225 Critical Zone Science: Intersection of Processes Linked to Geomorphology, Ecology, Fire and Climate (Posters)

This session welcomes interdisciplinary studies that investigate the rates and processes of soil development, regolith formation, carbon storage and the role of ecological and/or hydrologic feedbacks in shaping the landscape (both past and present).

Tuesday, 21 October 2025
8:00 AM - 5:30 PM
HBGCC, Hall 1

Spatiotemporal Patterns of Fire, Precipitation, and Vegetation Response across the Wetland-Savanna Mosaic of Brazil’s Pantanal

Paper number: 225-0
Program: Technical Sessions
Time: 8:00 AM – 8:00 AM

Authors

Abstract

The Pantanal is the world’s largest freshwater wetland and shaped by a composite of several alluvial fans and lowland river systems. Its low-gradient terrain supports a diverse vegetation mosaic that is controlled by seasonal flooding, drought, and fire activity. The frequency and intensity of these cycles, along with local hydrology, determines how the Pantanal’s diverse ecosystems are distributed across the landscape. Increasing climate extremes and land-use changes in recent decades raise questions about how these pressures impact the maintenance and recovery of flood- and fire-adapted ecosystems across the Pantanal.

We analyzed 23 years (2001–2023) of monthly remote-sensing data to quantify vegetation recovery across five land-cover types in the Pantanal: forest, savanna, grassland, wetland, and pasture. We evaluated monthly NDVI (MOD13A1), fire activity (MCD64A1), and precipitation (CHIRPS) across land-cover boundaries defined by MapBiomas. After deseasonalizing each series, we applied Spearman’s rank and lagged correlations (1–6 months) to assess how rainfall and fire influence vegetation greenness (i.e., NDVI). At the biome scale, precipitation peaks in January and NDVI in March, followed by drought and fire activity that culminate in September. Across the Pantanal, rainfall most strongly enhances NDVI at a one-month lag (ρ = 0.38, p < 0.001), with effects fading by four months. In contrast, fire sharply suppresses NDVI at a one-month lag (ρ = –0.44, p < 0.001), with recovery typically within three months.

Across land-cover types, grasslands record the largest burned area annually and experience the largest post-fire NDVI declines (ρ = –0.47 at lag 1). Savannas show the most prolonged fire effects (ρ = –0.23 at lag 3), while forests exhibit intermediate sensitivity to both drivers. Wetlands sustain elevated fire activity into October and November, well after fires subside in other land-cover types. Notably, in 2020, forests burned as extensively as fire-adapted savannas, while in 2023, wetlands burned as extensively as fire-prone grasslands; both patterns not seen elsewhere in the time series. Our results reveal that vegetation responses to fire and precipitation vary in timing, intensity, and duration across land-cover types, underscoring the need to better understand disturbance–recovery dynamics in complex ecosystem mosaics.

Geological Society of America Abstracts with Programs. Vol. 57, No. 6

doi: 10.1130/abs/2025AM-412470

© Copyright 2025 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.