Cenozoic

From Wikipedia, the free encyclopedia
  (Redirected from Cenozoic Era)
Jump to: navigation, search
Cenozoic Era
66 - 0 million years ago
Events of the Cenozoic
view • discuss • edit
-70 —
-60 —
-50 —
-40 —
-30 —
-20 —
-10 —
0 —
C
e
n
o
z
o
i
c
An approximate timescale of key Cenozoic events.
Axis scale: Ma before present.

The Cenozoic Era (/sɛnɵˈzɪk/ or /ˌsnɵˈzɪk/; also Cænozoic, Caenozoic or Cainozoic; meaning "new life", from Greek καινός kainos "new", and ζωή zoe "life"[1]) is the current and most recent of the three Phanerozoic geological eras, following the Mesozoic Era and covering the period from 66 million years ago to the present.

The Cenozoic is also known as the Age of Mammals, because the extinction of many groups allowed mammals to greatly diversify.

Early in the Cenozoic, following the K-Pg event, the planet was dominated by relatively small fauna, including small mammals, birds, reptiles, and amphibians. From a geological perspective, it did not take long for mammals and birds to greatly diversify in the absence of the large reptiles that had dominated during the Mesozoic. Some flightless birds grew larger than the average human. These species are sometimes referred to as "terror birds," and were formidable predators. Mammals came to occupy almost every available niche (both marine and terrestrial), and some also grew very large, attaining sizes not seen in most of today's terrestrial mammals.

Climate-wise, the Earth had begun a drying and cooling trend, culminating in the glaciations of the Pleistocene Epoch, and partially offset by the Paleocene-Eocene Thermal Maximum. The continents also began looking roughly familiar at this time and moved into their current positions.

Subdivisions[edit]

The Cenozoic is divided into three periods: The Paleogene, Neogene, and Quaternary; and seven epochs: The Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, and Holocene. The Quaternary Period was officially recognized by the International Commission on Stratigraphy in June 2009,[2] and the former Tertiary Period was officially disused in 2004 because of the necessity to divide the Cenozoic into periods more like that of the previous Paleozoic and Mesozoic eras..[3][why?] The common use of epochs during the Cenozoic helps paleontologists better organize and group the many significant events that occurred during this comparatively short interval of time. There is also more detailed knowledge of this era than any other because of the relatively young strata associated with it.

Tectonics[edit]

Geologically, the Cenozoic is the era when the continents moved into their current positions. Australia-New Guinea, having split from Pangea during the early Cretaceous, drifted north and, eventually, collided with South-east Asia; Antarctica moved into its current position over the South Pole; the Atlantic Ocean widened and, later in the era, South America became attached to North America.

India collided with Asia 55 to 45 million years ago; Arabia collided with Eurasia, closing the Tethys ocean, around 35 million years ago.[4]

Climate[edit]

The Paleocene–Eocene Thermal Maximum of 55.8 million years ago was a significant global warming event; however, since the Azolla event of 49 million years ago, the Cenozoic Era has been a period of long-term cooling. After the tectonic creation of Drake Passage, when South America fully detached from Antarctica during the Oligocene, the climate cooled significantly due to the advent of the Antarctic Circumpolar Current which brought cool deep Antarctic water to the surface. The cooling trend continued in the Miocene, with relatively short warmer periods. When South America became attached to North America creating the Isthmus of Panama, the Arctic region cooled due to the strengthening of the Humboldt and Gulf Stream currents,[5] eventually leading to the glaciations of the Quaternary ice age, the current interglacial of which is the Holocene Epoch.

Life[edit]

Mammals are the dominant terrestrial vertebrates of the Cenozoic.

During the Cenozoic, mammals proliferated from a few small, simple, generalized forms into a diverse collection of terrestrial, marine, and flying animals, giving this period its other name, the Age of Mammals, despite the fact that birds still outnumbered mammals two to one. The Cenozoic is just as much the age of savannas, the age of co-dependent flowering plants and insects, and the age of birds.[6] Grass also played a very important role in this era, shaping the evolution of the birds and mammals that fed on it. One group that diversified significantly in the Cenozoic as well were the snakes. Evolving in the Cenozoic, the variety of snakes increased tremendously, resulting in many colubrids, following the evolution of their current primary prey source, the rodents.

In the earlier part of the Cenozoic, the world was dominated by the gastornid birds, terrestrial crocodiles like Pristichampsus, and a handful of primitive large mammal groups like uintatheres, mesonychids, and pantodonts. But as the forests began to recede and the climate began to cool, other mammals took over.

The Cenozoic is full of mammals both strange and familiar, including chalicotheres, creodonts, whales, primates, entelodonts, saber-toothed cats, mastodons and mammoths, three-toed horses, giant rhinoceros like Indricotherium, the rhinoceros-like brontotheres, various bizarre groups of mammals from South America, such as the vaguely elephant-like pyrotheres and the dog-like marsupial relatives called borhyaenids and the monotremes and marsupials of Australia.


See also[edit]

References[edit]

  1. ^ "Cenozoic". Online Etymology Dictionary. 
  2. ^ Gibbard, P. L.; Head, M. J.; Walker, M. J. C. (2010). "Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma". Journal of Quaternary Science 25 (2): 96. Bibcode:2010JQS....25...96G. doi:10.1002/jqs.1338.  edit
  3. ^ International Stratigraphic Chart
  4. ^ Allen, M. B.; Armstrong, H. A. (2008). "Arabia-Eurasia collision and the forcing of mid Cenozoic global cooling". Palaeogeography Palaeoclimatology Palaeoecology 265 (1–2): 52–58. doi:10.1016/j.palaeo.2008.04.021.  edit
  5. ^ http://www.whoi.edu/oceanus/viewArticle.do?id=2508
  6. ^ http://www.ucmp.berkeley.edu/cenozoic/cenozoic.php

Bibliography[edit]

  • British Caenozoic Fossils, 1975, The Natural History Museum, London.
  • Geologic Time, by Henry Roberts.
  • After the Dinosaurs: The Age of Mammals, by Donald R. Prothero, Bloomington, Indiana: Indiana University Press, 2006. ISBN 0-253-34733-5
Preceded by Proterozoic Eon Phanerozoic Eon
Paleozoic Era Mesozoic Era Cenozoic Era
Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene 4ry