Climate variability of the southern Amazon inferred by a multi-proxy tree-ring approach using Cedrela fissilis Vell

Daigard Ricardo Ortega Rodriguez*, Raúl Sánchez-Salguero, Andrea Hevia, Daniela Granato-Souza, Bruno B.L. Cintra, Bruna Hornink, Laia Andreu-Hayles, Gabriel Assis-Pereira, Fidel A Roig, Mario Tomazello-Filho

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

The analysis of climate variability and development of reconstructions based on tree-ring records in tropical forests have been increasing in recent decades. In the Amazon region, ring width and stable isotope long-term chronologies have been used for climatic studies, however little is known about the potential of wood traits such as density and chemical concentrations. In this study, we used well-dated rings of Cedrela fissilis Vell. from the drought-prone southern Amazon basin to assess the potential of using inter-annual variations of annually-resolved ring width, wood density, stable oxygen isotope (δ18OTR) measured in tree-ring cellulose and concentration of Sulfur (STR) and Calcium (CaTR) in xylem cells to study climate variability. During wet years, Cedrela fissilis produced wider and denser rings with higher CaTR and lower STR, as well as depleted δ18OTR values. During dry years, a wider range of responses was observed in growth, density and STR, while lower CaTR and enriched δ18OTR values were found. The annual centennial chronologies spanning from 1835 to 2018 showed good calibration skills for reconstructing local precipitation, evapotranspiration (P-PET), Amazon-wide rainfall, as well as climate modes related to sea surface temperature (SST) anomalies such as El Niño South Oscillation (ENSO), Tropical Northern Atlantic (TNA), and the Western Hemisphere Warm Pool (WHWP) oscillations. CaTR explained 42 % of the variance of local precipitation (1975–2018), RW explained 30 % of the P-PET variance (1975–2018), while δ18OTR explained 60 % and 57 % of the variance of Amazon rainfall (1960–2018) and El Niño 3.4 (1920–2018), respectively. Our results show that a multi-proxy tropical tree-ring approach can be used for high-reliable reconstructions of climate variability over Amazon basin at inter-annual and multidecadal time scales.
Original languageEnglish
Article number162064
Number of pages15
JournalScience of the Total Environment
Volume871
Early online date8 Feb 2023
DOIs
Publication statusPublished - 1 May 2023

Bibliographical note

Acknowledgements:
We thank the Wood Anatomy and Tree-Ring Laboratory (LAIM) (FAPESP project: 2009/53951-7), Department of Forest Sciences, Luiz de Queiroz College of Agriculture (ESALQ). This research was supported by the Post-Graduate Program of Forest Resources (ESALQ-USP, Brazil), and FAPESP grants 2020/04608-7, 2018/22914-8 and 2017/50085-3. RSS was supported by VULBOS project (UPO-1263216), VURECLIM (P20_00813) and AH by PinCaR project (UHU-1266324) both by FEDER Funds, Andalusia Regional Government, Consejería de Economía, Conocimiento, Empresas y Universidad 2014-2020. RSS and AH were also supported by EQC2018-004821-P and IE19_074 UPO projects cofunded by Spanish “Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020” and “Plan Andaluz de Invetigación, Desarrollo e Innovación (PAIDI 2020)”, respectively. GAP was supported by CAPES (grant # 88887.199858/2018-00) in the National Academic Cooperation Program in the Amazon. Additional thanks to the logging company AMATA for their assistance in the field work.

Keywords

  • Wood traits
  • Dendroclimatology
  • Dendrochemistry
  • Tropical forests
  • ENSO
  • SST

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