The Virtual Petrified Wood Museum.  Dedicated to the Exhibition and Educational Study of Permineralized Plant Material
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Devonian Period: 416-359.2 Million Years Ago
Gallery: New York, USA

Eospermatopteris
Specimen at University of Illinois
Oldest known Forest Devonian 375 Million Years Ago
Gilboa, New York
Middle Devonian fossil trunks from Gilboa, New York provide a window into the earliest forests. Stumps with roots stretching out into a paleosol (fossil soil) have been preserved as casts at a site known as Riverside Quarry. The casts reveal only the outer structure of these tree stumps. From the 1870's and until recently the stumps have been assigned to various plant groups including Psaronius (the tree fern), Eospermatopteris (the accepted name) and a progymnosperm (Nudds & Selden, 2008, pp. 98 & 99). The mystery of Eospermatopteris identity was not solved until recently. In 2007 Stein et al. described the discovery of fossil trees from Shoharie County, New York uniting the crown of Wattieza with the trunk of Eospermatopteris. Wattieza is a genus of prehistoric tree that belongs to the class Cladoxylopsida. This class is currently placed within the division Pteridophyta. So, fossil stumps at Gilboa are cladoxylopsid trees related to ferns.

Bibliography

Stein, W.E., Mannonlini, F, VanAller Hernick, L., Landing, E. & Berry, C.M. (2007). Giant cladoxylpsid trees resolve the enigma of the Earth's earliest forest stumps at Gilboa. Nature, vol 446: pp. 904-907.

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