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 living fossils<br />
admired. The genus name <strong>of</strong> a small herbaceous plant <strong>of</strong> the<br />
north woods, Linnaea borealis, honors Linnaeus, and the<br />
species name <strong>of</strong> Abutilon theophrasti, the velvetleaf weed,<br />
honors the Greek philosopher Theophrastus. Both amateur<br />
naturalists and pr<strong>of</strong>essional scientists yearned for the immortality<br />
that would result from having a plant named for them.<br />
Even though he did not even think about evolution,<br />
Linnaeus included in his writings some intermediate forms<br />
based on hearsay. He was willing to believe them because he<br />
accepted the concept <strong>of</strong> the Great Chain <strong>of</strong> Being (see scala<br />
naturae). For example, he wrote about strange species <strong>of</strong><br />
humans such as Homo ferus, a feral human on all fours and<br />
unable to talk, and Homo caudatus, man with a tail. Linné<br />
died on January 10, 1778.<br />
Further <strong>Reading</strong><br />
Gould, Stephen Jay. “Ordering nature by budding and full-breasted<br />
sexuality.” Chap. 33 in Dinosaur in a Haystack: Reflections in<br />
Natural History. New York: Harmony, 1995.<br />
Schiebinger, Londa. “The private lives <strong>of</strong> plants: Sexual politics in<br />
Carl Linnaeus and Erasmus Darwin.” Pages 121–143 in M. Benjamin,<br />
ed., Science and Sensibility: Gender and Scientific Enquiry<br />
1780–1945. New York; Oxford University Press, 1991.<br />
———. “The loves <strong>of</strong> the plants.” Scientific American, February<br />
1996, 110–115.<br />
living fossils Living fossils is the popular term given<br />
to modern multicellular organisms that closely resemble<br />
forms that have been known from the fossil record for at<br />
least several million years (see figures and table). During<br />
their time on Earth, these organisms have experienced stasis<br />
(see punctuated equilibria) and stabilizing selection<br />
(see natural selection). While in most cases evolution<br />
has favored change and diversification, in these cases it has<br />
favored stability. For more information about these examples,<br />
see gymnosperms, evolution <strong>of</strong>; seedless plants,<br />
evolution <strong>of</strong>; invertebrates, evolution <strong>of</strong>; fishes,<br />
evolution <strong>of</strong>.<br />
Lucy See australopithecines.<br />
Lyell, Charles (1797–1875) Scottish Geologist Sir Charles<br />
Lyell changed the science <strong>of</strong> geology into its modern form by<br />
leading scientists away from catastrophism and toward<br />
uniformitarianism, a theory that had been proposed earlier<br />
(see Hutton, James). Although uniformitarianism is no longer<br />
accepted in the form that Lyell proposed it, it was Lyell<br />
who led geologists to understand that the history <strong>of</strong> the Earth<br />
has occurred by the operation <strong>of</strong> natural laws over a long<br />
period <strong>of</strong> time. Lyell’s geological theories laid the groundwork<br />
for the development <strong>of</strong> evolutionary science (see Darwin,<br />
Charles).<br />
Born November 14, 1797, Charles Lyell had a keen<br />
interest in natural history as he grew up. His father was a<br />
botanist, and young Lyell collected and studied insects. Lyell<br />
became interested in geology when he entered Oxford University<br />
and attended lectures by Rev. William Buckland.<br />
“Living Fossil” Plants and Animals<br />
Relatively<br />
Taxonomic unchanged<br />
Organism category since<br />
Plants:<br />
Dawn redwood gymnosperm Pliocene Epoch<br />
(Metasequoia) seed plant<br />
Ginkgo gymnosperm Jurassic period<br />
(Ginkgo) seed plant<br />
Monkey puzzle gymnosperm Triassic period<br />
(Auracaria) seed plant<br />
Cycad gymnosperm Permian period<br />
(Cycas) seed plant<br />
Horsetail<br />
(Equisetum)<br />
pteridophyte plant Permian period<br />
Animals:<br />
Horseshoe crab arthropod Triassic period<br />
(Limulus)<br />
Fairy shrimp arthropod Silurian period<br />
(Triops)<br />
Lampshell brachiopod Silurian period<br />
(Lingula)<br />
Coelacanth lobe-finned “fish” Cretaceous period<br />
(Latimeria)<br />
Buckland stimulated Lyell’s imagination, not the least by his<br />
unusual behavior. Buckland performed his fieldwork wearing<br />
academic gowns, kept many wild animals at his house,<br />
and ate any animal he could find. Guests might be treated to<br />
baked guinea pig, battered mice, roasted hedgehog, or boiled<br />
sea slug. Although Lyell was to publish works that overturned<br />
Buckland’s theories, Lyell learned from Buckland to<br />
be fearless in choosing direct observation and experience over<br />
tradition. Lyell trained for a law career but, after going on a<br />
geological expedition through Scotland with Buckland, gave<br />
up his legal career for science.<br />
After a geological expedition in Europe, Lyell began<br />
writing the Principles <strong>of</strong> Geology: An Attempt to Explain<br />
the Former Changes <strong>of</strong> the Earth’s Surface by Reference to<br />
Causes now in Operation. The first two volumes were published<br />
in 1830 and 1832. These two volumes began a tide <strong>of</strong><br />
success, going into a second edition before the third volume<br />
was published in 1833. The Principles went through 11 editions,<br />
each updated and revised with much new information,<br />
during Lyell’s lifetime, and he was working on the 12th edition<br />
when he died. Lyell’s Elements <strong>of</strong> Geology, focusing<br />
upon fossils and fossilization, first appeared in 1838 and<br />
went through six editions during Lyell’s lifetime. Lyell traveled<br />
extensively, gathering new observations; his visits to the<br />
United States, where he studied the rate <strong>of</strong> erosion <strong>of</strong> Niagara<br />
Falls and the rate <strong>of</strong> sedimentation in the Mississippi Delta,