TRACKING THE IMPACT OF LAND PLANTS ON EARTH SYSTEMS ON THE NORTHWESTERN LAURENTIAN MARGIN
Sampling efforts have focused on the Silurian-Devonian transition along the Alaska-Yukon border, which records continental margin sedimentation on the northwestern margin of Laurentia. Stratigraphic sections of the Ordovician-Silurian Road River Group at the Tatonduk River, and the Devonian McCann Hill Chert at its type section near Hillard Peak, Alaska, were measured and sampled. Here new programmed pyrolysis data constraining the thermal maturity of the sections will be presented and future plans for palynology, conodont biostratigraphy, Re-Os geochronology, and organic (biomarkers) and inorganic geochemical analyses will be discussed. If palynomorph and plant macrofossil diversity and abundance correlate with shifts in geochemical redox tracers this will allow for the detailed, high-resolution linkage of plant evolution and marine geochemistry through the Silurian-Devonian interval. The geochemical and palaeobotanical data from these Alaskan successions will provide well-calibrated records of redox change through the Silurian-Devonian transition, directly connected to palaeobotanical records, and thus one of the strongest tests to date of whether terrestrial evolution is temporally associated with redox changes in the marine realm.