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Comprehending conodonts

Geology Today, 2015
Conodonts were small, thin, elongate jawless creatures that were a common component of the marine fauna from the late Cambrian, throughout the Palaeozoic and into the Triassic. For the majority of conodont research history, speculations on conodont affinity were restricted to the histology and arrangement of their mineralized tissues—‘conodont elements’
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Early Evolution of Conodonts

Geological Society of America Bulletin, 1969
The known distribution of conodonts in the Cambrian of Europe, Asia, and North America is not uniform, but no major discrepancies in stratigraphic range of form species has been noted. The oldest reliably dated conodont known is a Hertzina species which is known in upper Middle Cambrian rocks in Nevada and Bornholm (Denmark).
DAVID L. CLARK, JAMES F. MILLER
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On the Affinities of Conodonts

1972
Conodonts are phosphatic, denticulated structures in the average size range from 0.1 to 1 mm. They grew by the centrifugal accretion of lamellae. Conodonts are a homogeneous group. Basic interpretations must apply to all kinds of conodonts. Internal and outer morphologic features indicate that they were skeletal elements designed to lend a certain ...
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Conodonts through time and space: Studies in conodont provincialism

1984
A computerized file of approximately twenty thousand records of conodont occurrences was used in a quantitative study of conodont provincialism. Although biases in the fossil record, in specimen collection, and in data collection preclude any rigid statistical testing, study of quantitative measures of similarity between faunas, when combined with ...
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Conodont paleoecology

Palaeogeography, Palaeoclimatology, Palaeoecology, 1978
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Conodonts

2021
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Conodonts

Geobios, 1987
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