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See also:WILLIAMSON, See also: Shortly afterwards he removed to Clapham, where he died on the 23rd of See also:June 1895. Williamson's teaching work was not confined to his university classes, for he was also a successful popular lecturer, especially for the Gilchrist Trustees. His scientific work, pursued with remarkable See also:energy throughout life, in the midst of See also:official and professional duties, had a wide See also:scope. In geology, his early work on the zones of See also:distribution of Mesozoic fossils (begun in 1834), and on the See also:part played by microscopic organisms in the formation of marine deposits (1845), was of fundamental importance. In zoology, his investigations of the development of the See also:teeth and bones of fishes (1842-1851), and on See also:recent See also:Foraminifera, a See also:group on which he wrote a monograph for the See also:Ray Society in 18J7, were no less valuable. In botany, in addition to a remarkable memoir on the See also:minute structure of Volvox (1852), his work on the structure of fossil plants established See also:British See also:palaeobotany on a scientific basis; on the ground of these researches Williamson may See also:rank with A. T. See also:Brongniart as one of the founders of this See also:branch of science. His contributions to fossil botany began in the earliest days of his career, and he returned to the subject from time to time during the See also:period of his geological and zoological activity. His investigation of the Mesozoic cycadioid fossil Zamia (now Williamsonia) gigas was the See also:chief palaeobotanical work of this intermediate period. His See also:long course of researches on the structure of Carboniferous plants belongs mainly to the latter part of his life, and his results are chiefly, though not wholly, embodied in a See also:series of nineteen See also:memoirs, ranging in date from 1871 to 1893, in the Philosophical Transactions. In this series, and in some See also:works (notably the monograph on Stigmaria ficoides, Palaeontographical Society, 1886), published elsewhere, Williamson elucidated the structure of every group of Palaeozoic vascular plants. Among the chief results of his researches may be mentioned the See also:discovery of plants intermediate between ferns and'cycads, the description of the true structure of the fructification in the See also:extinct cryptogamic See also:family Sphenophylleae, and the demonstration of the cryptogamic nature of the dominant Palaeozoic orders Calamarieae, Lepidodendreae and Sigillarieae, plants which on See also:account of the growth of their stems in thickness, after the manner of gymnospermous trees, were regarded as phanerogams by Brongniart and his followers. After a long controversy the truth of Williamson's views has been fully established, and it is now known that the mode of growth, characteristic in See also:present times, of See also:dicotyledons and See also:gymnosperms prevailed in Palaeozoic 'ages in every family of vascular cryptogams. Thus, as See also:Count Solms-Laubach has pointed out, palaeobotany for the first time spoke the decisive word in an important question of See also:general botany. Williamson's work in fossil botany was scarcely appreciated at the time as it deserved, for its great merits were somewhat obscured by the author's want of familiarity with the See also:modern technicalities of the science. Since, however, the subject has been seriously taken up by botanists of a newer school, the soundness of the See also:foundation he laid has become fully recognized. It may be added that he was a skilled draughtsman, illustrating all his works by his own drawings, and practising See also:water-See also:colour See also:painting as his favourite recreation. A full account of Williamson's career will be found in his auto-See also:biography, entitled Reminiscences of a Yorkshire Naturalist, edited by his wife (London, 1896). Among obituary notices may be mentioned that by Count Solms-Laubach, Nature (5th See also:September 1895), and one by D. H. See also:Scott in Proc. R.S. vol. Ix. (1897). (D. H. Additional information and CommentsThere are no comments yet for this article.
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