Micromorphological and geochemical signatures of soil in the Byers Peninsula, Antarctica
Byers Peninsula, micromorphology, geochemistry, pedogenesis, and climate change
Located on Livingston Island, Maritime Antarctica, on the Byers Peninsula, representing the largest ice-free area of the South Shetland archipelago, it possesses great pedological diversity and unique soil development conditions. This research sought to establish rules between microstructure and the physical and chemical properties of the soil in a highly climate-sensitive ecosystem where soils act as proxies in understanding global environmental changes, based on the hypothesis that features at the "micro" scale reveal moderate development in soils traditionally selected as incipient. The methodology integrates routine physicochemical analyses, mineralogy of the sand fraction by X-ray fluorescence (XRF), optically stimulated luminescence (OSL) dating and, primarily, the microscopic description of soil thin sections with preserved structure. The results identified five soil groups (Cryosols, Gleysols, Fluvisols, Cambisols, and Leptosols) distributed across volcanic ridges, cryoplaned surfaces, and marine terraces, exhibiting discontinuous permafrost and horizons marked by cryoturbation and solifluction. The conclusions and findings show that the genesis of the soils and uplifted marine terraces records glacio-isostatic adjustments and active freeze/thaw cycles since the Holocene, revealing that deglaciation and pedogenesis processes in the region are more complex and, in certain areas, older than previously thought, consolidating the Byers Peninsula as a critical indicator of landscape evolution and Antarctic climate regulation.