Centennial and millennial‐scale dynamics in Araucaria–Nothofagus forests in the southern Andes.

Aim: To assess the relative roles of long‐term (millennial‐scale) climatic change, fire and volcanic disturbance on the dynamics of Araucaria–Nothofagus forests of south‐central Chile. Through this analysis, we provide insight into how these iconic ecosystems may respond to future ash‐fall events under anticipated changes to climate and burning regimes. Location: Lago Cilantro is a small lake located in south‐central Chile (38°51′36.72 S, 71°17′14.52 W, 1,400 m asl), proximal to several active volcanos within the Southern Volcanic Zone of the Andes Mountain range. Taxon: Araucaria araucana (Araucariaceae); Nothofagus spp. (Nothofagaceae). Methods: We developed a continuous 8,700‐year long pollen and charcoal record from Lago Cilantro. We compared these results with proxies of regional climatic change and used a combination of principal component analysis and superposed epoch analysis to test the relationship between tephra deposition and pollen composition. Results: We detect a shift in dominance from Araucaria araucana to Nothofagus species between ~8.7 and ~5.5 ka (ka = 1,000 years before present‐1950 CE), in concert with increasing regional precipitation and decreasing local‐scale fire activity. A reversal in this trend occurred after ~4 ka, contemporaneous with a reduction in regional precipitation. Centennial‐scale increases in Araucaria araucana from ~0.2 to 0.9 ka, ~5.2 to 4.2 ka and ~8.6 to 7 ka are associated with reductions in fire return intervals. We found 24 tephra layers in this record; tephra >2 cm thickness are associated with short‐term (<100 year) compositional shifts in the pollen spectra, while a single large (255 cm) tephra at ~3 ka is associated with a substantial reduction in Nothofagus and no change in Araucaria. Main Conclusions: Climate change drove millennial‐scale shifts in Araucaria–Nothofagus forests and fire regimes near Lago Cilantro. A shortening of the fire return interval is associated with an increase in the importance of Araucaria, supporting the notion that recurrent fires are required to allow this tree species to compete with Nothofagus. Tephra deposition triggered short‐term compositional responses in this system that appears to be overwhelmed by climate and fire at longer time‐scales. Araucaria araucana can survive and potentially outcompete Nothofagus following the deposition of very thick tephra, thanks to its thick bark and tall canopy (>15 m). [ABSTRACT FROM AUTHOR]