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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,

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