1966
DOI: 10.1126/science.154.3756.1548
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Fluorine Content of Microsaur Teeth from the Carboniferous Rocks of Joggins, Nova Scotia

Abstract: Because the Carboniferous deposits at Joggins, Nova Scotia, contain the earliest fauna of terrestrial vertebrates, the extremely well-preserved teeth of these ancient animals are of special interest. The " mineral" composition of teeth from the Joggins microsaur Hylerpeton dawsoni is crystallochemically identical with francolite, a carbonate fluorapatite. The fluorine content of the fossilized dentin is 3.1 percent, which is much higher than any previoulsly recorded for fossil teeth.

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Cited by 5 publications
(2 citation statements)
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“…The standard used in the present study is the modern buried elephant femur in which the CO, content was previously determined by wet chemistry (Hassan, 1976 has an abnormally high F-concentration (3.96 percent) whereas the rest of the fossil bones have less than 1.9 percent and the fresh and modern bones contain less than 0.1 percent flouride (table 2). The fact that bone mineral dahllite may be converted into francolite because of fossilization, has been reported previously by Stevenson (1966).…”
Section: Introductionmentioning
confidence: 53%
“…The standard used in the present study is the modern buried elephant femur in which the CO, content was previously determined by wet chemistry (Hassan, 1976 has an abnormally high F-concentration (3.96 percent) whereas the rest of the fossil bones have less than 1.9 percent and the fresh and modern bones contain less than 0.1 percent flouride (table 2). The fact that bone mineral dahllite may be converted into francolite because of fossilization, has been reported previously by Stevenson (1966).…”
Section: Introductionmentioning
confidence: 53%
“…William Dawson, in particular, whose work has been summarized by Falcon-Lang and Calder (2005), Calder (2006) and Falcon-Lang (2006), extensively collected and studied fossils from Joggins. Many of the more recent discoveries and taxonomic studies are of the vertebrates, mainly amphibians, including the extinct groups of the microsaurs and labyrinthodonts; (e.g., Carroll 1963Carroll , 1966Carroll , 1967Stevenson and Stevenson 1966;Stevenson 1967;Baird 1982;Godfrey et al 1987Godfrey et al , 1991Milner 1996;Reisz and Modesto 1996;Holmes et al 1998;Robinson et. al 2005;Holmes and Carroll 2010).…”
Section: Paleobiologymentioning
confidence: 99%