Linking soil phosphorus with forest litterfall resistance and resilience to cyclone disturbance: A pantropical meta-analysis

Barbara Bomfim, Anthony P. Walker, William H. McDowell, Jess K. Zimmerman, Yanlei Feng, Lara M. Kueppers

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

Abstract

While tropical cyclone regimes are shifting with climate change, the mechanisms underpinning the resistance (ability to withstand disturbance-induced change) and resilience (capacity to return to pre-disturbance reference) of tropical forest litterfall to cyclones remain largely unexplored pantropically. Single-site studies in Australia and Hawaii suggest that litterfall on low-phosphorus (P) soils is more resistant and less resilient to cyclones. We conducted a meta-analysis to investigate the pantropical importance of total soil P in mediating forest litterfall resistance and resilience to 22 tropical cyclones. We evaluated cyclone-induced and post-cyclone litterfall mass (g/m2/day), and P and nitrogen (N) fluxes (mg/m2/day) and concentrations (mg/g), all indicators of ecosystem function and essential for nutrient cycling. Across 73 case studies in Australia, Guadeloupe, Hawaii, Mexico, Puerto Rico, and Taiwan, total litterfall mass flux increased from ~2.5 ± 0.3 to 22.5 ± 3 g/m2/day due to cyclones, with large variation among studies. Litterfall P and N fluxes post-cyclone represented ~5% and 10% of the average annual fluxes, respectively. Post-cyclone leaf litterfall N and P concentrations were 21.6 ± 1.2% and 58.6 ± 2.3% higher than pre-cyclone means. Mixed-effects models determined that soil P negatively moderated the pantropical litterfall resistance to cyclones, with a 100 mg P/kg increase in soil P corresponding to a 32% to 38% decrease in resistance. Based on 33% of the resistance case studies, total litterfall mass flux reached pre-disturbance levels within one-year post-disturbance. A GAMM indicated that soil P, gale wind duration and time post-cyclone jointly moderate the short-term resilience of total litterfall, with the nature of the relationship between resilience and soil P contingent on time and wind duration. Across pantropical forests observed to date, our results indicate that litterfall resistance and resilience in the face of intensifying cyclones will be partially determined by total soil P.

Original languageEnglish
Pages (from-to)4633-4654
Number of pages22
JournalGlobal Change Biology
Volume28
Issue number15
DOIs
StatePublished - Aug 2022

Funding

This manuscript has been co‐authored by UT‐Battelle, LLC under Contract No. DE‐AC05‐00OR22725 with the U.S. Department of Energy. The United States Government retains and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a non‐exclusive, paid‐up, irrevocable, worldwide license to publish, or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The Department of Energy will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe‐public‐access‐plan ). This research was supported as part of the Next Generation Ecosystem Experiments-Tropics (NGEE), funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research under contract number DE-AC02-05CH11231. ORNL is managed by UT-Battelle, LLC, for the DOE under contract DE-AC05-1008 00OR22725. This research utilized data from Luquillo Long-Term Ecological Research (LTER) Program which is currently supported by NSF grant DEB-1831952 to the Institute for Tropical Ecosystem Studies, University of Puerto Rico, and to the International Institute of Tropical Forestry USDA Forest Service. We thank Robinson Negrón-Juárez, Jeffrey Chambers, Ariel Lugo, Alonso Ramírez, Whendee Silver, Daniel Imbert, Rich Norby, Choy Huang, Hsueh-Ching for providing crucial insights and data for this research and two anonymous reviewers for helpful comments. This research was supported as part of the Next Generation Ecosystem Experiments‐Tropics (NGEE), funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research under contract number DE‐AC02‐05CH11231. ORNL is managed by UT‐Battelle, LLC, for the DOE under contract DE‐AC05‐1008 00OR22725. This research utilized data from Luquillo Long‐Term Ecological Research (LTER) Program which is currently supported by NSF grant DEB‐1831952 to the Institute for Tropical Ecosystem Studies, University of Puerto Rico, and to the International Institute of Tropical Forestry USDA Forest Service. We thank Robinson Negrón‐Juárez, Jeffrey Chambers, Ariel Lugo, Alonso Ramírez, Whendee Silver, Daniel Imbert, Rich Norby, Choy Huang, Hsueh‐Ching for providing crucial insights and data for this research and two anonymous reviewers for helpful comments.

Keywords

  • Biogeochemistry
  • ecosystem function
  • hurricane
  • litterfall
  • nitrogen
  • nutrient cycling
  • soil fertility
  • typhoon

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