A RE-EVALUATION OF THE TAXODIACEOUS TAXA PRESENT IN A LATE PALEOCENE DEPOSIT IN CENTRAL NORTH DAKOTA: A SCANNING ELECTRON ANALYSIS OF MORPHOLOGY AND ANATOMY
During the summer of 2004, new specimens of conifer remains were collected at the Almont fossil locality. Hand samples were removed from the bedrock using a pry bar and pick axe. At least six morphologically distinct shoot types were identified in a collection of 48 specimens, recovered over the course of three days. The fossils and reference specimens of modern Metasequoia and Taxodium were studied under a scanning electron microscope to note similarities and differences between morphotaxa. Needle shape, cell structure and stomatal patterns were used as distinguishing characteristics.
Results indicate the presence of more than one conifer taxon present in the Almont fossil flora based on dissimilar morphological and anatomical features of the analyzed needles. At least one fossil specimen has ribbon-like midrib cell alignment similar to modern Taxodium, though elongate ripple-margined epidermal cell structure and parallel lengthwise orientation of oval stomata are like that of modern Metasequoia, implying a closer affinity to this genus. Such evidence suggests that the recent assignment of the needles to the genus Parataxodium may not be valid for all taxa represented at this site. These findings could have implications towards the current understanding of the paleoenvironment of the area, as well as, the relationships between restricted floras of the Great Plains of the United States during the Late Paleocene.