TL;DR: The fossil flora underlying the Middle Pennsylvanian B-coal in the Bernice Basin is an in situ clastic swamp flora which contains the large-scale remains of six pteridosperm species.
TL;DR: The compression and permineralized fossil record of presumed medullosan plants is reviewed and evaluated and a phylogeny of Monoletespollen organs is proposed.
TL;DR: In this paper, the interpretation of pteridosperm leaf cuticles is discussed on the basis of three examples of well-known taxa whose cuticles have often been misinterpreted, i.e. Callipteris conferta, Alethopteris zeilleri and Karinopteris sp.
TL;DR: In this paper, the cuticles and cuticle-free compressions of three Carboniferous medullosan seed-fern leaf species (Macroneuropteris scheuchzeri, Neuropteris ovata var. simonii and Alethopteris lesquereuxii) were analyzed by elemental, 13C nuclear magnetic resonance (NMR), micro-FTIR (Fourier transform infrared) and coal petrographic techniques.
TL;DR: In this paper, a new reconstruction of the architecture of medullosan pteridosperms is proposed on the basis of three stems preserved as compression-impression fossils: one from the Southern Anthracite Coal Field of Pennsylvania (lower part of Llewellyn Formation, Pennsylvania, Westphalian D) probably belonging to Alethopteris foliage; a second stem from the roof shale of the Eagle coal bed (Kanawha Formation, Middle Pennsylvanian,Westphalian B) of West Virginia, associated with Neuropteris foliage.
Abstract: A new reconstruction of the architecture of medullosan pteridosperms is proposed on the basis of three stems preserved as compression-impression fossils: one from the Southern Anthracite Coal Field of Pennsylvania (lower part of Llewellyn Formation, Pennsylvania, Westphalian D) probably belonging to Alethopteris foliage; a second stem from the roof shale of the Eagle coal bed (Kanawha Formation, Middle Pennsylvanian, Westphalian B) of West Virginia, associated with Neuropteris foliage; and a third reported from the Stephanian of Commentry, France, in connection with Odontopteris foliage. The diameters of the Llewellyn, Eagle, and Commentry stems are 17 cm, 13 cm, and 6.5 cm, respectively. All three stems bear remnants of petioles up to several centimeters in length. The petolar remnants indicate that the living leaves grew upward at an angle of 30 60 degrees from the vertical, a growth habit that is common in present day tropical plants with similar overall architecture. Leaves drooped only when they were dying. After decay they broke off and left short petiolar remnants bent downward. The Llewellyn and Eagle stems represent plants with thick, straight stems, whereas the Commentry specimen shows a thin and slightly curved stem. Comments Copyright Delaware Valley Paleontological Society. Published in The Mosasaur, Volume 2, 1984, pages 1-8. This journal article is available at ScholarlyCommons: http://repository.upenn.edu/ees_papers/26