The carbon isotopic compositions of certain marine invertebrates and coals from the Australian Permian

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Scientific paper

C 13 analyses are reported for Permian and Devonian brachiopods, Permian crinoids and Permian coals. O 18 analyses of the marine invertebrates are also given. Only the Permian brachiopods are isotopically preserved. Their mean C 13 value is significantly more positive than Cretaceous and Recent brachiopods and molluscs measured elsewhere. A single coal seam sampled in detail was very constant in C 13 , and a trend towards values some 2·5%. more negative from lower to upper Permian was observed for a sequence of seams. The lower Permian coal C 13 was approximately the same as upper Carboniferous coal measured elsewhere. The meaning of this Permian isotopic distribution is discussed in terms of an age-effect, but there are other possible explanations.

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