Additional file 1 of Does climate change alter the nutrient trends of Cedrela fissilis Vell. trees in the southern Brazilian Amazon?
Creators: name: Ortega Rodriguez, Daigard R.
name: Sánchez-Salguero, Raúl
name: Hevia, Andrea
name: Bovi, Renata C.
name: Ferreira, Marciel J.
name: Speer, James H.
name: Roig, Fidel A.
name: Tomazello-Filho, Mario
Publisher: name: figshare
Year: 2024
Subjects: subject: Biochemistry
subject: Physiology
subject: FOS: Biological sciences
subject: Environmental Sciences not elsewhere classified
subject: Chemical Sciences not elsewhere classified
subject: Ecology
subject: Biological Sciences not elsewhere classified
subject: Cancer
subject: Plant Biology

description: Additional file 1: Fig. S1. a Map showing the location of Jamari National Forest, JNF (red triangle), Cedrela fissilis Vell. distribution (dark gray dots) and Amazon soil classification according to the Brazilian Soil Classification System (EMBRAPA 2006). Soils according to Soil taxonomy (Soil Survey Staff 2022): Ultisols (Argisols), Inceptisols (Cambisols), Entisols (Neosols, Gleysols), Oxisols (Latosols), Histosols (Organosols), Alfisols (Luvisols, Plinthosols), Spodosols (Spodosols). b Climate diagram of Walter and Lieth, based on regional meteorological and hydrological records from 1975 to 2018 (data source in Table S1), indicates dry months (solid orange area) and months with rainfall above 50 mm (solid blue areas). Green bars represent the estimated growing period of C. fissilis, which generally falls between September (previous year) and the end of May (current year) according to Lobão (2011). Phenology stages are represented by leaf icons based on C. fissilis data from Lobão (2011): open, gray filled and dark filled indicate periods of leaf fall, leaf flash and leaf fall/leaf flash (occurring simultaneously), respectively. c Anomalies (standardized values) of total annual precipitation, mean annual temperature, total annual difference between precipitation and potential evapotranspiration (P-PET) and total annual standardized precipitation evapotranspiration index (SPEI). Fig. S2. Mean index residual chronologies of molar ratios from C. fissilis trees from the southern Amazon and total annual difference between precipitation and potential evapotranspiration (P-PET, time-scales from prior September to current September). Vertical light red boxes represent extreme drought events registered in the southern Amazon basin in 1981–1983, 1997–1998, 2005–2007, 2010–2011, and 2014–2015 (Espinoza et al. 2019). On the right is the boxplot of normalized parameters in dry and wet years; a significant difference (SD) between means is also presented (p &lt; 0.05). Fig. S3. Boxplots showing standardized ring width (RW), wood density (RD), concentrations of aluminum (Al), sulfur (S), potassium (K), calcium (Ca) and calcium to manganese ratio (Ca/Mn) stability during extreme droughts from C. fissilis trees from the southern Amazon. Fig. S4. Boxplots showing standardized ring width (RW), wood density (RD), concentrations of aluminum (Al), sulfur (S), potassium (K), calcium (Ca) and calcium to manganese ratio (Ca/Mn) stability during extreme droughts from C. fissilis trees from the southern Amazon. Fig. S5. Pearson´s correlation of stability of tree-ring parameters: width (RW), wood density (RD), elements (aluminum, Al; phosphorus, P; sulfur, S; potassium, K; calcium, Ca; manganese, Mn; iron, Fe; strontium, Sr) and ratios (aluminum to calcium, Al/Ca; calcium to manganese, Ca/Mn; potassium to calcium, K/Ca; strontium to calcium, Sr/Ca; manganese to sulfur, Mn/S) of C. fissilis. Statistical significance of Pearson´s correlation: *p &lt; 0.05. Table S1. Information from meteorological stations for collected precipitation (P, 1975–2018) and temperature (T, 1957–2018) data.