Haskell County Fossils

PLANT Lycopsida Roots Stigmaria

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INVERTEBRATE TRACE Unidentified Possible Worms and Burrows
INVERTEBRATE TRACE Ichnofauna
PLANT Fossilized Wood
PLANT Sphenopsida Calamites
PLANT Lycopsida Roots Stigmaria
PLANT Lycopsida Bark Sigillaria
PLANT Unidentified (Possible)
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UNIDENTIFIED Possible Mummified
UNIDENTIFIED Possible Mummified Continued
UNIDENTIFIED Various Specimens
ROCK Picture Rock
ROCK With Large Depression

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Katina Roye Peevyhouse retains all rights and owns the copyright of all photos shown on this page.

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Stigmaria is the name for fossilized roots of lycopsids.  Stigmaria is one of the more common fossils found in Haskell County.  This specimen is an unusual dark gray and black color. 

This closeup view of the black and gray specimen shows the incredible detail that has been preserved.   

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Stigmaria comes in many color variations, including brown.   

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This specimen is almost white in color.   

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This specimen is another unusual gray.     

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Stigmaria-Tracheophyta-Lycopsida-Lepidodendrales;
Lower Carboniferous-Permian

LYCOPSIDS

Also known as: Lycopods

Informal group: Land plants

Age range: Silurian-Recent

Found in OK: Pennsylvanian rocks, eastern Oklahoma

Most species in these families are small, easily overlooked plants that live in damp forests, along rivers or on the branches of other trees. However this was certainly not true of the lycopsids that lived during the Pennsylvanian. During the Pennsylvanian, some lycopsids grew to be trees standing over 27 meters (90 feet) tall. Unlike most other plants, tree lycopsids appear to have preferred places in the swamp that were flooded by water. When they died, their bark, wood, leaves and roots fell into the swamp. Because of the high water level, the plant pieces did did not break apart completely. The bark, leaves and roots of lycopsids were buried and over time became coal. As much as 70% of coal may be composed of the lycopsid plant parts.

 

Ferns...

Stromatalites...

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