Pecopteris Plumosa
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Pecopteris Plumosa
''Pecopteris'' is a very common form genus of leaf, leaves. Most ''Pecopteris'' leaves and fronds are associated with the marattialean tree fern ''Psaronius''. However, ''Pecopteris''-type foliage also is borne on several Filicales, filicalean ferns, and at least one Pteridospermatophyta, seed fern. Pecopteris first appeared in the Devonian period, but flourished in the Carboniferous, especially the Pennsylvanian (geology), Pennsylvanian. Plants bearing these leaves became extinct in the Permian period, due to swamps disappearing and temperatures on Earth dropping. Etymology ''Pecopteris'' is derived from the Greek ''pekin'', (to comb), and ''pteris'', (a fern). This is because the leaflets of ''Pecopteris'' fronds are arranged like the teeth on a comb. Species As of 1997, there have been 250-300 species assigned to ''Pecopteris''. In Brazil, fossil of form genus ''Pecopteris'' was located in outcrop ''Morro Papalé'' in the city of Mariana Pimentel. They are in the geop ...
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Late Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating al ...
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