LATE PALEOZOIC REGIONAL PALEOCLIMATE OF THE PROTOPRECORDILLERAN GONDWANA MARGIN: A CASE STUDY IN THE PAGANZO BASIN

LEVI MOXNESS; PABLO JOAQUIN ALONSO MURUAGA; JOHN ISBELL; SHENCKMAN JAZMIN; KATHRYN PAULS; CARLOS O. LIMARINO

Congreso; GSA Annual Meeting in Indianapolis, Indiana, USA - 2018; 2018

During the mid-Carboniferous, ice centers located in present-day western Argentina disappeared until the late Cenozoic with glaciationof the Andes. The disappearance of mid-Carboniferous glaciers, and the subsequent climate shift, recorded in the Paganzo Basin hasbeen attributed to global events and drivers, such as increased atmospheric CO2 concentrations and the shifting position ofGondwana across the South Pole. However, glaciers continued at the same paleolatitude in eastern South America and did notdisappear from Gondwana until the Late Permian. This study looks at links to local drivers that acted in combination with other globaldrivers to explain the early deglaciation along the western margin of Gondwana. To do this, several localities within the Paganzo andCalingasta-Uspallata basins in western Argentina were sampled for geochemical analyses. Here, we test the applicability of theChemical Index of Alteration on strata in the Olta-Malanzán paleovalley in the eastern Paganzo Basin that historically was thought tohave been glaciated. A recent study by the authors has shown that the paleovalley was not glaciated, but owes its origin to extensionand excavation by fluvial processes. However, the late Paleozoic stratigraphy is similar to the rest of the Paganzo Basin. The resultsfrom the paleovalley samples show that this area was intermittently humid and arid through time, but with an overall arid profile. Thissignature is predominantly due to the nature of the paleovalley, which was subject to rapid burial from frequent rock falls, progradationalluvial fans/fan deltas, and lacustrine sediment gravity flows (Malanzán Fm.), which prevented any significant chemical weathering.While the overall Pennsylvanian climatic signature appears to be relatively arid (Malanzán, Loma Larga, and Solca Fms.), it seemsthat the climate during the deposition of the late Pennsylvanian and Permian La Colina Formation, was more humid than previouslythought. Further analysis is needed to assess the overall climate for the rest of the Paganzo Basin.