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In the Barro Colorado Island 50-ha plot (1982–2015), the stem shift toward dry-site tree species stopped by 2000–2005, as a drought legacy predicts, and did not continue as drying predicts

Feeley et al. (2011) reported a shift toward drought-tolerant tree species in the Barro Colorado Island (BCI) 50-ha plot, Panama, in about 1982-2005. They gave two possible causes: a legacy of the 1982-83 El Nino drought, or continuing drying. We used the 2010 and 2015 censuses as an out-of-sample test. A legacy predicts that the shift stops; continuing drying predicts that it continues. We calculated the community-weighted mean (CWM) of two species moisture affinities for all living stems of 10 mm dbh or more: (1) the dry-season soil water potential at the 1982 stem positions in the plot, and (2) the dry-season moisture deficit of 42 other Panama plots where the species occurs. For affinity (1), the CWM moved toward dry-site species at -0.023 SD per decade in 1985-2005 (95% 1-ha block bootstrap -0.028 to -0.016) and at +0.003 in 2005-2015 (-0.003 to +0.009). The rate change has 95% intervals above zero for 1-ha blocks, 250 m blocks and a species bootstrap. The rate per census interval decreased to about zero after 2000. Species with wetter affinity declined more in 1985-2005 (Spearman rho -0.19, p = 0.004) but not in 2005-2015 (rho +0.06, p = 0.41). Affinity (2) gave no robust 1985-2005 shift: one species, Faramea occidentalis, made all of it, and after 2005 the CWM moved toward wetter species. The BCI rain gauge shows no drying: January-April rain was 259 mm in 1985-2004 and 236 mm in 2005-2014. Thus the stem data agree with a drought legacy. Limitations: the shifts are small (about 0.05 SD in total) and are not different from random permutation of affinities among species (p = 0.17-0.90). Few abundant species control them. In trees of 100 mm or more, the within-plot shift continued after 2005 at a similar rate, so the test does not separate the causes for large trees. Our affinity values are not the exact values of Feeley et al., and the data end in 2015.

tropical forest · Barro Colorado Island · drought tolerance · community weighted mean · species composition change · El Nino · out-of-sample test · soil water potential · ForestGEO · Panama

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References

10
  1. doi:10.1890/10-0724.1

    Reports the 1982-2005 shift toward drought-tolerant species and the two possible causes that we test with the 2010 and 2015 censuses. Our stem data agree with its legacy explanation, but the shift is not different from random affinity permutation.

  2. supportsdoi:10.1186/s40663-017-0103-1

    Condit et al. 2017 report that most moisture-demanding species recovered after the 1980s droughts; our community-level test agrees.

  3. supportsdoi:10.1002/ecy.1952

    Katabuchi et al. 2017 found that few species cause BCI community trait shifts; we find the same for moisture affinities.

  4. usesdoi:10.15146/5xcp-0d46

    BCI 50-ha plot tree census tables, species table and elevation grid.

  5. usesdoi:10.15146/mdpr-pm59

    Panama plot census tables for the rainfall-gradient affinity.

  6. usesdoi:10.7291/D1B963

    Plot dry-season moisture deficit values.

  7. usesdoi:10.5061/dryad.1023m1d

    Dry-season soil water potential at 200 sites in the 50-ha plot.

  8. doi:10.1038/s41597-019-0072-z

    Description of the BCI soil water potential measurements.

  9. usesdoi:10.60635/C3091D

    BCI clearing daily rainfall record.

  10. doi:10.1073/pnas.1218042110

    Species distributions along the Panama dry-season gradient; our presence-based affinity is a simpler measure.

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