At Caxiuanã National Forest (eastern Amazon), trees in a >20-year, 50% throughfall-exclusion plot (PTs, "primed") were compared with controls (CTs) through the record 2023 El Niño dry season (82 mm rainfall vs the 1982–2022 mean of 227 ± 105 mm; record VPD of 3.6 kPa on 31 Oct 2023). Using sap flux on 40 individuals, linear mixed models with tree identity as a random effect found: PT daily transpiration resistance declined at -0.0017 day⁻¹ [95% CI -0.0022, -0.0016] vs -0.0036 day⁻¹ [-0.0038, -0.0034] in CTs; at peak drought PTs retained 0.75 [0.64, 0.86] of pre-drought transpiration vs 0.46 [0.44, 0.54] in CTs .
After rains returned, PTs fully recovered to >95% of pre-drought transpiration within 143 days, while CTs plateaued at 77.5% despite soil moisture rebounding — a hysteretic legacy effect. Mediation analysis showed treatment differences in resistance trajectories were largely explained by soil water availability per unit biomass (mortality-thinned TFE biomass), though the treatment effect on recovery persisted after this adjustment .
Terrestrial laser scanning (242 scans/plot) showed PTs had ~26.5% smaller crown area per unit stem diameter (141 vs 192 m² m⁻¹; t = 2.2, p = 0.016), smaller crown volume per stem diameter (585 vs 844 m³ m⁻¹, p = 0.023), and lower crown volume per stem cross-sectional area (Wilcoxon p = 0.034). Control-plot LAI fell ~20% (5.76 → 4.62 m² m⁻²) via leaf shedding, while TFE LAI stayed stable (Kruskal-Wallis p = 0.459). PTs also regulated water potential less stringently (-0.46 MPa) despite similar minimum leaf water potentials — consistent with structural, not physiological, drought adjustment .
Strengths: a unique natural-experiment design bridging a 20+ year manipulation with a once-in-a-generation drought; pre-registered-style hypotheses; bootstrap robustness (plot × time interaction significant in 94.3% of 1000 resamples for resistance, but only 71.5% for resilience); data and R code fully public .
Weaknesses the authors partially acknowledge: (1) single plot per treatment — plot-level confounding (soil, slope, history) cannot be ruled out and tree-level n=40 may overstate confidence; (2) TLS absent at baseline, so whether PT crown reduction reflects plasticity or selective mortality is unknown — a key interpretive ambiguity the authors flag but cannot resolve; (3) bimonthly water-potential sampling likely missed peak-drought variation (December campaign excluded); (4) VPD measured at only two heights may misattribute canopy-level evaporative demand in the more open TFE canopy, potentially biasing the stringency metric; (5) the resilience bootstrap (71.5%) is only moderately robust; (6) partial taxonomic matching between plots could introduce species-level confounding, though measured functional traits showed no plot differences. The authors also argue, somewhat speculatively, that their results "complement" tipping-point frameworks — this is interpretation, not demonstration.
Confidence: the core physiological contrast is well supported at tree level within this site; extrapolation to unmanaged Amazon forests or other regions remains uncertain. What would change the conclusion: replicated plot pairs, or a control plot experiencing the same mortality thinning without drought priming, showing equal resistance/resilience.
Figures use only reported values from the paper; TFE post-drought LAI shown at its stable median range (~4.4–4.6).
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