In a French version, , in 1839 Lyell called the Older Pliocene the Pliocene and the Newer Pliocene the Pleistocene (Pleist-, "most"). Then in Antiquity of Man in 1863 he reverted to his previous scheme, adding "Post-Tertiary" and "Post-Pliocene". In 1873 the Fourth Edition of Antiquity of Man restores Pleistocene and identifies it with Post-Pliocene. As this work was posthumous, no more was heard from Lyell. Living or deceased, his work was immensely popular among scientists and laymen alike. "Pleistocene" caught on immediately; it is entirely possible that he restored it by popular demand. In 1880 Dawkins published The Three Pleistocene Strata containing a new manifesto for British archaeology: The continuity between geology, prehistoric archaeology and history is so direct that it is impossible to picture early man in this country without using the results of all these three sciences.
In a French version, , in 1839 Lyell called the Older Pliocene the Pliocene and the Newer Pliocene the Pleistocene (Pleist-, "most"). Then in Antiquity of Man in 1863 he reverted to his previous scheme adding "Post-Tertiary" and "Post-Pliocene". In 1873 the Fourth Edition of Antiquity of Man restores Pleistocene and identifies it with Post-Pliocene As this work was posthumous, no more was heard from Lyell. Living or deceased, his work was immensely popular among scientists and laymen alike. "Pleistocene" caught on immediately; it is entirely possible that he restored it by popular demand. In 1880 Dawkins published The Three Pleistocene Strata containing a new manifesto for British archaeology: The continuity between geology, prehistoric archaeology and history is so direct. that it is impossible to picture early man in this country without using the results, of all these three sciences.