Encyclopedia of Evolution.pdf - Online Reading Center
Encyclopedia of Evolution.pdf - Online Reading Center
Encyclopedia of Evolution.pdf - Online Reading Center
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0 Cenozoic era<br />
opens the way to an understanding <strong>of</strong> mass extinctions,<br />
followed by rapid evolution, that punctuate the history <strong>of</strong> life<br />
on Earth (see punctuated equilibria). Modern geology, by<br />
presenting a background <strong>of</strong> uniformitarian processes punctuated<br />
by catastrophes such as asteroid impacts (see Permian<br />
extinction; Cretaceous extinction), has preserved the<br />
best <strong>of</strong> both 19th-century approaches: uniformitarianism and<br />
catastrophism.<br />
Further <strong>Reading</strong><br />
Benton, Michael. “The death <strong>of</strong> catastrophism.” Chap. 3 in When<br />
Life Nearly Died: The Greatest Mass Extinction <strong>of</strong> All Time.<br />
London: Thames and Hudson, 2003.<br />
Gould, Stephen Jay. “Uniformity and catastrophe.” Chap. 18 in Ever<br />
Since Darwin: Reflections in Natural History. New York: Norton,<br />
1977.<br />
Cenozoic era The Cenozoic era (the era <strong>of</strong> “recent life”)<br />
is the third era <strong>of</strong> the Phanerozoic Eon, or period <strong>of</strong> visible<br />
multicellular life, which followed the Precambrian time in<br />
Earth history (see geological time scale). The Cenozoic<br />
era, which is the current era <strong>of</strong> Earth history, began with the<br />
mass extinction event that occurred at the end <strong>of</strong> the Cretaceous<br />
period <strong>of</strong> the Mesozoic era (see mass extinctions;<br />
Cretaceous extinction). The Cenozoic era is traditionally<br />
divided into two geological periods, the Tertiary period<br />
and the Quaternary period.<br />
The Cretaceous extinction left a world in which many<br />
organisms had died and much space and many resources were<br />
available for growth. The dinosaurs had become extinct,<br />
as well as numerous lineages within the birds, reptiles, and<br />
mammals (see birds, evolution <strong>of</strong>; reptiles, evolution<br />
<strong>of</strong>; mammals, evolution <strong>of</strong>). The conifers that had dominated<br />
the early Mesozoic forests came to dominate only the<br />
forests <strong>of</strong> cold or nutrient-poor mountainous regions in the<br />
Cenozoic (see gymnosperms, evolution <strong>of</strong>). The flowering<br />
plants evolved in the Cretaceous period but proliferated during<br />
the Cenozoic era, into the forest trees that dominate the<br />
temperate and tropical regions, and many shrubs and herbaceous<br />
species (see angiosperms, evolution <strong>of</strong>). The explosive<br />
speciation <strong>of</strong> flowering plants paralleled that <strong>of</strong> insect<br />
groups such as bees, butterflies, and flies, a pattern most scientists<br />
attribute to coevolution.<br />
The Cenozoic world was cooler and drier than most <strong>of</strong><br />
previous Earth history. Climatic conditions became cooler and<br />
drier during the late Cenozoic than they had been early in the<br />
Cenozoic. During the middle <strong>of</strong> the Tertiary period, dry conditions<br />
allowed the adaptation <strong>of</strong> grasses and other plants to aridity,<br />
and the spread <strong>of</strong> grasslands and deserts. Grazing animals<br />
evolved from browsing ancestors, taking advantage <strong>of</strong> the grass<br />
food base (see horses, evolution <strong>of</strong>). Five million years ago,<br />
the Mediterranean dried up into a salt flat. The coolest and driest<br />
conditions began with the Quaternary period. About every<br />
hundred thousand years, glaciers build up around the Arctic<br />
Ocean and push southward over the northern continents (see<br />
ice ages). Meanwhile, lower sea levels and reduced evaporation<br />
result in drier conditions in the equatorial regions.<br />
Many evolutionary scientists and geologists now divide<br />
the Cenozoic era into the Paleogene (Paleocene, Eocene, Oligocene)<br />
and the Neogene (Miocene, Pliocene, Pleistocene,<br />
Holocene) rather than the traditional Tertiary and Quaternary<br />
periods.<br />
Chambers, Robert (1802–1871) British Publisher Born<br />
July 10, 1802, Robert Chambers was a British publisher,<br />
whose role in the development <strong>of</strong> evolutionary theory was<br />
not widely known until after his death. Long before Darwin<br />
(see Darwin, Charles) wrote his famous book (see origin<br />
<strong>of</strong> species [book]), evolutionary thought was in the air in<br />
Europe. The naturalist Buffon (see Buffon, Georges) had<br />
presented a limited evolutionary theory in France in the 18th<br />
century. Charles Darwin’s grandfather (see Darwin, Erasmus)<br />
had speculated about the possibility, and the French scientist<br />
Lamarck had proposed a scientific evolutionary theory<br />
(see Lamarckism). In October <strong>of</strong> 1844, an anonymous British<br />
book, Vestiges <strong>of</strong> the Natural History <strong>of</strong> Creation, presented<br />
an evolutionary history <strong>of</strong> the Earth, from the formation <strong>of</strong><br />
the solar system and plant and animal life, including even<br />
the origins <strong>of</strong> humankind. More than 20,000 copies sold in<br />
a decade. Political leaders like American president Abraham<br />
Lincoln, British Queen Victoria, and British statesmen William<br />
Gladstone and Benjamin Disraeli read it. Poets, such as Alfred<br />
Tennyson, and philosophers like John Stuart Mill did also.<br />
Many scientists also read it (see Huxley, Thomas Henry).<br />
The purpose <strong>of</strong> the book, said its author, was to provoke scientific<br />
and popular discussion about evolution.<br />
It certainly succeeded in this objective. Responses ranged<br />
from enthusiasm to condemnation. A British medical journal,<br />
Lancet, described Vestiges as “a breath <strong>of</strong> fresh air.” Physicist<br />
Sir David Brewster wrote that Vestiges raised the risk <strong>of</strong> “poisoning<br />
the fountains <strong>of</strong> science, and sapping the foundations<br />
<strong>of</strong> religion.” Scottish geologist Hugh Miller published an<br />
entire book, Foot-Prints <strong>of</strong> the Creator, as a rebuttal to Vestiges.<br />
Charles Darwin called it a “strange, unphilosophical,<br />
but capitally-written book,” and noted that some people had<br />
suspected him <strong>of</strong> being the author. Huxley recognized it as<br />
the work <strong>of</strong> an amateur whose author could “indulge in science<br />
at second-hand and dispense totally with logic.” A pr<strong>of</strong>essional<br />
scientist would have dismissed the fraudulent claim<br />
<strong>of</strong> the amateur scientist, Mr. W. H. Weekes, who claimed to<br />
have created living mites by passing electric currents through<br />
a solution <strong>of</strong> potassium ferrocyanate, a claim that the Vestiges<br />
author was credulous enough to believe.<br />
It was not until 1884, after Darwin’s death and evolutionary<br />
science had become respectable, that the author was<br />
<strong>of</strong>ficially revealed to be Robert Chambers, one <strong>of</strong> Britain’s<br />
most successful publishers. Chambers had chosen to remain<br />
anonymous because he feared the reputation <strong>of</strong> Vestiges<br />
would hurt his business. (His company published, among<br />
many other things, Bibles.) Because <strong>of</strong> Chambers’s interest in<br />
science, some people, including Darwin, had already guessed<br />
the identity <strong>of</strong> the notorious “Mr. Vestiges.”<br />
Chambers and his older brother had begun their publishing<br />
business by selling cheap Bibles and schoolbooks from