Source: Wikipedia, the free encyclopedia.
23.03 ± 0.3 – 2.588 ± 0.04 Ma
Stratigraphic unitSystem
Time span formalityFormal
Lower boundary definition
Lower boundary GSSPLemme-Carrosio Section, Carrosio, Italy
44°39′32″N 8°50′11″E / 44.6589°N 8.8364°E / 44.6589; 8.8364
Lower GSSP ratified1996[4]
Upper boundary definition
Upper boundary GSSPMonte San Nicola Section,

(1 times pre-industrial)
Mean surface temperaturec. 14 °C
(0 °C above modern)

The Neogene (

epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary.[8] The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868).[9] The earlier term Tertiary Period was used to define the span of time now covered by Paleogene and Neogene and, despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use.[10]

During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (Homo habilis) appeared in Africa near the end of the period.[11] Some continental movements 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 throughout the Neogene, culminating in a series of continental glaciations in the Quaternary Period that follows.


In ICS terminology, from upper (later, more recent) to lower (earlier):

The Pliocene Epoch is subdivided into two ages:

The Miocene Epoch is subdivided into six ages:

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.


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.


The global climate became more seasonal and continued an overall drying and cooling trend which began during the

Green Sahara phases of wet conditions in North Africa were frequent and occurred about every 21 kyr, being especially intense when Earth's orbit's eccentricity was high.[17] The PWI had similar levels of atmospheric carbon dioxide to contemporary times and is often seen as an analogous climate to the projected climate of the near future as a result of anthropogenic global warming.[18] Towards the end of the Pliocene, decreased heat transport towards the Antarctic resulting from a weakening of the Indonesian Throughflow (ITF) cooled the Earth, a process that exacerbated itself in a positive feedback as sea levels dropped and the ITF diminished and further limited the heat transported southward by the Leeuwin Current.[19] By the end of the period the first of a series of glaciations of the current Ice Age began.[20]

Flora and fauna

Marine and continental flora and fauna have a modern appearance. The reptile group Choristodera went extinct in the early part of the period, while the amphibians known as Allocaudata disappeared at the end of it. Neogene also marked the end of the reptilian genera Langstonia and Barinasuchus, terrestrial predators that were the last surviving members of Sebecosuchia, a group related to crocodiles. The oceans were dominated by large carnivores like megalodons and livyatans, and 19 million years ago about 70% of all pelagic shark species disappeared.[21] Mammals and birds continued to be the dominant terrestrial vertebrates, and took many forms as they adapted to various habitats. An explosive radiation of ursids took place at the Miocene-Pliocene boundary.[22] The first hominins, the ancestors of humans may have appeared in southern Europe and migrated into Africa.[23][24] The first humans (belonging to the species Homo habilis) appeared in Africa near the end of the period.[11]

About 20 million years ago gymnosperms in the form of some conifer and cycad groups started to diversify and produce more species due to the changing conditions.[25] 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. Ice age mammals like the mammoths and woolly rhinoceros were common in Pliocene. With lower levels of CO2 in the atmosphere, C4 plants expanded and reached ecological dominance in grasslands during the last 10 million years. Also Asteraceae (daisies) went through a significant adaptive radiation.[26] Eucalyptus fossil leaves occur in the Miocene of New Zealand, where the genus is not native today, but have been introduced from Australia.[27]


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.[8] 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.


Gauss-Matuyama magnetostratigraphic boundary.[29][30] In 2006 ICS and INQUA reached a compromise that made Quaternary a sub-era, 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.[31]

Following formal discussions at the 2008 International Geological Congress in Oslo, Norway,[32] 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.[33] Thus the Neogene Period ends bounding the succeeding Quaternary Period at 2.58 Mya.


  1. .
  2. . Retrieved 2008-02-11.
  3. ^ "ICS Timescale Chart" (PDF).
  4. .
  5. . Retrieved 8 December 2020.
  6. ^ "Neogene". Dictionary.
  7. ^ "Neogene". Unabridged (Online). n.d.
  8. ^ .
  9. . 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.)
  10. ^ "GeoWhen Database – What Happened to the Tertiary?".
  11. ^
    S2CID 4470282
  12. ^
    S2CID 233579194. Archived from the original on 8 January 2021. Retrieved 17 July 2023. Alt URL
  13. . Retrieved 30 November 2022.
  14. .
  15. .
  16. . Retrieved 17 March 2023.
  17. .
  18. .
  19. . Retrieved 13 April 2024 – via Elsevier Science Direct.
  20. .
  21. ^ Almost 20 Million Years Ago, Sharks Nearly Went Extinct
  22. PMID 18662376
  23. ^ "Scientists find 7.2-million-year-old pre-human remains in the Balkans". Retrieved 17 December 2017.
  24. ^ "9.7 million-year-old teeth found in Germany resemble those of human ancestors in Africa". ResearchGate. Retrieved 17 December 2017.
  25. ^ DNA duplication linked to the origin and evolution of pine trees and their relatives
  26. PMID 35022396
  27. ^ "Eucalyptus fossils in New Zealand – the thin end of the wedge – Mike Pole". 22 September 2014.
  28. ^ 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.
  29. ^ 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)
  30. ISSN 1040-6182. Archived from the original
    (PDF) on 2006-09-23. Retrieved 2006-09-23.
  31. ^ "ICS: Consolidated Annual Report for 2006" (PDF). Retrieved 15 June 2007.
  32. ^ "Geoparks and Geotourism – Field Excursion of South America". Retrieved 17 December 2017.
  33. ^ "See the 2009 version of the ICS geologic time scale". Retrieved 17 December 2017.

External links