THE publication of Saporta and Marion's “Evolution of the Cryptogams” (see NATURE, vol. xxiv. p. 75, 558) has been followed by a work in which Dr. Nathorst has endeavoured to prove that nearly the whole of the supposed fossil marine Algæ, especially from the older rocks, are either tracks of Invertebrata or were produced by mechanical agency. “Florideæ, Laminarieæ, Chondriteæ, Alectorurideæ, Arthrophyceæ, Bilobites, and other algæ; comprising among them forms curious and remark. able by the regularity of their branching thallus, their phyllome with raised periphery and striated surface; all had disappeared as if by enchantment, and in their place there remained but tracks of Invertebrata, moving upon the ooze, swimming or creeping, and impressing the exare tremities of their tentaculary palpæ around them, or of larvæ gliding through the slimy mud.” When these are insufficient, the movement of water acting on inert bodies, or waving tufts of sea-weed, are appealed to, for no fossil imprint either sunk or in relief, unless preserving carbonaceous matter, is admitted in Dr. Nathorst's hypoProximity thesis to have ever been a plant. This view is eneror getically combated by Saporta in the present work. The issue however does not very materially affect either the general theory of plant-evolution, as traced by Saporta and Marion, since this relies but little upon the evidence of doubtful fossil alg, or the succession of marine algæ in time, which seems to have been probably Laminarieæ, Fucaceæ, and Florideæ. The main point in dispute is whether the supposed primordial algæ, Eophyton and Bilobites, are of vegetable or of other origin. There are numerous a priori reasons for supposing pl ant life to have existed in palæozoic seas, and the complexity of life seen in even the older rocks renders their presence almost a necessity. The question is whether certain impressions which are abundant in Silurian rocks reproduce some of these forms, or whether we are still without indications of the primæval algæ.
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