Neogene
| Neogene Period 23.03–2.58 million years ago | |
Geography of the Earth around Pliocene | |
| Mean atmospheric O 2 content over period duration |
c. 21.5 vol % (108 % of modern level) |
| Mean atmospheric CO 2 content over period duration |
c. 280 ppm (1 times pre-industrial level) |
| Mean surface temperature over period duration | c. 14 °C (0 °C above modern level) |
Key events in the Neogene -24 — – -22 — – -20 — – -18 — – -16 — – -14 — – -12 — – -10 — – -8 — – -6 — – -4 — – -2 — An approximate timescale of key Neogene events. Vertical axis: millions of years ago. | |
The Neogene ( /ˈniː.əˌdʒiːn, ˈniː.oʊ-/ NEE-ə-jeen, NEE-oh-)[3][4] (informally Upper Tertiary or Late Tertiary) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.03 million years ago (Mya) to the beginning of the present Quaternary Period 2.58 Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists[who?] assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868).[5]
During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. Early hominids, the ancestors of humans, appeared in Africa near the end of the period.[citation needed] Some continental movement took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to the Atlantic Ocean, leaving only the Gulf Stream to transfer heat to the Arctic Ocean. The global climate cooled considerably over the course of the Neogene, culminating in a series of continental glaciations in the Quaternary Period that follows.
Divisions[edit]
In ICS terminology, from upper (later, more recent) to lower (earlier):
The Pliocene Epoch is subdivided into 2 ages:
- Piacenzian Age, preceded by
- Zanclean Age
The Miocene Epoch is subdivided into 6 ages:
- Messinian Age, preceded by
- Tortonian Age
- Serravallian Age
- Langhian Age
- Burdigalian Age
- Aquitanian Age
In different geophysical regions of the world, other regional names are also used for the same or overlapping ages and other timeline subdivisions.
The terms Neogene System (formal) and Upper Tertiary System (informal) describe the rocks deposited during the Neogene Period.
Geography[edit]
The continents in the Neogene were very close to their current positions. The Isthmus of Panama formed, connecting North and South America. The Indian subcontinent continued to collide with Asia, forming the Himalayas. Sea levels fell, creating land bridges between Africa and Eurasia and between Eurasia and North America.
Climate[edit]
The global climate became seasonal and continued an overall drying and cooling trend which began at the start of the Paleogene. The ice caps on both poles began to grow and thicken, and by the end of the period the first of a series of glaciations of the current Ice Age began.
Flora and fauna[edit]
Marine and continental flora and fauna have a modern appearance. The reptile group Choristodera became extinct in the early part of the period, while the amphibians known as Allocaudata disappeared at the end. Mammals and birds continued to be the dominant terrestrial vertebrates, and took many forms as they adapted to various habitats. The first hominins, the ancestors of humans, may have appeared in southern Europe and migrated into Africa.[6][7]
In response to the cooler, seasonal climate, tropical plant species gave way to deciduous ones and grasslands replaced many forests. Grasses therefore greatly diversified, and herbivorous mammals evolved alongside it, creating the many grazing animals of today such as horses, antelope, and bison. Eucalyptus fossil leaves occur in the Miocene of New Zealand, where the genus is not native today, but have been introduced from Australia.[8]
Disagreements[edit]
The Neogene traditionally ended at the end of the Pliocene Epoch, just before the older definition of the beginning of the Quaternary Period; many time scales show this division.
However, there was a movement amongst geologists (particularly marine geologists) to also include ongoing geological time (Quaternary) in the Neogene, while others (particularly terrestrial geologists) insist the Quaternary to be a separate period of distinctly different record. The somewhat confusing terminology and disagreement amongst geologists on where to draw what hierarchical boundaries is due to the comparatively fine divisibility of time units as time approaches the present, and due to geological preservation that causes the youngest sedimentary geological record to be preserved over a much larger area and to reflect many more environments than the older geological record.[9] By dividing the Cenozoic Era into three (arguably two) periods (Paleogene, Neogene, Quaternary) instead of seven epochs, the periods are more closely comparable to the duration of periods in the Mesozoic and Paleozoic eras.
The International Commission on Stratigraphy (ICS) once proposed that the Quaternary be considered a sub-era (sub-erathem) of the Neogene, with a beginning date of 2.58 Ma, namely the start of the Gelasian Stage. In the 2004 proposal of the ICS, the Neogene would have consisted of the Miocene and Pliocene epochs.[10] The International Union for Quaternary Research (INQUA) counterproposed that the Neogene and the Pliocene end at 2.58 Ma, that the Gelasian be transferred to the Pleistocene, and the Quaternary be recognized as the third period in the Cenozoic, citing key changes in Earth's climate, oceans, and biota that occurred 2.58 Ma and its correspondence to the Gauss-Matuyama magnetostratigraphic boundary.[11][12] In 2006 ICS and INQUA reached a compromise that made Quaternary a subera, subdividing Cenozoic into the old classical Tertiary and Quaternary, a compromise that was rejected by International Union of Geological Sciences because it split both Neogene and Pliocene in two.[13]
Following formal discussions at the 2008 International Geological Congress in Oslo, Norway,[14] the ICS decided in May 2009 to make the Quaternary the youngest period of the Cenozoic Era with its base at 2.58 Mya and including the Gelasian age, which was formerly considered part of the Neogene Period and Pliocene Epoch.[15] Thus the Neogene Period ends bounding the succeeding Quaternary Period at 2.58 Mya.
References[edit]
- ^ Krijgsman, W.; Garcés, M.; Langereis, C. G.; Daams, R.; Van Dam, J.; Van Der Meulen, A. J.; Agustí, J.; Cabrera, L. (1996). "A new chronology for the middle to late Miocene continental record in Spain". Earth and Planetary Science Letters. 142 (3–4): 367–380. Bibcode:1996E&PSL.142..367K. doi:10.1016/0012-821X(96)00109-4.
- ^ Retallack, G. J. (1997). "Neogene Expansion of the North American Prairie". PALAIOS. 12 (4): 380–390. doi:10.2307/3515337. JSTOR 3515337. Retrieved 2008-02-11.
- ^ "Neogene". Merriam-Webster Dictionary.
- ^ "Neogene". Dictionary.com Unabridged. Random House.
- ^ Hörnes, M. (1853). "Mittheilungen an Professor Bronn gerichtet" [Reports addressed to Professor Bronn]. Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefakten-kunde [New Yearbook for Mineralogy, Geognosy, Geology, and the Study of Fossils] (in German): 806–810. hdl:2027/hvd.32044106271273.
From p. 806: "Das häufige Vorkommen der Wiener Mollusken … im trennenden Gegensatze zu den eocänen zusammenzufassen." (The frequent occurrence of Viennese mollusks in typical Miocene as well as in typical Pliocene deposits motivated me – in order to avoid the perpetual monotony [of providing] details about the deposits – to subsume both deposits provisionally under the name "Neogene" (νεος new and γιγνομαι to arise) in distinguishing contrast to the Eocene.)
- ^ "Scientists find 7.2-million-year-old pre-human remains in the Balkans". Phys.org. Retrieved 17 December 2017.
- ^ "9.7 million-year-old teeth found in Germany resemble those of human ancestors in Africa". ResearchGate. Retrieved 17 December 2017.
- ^ "Eucalyptus fossils in New Zealand - the thin end of the wedge - Mike Pole".
- ^ Tucker, M.E. (2001). Sedimentary petrology : an introduction to the origin of sedimentary rocks (3rd ed.). Osney Nead, Oxford, UK: Blackwell Science. ISBN 978-0-632-05735-1.
- ^ Lourens, L., Hilgen, F., Shackleton, N.J., Laskar, J., Wilson, D., (2004) “The Neogene Period”. In: Gradstein, F., Ogg, J., Smith, A.G. (Eds.), Geologic Time Scale, Cambridge University Press, Cambridge.
- ^ Clague, John et al. (2006) "Open Letter by INQUA Executive Committee" Archived 2006-09-23 at the Wayback Machine Quaternary Perspective, the INQUA Newsletter International Union for Quaternary Research 16(1)
- ^ Clague, John; et al. (2006). "Open Letter by INQUA Executive Committee" (PDF). Quaternary Perspective, the INQUA Newsletter. International Union for Quaternary Research. 16 (1): 158–159. doi:10.1016/j.quaint.2006.06.001. ISSN 1040-6182. Archived from the original (PDF) on 2006-09-23. Retrieved 2006-09-23.
- ^ "ICS: Consolidated Annual Report for 2006" (PDF). Stratigraphy.org. Retrieved 15 June 2007.
- ^ "Geoparks and Geotourism - Field Excursion of South America". 33igc.org. Retrieved 17 December 2017.
- ^ "See the 2009 version of the ICS geologic time scale". Quaternary.stratigraphy.org.uk. Retrieved 17 December 2017.
External links[edit]
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Wikimedia Commons has media related to Neogene. |
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Wikisource has original works on the topic: Cenozoic#Neogene |
- "Digital Atlas of Neogene Life for the Southeastern United States". San Jose State University. Archived from the original on 2013-04-23. Retrieved 21 September 2018.
