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{{short description|Timeline of notable events in the sudy of ancient life}}
{{short description|none}} <!-- "none" is preferred when the title is sufficiently descriptive; see [[WP:SDNONE]] -->
{{paleontology}}
{{paleontology}}
'''[[Chronology|Timeline]] of [[paleontology]]'''
'''[[Chronology|Timeline]] of [[paleontology]]'''


==Antiquity - XVI century==
==Antiquity 16th century==
* 6th century B.C.&nbsp;— The [[pre-Socratic]] Greek philosopher [[Xenophanes]] of Colophon argues that fossils of marine organisms show that dry land was once under water.<ref>{{cite web|url=http://www.ucmp.berkeley.edu/history/ancient.html|title=Evolution and Paleontology in the Ancient World|publisher=University of California Museum of Paleontology|access-date=2012-07-05}}</ref>
* 6th century B.C.&nbsp;— The [[pre-Socratic]] Greek philosopher [[Xenophanes]] of Colophon argues that fossils of marine organisms show that dry land was once under water.<ref>{{cite web|url=http://www.ucmp.berkeley.edu/history/ancient.html|title=Evolution and Paleontology in the Ancient World|publisher=University of California Museum of Paleontology|access-date=2012-07-05}}</ref>
* 4th century B.C.&nbsp;—[[Aristotle]] posits that the [[Rock (geology)|stoniness]] of [[fossil]]s is caused by vaporous exhalations.<ref name=Rudwick />
* 4th century B.C.&nbsp;—&nbsp;[[Aristotle]] posits that the [[Rock (geology)|stoniness]] of [[fossil]]s is caused by vaporous exhalations.<ref name=Rudwick />
* 1027&nbsp;— The [[Islamic geography|Persian naturalist]] [[Avicenna]] elaborates on Aristotle's speculations in ''[[The Book of Healing]]'' by proposing that fossils are caused by [[Petrifaction|petrifying]] fluids (''succus lapidificatus'').<ref name=Rudwick>{{Cite book|title=The Meaning of Fossils: Episodes in the History of Palaeontology|first=M. J. S.|last=Rudwick|year=1985|publisher=[[University of Chicago Press]]|isbn=0-226-73103-0|page=24}}</ref>
* 1027&nbsp;— The [[Islamic geography|Persian naturalist]] [[Avicenna]] elaborates on Aristotle's speculations in ''[[The Book of Healing]]'' by proposing that fossils are caused by [[Petrifaction|petrifying]] fluids (''succus lapidificatus'').<ref name=Rudwick>{{Cite book|title=The Meaning of Fossils: Episodes in the History of Palaeontology|first=M. J. S.|last=Rudwick|year=1985|publisher=[[University of Chicago Press]]|isbn=0-226-73103-0|page=24}}</ref>
* 1031-1095&nbsp;— The [[History of science and technology in China|Chinese naturalist]] [[Shen Kuo]] uses evidence of [[Marine (ocean)|marine]] fossils found in the [[Taihang Mountains]] to infer geological processes caused shifting of seashores over time,<ref>[[Shen Kuo]],''Mengxi Bitan'' (梦溪笔谈; ''[[Dream Pool Essays]]'') (1088)</ref> and uses petrified [[bamboo]]s found underground in [[Yan'an]], to argue for gradual [[climate change (general concept)|climate change]].<ref name="needham volume 3 614">{{cite book|last=Needham|first=Joseph|author-link=Joseph Needham|title=''Science and Civilization in China: Volume 3, Mathematics and the Sciences of the Heavens and the Earth''|publisher=Caves Books Ltd|year=1986|isbn=0-253-34547-2|page=614}}</ref>
* 1031-1095&nbsp;— The [[History of science and technology in China|Chinese naturalist]] [[Shen Kuo]] uses evidence of [[Marine (ocean)|marine]] fossils found in the [[Taihang Mountains]] to infer geological processes caused shifting of seashores over time,<ref>[[Shen Kuo]],''Mengxi Bitan'' (梦溪笔谈; ''[[Dream Pool Essays]]'') (1088)</ref> and uses petrified [[bamboo]]s found underground in [[Yan'an]], to argue for gradual [[climate change (general concept)|climate change]].<ref name="needham volume 3 614">{{cite book|last=Needham|first=Joseph|author-link=Joseph Needham|title=''Science and Civilization in China: Volume 3, Mathematics and the Sciences of the Heavens and the Earth''|publisher=Caves Books Ltd|year=1986|isbn=0-253-34547-2|page=614}}</ref>
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==17th century==
==17th century==
* 1665&nbsp;— In his book ''[[Micrographia]]'' [[Robert Hooke]] compares [[petrified wood]] to wood, concludes that petrified wood formed from wood soaked in mineral-rich water, and argues that fossils like ''[[Ammonite]]'' shells were produced the same way, sparking debate over the organic origin of fossils and the possibility of [[extinction]]. <ref name="Rudwick45_68">{{Cite book|title=The Meaning of Fossils: Episodes in the History of Palaeontology|first=M. J. S.|last=Rudwick|year=1985|publisher=[[University of Chicago Press]]|isbn=0-226-73103-0|pages=45–68}}</ref>
* 1665&nbsp;— In his book ''[[Micrographia]]'' [[Robert Hooke]] compares [[petrified wood]] to wood, concludes that petrified wood formed from wood soaked in mineral-rich water, and argues that fossils like ''[[Ammonite]]'' shells were produced the same way, sparking debate over the organic origin of fossils and the possibility of [[extinction]].<ref name="Rudwick45_68">{{Cite book|title=The Meaning of Fossils: Episodes in the History of Palaeontology|first=M. J. S.|last=Rudwick|year=1985|publisher=[[University of Chicago Press]]|isbn=0-226-73103-0|pages=45–68}}</ref>
* 1669&nbsp;— [[Nicholas Steno]] writes that [[sedimentary rock|some kinds of rock]] formed from layers of sediment deposited in water, and that fossils were organic remains buried in the process.<ref name="Rudwick45_68"/>
* 1669&nbsp;— [[Nicolas Steno]] writes that [[sedimentary rock|some kinds of rock]] formed from layers of sediment deposited in water, and that fossils were organic remains buried in the process.<ref name="Rudwick45_68"/>
* 1699&nbsp;- [[Edward Lhuyd]] names the new sauropod genus and species "''[[List of informally named dinosaurs|Ruttelum implicatum]]''". By doing so, he names the first prehistoric creature that is recognizable as a dinosaur.
* 1699&nbsp;- [[Edward Lhuyd]] names the new sauropod genus and species "''[[List of informally named dinosaurs|Ruttelum implicatum]]''". By doing so, he names the first prehistoric creature that is recognizable as a dinosaur.{{Fact|date=August 2023}}


==18th century==
==18th century==
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==19th century==
==19th century==
* 1808&nbsp;— Cuvier and [[Alexandre Brongniart]] publish preliminary results of their survey of the geology of the [[Paris Basin]] that uses the fossils found in different strata to reconstruct the geologic history of the region.<ref> Rudwick, Martin, ''Georges Cuvier: Fossil Bones and Geological Catastrophes'' (1997), pp. 127-156</ref>
* 1804&nbsp;— Cuvier writes about fossils of extinct mammals from the [[Paris Basin]], arguing that they are similar to other mammals such as ruminants but also differ by dental and postcranial morphologies. He named two genera ''[[Palaeotherium]]'' and ''[[Anoplotherium]]''.
* 1808&nbsp;— Cuvier and [[Alexandre Brongniart]] publish preliminary results of their survey of the geology of the Paris Basin that uses the fossils found in different strata to reconstruct the geologic history of the region.<ref> Rudwick, Martin, ''Georges Cuvier: Fossil Bones and Geological Catastrophes'' (1997), pp. 127-156</ref>
* 1811&nbsp;— [[Mary Anning]] and her brother Joseph discover the fossilized remains of an ''[[Ichthyosaur]]'' at [[Lyme Regis]].
* 1811&nbsp;— [[Mary Anning]] and her brother Joseph discover the fossilized remains of an ''[[Ichthyosaur]]'' at [[Lyme Regis]].
* 1812&nbsp;- Cuvier draws skeletal reconstructions of "''Palaeotherium''" ''minor'' (= ''[[Plagiolophus (mammal)|Plagiolophus]] minor''), "''Anoplotherium medium''" (= ''[[Xiphodon]] gracilis''), and, most famously, ''Anoplotherium commune'' based on known fossil remains (of which ''A. commune'' was the most nearly complete) and publishes them in his 1812 summary of fossil mammals from Paris. He also drew speculative reconstructions of the muscles of ''A. commune'' to showcase its robustness but did not publish them out of concern of negative perceptions on speculations.
* 1815&nbsp;— [[William Smith (geologist)|William Smith]] published ''[[The Map that Changed the World]]'', the first geologic map of England, Wales, and southern Scotland, using fossils to correlate rock strata.
* 1815&nbsp;— [[William Smith (geologist)|William Smith]] published ''[[The Map that Changed the World]]'', the first geologic map of England, Wales, and southern Scotland, using fossils to correlate rock strata.
* 1821&nbsp;— [[William Buckland]] analyzes [[Kirkdale Cave]] in [[Yorkshire]], containing the bones of [[lions]], [[elephants]] and [[rhinoceros]], and concludes it was a prehistoric [[hyena]] den.
* 1821&nbsp;— [[William Buckland]] analyzes [[Kirkdale Cave]] in [[Yorkshire]], containing the bones of [[lions]], [[elephants]] and [[rhinoceros]], and concludes it was a prehistoric [[hyena]] den.
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* 1829&nbsp;— Buckland publishes paper on work he and Mary Anning had done identifying and analyzing fossilized feces found at Lyme Regis and elsewhere. Buckland coins the term "[[coprolite]]" for them, and uses them to analyze ancient [[food chains]].<ref>Rudwick, Martin ''Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform'' (2008) pp. 153-155</ref>
* 1829&nbsp;— Buckland publishes paper on work he and Mary Anning had done identifying and analyzing fossilized feces found at Lyme Regis and elsewhere. Buckland coins the term "[[coprolite]]" for them, and uses them to analyze ancient [[food chains]].<ref>Rudwick, Martin ''Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform'' (2008) pp. 153-155</ref>
* 1830&nbsp;— The [[Cuvier–Geoffroy debate]] in Paris on the determination of animal structure
* 1830&nbsp;— The [[Cuvier–Geoffroy debate]] in Paris on the determination of animal structure
* 1831&nbsp;— Mantell publishes an influential paper entitled "The Age of Reptiles" summarizing evidence of an extended period during which large reptiles had been the dominant animals.<ref>Cadbury, Deborah ''The Dinosaur Hunters (2000) pp. 171-175.</ref>
* 1831&nbsp;— Mantell publishes an influential paper entitled "The Age of Reptiles" summarizing evidence of an extended period during which large reptiles had been the dominant animals.<ref>Cadbury, Deborah ''The Dinosaur Hunters'' (2000) pp. 171-175.</ref>
* 1832&nbsp;— Mantell finds partial skeleton of the dinosaur ''[[Hylaeosaurus]]''.
* 1832&nbsp;— Mantell finds partial skeleton of the dinosaur ''[[Hylaeosaurus]]''.
* 1836&nbsp;— [[Edward Hitchcock]] describes footprints ([[Eubrontes]] and [[Otozoum]]) of giant birds from Jurassic formations in Connecticut. Later they would be recognized as dinosaur tracks.
* 1836&nbsp;— [[Edward Hitchcock]] describes footprints ([[Eubrontes]] and [[Otozoum]]) of giant birds from Jurassic formations in Connecticut. Later they would be recognized as dinosaur tracks.
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* 1856&nbsp;— Fossils are found in the [[Neandertal|Neander Valley]] in Germany that [[Johann Carl Fuhlrott]] and [[Hermann Schaaffhausen]] recognize as a human different from modern people. A few years later [[William King (geologist)|William King]] names ''[[Neanderthal|Homo neanderthalensis]]''.
* 1856&nbsp;— Fossils are found in the [[Neandertal|Neander Valley]] in Germany that [[Johann Carl Fuhlrott]] and [[Hermann Schaaffhausen]] recognize as a human different from modern people. A few years later [[William King (geologist)|William King]] names ''[[Neanderthal|Homo neanderthalensis]]''.
* 1858&nbsp;— The first dinosaur skeleton found in the United States, ''[[Hadrosaurus]]'', is excavated and described by [[Joseph Leidy]].
* 1858&nbsp;— The first dinosaur skeleton found in the United States, ''[[Hadrosaurus]]'', is excavated and described by [[Joseph Leidy]].
* 1859&nbsp;— [[Charles Darwin]] publishes ''[[On The Origin of Species]]''.
* 1859&nbsp;— [[Charles Darwin]] publishes ''[[On the Origin of Species]]''.
* 1861&nbsp;— The first ''[[Archaeopteryx]]'', skeleton is found in [[Bavaria]], [[Germany]], and recognized as a [[transitional fossil|transitional form]] between reptiles and birds.
* 1861&nbsp;— The first ''[[Archaeopteryx]]'', skeleton is found in [[Bavaria]], [[Germany]], and recognized as a [[transitional fossil|transitional form]] between reptiles and birds.
* 1869&nbsp;— [[Joseph Lockyer]] starts the [[scientific journal]] ''[[Nature (journal)|Nature]]''.
* 1869&nbsp;— [[Joseph Lockyer]] starts the [[scientific journal]] ''[[Nature (journal)|Nature]]''.
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* 1947&nbsp;— [[Willard Libby]] introduces [[Radiocarbon dating|carbon-14 dating]].
* 1947&nbsp;— [[Willard Libby]] introduces [[Radiocarbon dating|carbon-14 dating]].
* 1953&nbsp;— [[Stanley A. Tyler]] discovers [[fossils#Microfossils|microfossils]] in the [[gunflint chert]] formation of [[cyanobacteria]] that created pre-Cambrian [[stromatolites]] approximately 2 billion years ago.
* 1953&nbsp;— [[Stanley A. Tyler]] discovers [[fossils#Microfossils|microfossils]] in the [[gunflint chert]] formation of [[cyanobacteria]] that created pre-Cambrian [[stromatolites]] approximately 2 billion years ago.
* 1967&nbsp;— [[Paul Schultz Martin|Paul S. Martin]] proposes the [[Quaternary extinction event#Overkill hypothesis|overkill hypothesis]], that the extinction of the [[Pleistocene megafauna]] in North America resulted from over hunting by Native Americans.
* 1972&nbsp;— [[Niles Eldredge]] and [[Stephen Jay Gould]] propose [[punctuated equilibrium]], claiming that the evolutionary history of most species involves long intervals of stasis between relatively short periods of rapid change.
* 1972&nbsp;— [[Niles Eldredge]] and [[Stephen Jay Gould]] propose [[punctuated equilibrium]], claiming that the evolutionary history of most species involves long intervals of stasis between relatively short periods of rapid change.
* 1974&nbsp;— [[Donald Johanson]] and Tom Gray discover a 3.5 million-year-old female hominid fossil that is 40% complete and name it "[[Lucy (Australopithecus)|Lucy]]."
* 1974&nbsp;— [[Donald Johanson]] and Tom Gray discover a 3.5 million-year-old female hominid fossil that is 40% complete and name it "[[Lucy (Australopithecus)|Lucy]]."
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* 2004&nbsp;— ''[[Tiktaalik]]'', a [[transitional fossil|transitional form]] between [[Sarcopterygii|lobe-finned fish]] and [[tetrapods]] is discovered in Canada by [[Ted Daeschler]], [[Neil H. Shubin]], and [[Farish A. Jenkins Jr]].
* 2004&nbsp;— ''[[Tiktaalik]]'', a [[transitional fossil|transitional form]] between [[Sarcopterygii|lobe-finned fish]] and [[tetrapods]] is discovered in Canada by [[Ted Daeschler]], [[Neil H. Shubin]], and [[Farish A. Jenkins Jr]].
* 2009&nbsp;— Fossils of ''[[Titanoboa]]'', a giant snake, are unearthed in the coal mines of [[Cerrejón]] in [[La Guajira]], [[Colombia]], suggesting [[paleocene]] equatorial temperatures were higher than today.<ref>{{cite journal|last=Head|first=Jason J.|author2=Jonathan I. Bloch |author3=Alexander K. Hastings |author4=Jason R. Bourque |author5=Edwin A. Cadena |author6=Fabiany A. Herrera |author7=P. David Polly |author8=Carlos A. Jaramillo |title=Giant boid snake from the paleocene neotropics reveals hotter past equatorial temperatures.|journal=[[Nature (journal)|Nature]]|volume=457|issue=7230|pages=715–718|doi=10.1038/nature07671|pmid=19194448|year=2009}}</ref>
* 2009&nbsp;— Fossils of ''[[Titanoboa]]'', a giant snake, are unearthed in the coal mines of [[Cerrejón]] in [[La Guajira]], [[Colombia]], suggesting [[paleocene]] equatorial temperatures were higher than today.<ref>{{cite journal|last=Head|first=Jason J.|author2=Jonathan I. Bloch |author3=Alexander K. Hastings |author4=Jason R. Bourque |author5=Edwin A. Cadena |author6=Fabiany A. Herrera |author7=P. David Polly |author8=Carlos A. Jaramillo |title=Giant boid snake from the paleocene neotropics reveals hotter past equatorial temperatures.|journal=[[Nature (journal)|Nature]]|volume=457|issue=7230|pages=715–718|doi=10.1038/nature07671|pmid=19194448|year=2009}}</ref>
* 2016&nbsp;— Tail fossils of a baby species of ''[[Coelurosaur]],'' fully preserved in amber including soft tissue, are found in [[Myanmar]] by Lida Xing<ref>{{cite web|url=https://www.nationalgeographic.com/animals/article/feathered-dinosaur-tail-amber-theropod-myanmar-burma-cretaceous|last=Romey|first=Kristin|title=WATCH: PICTURES OF THE FIRST DINOSAUR TAIL EVER PRESERVED IN AMBER|publisher=National Geographic|access-date=2021-06-26}}</ref>
* 2016&nbsp;— Tail fossils of a baby species of ''[[Coelurosaur]],'' fully preserved in amber including soft tissue, are found in [[Myanmar]] by Lida Xing<ref>{{cite web|url=https://www.nationalgeographic.com/animals/article/feathered-dinosaur-tail-amber-theropod-myanmar-burma-cretaceous|archive-url=https://web.archive.org/web/20210225114107/https://www.nationalgeographic.com/animals/article/feathered-dinosaur-tail-amber-theropod-myanmar-burma-cretaceous|url-status=dead|archive-date=February 25, 2021|last=Romey|first=Kristin|title=WATCH: PICTURES OF THE FIRST DINOSAUR TAIL EVER PRESERVED IN AMBER|publisher=National Geographic|access-date=2021-06-26}}</ref>


==See also==
==See also==

Latest revision as of 10:43, 18 July 2024

Timeline of paleontology

Antiquity – 16th century

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17th century

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18th century

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19th century

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20th century

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21st century

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See also

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References

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  1. ^ "Evolution and Paleontology in the Ancient World". University of California Museum of Paleontology. Retrieved 2012-07-05.
  2. ^ a b c Rudwick, M. J. S. (1985). The Meaning of Fossils: Episodes in the History of Palaeontology. University of Chicago Press. p. 24. ISBN 0-226-73103-0.
  3. ^ Shen Kuo,Mengxi Bitan (梦溪笔谈; Dream Pool Essays) (1088)
  4. ^ Needham, Joseph (1986). Science and Civilization in China: Volume 3, Mathematics and the Sciences of the Heavens and the Earth. Caves Books Ltd. p. 614. ISBN 0-253-34547-2.
  5. ^ Baucon, A. 2010. Leonardo da Vinci, the founding father of ichnology. Palaios 25. Abstract available from the author's homepage
  6. ^ a b Rudwick, M. J. S. (1985). The Meaning of Fossils: Episodes in the History of Palaeontology. University of Chicago Press. pp. 45–68. ISBN 0-226-73103-0.
  7. ^ Rudwick, Martin, Georges Cuvier: Fossil Bones and Geological Catastrophes (1997), p. 158
  8. ^ "Mosasaurus hoffmanni - The First Discovery of a Mosasaur?". Oceans of Kansas. Retrieved 2012-07-22.
  9. ^ Rudwick, Martin, Georges Cuvier: Fossil Bones and Geological Catastrophes (1997), pp. 25-32
  10. ^ Rudwick, M. J. S. (1985). The Meaning of Fossils: Episodes in the History of Palaeontology. University of Chicago Press. pp. 101–109. ISBN 0-226-73103-0.
  11. ^ Rudwick, Martin, Georges Cuvier: Fossil Bones and Geological Catastrophes (1997), pp. 127-156
  12. ^ Rudwick, Martin Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform (2008) pp. 77-79
  13. ^ Rudwick, Martin Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform (2008) pp. 153-155
  14. ^ Cadbury, Deborah The Dinosaur Hunters (2000) pp. 171-175.
  15. ^ Lewin, Roger (1987), Bones of Contention, ISBN 0-671-52688-X
  16. ^ Head, Jason J.; Jonathan I. Bloch; Alexander K. Hastings; Jason R. Bourque; Edwin A. Cadena; Fabiany A. Herrera; P. David Polly; Carlos A. Jaramillo (2009). "Giant boid snake from the paleocene neotropics reveals hotter past equatorial temperatures". Nature. 457 (7230): 715–718. doi:10.1038/nature07671. PMID 19194448.
  17. ^ Romey, Kristin. "WATCH: PICTURES OF THE FIRST DINOSAUR TAIL EVER PRESERVED IN AMBER". National Geographic. Archived from the original on February 25, 2021. Retrieved 2021-06-26.