Long-Term Landscape Evolution in Response to Climate Change, Ecosystem Dynamics, and Fire in a Basaltic Catchment on the Colorado Plateau
Metadatos
Mostrar el registro completo del ítemAutor
Staley, Spencer E.; Fawcett, Peter J.; Jiménez Moreno, Gonzalo; Anderson, R. Scott; Markgraf, Vera; Brown, Erik T.Editorial
Wiley
Fecha
2023-12-14Referencia bibliográfica
Staley, S. E., Fawcett, P. J., Jiménez-Moreno, G., Anderson, R. S., Markgraf, V., & Brown, E. T. (2023). Long-term landscape evolution in response to climate change, ecosystem dynamics, and fire in a basaltic catchment on the Colorado Plateau. Journal of Geophysical Research: Earth Surface, 128, e2023JF007266.https://doi. org/10.1029/2023JF007266
Patrocinador
CSD Facility (formerly LACCORE) at the University of Minnesota; XRF Laboratory of the Large Lakes Observatory at the University of Minnesota; UNM's Analytical Chemistry Laboratory; UNM's Electron Microbeam Facility; UNM's X-Ray Diffraction Laboratory/Center for MicroEngineered Materials; US Forest Service; Pilot Grant Program (PGP) grant from NAU; Ministerio de Ciencia, Innovación y Universidades, Grants PRX18/00080 and PRX21/00127; Arizona TRIF research program (Project 1002654); “Mega-droughts, climate change and the Southwest: STL, AZ, Paleoenvironments Drilling Project”Resumen
Predicting responses of semi-arid to montane landscapes in southwestern North America to ongoing anthropogenic changes requires understanding of past interplay among geomorphic, ecologic, and climatic factors. This study utilizes modern weathering and sediment transport processes to inform the interpretation of a 250-kyr lacustrine sediment record of paleoecology, hydrology, and erosion from a small, closed basin, basaltic catchment on the southwestern edge of the Colorado Plateau. Geochemical and mineralogical analyses of bedrock, colluvium, and lake sediments indicate that clastic sediments in the basin are a mixture of local physical weathering products (albite and ilmenite) and eolian dust (quartz, illite, and zircon). Dust fractions increase during glacial periods coincident with lower overall sedimentation rates, suggesting this pattern results from decreased local erosion rates and not increased dust deposition. Titanium counts from X-ray fluorescence core scanning, a proxy for ilmenite content, traces past local erosion rates. The highest erosion rates, inferred from the highest Ti counts, follow climatic transitions toward interglacial conditions (Marine Isotope Stage 5e, 3a, and the Holocene), periods characterized by vegetation changeover (observed in the core's palynology), higher temperatures (piñon-juniper-oak pollen abundance), lower effective precipitation (shallow lake facies), and increased wildfire activity (microscopic charcoal particle counts and sizes). While brief inferred episodes of erosion occur following abrupt transitions to cooler and wetter conditions, indicated by the abundance of subalpine tree (spruce and fir) pollen and deeper lake facies, landscapes appear more stable during glacial periods. This long-term perspective suggests that aridification and resulting vegetation succession and increased wildfires will increase erosion rates in similar settings regionwide.