Long-lived topography along rifted margins: Insights from Aparados da Serra escarpment, Southeast Brazil

The Brazilian margin is one of the longest elevated passive margins (EPMs) in the world. However, both the timing of uplift and the long-term evolution of this EPM remain highly debated. In this study, we present a new suite of apatite (U-Th-Sm)/He (AHe) and fission track (AFT) ages for the southern end of the Brazilian EPM, in the Aparados da Serra plateau. Combined with literature data, our results reveal that mean AHe ages range from 43 to 112 Ma, while AFT ages range from 46 to 222 Ma. Thermal history models suggest monotonic exhumation rates in the Aparados da Serra, with post-rifting rates <50 m Myr −1 in the coastal plain and < 25 m Myr −1 in the volcanic plateau. Collectively, our results imply a total erosion of 2–4 km of material from the coast and < 2 km from the plateau since rifting ca. 120–100 Ma. AHe and AFT data indicate no detectable accelerated phase of exhumation during the Cenozoic, implying that recent uplift along the margin was either absent or minimal, and that the relief observed in the Aparados da Serra is likely a consequence of sustained rift topography. Based on the absence of major recent tectonic events, we argue that Cenozoic exhumation patterns in the Aparados da Serra were largely controlled by geomorphologic processes (e.g., differential erosion). Lastly, the equivalence between long (AFT and AHe) and short-term (catchment-averaged) erosion rates argues for sustained stability of the margin over geological timescales. • Total denudation of ~2–4 km since rifting (~120 Ma). • Post-rift erosion persistently <50 m/Myr through Late Cretaceous. • No evidence of Cenozoic uplift; erosion rater <25 m/Myr. • Present relief likely reflects inherited rift topography.