Chironomidae has been used as climate proxy in Europe and North America, particularly in temperate lakes. However, attempts in the Southern Hemisphere remains extremely limited. In Brazil, this study represents the first attempt to establish Chironomidae as a climate proxy, while combining total head capsule counts retrieved from a dated sediment core with environmental variables, including air temperature, precipitation, sea-level rise, extreme rainfall, geochemistry, among others. In this case, we have retrieved a 66cm-sediment core from a mangrove site at Ilha Grande Island (Rio de Janeiro State/Southeast Brazil). Half of the core was used for Chironomidae identification and counts, and the other half for 210Pb dating and elemental analysis. Our results showed significant correlation between (r = 0.83; p = 0.0014) Chironomidae and air temperature and Chironomidae and de Martone Index (climate index). Chironomidae abundance increased gradually from mid-1970s to 2020. Between 2022 and 2024 we observed an exponential surge, accompanying recent. Extreme rainfall events and a warmer condition. Such events may rework sediments in the mangrove environment, enhance nutrient availability, boost primary productivity and support higher zooplankton abundance and make a favorable condition to the increase of Chironomidae. Our finding in Brazil aligns with other tropical studies in Latin America using Chironomidae as a climate proxy, demonstrating the reliability of Ilha Grande Island mangrove records for reconstructing past climate and associated environmental changes.