Williamson in 1877 pointed out that we learn from the large number of different kinds of Palaeozoic seeds that ‘there were in the Carboniferous forests many gymnospermous stems clothed with foliage of which we have not yet discovered any traces, probably because these Gymnosperms did not flourish upon the low swampy grounds which were the homes of the great mass of the coal-producing plants[803].’ Prof. Zeiller[804] has also drawn attention to the numerical excess of seeds over vegetative organs. This discrepancy has to a large extent been explained by the discovery that many of the supposed Ferns were seed-bearing plants, and a further explanation is suggested by the superiority of seeds over stems and leaves in their adaptation to dispersal by water. In 1874 Brongniart[805] described several petrified seeds from material discovered by Grand’Eury in the St Étienne coal-field, and seven years later his descriptions were republished[806], with the addition of several beautifully executed drawings, as a posthumous volume edited by his distinguished pupil Renault. Williamson’s researches supplied much additional information, and in recent years the more detailed study of French and English seeds by Bertrand and particularly by Oliver and his pupils has further emphasised the interest and importance of this field of work. Brongniart proposed a two-fold classification of French seeds: (i) bilaterally symmetrical seeds, more or less flattened in section, which he believed to be Cordaitean; (ii) radially symmetrical seeds, circular in transverse section: the latter group he considered to be less closely allied to recent types. The employment of the terms Platyspermeae and Radiospermeae, proposed by Oliver[807] for Brongniart’s divisions, serves a useful purpose if due regard is paid to the adequacy of the evidence as to symmetry and if it is recognised that this classification cannot be rigidly employed in all cases. It was pointed out by Brongniart that the occasional occurrence of tricarinate seeds of _Ginkgo_ (fig. 631) and _Taxus_ is an exception to the general rule of bilateral symmetry: seeds of _Cycas_ are normally bilateral, but radially symmetrical forms also occur[808]. The genus _Conostoma_ (fig. 494, B) represents an intermediate type which, though almost radially symmetrical, exhibits a slight tendency towards platyspermy. Evidence recently brought forward by Nathorst[809] renders probable a connexion of a presumably radiospermic seed _Lagenospermum Arberi_[810] with the Lower Carboniferous fronds _Adiantites bellidulus_ Heer, and this furnishes an interesting illustration of the association of both platyspermic and radiospermic seeds with the same generic type of foliage. While retaining Radiosperm and Platysperm as convenient descriptive terms, I have not adopted them as group-designations on the ground that they do not in themselves serve as trustworthy criteria of relationship. Attention is called