Multiproxy Approach to Reconstruct the Fire History of Araucaria araucana Forests in the Nahuelbuta Coastal Range, Chile

Author:

Muñoz Ariel A.1234ORCID,González Mauro E.356,Schneider-Valenzuela Isadora12ORCID,Klock-Barría Karin17,Madariaga-Burgos Marcelo12ORCID,Rodríguez Carmen Gloria5,Abarzúa Ana M.8,Solari María Eugenia9ORCID,Martel-Cea Alejandra810ORCID,Velásquez Bárbara8,Paredes Beatriz8,Guerrero Fabián11ORCID,Montiel Mauricio7,Tapia-Marzán Valeria1,Riquelme Tomás7,Sheppard Paul R.12

Affiliation:

1. Laboratorio de Dendrocronología y Estudios Ambientales, Instituto de Geografía, Pontificia Universidad Católica de Valparaíso, Valparaíso 2362807, Chile

2. Centro de Acción Climática, Pontificia Universidad Católica de Valparaíso, Valparaíso 2362807, Chile

3. Center for Climate and Resilience Research, CR2, Santiago 8370449, Chile

4. Fundación San Ignacio del Huinay, Hualaihué 5860000, Chile

5. Laboratorio de Ecología de Bosques, Laboratorio de Dendrocronología y Cambio Global, Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia 5090000, Chile

6. Center of Fire and Socioecosystem Resilience (FireSES), Valdivia 5090000, Chile

7. Escuela de Graduados, Facultad de Ciencias Forestales y Recursos Naturales, Universidad Austral de Chile, Valdivia 5090000, Chile

8. Laboratorio de Palinología y Reconstrucciones Ambientales, Instituto Ciencias de la Tierra, Universidad Austral de Chile, Valdivia 5090000, Chile

9. Laboratorio de Arqueobotánica e Historia Ambiental, I. de Estudios Antropológicos, Universidad Austral de Chile, Valdivia 5090000, Chile

10. Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena 1780000, Chile

11. Department of Mechanical Engineering, Universidad Técnica Federico Santa María, Avenida España 1680, Valparaíso 2340000, Chile

12. Laboratory of Tree-Ring Research, 407 Bryant Bannister Tree-Ring Building, University of Arizona, Tucson, AZ 85721, USA

Abstract

Multiproxy reconstructions of fire regimes in forest ecosystems can provide a clearer understanding of past fire activity and circumvent some limitations of single proxy reconstructions. While inferring fire history from scars in trees is the most precise method to reconstruct temporal fire patterns, this method is limited in Araucaria araucana forests by rot after fire injuries, successive fires that destroy the evidence and the prohibition of sample extraction from living Araucaria trees. In this context, dendrochemical studies in Araucaria trees and charcoal analysis from sediment cores can complement and extend the time perspective of the fire history in the relictual Araucaria-Nothofagus forests of the coastal range. We used dendrochemical, fire scar and charcoal records from the Nahuelbuta Coastal Range (37.8° S; 73° W) spanning the last 1000 years to reconstruct the fire history. The results indicate that periods with higher fire activity occurred between 1400 and 1650 AD. Long-term changes in the fire regime are related to increased climate variability over the last 1000 years, and especially with the arrival of settlers to the area after 1860 CE. The most severe fire events in the Nothofagus and Araucaria forests occurred when suitable fire-prone conditions were superimposed with high human densities.

Funder

Fondecyt/ANID

FONDAP-ANID

Publisher

MDPI AG

Subject

Forestry

Reference144 articles.

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