History of ichnology: The correspondence between the reverend Henry Duncan and the reverend William Buckland and the discovery of the first vertebrate footprints

被引:1
作者
Pemberton, S. George [1 ]
McCrea, Richard [1 ]
Gingras, Murray K. [1 ]
Sarjeant, William A. S. [2 ]
MacEachern, James A. [3 ]
机构
[1] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
[2] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 0W0, Canada
[3] Simon Fraser Univ, Dept Earth Sci, Burnaby, BC V5A 1S6, Canada
来源
ICHNOS-AN INTERNATIONAL JOURNAL FOR PLANT AND ANIMAL TRACES | 2008年 / 15卷 / 01期
关键词
history of ichnology; Henry Duncan; William Buckland; vertebrate ichnology;
D O I
10.1080/10420940600864670
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The Reverend Henry Duncan (1774-1846), clergyman, philosopher, writer, politician, archeologist, poet, educator, social reformer, and the founder of savings banks, was indeed a Man for All Seasons. In 1824, while Minister of the Church of Scotland at Ruthwell, Dumfriesshire, he was presented with a slab of red sandstone from the Corneockle Muir quarry in Annandale, exhibiting a set of footprints on it. Although Duncan felt from the start that he was dealing with the tracks of an animal, he wrote to the Reverend William Buckland, Reader in Mineralogy and Geology at the University of Oxford, to solicit his opinion on the origin of these curious markings. Buckland was at first skeptical, but after receiving casts of the markings from Duncan, he became convinced that they did in fact represent footprints. Duncan and Buckland maintained a correspondence about the footprints, and on January 7, 1828, Duncan described the Corncockle Muir footprints to the Royal Society of Edinburgh and quoted Buckland's findings. Duncan's paper was not published by the Society until 1831, but it aroused considerable interest-"Footsteps before the Flood"!-and was reported in several newspapers. This was the first scientific report of a fossil track; although a schoolboy, Pliny Moody, had found fossil footprints in Connecticut in 1802, they were not scientifically described until 1836. The Scottish tracks are now considered to be not reptilian but of synapsid origin and the rocks containing them are now known to be of Permian age.
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收藏
页码:5 / 18
页数:14
相关论文
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