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Lepidodendron Stem
LepododendronStemAxis
Lepidodendron johnsonii
Pennsylvanian; Webber Formation
Trout Creek Pass, Chaffee County, CO
Colorado School of Mines Geology Museum

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Plant remains of a Lower Pennsylvanian lycopod forest can be found near Trout Creek Pass in central Colorado. Plant remains at Trout Creek include portions of silicified trunks that contain vascular axes. Numerous shale fragments bearing imprints of Lepidodendron and Lepidophloios are associated with the trunk fragments. Fragments of plant axes preserve the pith, primary xylem, secondary xylem, portions of the cortex and periderm. Preservation can be very good; however, the structure is destroyed by hydrofluoric acid because very little organic matter remains. Thus the cellulose peels used for lycopod material in coal balls can not be utilized with the silicified Trout Creek material (Arnold, 1940, p. 31).

A section from the material used as the type specimen for Lepidodendron johnsonii is pictured above. This scale tree was named by Chester A. Arnold for J. Harlan Johnson who announced discovery of the Trout Creek fossil deposit in 1932. Silicified axes of L. johnsonii are mineralized with fibrous chalcedony, large intergrown quartz grains, and euhedral quartz crystals (Stein, 1982, p. 1280). The mineralized stem section pictured above consists of pith, primary xylem, secondary xylem, and some cortex tissue. The phloem, outer cortex tissue and periderm are not present in this specimen. Like most axes found at this site the pith is filled with debris and invaded by Stigmaria roots. Thus, the actual pith tissue is not preserved in the above specimen. Roots of lycopod trees must have grown around and through plants buried within the soil. This would explain why many specimens found at this site have Stigmaria roots penetrating through the tissues.

A series of images below "zooms" in on the primary and secondary xylem rings. The first two images were taken with a Canon PowerShot SD770 IS Digital ELPH 10.0 MEGA PIXELS, cropped and resized in Adobe Photoshop CS6. The third image was taken at 50x with a Dino-Lite AD7013 MT 5.0 MP, courtesy of Hugh Lawrence.

Lepidodendron stem cross-section

In the image above we can see from left to right: pith area filled with debris and invaded by Stigmaria roots, primary xylem ring, secondary xylem ring and inner cortex at the edge of the photo.

Lepidodendron cross-section of primary and secondary xylem ring
In the image above we can see: pith area on the left, primary xylem ring in the center, and secondary xylem ring to the right.
Lepidodendron metaxylem and secondary xylem

In the image above we can see the transition zone between the primary xylem (large metaxylem cells and protoxylem) and secondary xylem (radially aligned tracheids).

Lycopod bark impressions associated with the plant axes are pictured below. Bark impressions with leaf scars representing both Lepidodendron and Lepidophloios are easily found.

Lepidodendron bark impressipons
Lycopod Bark Impression
Bibliography

Arnold, C.A. (1940). Lepidodendron johnsonii, sp. nov., from the Lower Pennsylvanian of Central Colorado. Contributions from the Museum of Paleontology, University of Michigan vol 6, no 2, pp. 21-52.

Stein, C.L. (1982). Silica Recrystallization in Petrified Wood. Journal of Sedimentary Petrology, vol 52, no 4. pp. 1277-1282.

 

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