Information about Radiation (biology)

Evolutionary radiation is a term used by biologists and palaeontologists to describe a dramatic and rapid (in geological terms) increase in the taxonomic diversity of a particular group of organisms. Typically, this diversification reveals a trend from a small number of similar ecological niches to a wide range of dissimilar ones. In other words, where a particular taxonomic group initially occupied one particular way of life, after a few million years it occupies many different ways of life.

Perhaps the most familiar example of an evolutionary radiation is that of placental mammals immediately after the extinction of the dinosaurs at the end of the Cretaceous, about 65 million years ago. At that time, the placental mammals were mostly small, insect-eating animals similar in size and shape to modern shrews. By the Eocene (58-37 million years ago), they had evolved into such diverse forms as bats, whales, and horses. [1]

Evolutionary radiation in the fossil record

Much of the work carried out by palaeontologists studying evolutionary radiations has been using marine invertebrate fossils simply because these tend to be much more numerous and easy to collect in quantity than large land vertebrates such as mammals or dinosaurs. Brachiopods, for example, underwent major bursts of evolutionary radiation in the Early Cambrian, Early Ordovician, to a lesser degree throughout the Silurian and Devonian, and then again during the Carboniferous. During these periods, different species of brachiopods independently assumed a similar morphology, and presumably mode of life, to species that had lived millions of years before. This phenomenon, known as homeomorphy is explained by convergent evolution: when subjected to similar selective pressures, organisms will often evolve similar adaptations. [2]. Further examples of rapid evolutionary radiation can be observed among ammonites, which suffer a series of extinctions from which they repeatedly re-diversify; and trilobites which, during the Cambrian, rapidly evolved into a variety of forms occupying many of the niches exploited by crustaceans today [3], [4], [5]

Recent evolutionary radiations

A number of groups have undergone evolutionary radiation in relatively recent times. The cichlids in particular have been much studied by biologists. In places such as Lake Malawi they have evolved into a very wide variety of forms, including species that are filter feeders, snail eaters, brood parasites, algal grazers, and fish-eaters. [6] Grasses have been another success, evolving in parallel with grazing herbivores such as horses and antelope [1].

What causes evolutionary radiation?

In some cases, evolutionary radiation was likely driven by the sudden removal of whatever group of animal was dominant at the time. For the mammals, it seems most likely that they were limited to shrew-like lifestyles because the dinosaurs occupied all the other niches that the primitive mammals might have exploited. In other cases, evolutionary 'breakthroughs' suddenly allowed new groups of organisms to occupy niches that simply didin't exist beforehand. This is likely what drove the rapid evolution of birds and terrestrial plants, for example [7], [8].

References

1. ^ This topic is covered in a very accessible manner in Chapter 11 of Richard Fortey's Life: An Unauthorised Biography (1997)
2. ^ Living and Fossil Brachiopods by M. J. S. Rudwick (1970)
3. ^ Aquagenesis, The Origins and Evolution of Life in the Sea by Richard Ellis (2001)
4. ^ Ammonites by Neale Monks & Philip Palmer (2002)
5. ^ Trilobite, Eyewitness to Evolution by Richard Fortey (2000)
6. ^ The Cichlid Fishes: Nature's Grand Experiment in Evolution by George Barlow (2002)
7. ^ The Origin and Evolution of Birds by Alan Feduccia (1999)
8. ^ From the Beginning by Katie Edwards & Brian Rosen (2000)


Taxonomy is the practice and science of classification. The word comes from the Greek τάξις, taxis, 'order' +
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niche (pronounced nich, neesh or nish)[] is a term describing the relational position of a species or population in its ecosystem[1]. The ecological niche describes how an organism or population responds to the distribution of resources and competitors (e. g.
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Eutheria

Orders[1]
  • Bobolestes
  • Eomaia
  • Maelestes
  • Montanalestes
  • Murtoilestes
  • Prokennalestes
  • Placentalia
  • Superorder

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extinction is the cessation of existence of a species or group of taxa, reducing biodiversity. The moment of extinction is generally considered to be the death of the last individual of that species (although the capacity to breed and recover may have been lost before this point).
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Dinosauria *
Owen, 1842

Orders & Suborders
  • Ornithischia
  • Cerapoda
  • Thyreophora
  • Saurischia

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The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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Soricidae
G. Fischer, 1814

Subfamilies

Crocidurinae
Myosoricinae
Soricinae
Shrews are small, superficially mouse-like mammals of the family Soricidae.
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The Eocene epoch (55.8 ± 0.2 - 33.9 ± 0.1 Ma) is a major division of the geologic timescale and the second epoch of the Palaeogene period in the Cenozoic era. The Eocene spans the time from the end of the Paleocene epoch to the beginning of the Oligocene epoch.
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Invertebrate is an English word that describes any animal without a spinal column. The group includes 97% of all animal species — all animals except those in the Chordate subphylum Vertebrata (fish, reptiles, amphibians, birds and mammals).
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For other uses of the term, see Fossil (disambiguation)


FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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Vertebrata
Cuvier, 1812

Classes and Clades

See below
Vertebrates are members of the subphylum Vertebrata (within the phylum Chordata), specifically, those chordates with backbones or spinal columns.
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The Cambrian is a major division of the geologic timescale that begins about 542 ± 1.0 Ma (million years ago) at the end of the Proterozoic eon and ended about 488.3 ± 1.7 Ma with the beginning of the Ordovician period (ICS, 2004).
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The Ordovician period is the second of the six (seven in North America) periods[1] of the Paleozoic era, and covers the time roughly between 490 to 440 million years ago. It follows the Cambrian period and is followed by the Silurian period.
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The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443.7 ± 1.5 Ma (million years ago), to the beginning of the Devonian period, about 416.0 ± 2.8 Ma (ICS 2004).
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Devonian is a geologic period of the Paleozoic era spanning from roughly 416 to 359 million years ago. It is named after Devon, England, where rocks from this period were first studied.
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The Carboniferous is a major division of the geologic timescale that extends from the end of the Devonian period, about 359.2 ± 2.5 Ma (million years ago), to the beginning of the Permian period, about 299.0 ± 0.8 Ma (ICS 2004).
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In evolutionary biology, convergent evolution is the process whereby organisms not closely related (not monophyletic), independently evolve similar traits as a result of having to adapt to similar environments or ecological niches[1].
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Trilobita
Walch, 1771

Orders
  • Agnostida
  • Nectaspida
  • Redlichiida
  • Corynexochida
  • Lichida
  • Phacopida
Subclass: Librostoma
  • Proetida
  • Asaphida
  • Harpetida
  • Ptychopariida


Trilobites
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crustaceans (Crustacea) are a large group of arthropods, comprising approximately 52,000 described species [1], and are usually treated as a subphylum [2].
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Cichlidae

Subfamilies

Astronotinae
Cichlasomatinae
Cichlinae
Etroplinae
Geophaginae
Heterochromidinae
Paratilapiinae
Pseudocrenilabrinae
Ptychochrominae
Retroculinae
For genera, see below.
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Coordinates Coordinates:
Lake type Rift lake
Primary sources Ruhuhu[]

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Grass is a common word that generally describes a monocotyledonous green plant in the family Gramineae (Poaceae). True grasses include most plants grown as grains, for pasture, and for lawns (turf).
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Grazing generally describes a type of predation in which an herbivore feeds on plants (such as grasses), or more broadly on a multicellular autotrophs (such as kelp). Grazing differs from true predation because the organism being eaten is not killed, and it differs from parasitism
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H.O.R.S.E. is a form of poker commonly played at the high stakes tables of casinos. It consists of rounds of play cycling among:
  • Texas Hold 'em,
  • Omaha eight or better,
  • Razz,
  • Seven card Stud, and
  • Seven card stud E

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Antelope are herbivorous mammals of the family Bovidae, often noted for their horns. These animals are spread relatively evenly throughout the various subfamilies of the Bovidae and many are more closely related to cows or goats than to each other.
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Aves
Linnaeus, 1758

Orders

About two dozen - see section below

Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
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Plantae
Haeckel, 1866[1]

Divisions

Green algae
  • Chlorophyta
  • Charophyta
Land plants (embryophytes)
  • Non-vascular land plants (bryophytes)

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