A multistage model of preservation in fossil plants from the Llewellyn Formation (Pennsylvanian), St. Clair, Pennsylvania, U.S.A

• Published in: Review of palaeobotany and palynology 2023-09, Vol.316, p.104941, Article 104941
• Main Authors: Peterson, Stephen P., Myer, George H., Grandstaff, Barbara S., Grandstaff, David E.
• Format: Article
• Language: English
• Subjects: Fossilization; Llewellyn Formation; Pennsylvania; Pyrophyllite; St. Clair
• ISSN: 0034-6667
• DOI: 10.1016/j.revpalbo.2023.104941

Exceptionally preserved plant fossils from St. Clair, Pennsylvania, have long been part of museum and private collections. Fossil leaf fragments and stems from the underclay of the Buck Mountain Coal (Reading Anthracite Company quarry), lowest Llewellyn Formation (late Pennsylvanian, Virgilian), combine outer layers of coalified organic material (phytoleim) with strikingly white kaolinite, quartz, and the low-grade metamorphic mineral pyrophyllite in the interior. The surficial dark, coalified material appears to preserve the dense outer layers (cuticle, epidermis, and palisade layer) and some cells of the spongy mesophyll in the fossilized leaves. XRD spectra of separated phytoleim contain graphite peaks. Raman spectra with peaks near 1600 and 1320 cm−1 indicate that the phytoleim is composed of disordered graphitic material. ID/IG ratios from ca. 0.3 to 0.45 are consistent with greenschist facies metamorphic conditions forming the anthracite coal. The interior pyrophyllite is highly crystalline, with large crystals often oriented perpendicular to leaf surfaces. Hydrothermal formation of pyrophyllite requires relatively limited groundwater flow conditions and temperatures between ca. 275 and 350 °C. Although many fossil leaves are compressed, some are near their original thickness. We infer that the remains were replaced prior to significant burial and compression of the sediment by an early-forming mineral phase, possibly pyrite, which was in turn replaced by kaolinite and then pyrophyllite at higher temperature and pressure. Woody structures such as cuticle and veins, which had resisted replacement by the initial low temperature phase, were coalified at higher temperatures. •Distinctive fossils from St. Clair, Pennsylvania are composed of pyrophyllite, kaolinite, and pyrite.•Fern fossils may be only slightly compressed and must have formed by a multi-stage process.•Pyrophyllite in the fossils indicates a low-grade metamorphic origin, consistent with the formation of anthracite coal.