Abstract

(1) Background: Frequent fire, climate variability, and human activities collectively influence savanna ecosystems. The relative role of these three factors likely varies on interannual, decadal, and centennial timescales. Here, we tested if Euro-American activities uncoupled drought and fire frequencies relative to previous centuries in a temperate savanna site. (2) Methods: We combined records of fire frequency from tree ring fire scars and sediment charcoal abundance, and a record of fuel type based on charcoal particle morphometry to reconstruct centennial scale shifts in fire frequency and fuel sources in a savanna ecosystem. We also tested the climate influence on fire occurrence with an independently derived tree-ring reconstruction of drought. We contextualized these data with historical records of human activity. (3) Results: Tree fire scars revealed eight fire events from 1822–1924 CE, followed by localized suppression. Charcoal signals highlight 13 fire episodes from 1696–2001. Fire–climate coupling was not clearly evident both before and after Euro American settlement The dominant fuel source shifted from herbaceous to woody fuel during the early-mid 20th century. (4) Conclusions: Euro-American settlement and landscape fragmentation disrupted the pre-settlement fire regime (fire frequency and fuel sources). Our results highlight the potential for improved insight by synthesizing interpretation of multiple paleofire proxies, especially in fire regimes with mixed fuel sources.

Highlights

  • Fire and climate, together, are the main drivers of ecosystem structure and function over millennia [1,2]

  • Subtle changes in fire frequency can lead to substantial changes in the structure and composition of vegetation communities with varying tree cover such as savannas [7], yet clarifying the relative and interactive roles of historical fire and climate variability in savanna dynamics has been difficult because of challenges in obtaining long records of fire activity through dendrochronology or charcoal particles preserved in sedimentary records [8,9]

  • These samples were dated against a 206-year ring-width chronology based on measurements of 114 increment core samples from 51 living trees, including the living tree sampled for fire scars

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Summary

Introduction

Together, are the main drivers of ecosystem structure and function over millennia [1,2]. Savannas are found at the climate-mediated interface between closed-canopy forests with multidecadal to centennial fire return intervals and grasslands with annual fire return intervals [4,5,6]. The climate system affects ecosystem structure and function directly through variation in precipitation, temperature, soil moisture, and evaporation. Drought is a hydroclimate extreme that integrates these variables and constitutes a key type of disturbance affecting ecosystem dynamics and vegetation composition [10,11]. Drought variability modulates overall ecosystem productivity, Fire 2019, 2, 51; doi:10.3390/fire2030051 www.mdpi.com/journal/fire

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