Array ( [0] => {{short description|First period of the Cenozoic Era (66–23 million years ago)}} [1] => {{Distinguish|Paleocene}} [2] => {{Multiple issues| [3] => {{rewrite|date=November 2023}} [4] => {{Expert|Geology|ex2=Palaeontology|reason=Too technical: See [[talk:Paleogene#Scientific journal|talk page]]|date=November 2023}} [5] => }} [6] => {{Infobox geologic timespan [7] => | name = Paleogene [8] => | color = Paleogene [9] => | top_bar = [10] => | time_start = 66.0 [11] => | time_end = 23.03 [12] => | image_map =40 Ma paleoglobe.png [13] => | caption_map = A map of Earth as it appeared during the Eocene epoch, {{circa}} 40 Ma. [14] => | image_outcrop = [15] => | caption_outcrop = [16] => | image_art = [17] => | caption_art = [18] => [19] => | timeline = Paleogene [20] => [21] => | name_formality = Formal [22] => | name_accept_date = [23] => | alternate_spellings = Palaeogene, Palæogene [24] => | synonym1 = [25] => | synonym1_coined = [26] => | synonym2 = [27] => | synonym2_coined = [28] => | synonym3 = [29] => | synonym3_coined = [30] => | nicknames = [31] => | former_names = [32] => | proposed_names = [33] => [34] => | celestial_body = earth [35] => | usage = Global ([[International Commission on Stratigraphy|ICS]]) [36] => | timescales_used = ICS Time Scale [37] => | formerly_used_by = [38] => | not_used_by = [39] => [40] => | chrono_unit = Period [41] => | strat_unit = System [42] => | proposed_by = [43] => | timespan_formality = Formal [44] => | lower_boundary_def = [[Iridium]] enriched layer associated with a major meteorite impact and subsequent [[K-Pg extinction event]]. [45] => | lower_gssp_location = El Kef Section, [[El Kef]], [[Tunisia]] [46] => | lower_gssp_coords = {{Coord|36.1537|N|8.6486|E|display=inline}} [47] => | lower_gssp_accept_date = 1991{{cite journal|last1=Molina |first1=Eustoquio |last2=Alegret |first2=Laia |last3=Arenillas |first3=Ignacio |author4=José A. Arz |last5=Gallala |first5=Njoud |last6=Hardenbol |first6=Jan |author7=Katharina von Salis |last8=Steurbaut |first8=Etienne |last9=Vandenberghe |first9=Noel |author10=Dalila Zaghibib-Turki |title=The Global Boundary Stratotype Section and Point for the base of the Danian Stage (Paleocene, Paleogene, "Tertiary", Cenozoic) at El Kef, Tunisia - Original definition and revision |journal=Episodes |year=2006 |volume=29 |issue=4 |pages=263–278 |doi=10.18814/epiiugs/2006/v29i4/004 |doi-access=free }} [48] => | upper_boundary_def = [49] => * Base of magnetic polarity [[chronozone]] C6Cn.2n. [50] => * Near first appearance of the [[Foraminifera|Planktonic foraminiferan]] ''[[Paragloborotalia|Paragloborotalia kugleri]]''. [51] => | upper_gssp_location = Lemme-Carrosio Section, [[Carrosio]], [[Italy]] [52] => | upper_gssp_coords = {{Coord|44.6589|N|8.8364|E|display=inline}} [53] => | upper_gssp_accept_date = 1996{{cite journal|last=Steininger|first=Fritz F. |author2=M. P. Aubry |author3=W. A. Berggren |author4=M. Biolzi |author5=A. M. Borsetti |author6=Julie E. Cartlidge |author7=F. Cati |author8=R. Corfield |author9=R. Gelati |author10=S. Iaccarino |author11=C. Napoleone |author12=F. Ottner |author13=F. Rögl |author14=R. Roetzel |author15=S. Spezzaferri |author16=F. Tateo |author17=G. Villa |author18=D. Zevenboom |title=The Global Stratotype Section and Point (GSSP) for the base of the Neogene|journal=Episodes|year=1997|volume=20|issue=1|pages=23–28|url=http://www.stratigraphy.org/GSSP/file9.pdf|doi=10.18814/epiiugs/1997/v20i1/005 |doi-access=free }} [54] => [55] => | o2 = 26 [56] => | co2 = 500 [57] => | temp = 18 [58] => | sea_level = [59] => }} [60] => The '''Paleogene Period''' ({{IPAc-en|ipa|ˈ|p|eɪ|l|i|.|ə|dʒ|iː|n|,_|-|l|i|.|oʊ|-|,_|ˈ|p|æ|l|i|-}} {{respell|PAY|lee|ə|jeen|,_|-|lee|oh|-|,_|PAL|ee|-}}; [[British English|also spelled]] '''Palaeogene''' or '''Palæogene''') is a [[geologic period|geologic period and system]] that spans 43 million years from the end of the [[Cretaceous]] Period {{period end|Cretaceous}} million years ago ([[annum|Mya]]) to the beginning of the [[Neogene]] Period {{period start|neogene}} Mya. It is the first part of the [[Cenozoic]] [[Era]] of the present [[Phanerozoic]] Eon. The earlier term [[Tertiary]] Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognized as a formal [[stratigraphy|stratigraphic term]], "Tertiary" still sometimes remains in informal use.{{Cite web|url=http://www.stratigraphy.org/bak/geowhen/TQ.html|title=GeoWhen Database – What Happened to the Tertiary?|website=www.stratigraphy.org}} Paleogene is often abbreviated "Pg", although the [[United States Geological Survey]] uses the abbreviation "{{sc1|Pe}}" for the Paleogene on the Survey's geologic maps.{{cite web |last1=Federal Geographic Data Committee |title=FGDC Digital Cartographic Standard for Geologic Map Symbolization |url=https://ngmdb.usgs.gov/fgdc_gds/geolsymstd/fgdc-geolsym-sec32.pdf |website=The National Geologic Map Database |publisher=United States Geological Survey |access-date=29 January 2022}}{{cite web |last1=Orndorff |first1=R.C. |title=Divisions of Geologic Time—Major Chronostratigraphic and Geochronologic Units |url=https://pubs.usgs.gov/fs/2007/3015/fs2007-3015.pdf |publisher=United States Geological Survey |access-date=29 January 2022 |date=20 July 2010}} [61] => [62] => During the Paleogene period, [[evolution of mammals|mammals continued to diversify]] from relatively small, simple forms into a large group of diverse [[animal]]s in the wake of the [[Cretaceous–Paleogene extinction event]] that ended the preceding [[Cretaceous]] Period.{{cite journal |last1=Meredith |first1=R. W. |last2=Janecka |first2=J. E. |last3=Gatesy |first3=J. |last4=Ryder |first4=O. A. |last5=Fisher |first5=C. A. |last6=Teeling |first6=E. C. |last7=Goodbla |first7=A. |last8=Eizirik |first8=E. |last9=Simao |first9=T. L. L. |last10=Stadler |first10=T. |last11=Rabosky |first11=D. L. |last12=Honeycutt |first12=R. L. |last13=Flynn |first13=J. J. |last14=Ingram |first14=C. M. |last15=Steiner |first15=C. |last16=Williams |first16=T. L. |last17=Robinson |first17=T. J. |last18=Burk-Herrick |first18=A. |last19=Westerman |first19=M. |last20=Ayoub |first20=N. A. |last21=Springer |first21=M. S. |last22=Murphy |first22=W. J. |title=Impacts of the Cretaceous Terrestrial Revolution and KPg Extinction on Mammal Diversification |journal=Science |date=28 October 2011 |volume=334 |issue=6055 |pages=521–524 |doi=10.1126/science.1211028|pmid=21940861 |bibcode=2011Sci...334..521M |s2cid=38120449 }} [63] => [64] => This period consists of the [[Paleocene]], [[Eocene]], and [[Oligocene]] epochs. The end of the Paleocene (56 Mya) was marked by the [[Paleocene–Eocene Thermal Maximum]], one of the most significant periods of global change during the Cenozoic, which changed oceanic and atmospheric circulation and resulted in the extinction of numerous deep-sea benthic [[foraminifera]] and on land, a major extinction of mammals. The term "Paleogene System" applies to the rocks deposited during the Paleogene Period. [65] => [66] => ==Climate== [67] => The global climate of the Palaeogene began with the brief but intense "[[impact winter]]" caused by the Chicxulub impact. This cold period was terminated by an abrupt warming. After temperatures stabilised, the steady cooling and drying of the Late Cretaceous-Early Palaeogene Cool Interval (LKEPCI) that had spanned the last two stages of the [[Late Cretaceous]] continued.{{Cite journal |last1=Scotese |first1=Christopher Robert |last2=Song |first2=Haijun |last3=Mills |first3=Benjamin J.W. |last4=van der Meer |first4=Douwe G. |date=April 2021 |title=Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years |url=https://linkinghub.elsevier.com/retrieve/pii/S0012825221000027 |journal=[[Earth-Science Reviews]] |language=en |volume=215 |page=103503 |doi=10.1016/j.earscirev.2021.103503 |bibcode=2021ESRv..21503503S |s2cid=233579194 |access-date=23 September 2023}} About 62.2 Ma, the [[Danian#Latest Danian Event|Latest Danian Event]], a hyperthermal event, took place.{{cite journal |last1=Jehle |first1=Sofie |last2=Bornemann |first2=André |last3=Lägel |first3=Anna Friederike |last4=Deprez |first4=Arne |last5=Speijer |first5=Robert P. |date=1 July 2019 |title=Paleoceanographic changes across the Latest Danian Event in the South Atlantic Ocean and planktic foraminiferal response |url=https://www.sciencedirect.com/science/article/abs/pii/S003101821830854X#! |journal=[[Palaeogeography, Palaeoclimatology, Palaeoecology]] |volume=525 |pages=1–13 |bibcode=2019PPP...525....1J |doi=10.1016/j.palaeo.2019.03.024 |s2cid=134929774 |access-date=30 December 2022}}{{cite journal |last1=Jehle |first1=Sofie |last2=Bornemann |first2=André |last3=Deprez |first3=Arne |last4=Speijer |first4=Robert P. |date=25 November 2015 |title=The Impact of the Latest Danian Event on Planktic Foraminiferal Faunas at ODP Site 1210 (Shatsky Rise, Pacific Ocean) |journal=[[PLOS ONE]] |volume=10 |issue=11 |pages=e0141644 |bibcode=2015PLoSO..1041644J |doi=10.1371/journal.pone.0141644 |pmc=4659543 |pmid=26606656 |doi-access=free}}{{cite journal |last1=Sprong |first1=M. |last2=Youssef |first2=J. A. |last3=Bornemann |first3=André |last4=Schulte |first4=P. |last5=Steurbaut |first5=E. |last6=Stassen |first6=P. |last7=Kouwenhoven |first7=T. J. |last8=Speijer |first8=Robert P. |date=September 2011 |title=A multi-proxy record of the Latest Danian Event at Gebel Qreiya, Eastern Desert, Egypt |url=https://core.ac.uk/download/pdf/34511141.pdf |journal=Journal of Micropalaeontology |volume=30 |issue=2 |pages=167–182 |doi=10.1144/0262-821X10-023 |bibcode=2011JMicP..30..167S |s2cid=55038043 |access-date=30 December 2022 |archive-date=28 June 2023 |archive-url=https://web.archive.org/web/20230628093332/https://core.ac.uk/download/pdf/34511141.pdf |url-status=dead }} About 59 Ma, the LKEPCI was brought to an end by the Thanetian Thermal Event, a change from the relative cool of the [[Early Paleocene|Early]] and [[Middle Paleocene|Middle Palaeocene]] and the beginning of an intense supergreenhouse effect. [68] => [69] => From about 56 to 48 Mya, annual air temperatures over land and at mid-latitude averaged about 23–29 °C (± 4.7 °C), which is 5–10 °C warmer than most previous estimates.{{cite journal |author=Naafs, B. D. A. |author2=Rohrssen, M. |author3=Inglis, G. N. |author4=Lähteenoja, O. |author5=Feakins, S. J. |author6=Collinson, M. E. |author7=Kennedy, E. M. |author8=Singh, P. K. |author9=Singh, M. P. |author10=Lunt, D. J. |author11=Pancost, R. D. |year=2018 |title=High temperatures in the terrestrial mid-latitudes during the early Palaeogene |url=https://research-information.bristol.ac.uk/files/159708447/Combined_manuscript_submitted_June_2018.pdf |journal=[[Nature Geoscience]] |volume=11 |issue=10 |pages=766–771 |bibcode=2018NatGe..11..766N |doi=10.1038/s41561-018-0199-0 |s2cid=135045515 |hdl=1983/82e93473-2a5d-4a6d-9ca1-da5ebf433d8b}}{{cite news |last1=University of Bristol |date=30 July 2018 |title=Ever-increasing CO2 levels could take us back to the tropical climate of Paleogene period |work=ScienceDaily}}{{cite web |year=2018 |title=Ever-increasing CO2 levels could take us back to the tropical climate of Paleogene period |url=https://www.bristol.ac.uk/news/2018/july/co2-levels-paleogene-period.html |work=University of Bristol}} For comparison, this was 10 to 15 °C greater than the current annual mean temperatures in these areas. At the Palaeocene-Eocene boundary occurred the [[Paleocene–Eocene Thermal Maximum]] (PETM),{{Cite journal |last=Wing |first=S. L. |date=11 November 2005 |title=Transient Floral Change and Rapid Global Warming at the Paleocene-Eocene Boundary |url=https://www.science.org/doi/10.1126/science.1116913 |journal=Science |volume=310 |issue=5750 |pages=993–996 |bibcode=2005Sci...310..993W |doi=10.1126/science.1116913 |issn=0036-8075 |pmid=16284173 |s2cid=7069772 |access-date=23 September 2023}} one of the warmest times of the Phanerozoic eon, during which global mean surface temperatures increased to 31.6.{{Cite journal |last1=Inglis |first1=Gordon N. |last2=Bragg |first2=Fran |last3=Burls |first3=Natalie J. |last4=Cramwinckel |first4=Margot J. |last5=Evans |first5=David |last6=Foster |first6=Gavin L. |last7=Huber |first7=Matthew |last8=Lunt |first8=Daniel J. |last9=Siler |first9=Nicholas |last10=Steinig |first10=Sebastian |last11=Tierney |first11=Jessica E. |last12=Wilkinson |first12=Richard |last13=Anagnostou |first13=Eleni |last14=de Boer |first14=Agatha M. |last15=Dunkley Jones |first15=Tom |date=26 October 2020 |title=Global mean surface temperature and climate sensitivity of the early Eocene Climatic Optimum (EECO), Paleocene–Eocene Thermal Maximum (PETM), and latest Paleocene |url=https://cp.copernicus.org/articles/16/1953/2020/ |journal=[[Climate of the Past]] |language=en |volume=16 |issue=5 |pages=1953–1968 |doi=10.5194/cp-16-1953-2020 |bibcode=2020CliPa..16.1953I |issn=1814-9332 |access-date=23 September 2023 |doi-access=free |hdl=1983/24a30f12-51a6-4544-9db8-b2009e33c02a |hdl-access=free }} It was followed by the less severe [[Eocene Thermal Maximum 2]] (ETM2) about 53.69 Ma.{{Cite journal |author=Stap, L. |author2=Lourens, L.J. |author3=Thomas, E. |author4=Sluijs, A. |author5=Bohaty, S. |author6=Zachos, J.C. |date=1 July 2010 |title=High-resolution deep-sea carbon and oxygen isotope records of Eocene Thermal Maximum 2 and H2 |url=https://pubs.geoscienceworld.org/gsa/geology/article-abstract/38/7/607/130287/High-resolution-deep-sea-carbon-and-oxygen-isotope?redirectedFrom=fulltext |journal=[[Geology (journal)|Geology]] |volume=38 |issue=7 |pages=607–610 |bibcode=2010Geo....38..607S |doi=10.1130/G30777.1 |s2cid=41123449 |hdl=1874/385773|hdl-access=free }} Eocene Thermal Maximum 3 (ETM3) occurred about 53 Ma. The Early Eocene Climatic Optimum was brought to an end by the [[Azolla event]], a change of climate about 48.5 Mya, believed to have been caused by a proliferation of aquatic ferns from the genus ''[[Azolla]]'', resulting in the sequestering of large amounts of carbon dioxide by those plants. From this time until about 34 Mya, there was a slow cooling trend known as the Middle-Late Eocene Cooling (MLEC). Approximately 41.5 Ma, this cooling was interrupted temporarily by the Middle Eocene Climatic Optimum (MECO).{{Cite journal |last1=Bohaty |first1=Steven M. |last2=Zachos |first2=James C. |date=1 November 2003 |title=Significant Southern Ocean warming event in the late middle Eocene |url=https://pubs.geoscienceworld.org/geology/article/31/11/1017-1020/29164 |journal=[[Geology (journal)|Geology]] |language=en |volume=31 |issue=11 |page=1017 |doi=10.1130/G19800.1 |bibcode=2003Geo....31.1017B |issn=0091-7613 |access-date=23 September 2023}} Then, about 39.4 Mya, a temperature decrease termed the Late Eocene Cool Event (LECE) is detected in the oxygen isotope record. A rapid decrease of global temperatures and formation of continental glaciers on Antarctica marked the end of the Eocene.{{Cite journal |last1=Pearson |first1=Paul N. |last2=Foster |first2=Gavin L. |last3=Wade |first3=Bridget S. |date=13 September 2009 |title=Atmospheric carbon dioxide through the Eocene–Oligocene climate transition |url=https://www.nature.com/articles/nature08447 |journal=[[Nature (journal)|Nature]] |language=en |volume=461 |issue=7267 |pages=1110–1113 |doi=10.1038/nature08447 |pmid=19749741 |bibcode=2009Natur.461.1110P |s2cid=205218274 |issn=0028-0836 |access-date=23 September 2023}} This sudden cooling was caused partly by the formation of the [[Antarctic Circumpolar Current]],{{Cite journal |last1=Sauermilch |first1=Isabel |last2=Whittaker |first2=Joanne M. |last3=Klocker |first3=Andreas |last4=Munday |first4=David R. |last5=Hochmuth |first5=Katharina |last6=Bijl |first6=Peter K. |last7=LaCasce |first7=Joseph H. |date=9 November 2021 |title=Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling |journal=[[Nature Communications]] |language=en |volume=12 |issue=1 |page=6465 |doi=10.1038/s41467-021-26658-1 |pmid=34753912 |pmc=8578591 |bibcode=2021NatCo..12.6465S |issn=2041-1723 }} which significantly lowered oceanic water temperatures.{{Cite journal |last1=Barker |first1=P.F. |last2=Thomas |first2=E. |date=June 2004 |title=Origin, signature and palaeoclimatic influence of the Antarctic Circumpolar Current |url=https://linkinghub.elsevier.com/retrieve/pii/S0012825203001272 |journal=[[Earth-Science Reviews]] |language=en |volume=66 |issue=1–2 |pages=143–162 |doi=10.1016/j.earscirev.2003.10.003 |bibcode=2004ESRv...66..143B |access-date=23 September 2023}} [70] => [71] => During the earliest Oligocene occurred the Early Oligocene Glacial Maximum (Oi1), which lasted for about 200 thousand years.{{Cite journal |last1=Zachos |first1=James C. |last2=Lohmann |first2=Kyger C. |last3=Walker |first3=James C. G. |last4=Wise |first4=Sherwood W. |date=March 1993 |title=Abrupt Climate Change and Transient Climates during the Paleogene: A Marine Perspective |url=https://www.journals.uchicago.edu/doi/10.1086/648216 |journal=[[The Journal of Geology]] |language=en |volume=101 |issue=2 |pages=191–213 |doi=10.1086/648216 |pmid=11537739 |bibcode=1993JG....101..191Z |s2cid=29784731 |issn=0022-1376 |access-date=23 September 2023}} After Oi1, global mean surface temperature continued to decrease gradually during the [[Rupelian]] Age. Another major cooling event occurred at the end of the Rupelian; its most likely cause was extreme biological productivity in the Southern Ocean fostered by tectonic reorganisation of ocean currents and an influx of nutrients from Antarctica.{{Cite journal |last1=Hochmuth |first1=Katharina |last2=Whittaker |first2=Joanne M. |last3=Sauermilch |first3=Isabel |last4=Klocker |first4=Andreas |last5=Gohl |first5=Karsten |last6=LaCasce |first6=Joseph H. |date=9 November 2022 |title=Southern Ocean biogenic blooms freezing-in Oligocene colder climates |journal=[[Nature Communications]] |language=en |volume=13 |issue=1 |page=6785 |doi=10.1038/s41467-022-34623-9 |pmid=36351905 |pmc=9646741 |bibcode=2022NatCo..13.6785H |issn=2041-1723 }} In the [[Chattian|Late Oligocene]], global temperatures began to warm slightly, though they continued to be significantly lower than during the previous epochs of the Palaeogene and polar ice remained. [72] => [73] => == Palaeogeography == [74] => During the Paleogene, the continents continued to [[plate tectonics|drift]] closer to their current positions. [[India]] was in the process of colliding with Asia, forming the [[Himalayas]]. The [[Atlantic Ocean]] continued to widen by a few centimeters each year. Africa was moving north to collide with Europe and form the [[Mediterranean Sea]], while South America was moving closer to North America (they would later connect at the [[Isthmus of Panama]]). Inland seas retreated from [[North America]] early in the period. Australia had also separated from Antarctica and was drifting toward Southeast Asia. The 1.2 Myear [[Milankovitch cycles|cycle of obliquity amplitude modulation]] governed [[eustatic sea level]] changes on shorter timescales, with periods of low amplitude coinciding with intervals of low sea levels and vice versa.{{cite journal |last1=Liu |first1=Yang |last2=Huang |first2=Chunju |last3=Ogg |first3=James G. |last4=Algeo |first4=Thomas J. |last5=Kemp |first5=David B. |last6=Shen |first6=Wenlong |date=15 September 2019 |title=Oscillations of global sea-level elevation during the Paleogene correspond to 1.2-Myr amplitude modulation of orbital obliquity cycles |url=https://www.sciencedirect.com/science/article/abs/pii/S0012821X19303620 |journal=[[Earth and Planetary Science Letters]] |volume=522 |pages=65–78 |doi=10.1016/j.epsl.2019.06.023 |bibcode=2019E&PSL.522...65L |s2cid=198431567 |access-date=24 November 2022}} [75] => [76] => ==Flora and fauna== [77] => Tropical taxa diversified faster than those at higher latitudes after the Cretaceous–Paleogene extinction event, resulting in the development of a significant latitudinal diversity gradient.{{cite journal |last1=Crame |first1=J. Alistair |date=March 2020 |title=Early Cenozoic evolution of the latitudinal diversity gradient |journal=[[Earth-Science Reviews]] |volume=202 |page=103090 |doi=10.1016/j.earscirev.2020.103090 |bibcode=2020ESRv..20203090C |s2cid=214219923 |doi-access=free }} [[Mammal]]s began a rapid [[Biodiversity|diversification]] during this period. After the Cretaceous–Paleogene extinction event, which saw the demise of the non-avian [[dinosaur]]s, mammals began to evolve from a few small and generalized forms into most of the modern varieties we see presently. Some of these mammals evolved into large forms that dominated the land, while others became capable of living in [[ocean|marine]], specialized terrestrial, and airborne environments. Those that adapted to the oceans became modern [[cetacean]]s, while those that adapted to trees became [[primate]]s, the group to which humans belong. [[Birds]], extant [[dinosaurs]] which were already well established by the end of the [[Cretaceous]], also experienced [[adaptive radiation]] as they took over the skies left empty by the now extinct [[pterosaur]]s. Some flightless birds such as [[penguin]]s, [[ratites]], and [[terror birds]] also filled niches left by the [[hesperornithes]] and other extinct dinosaurs. [78] => [79] => Pronounced cooling in the [[Oligocene]] resulted in a massive floral shift, and many extant modern plants arose during this time. [[Poaceae|Grasses]] and herbs, such as ''[[Artemisia (genus)|Artemisia]]'', began to proliferate, at the expense of tropical plants, which began to decrease. [[Pinophyta|Conifer]] forests developed in mountainous areas. This cooling trend continued, with major fluctuation, until the end of the [[Pleistocene]] period.{{Cite book|title=Paleopalynology|author=Traverse, Alfred|date=1988|publisher=Unwin Hyman|isbn=978-0-04-561001-3|oclc=17674795}} This evidence for this floral shift is found in the [[Palynology|palynological]] record.{{Cite journal|last=Muller|first=Jan|date=January 1981|title=Fossil pollen records of extant angiosperms|journal=The Botanical Review|volume=47|issue=1|pages=1–142|doi=10.1007/bf02860537|bibcode=1981BotRv..47....1M |s2cid=10574478|issn=0006-8101}} {{clear left}} [80] => [81] => ==See also== [82] => *{{annotated link|Cretaceous–Paleogene boundary}} [83] => [84] => ==References== [85] => {{reflist}} [86] => [87] => ==External links== [88] => {{Wikisource portal|Cenozoic#Paleogene}} [89] => {{Commons category|Paleogene}} [90] => *[http://www.foraminifera.eu/querydb.php?period=Paleogene&aktion=suche Paleogene Microfossils: 180+ images of Foraminifera] [91] => *[https://ghkclass.com/ghkC.html?paleogene Paleogene (chronostratigraphy scale)] [92] => [93] => {{Paleogene Footer}} [94] => {{Geological history|p|c}} [95] => [96] => {{Authority control}} [97] => [98] => [[Category:Paleogene| ]] [99] => [[Category:Geological periods]] [] => )
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Paleogene

The Paleogene period is a geologic time period that spans from about 66 million years ago to 23 million years ago. It is part of the Cenozoic Era and follows the Cretaceous period and the mass extinction event that wiped out the dinosaurs.

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It is part of the Cenozoic Era and follows the Cretaceous period and the mass extinction event that wiped out the dinosaurs. The Paleogene is divided into three epochs: the Paleocene, Eocene, and Oligocene. During the Paleogene, the Earth experienced significant climatic changes, including a rapid warming event known as the Paleocene-Eocene Thermal Maximum. This warming led to the expansion of tropical forests and the development of new ecosystems. The period also saw the rise of mammals, which diversified and evolved to take on various ecological niches. Notable mammalian groups that emerged during this time include primates, which eventually gave rise to humans, as well as modern groups such as rodents and carnivores. In addition to the diversification of mammals, the Paleogene also witnessed the evolution of birds, reptiles, and fish. Many modern bird groups, such as songbirds, ducks, and raptors, began to appear during this time. Reptiles, including crocodiles and turtles, also underwent diversification, while fish continued to adapt to different environments. The Paleogene period is significant for its important fossil record, which provides valuable insights into the evolution of life on Earth after the Cretaceous mass extinction. Fossils from this period have been found on every continent, and they have contributed greatly to our understanding of the origins and early evolution of many modern plant and animal groups. Overall, the Paleogene period represents a critical time in Earth's history, following the extinction of the dinosaurs and marking the early stages of the dramatic diversification and evolution of mammals and other life forms that continue to shape the planet today.

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