Abstract
IN answer to the inquiry of your correspondent in the last number of NATURE (p. 173) I beg to inform him that the shells of the Pliocene formation in the Morea have been long since investigated, as is shown by the great and well-known work of Hömes. And Dr. Fischer has published a list of the fossil shells from the same formation at Rhodes. These subapennine beds extend over the whole of the south of Europe. For many of those species which are still living I have given the localities of the Morea and Rhodes as fossil in the Proceedings of the Zoological Society.
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JEFFREYS, J. Geology of Cephalonia. Nature 28, 199 (1883). https://doi.org/10.1038/028199a0
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DOI: https://doi.org/10.1038/028199a0
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