan Hulu, Kampar, Kuantan Singingi, and Inderagiri Hulu Regency in the southeast. The Palaeogene sediments also represent potential exploration objectives in Central Sumatra Basin, especially in the mountain front area. Limited detailed Palaeogene sedimentology information cause difficulties in hydrocarbon expl

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4

ZAGORCHEV, IVAN S. "Pre-Priabonian Palaeogene formations in southwestern Bulgaria and northern Greece: stratigraphy and tectonic implications." Geological Magazine 135, no. 1 (1998): 101–19. http://dx.doi.org/10.1017/s0016756897008285.

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The Paril Formation (South Pirin and Slavyanka Mountains, southwestern Bulgaria) and the Prodromos Formation (Orvilos and Menikion Mountains, northern Greece) consist of breccia and olistostrome built up predominantly of marble fragments from the Precambrian Dobrostan Marble Formation (Bulgaria) and its equivalent Bos-Dag Marble Formation (Greece). The breccia and olistostrome are interbedded with thin layers of calcarenites (with occasional marble pebbles), siltstones, sandstones and limestones. The Paril and Prodromos formations unconformably cover the Precambrian marbles, and are themselves

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5

Schulz, Bo Pagh, Madeleine Larissa Vickers, Jennifer Huggett, et al. "Palaeogene glendonites from Denmark." Bulletin of the Geological Society of Denmark 68 (April 1, 2020): 23–35. http://dx.doi.org/10.37570/bgsd-2020-68-03.

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Pristinely preserved mineral pseudomorphs called glendonites, up to 1.6 m long, from the Palaeogene strata of Denmark allow detailed crystallographic characterisation and add to the understanding of the transformation of the precursor mineral, ikaite (CaCO3·6H2O), to calcite, which constitutes the glendonite. We describe Danish pseudomorphs after ikaite from two localities and formations: the Early Eocene Fur Formation and the Late Oligocene Brejning Formation. This detailed study highlights that key aspects such as morphology and mode of occurrence of these ancient glendonites are identical t

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6

Schultz, Bo Pagh, Madeleine L. Vickers, Jennifer Huggett, et al. "Palaeogene glendonites from Denmark." Bulletin of the Geological Society of Denmark 68 (March 29, 2022): 23–35. http://dx.doi.org/10.37570/bgsd-2020-68-03-rev.

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Pristinely preserved mineral pseudomorphs called glendonites, up to 1.6 m long, from the Palaeogene strata of Denmark allow detailed crystallographic characterisation and add to the understanding of the transformation of the precursor mineral, ikaite (CaCO3·6H2O), to calcite, which constitutes the glendonite. We describe Danish pseudomorphs after ikaite from two localities and formations: the Early Eocene Fur Formation and the Late Oligocene Brejning Formation. This detailed study highlights that key aspects such as morphology and mode of occurrence of these ancient glendonites are identical t

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7

Jenkins, D. Graham, John E. Whittaker, and Dennis Curry. "Palaeogene triserial planktonic foraminifera." Journal of Micropalaeontology 17, no. 1 (1998): 61–70. http://dx.doi.org/10.1144/jm.17.1.61.

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Abstract. Triserial planktonic foraminiferal species from the Palaeogene are classified into the Early Danian Guembelitria, with pore mounds on the test surface, and the Early Eocene-Late Oligocene Jenkinsina, which are also microperforate but lack pore mounds. The stratigraphic and palaeogeographic ranges are discussed, the holotype of G. cretacea Cushman (the type species of Guembelitria) is re-illustrated, and neotypes designated for G. danica (Hofker) and Jenkinsina triseriata (Terquem). Chiloguembelitria is shown to be a junior synonym of Guembelitria.

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8

Golovneva, Lena B. "Palaeogene climates of Spitsbergen." GFF 122, no. 1 (2000): 62–63. http://dx.doi.org/10.1080/11035890001221062.

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9

Bande, M. B. "The Palaeogene vegetation of peninsular India (Megafossil evidences)." Journal of Palaeosciences 40 (December 31, 1991): 275–84. http://dx.doi.org/10.54991/jop.1991.1779.

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The Palaeogene represents the age of spread and diversification of angiosperms in the Indian sub-continent. A comprehensive knowledge of the Palaeogene flora of peninsular India is, therefore, necessary to decipher the history of the modern flora of India. The Palaeogene plant megafossils of this region can broadly be considered under (i) Deccan Intertrappean flora, (ii) Eocene flora of Kutch, (iii) Eocene plant fossils described from the Fuller's earth deposits near Barmer in Rajasthan, and (iv) Eocene plant records from Meghalaya. The flora as a whole is characteristically tropical in

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10

Dernov, V. S. "THE FIRST RECORD OF THE GENUS DELTOIDONAUTILUS SPATH, 1927 (NAUTILIDA: CEPHALOPODA) IN THE PALAEOGENE OF THE CRIMEAN PENINSULA, UKRAINE." Odesa National University Herald. Geography and Geology 29, no. 2(45) (2025): 139–49. https://doi.org/10.18524/2303-9914.2024.2(45).318037.

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The article describes a first record of a species of the genus Deltoidonautilus Spath, 1927 (D. cf. sowerbyi (Wetherell in Sowerby, 1843)) in the Palaeogene (Ypresian or lower Lutetian) deposits of the Crimean Peninsula, southern Ukraine. The data obtained expand the geographical distribution of this genus and complement the palaeontological characteristics of the Palaeogene succession of southern Ukraine.

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11

Zagorchev, Ivan, Aleksander Goranov, Veselin Vulkov, and Ivan Boyanov. "Palaeogene sediments in the Padala graben, northwestern Rila Mountain, Bulgaria." Geologica Balcanica 29, no. 3-4 (1999): 59–69. http://dx.doi.org/10.52321/geolbalc.29.3-4.59.

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The Padala Formation represents the sedimentary filling of the Padala graben. It is built up mostly of polymictic breccia and conglomerate interbedded with thin sandstone beds containing coalefied plant debris and thin coal lenses. The formation is of Palaeogene age. The Padala Formation belonged to a larger Palaeogene basin, and was situated close to the source area of the terrigeneous material.

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12

Yu-Sheng, L., W. Wei-Ming, and A. Momohara. "China's Beech Forests in the Pre-Quaternary." Fossil Record 1, no. 1 (1998): 151–65. http://dx.doi.org/10.5194/fr-1-151-1998.

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<i>Fagus</i> in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus <i>Fagus</i> was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements of <i>Fagus</i> in the Palaeogene seem much broader than those in the Neogene onwards. This is because the Palaeogene floras containing <i>Fagus</i> lived in various conditions from an arid and hot climate to a humid and warm habitat. Additionally, <i>Fagus</i> th

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13

Capobianco, Alessio, Hermione T. Beckett, Etienne Steurbaut, Philip D. Gingerich, Giorgio Carnevale, and Matt Friedman. "Large-bodied sabre-toothed anchovies reveal unanticipated ecological diversity in early Palaeogene teleosts." Royal Society Open Science 7, no. 5 (2020): 192260. http://dx.doi.org/10.1098/rsos.192260.

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Many modern groups of marine fishes first appear in the fossil record during the early Palaeogene (66–40 Ma), including iconic predatory lineages of spiny-rayed fishes that appear to have originated in response to ecological roles left empty after the Cretaceous/Palaeogene extinction. The hypothesis of extinction-mediated ecological release likewise predicts that other fish groups have adopted novel predatory ecologies. Here, we report remarkable trophic innovation in early Palaeogene clupeiforms (herrings and allies), a group whose modern representatives are generally small-bodied planktivore

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14

Luo, Rui, Ming Zha, Chang Hai Gao, and Hao He. "Geologic and Geochemical Conditions of Shale Oil of Paleogene in NanPu Sag of Bohai Bay Basin." Applied Mechanics and Materials 522-524 (February 2014): 1307–12. http://dx.doi.org/10.4028/www.scientific.net/amm.522-524.1307.

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The exploration practice in NanPu Sag suggests that shale oil&gas as an unconventional natural gas resource,is a kind of current alternative energy resource. According to measured data of geochemistry,mineral,logging and drilling on the Palaeogene strata in NanPu Sag,the shale in palaeogene characterised by large thickness,high abundance of organic matter, favorable types and wide range of thermal maturity, shows that it has the material basis for the formation of shale oil. In addition,the shale of palaeogene in NanPu Sag generally developed fractures,which has fine reservoir property. Th

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15

Seyitoǧlu, Gürol, and Barry Scott. "Late Cenozoic crustal extension and basin formation in west Turkey." Geological Magazine 128, no. 2 (1991): 155–66. http://dx.doi.org/10.1017/s0016756800018343.

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AbstractIt is proposed that north–south crustal extension and related sedimentary basin formation commenced in the early Miocene. This extension is believed to be related to a spreading of a thickened crust as a result of Palaeogene compression. That such spreading commenced virtually immediately after the cessation of this compression is considered to be due to the high thermal profile of the crust in that area at the end of the Palaeogene.

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16

Martin, A. R. H. "Palaeogene proteaceous pollen and phylogeny." Alcheringa: An Australasian Journal of Palaeontology 19, no. 1 (1995): 27–40. http://dx.doi.org/10.1080/03115519508619096.

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17

Wan, Xiaoqiao, Tian Jiang, Yiyi Zhang, Dangpeng Xi, and Guobiao Li. "Palaeogene marine stratigraphy in China." Lethaia 47, no. 3 (2014): 297–308. http://dx.doi.org/10.1111/let.12071.

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18

Neubert, Eike, and Dirk van Damme. "Palaeogene continental molluscs of Oman." Contributions to Natural History 20 (December 21, 2012): 1–28. https://doi.org/10.5169/seals-787080.

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19

Apesteguía, Sebastián, Raúl O. Gómez, and Guillermo W. Rougier. "The youngest South American rhynchocephalian, a survivor of the K/Pg extinction." Proceedings of the Royal Society B: Biological Sciences 281, no. 1792 (2014): 20140811. http://dx.doi.org/10.1098/rspb.2014.0811.

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Rhynchocephalian lepidosaurs, though once widespread worldwide, are represented today only by the tuatara ( Sphenodon ) of New Zealand. After their apparent early Cretaceous extinction in Laurasia, they survived in southern continents. In South America, they are represented by different lineages of Late Cretaceous eupropalinal forms until their disappearance by the Cretaceous/Palaeogene (K/Pg) boundary. We describe here the only unambiguous Palaeogene rhynchocephalian from South America; this new taxon is a younger species of the otherwise Late Cretaceous genus Kawasphenodon . Phylogenetic ana

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20

Hancock, Haidi J. L., George C. Chaproniere, Gerald R. Dickens, and Robert A. Henderson. "Early Palaeogene planktic foraminiferal and carbon isotope stratigraphy, Hole 762C, Exmouth Plateau, northwest Australian margin." Journal of Micropalaeontology 21, no. 1 (2002): 29–42. http://dx.doi.org/10.1144/jm.21.1.29.

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Abstract. Although the northwest margin of Australia is an important region for petroleum exploration and palaeoceanographic investigations, its Palaeogene stratigraphy is poorly documented, especially in terms of a foraminiferal biozonation. Early Palaeogene cores from 502.96 to 307.80 m below sea floor at Ocean Drilling Program Site 762 on the Exmouth Plateau were examined in this study for their planktic foraminiferal assemblages and the carbon isotopic compositions of Subbotina spp. Planktic foraminifera are generally well preserved and belong to 74 species and 17 genera. In spite of a mid

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21

Zagorchev, Ivan. "Pre-Paleogene Alpine tectonics in Southwestern Bulgaria." Geologica Balcanica 25, no. 5-6 (1995): 91–112. http://dx.doi.org/10.52321/geolbalc.25.5-6.91.

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The pre-Palaeogene Alpine structure of SW Bulgaria consists of the Srednogorie, Morava, Struma and Rhodope Superunits and the Ograzhden Unit. They are characterized by different pre-Alpine and Mesozoic histories. The Mid-Cretaceous and Late Cretaceous thrusts and thrust structure are discordantly and obliquely superimposed over the pre-existing (Triassic and Jurassic – Early Cretaceous) structural and sedimentation environments. The boundaries between the tectonic units are thrust surfaces and zones often hidden by intersecting younger normal faults or/and stitching intrusive bodies or sealed

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22

During, Melanie A. D., Jan Smit, Dennis F. A. E. Voeten, et al. "The Mesozoic terminated in boreal spring." Nature 603, no. 7899 (2022): 91–94. http://dx.doi.org/10.1038/s41586-022-04446-1.

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AbstractThe Cretaceous–Palaeogene mass extinction around 66 million years ago was triggered by the Chicxulub asteroid impact on the present-day Yucatán Peninsula1,2. This event caused the highly selective extinction that eliminated about 76% of species3,4, including all non-avian dinosaurs, pterosaurs, ammonites, rudists and most marine reptiles. The timing of the impact and its aftermath have been studied mainly on millennial timescales, leaving the season of the impact unconstrained. Here, by studying fishes that died on the day the Mesozoic era ended, we demonstrate that the impact that cau

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23

Price, S. A., L. Schmitz, C. E. Oufiero, et al. "Two waves of colonization straddling the K–Pg boundary formed the modern reef fish fauna." Proceedings of the Royal Society B: Biological Sciences 281, no. 1783 (2014): 20140321. http://dx.doi.org/10.1098/rspb.2014.0321.

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Living reef fishes are one of the most diverse vertebrate assemblages on Earth. Despite its prominence and ecological importance, the origins and assembly of the reef fish fauna is poorly described. A patchy fossil record suggests that the major colonization of reef habitats must have occurred in the Late Cretaceous and early Palaeogene, with the earliest known modern fossil coral reef fish assemblage dated to 50 Ma. Using a phylogenetic approach, we analysed the early evolutionary dynamics of modern reef fishes. We find that reef lineages successively colonized reef habitats throughout the La

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24

Belcher, C. M. "Reigniting the Cretaceous-Palaeogene firestorm debate." Geology 37, no. 12 (2009): 1147–48. http://dx.doi.org/10.1130/focus122009.1.

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Li, Q., and S. Radford. "Poster: Evolution of palaeogene planktonic foraminifera." Marine and Petroleum Geology 6, no. 4 (1989): 382. http://dx.doi.org/10.1016/0264-8172(89)90062-7.

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SARASWATI, PRATUL KUMAR, RENGASWAMY RAMESH, and SURESH VASUDEV NAVADA. "Palaeogene isotopic temperatures of western India." Lethaia 26, no. 1 (1993): 89–98. http://dx.doi.org/10.1111/j.1502-3931.1993.tb01515.x.

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GREGORY, J. W. "VIII. On the British Palaeogene Bryozoa." Transactions of the Zoological Society of London 13, no. 6 (2010): 219–79. http://dx.doi.org/10.1111/j.1096-3642.1893.tb00050.x.

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Mourer-Chauviré, Cécile, Martin Pickford, and Brigitte Senut. "The first Palaeogene galliform from Africa." Journal of Ornithology 152, no. 3 (2010): 617–22. http://dx.doi.org/10.1007/s10336-010-0630-9.

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Eronen, Jussi T., Christine M. Janis, C. Page Chamberlain, and Andreas Mulch. "Mountain uplift explains differences in Palaeogene patterns of mammalian evolution and extinction between North America and Europe." Proceedings of the Royal Society B: Biological Sciences 282, no. 1809 (2015): 20150136. http://dx.doi.org/10.1098/rspb.2015.0136.

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Patterns of late Palaeogene mammalian evolution appear to be very different between Eurasia and North America. Around the Eocene–Oligocene (EO) transition global temperatures in the Northern Hemisphere plummet: following this, European mammal faunas undergo a profound extinction event (the Grande Coupure), while in North America they appear to pass through this temperature event unscathed. Here, we investigate the role of surface uplift to environmental change and mammalian evolution through the Palaeogene (66–23 Ma). Palaeogene regional surface uplift in North America caused large-scale reorg

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Kaasalainen, Ulla, Jouko Rikkinen, and Alexander R. Schmidt. "Fossil Usnea and similar fruticose lichens from Palaeogene amber." Lichenologist 52, no. 4 (2020): 319–24. http://dx.doi.org/10.1017/s0024282920000286.

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AbstractFruticose lichens of the genus Usnea Dill. ex Adans. (Parmeliaceae), generally known as beard lichens, are among the most iconic epiphytic lichens in modern forest ecosystems. Many of the c. 350 currently recognized species are widely distributed and have been used as bioindicators in air pollution studies. Here we demonstrate that usneoid lichens were present in the Palaeogene amber forests of Europe. Based on general morphology and annular cortical fragmentation, one fossil from Baltic amber can be assigned to the extant genus Usnea. The unique type of cortical cracking indirectly de

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Hansen, Thomas. "Gastropods from the Cretaceous-Palaeogene boundary in Denmark." Zootaxa 4654, no. 1 (2019): 1–196. https://doi.org/10.11646/zootaxa.4654.1.1.

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Schiøler, Poul, Jan Andsbjerg, Ole R. Clausen, et al. "A revised lithostratigraphy for the Palaeogene – lower Neogene of the Danish North Sea." Geological Survey of Denmark and Greenland (GEUS) Bulletin 7 (July 29, 2005): 21–24. http://dx.doi.org/10.34194/geusb.v7.4825.

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Intense drilling activity following the discovery of the Siri Field in 1995 has resulted in an improved understanding of the siliciclastic Palaeogene succession in the Danish North Sea sector (Fig. 1). Many of the new wells were drilled in the search for oil reservoirs in sand bodies of Paleocene–Eocene age. The existing lithostratigraphy was based on data from a generation of wells that were drilled with deeper stratigraphic targets, with little or no interest in the overlying Palaeogene sediments, and thus did not adequately consider the significance of the Palaeogene sandstone units in the

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Figus, Cécile, Johan Renaudie, Or M. Bialik, and Jakub Witkowski. "Controls on Palaeogene deep-sea diatom-bearing sediment deposition and comparison with shallow marine environments." Biogeosciences 22, no. 12 (2025): 3029–46. https://doi.org/10.5194/bg-22-3029-2025.

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Abstract. Diatoms are the key players in the present-day global biogeochemical cycles. Yet, the diatom flux response to the dynamically changing climates of the Palaeogene has long been subject to divergent interpretations. We present a synthesis of Palaeogene deep-sea diatom-bearing sediment occurrences in time and space in order to gain new insight into inter-basin and latitudinal distribution of diatom accumulation zones from the Cretaceous–Palaeogene boundary to the Oligocene–Miocene transition. Our dataset includes 189 sites drilled in the Atlantic, Pacific, and Indian oceans and in the A

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ANGST, D., E. BUFFETAUT, C. LÉCUYER, et al. "Fossil avian eggs from the Palaeogene of southern France: new size estimates and a possible taxonomic identification of the egg-layer." Geological Magazine 152, no. 1 (2014): 70–79. http://dx.doi.org/10.1017/s0016756814000077.

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AbstractEggshell fragments attributed to large birds have been known from the Palaeogene of southern France for half a century, but reconstructing their original dimensions and identifying the birds that laid the eggs has been fraught with difficulties. On the basis of numerous newly collected specimens and using geometrical calculations, the original size of the thick-shelled eggs is reconstructed, showing that they were slightly larger than ostrich eggs, with a greatest length of 17.8 cm and a mean diameter of 12.0 cm in transversal section. The estimated volume is 1330.4 cm3. The fossil egg

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35

Neal, J. E., J. A. Stein, and J. H. Gamber. "Graphic correlation and sequence stratigraphy in the Palaeogene of NW Europe." Journal of Micropalaeontology 13, no. 1 (1994): 55–80. http://dx.doi.org/10.1144/jm.13.1.55.

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Abstract. A sequence stratigraphic analysis of well log, seismic, and biostratigraphic data has documented a pattern of cyclic sedimentation for the Palaeogene of the Central North Sea. Previously published research has also documented cyclic sedimentation related to sea level changes. Integrating Central North Sea subsurface sections with Palaeogene outcrop from NW Europe, using sequence stratigraphic first principles and the graphic correlation method, has produced a chronostratigraphic framework for the Palaeogene of NW Europe.Northwestern Europe basins (London–Hampshire, Paris, and Belgian

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Andersen, T., G. A. Botha, and M. A. Elburg. "A late Mesozoic – early Cenozoic sedimentary recycling system on the Gondwana rifted margin of southeast Africa." South African Journal of Geology 123, no. 3 (2020): 343–56. http://dx.doi.org/10.25131/sajg.123.0023.

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Abstract Detrital zircons in late Cretaceous – Palaeogene, calcareous sandstone and conglomerate deposited in continental basins on the southeastern African margin after the breakup of Gondwana have characteristic combinations of age and epsilon-Hf that indicate an origin by recycling of Palaeoproterozoic (Waterberg, Soutpansberg and Pretoria groups) and Phanerozoic (Karoo Supergroup) cover successions. The latter is dominant in the south and east (Boane, Mahosi, Chilojo Cliffs), and the Palaeoproterozoic sources in the northwest (Pafuri, Wright’s Tower, Masisi). This recycling and mixing regi

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Wedmann, Sonja, Jean-Marc Pouillon, and André Nel. "New Palaeogene horntail wasps (Hymenoptera, Siricidae) and a discussion of their fossil record." Zootaxa 3869, no. 1 (2014): 33–43. https://doi.org/10.11646/zootaxa.3869.1.3.

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Wedmann, Sonja, Pouillon, Jean-Marc, Nel, André (2014): New Palaeogene horntail wasps (Hymenoptera, Siricidae) and a discussion of their fossil record. Zootaxa 3869 (1): 33-43, DOI: 10.11646/zootaxa.3869.1.3

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Nielsen, O. B., and C. Heilmann-Clausen. "Palaeogene volcanism: the sedimentary record in Denmark." Geological Society, London, Special Publications 39, no. 1 (1988): 395–405. http://dx.doi.org/10.1144/gsl.sp.1988.039.01.35.

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Pomerol, Charles. "Stratigraphy of the Palaeogene: hiatuses and transitions." Proceedings of the Geologists' Association 100, no. 3 (1989): 313–24. http://dx.doi.org/10.1016/s0016-7878(89)80051-3.

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Hamblin, Richard. "The Palaeogene Haldon Formation of South Devon." Proceedings of the Geologists' Association 125, no. 5-6 (2014): 591–99. http://dx.doi.org/10.1016/j.pgeola.2014.10.003.

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Nel, André, and Julián F. Petrulevicius. "New Palaeogene bees from Europe and Asia." Alcheringa: An Australasian Journal of Palaeontology 27, no. 4 (2003): 277–93. http://dx.doi.org/10.1080/03115510308619108.

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Stevens, Nancy J., Robert V. Hill, Mohammed Al-Wosabi, et al. "A middle Eocene mesoeucrocodylian (Crocodyliformes) from the Kaninah Formation, Republic of Yemen." Geologos 19, no. 3 (2013): 175–83. http://dx.doi.org/10.2478/logos-2013-0010.

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Abstract During the Cenozoic, the Arabian Plate separated from continental Africa and assumed a closer geographical relationship with Eurasia. As such, the vertebrate fossil record of the Arabian Peninsula has great potential for documenting faunal interchanges that occurred as a result of such tectonic events, with a shift from a primarily Afro-Arabian fauna in the Palaeogene to a more cosmopolitan fauna in the Neogene. Understanding of the sequence and timing of this faunal interchange has long been hampered by a lack of palaeontological data. Recently recovered fossils from the Middle Eocen

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Dernov, Vitaly. "Beloptera Longa Naef, 1922 (Cephalopoda: Coleoidea) From The Late Eocene (Palaeogene) Of Ukraine." Acta Palaeontologica Romaniae 20, no. 2 (2024): 3–10. https://doi.org/10.35463/j.apr.2024.02.01.

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Dernov, Vitaly (2024): Beloptera Longa Naef, 1922 (Cephalopoda: Coleoidea) From The Late Eocene (Palaeogene) Of Ukraine. Acta Palaeontologica Romaniae 20 (2): 3-10, DOI: 10.35463/j.apr.2024.02.01, URL: https://doi.org/10.35463/j.apr.2024.02.01

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Szwedo, Jacek, Thierry Bourgoin, and Fabrice Lefebvre. "New Mnemosynini taxa (Hemiptera, Fulgoromorpha: Cixiidae) from the Palaeogene of France with notes on their early association with host plants." Zootaxa 1122 (December 31, 2006): 25–45. https://doi.org/10.5281/zenodo.171746.

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Szwedo, Jacek, Bourgoin, Thierry, Lefebvre, Fabrice (2006): New Mnemosynini taxa (Hemiptera, Fulgoromorpha: Cixiidae) from the Palaeogene of France with notes on their early association with host plants. Zootaxa 1122: 25-45, DOI: 10.5281/zenodo.171746

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Figus, Cécile, Or M. Bialik, Andrey Y. Gladenkov, et al. "Climatic and tectonic controls on shallow-marine and freshwater diatomite deposition throughout the Palaeogene." Climate of the Past 20, no. 11 (2024): 2629–44. http://dx.doi.org/10.5194/cp-20-2629-2024.

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Abstract. Diatoms play a major role in carbon and silicon cycles, and thus diatom-bearing sediments represent an archive of past climatic and environmental settings. In shallow-marine and freshwater environments, the accumulation of diatom frustules forms a sedimentary rock called diatomite. While most global-scale studies of diatom-bearing sediments focus on deep-sea sites, shallow-marine and freshwater diatomites are studied mainly at a regional level. To address this problem, we present a global-scale compilation of diatomite occurrences spanning the Palaeogene (∼66 to ∼23 Ma). This period

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Głuszyński, Andrzej, and Paweł Aleksandrowski. "Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)." Solid Earth 13, no. 8 (2022): 1219–42. http://dx.doi.org/10.5194/se-13-1219-2022.

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Abstract. A brief, regional-scale review of the Late Cretaceous–early Palaeogene inversion-related tectonic structures affecting the Sudety Mountains and their foreland at the NE margin of the Bohemian Massif is presented and complemented with results of new seismic studies. The Sudetes expose Variscan-deformed basement, partly overlain by post-orogenic Permo-Mesozoic cover, containing a wide spectrum of tectonic structures, both brittle and ductile, in the past in this area referred to as young Saxonian or Laramide. We have used newly reprocessed legacy seismics to study these structures in t

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Uchman, Alfred, and Andreas Wetzel. "Hidden subsurface garden on own faeces - the trace fossil Tubulichnium rectum (Fischer-Ooster, 1858) from the Cretaceous-Palaeogene deep-sea sediments." Palaeontologia Electronica 4, no. 4 (2017): 1–18. https://doi.org/10.26879/777.

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Uchman, Alfred, Wetzel, Andreas (2017): Hidden subsurface garden on own faeces - the trace fossil Tubulichnium rectum (Fischer-Ooster, 1858) from the Cretaceous-Palaeogene deep-sea sediments. Palaeontologia Electronica 4 (4): 1-18, DOI: 10.26879/777, URL: http://dx.doi.org/10.26879/777

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Marivaux, Laurent, and Myriam Boivin. "Emergence of hystricognathous rodents: Palaeogene fossil record, phylogeny, dental evolution and historical biogeography." Zoological Journal of the Linnean Society 187, no. 3 (2019): 929–64. https://doi.org/10.1093/zoolinnean/zlz048.

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Marivaux, Laurent, Boivin, Myriam (2019): Emergence of hystricognathous rodents: Palaeogene fossil record, phylogeny, dental evolution and historical biogeography. Zoological Journal of the Linnean Society 187 (3): 929-964, DOI: 10.1093/zoolinnean/zlz048, URL: https://academic.oup.com/zoolinnean/article/187/3/929/5559773

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Podobina, V. M., V. M. Kabanova, and T. G. Kseneva. "Change of micropaleontological assemblages at the Cretaceous-Paleogene Boundary in Western Siberia." Journal of Palaeosciences 46, no. (1-2) (1997): 156–60. http://dx.doi.org/10.54991/jop.1997.1332.

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The foraminiferal and spore-pollen complexes were studied at the boundary of Maastrichtian-Danian (CretaceousPalaeogene) in Western Siberia. Terrigenic-argillaceous rocks with admixture of carbonaceous material from the upper part of Gankinsky Suite and lower layers of Talitsky Suite belong to this stratigraphical interval. Carbonaceous secreted and secreted agglutinated shells predominate among benthic Foraminifers. Planktonic forms were seldom and consist of representatives of the genera - Rugoglobigerina and Guembelina in the Maastrichtian and genera Globigerina and (rarely) Globorotalia in

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Do Campo, M., C. del Papa, J. Jiménez-Millán, and F. Nieto. "Clay mineral assemblages and analcime formation in a Palaeogene fluvial–lacustrine sequence (Maíz Gordo Formation Palaeogen) from northwestern Argentina." Sedimentary Geology 201, no. 1-2 (2007): 56–74. http://dx.doi.org/10.1016/j.sedgeo.2007.04.007.

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