Your browser doesn't support javascript.
loading
Role of tree size in moist tropical forest carbon cycling and water deficit responses.
Meakem, Victoria; Tepley, Alan J; Gonzalez-Akre, Erika B; Herrmann, Valentine; Muller-Landau, Helene C; Wright, S Joseph; Hubbell, Stephen P; Condit, Richard; Anderson-Teixeira, Kristina J.
Affiliation
  • Meakem V; Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, 22630, USA.
  • Tepley AJ; Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, 22630, USA.
  • Gonzalez-Akre EB; Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, 22630, USA.
  • Herrmann V; Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, 22630, USA.
  • Muller-Landau HC; Center for Tropical Forest Science, Smithsonian Tropical Research Institute, Balboa Ancon, Panama, Republic of Panama.
  • Wright SJ; Center for Tropical Forest Science, Smithsonian Tropical Research Institute, Balboa Ancon, Panama, Republic of Panama.
  • Hubbell SP; Center for Tropical Forest Science, Smithsonian Tropical Research Institute, Balboa Ancon, Panama, Republic of Panama.
  • Condit R; Department of Ecology and Evolutionary Biology, University of California, Los Angeles, Los Angeles, CA, 90095, USA.
  • Anderson-Teixeira KJ; Center for Tropical Forest Science, Smithsonian Tropical Research Institute, Balboa Ancon, Panama, Republic of Panama.
New Phytol ; 219(3): 947-958, 2018 08.
Article in En | MEDLINE | ID: mdl-28585237
Drought disproportionately affects larger trees in tropical forests, but implications for forest composition and carbon (C) cycling in relation to dry season intensity remain poorly understood. In order to characterize how C cycling is shaped by tree size and drought adaptations and how these patterns relate to spatial and temporal variation in water deficit, we analyze data from three forest dynamics plots spanning a moisture gradient in Panama that have experienced El Niño droughts. At all sites, aboveground C cycle contributions peaked below 50-cm stem diameter, with stems ≥ 50 cm accounting for on average 59% of live aboveground biomass, 45% of woody productivity and 49% of woody mortality. The dominance of drought-avoidance strategies increased interactively with stem diameter and dry season intensity. Although size-related C cycle contributions did not vary systematically across the moisture gradient under nondrought conditions, woody mortality of larger trees was disproportionately elevated under El Niño drought stress. Thus, large (> 50 cm) stems, which strongly mediate but do not necessarily dominate C cycling, have drought adaptations that compensate for their more challenging hydraulic environment, particularly in drier climates. However, these adaptations do not fully buffer the effects of severe drought, and increased large tree mortality dominates ecosystem-level drought responses.
Subject(s)
Key words

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Trees / Tropical Climate / Forests / Carbon Cycle Country/Region as subject: America central / Panama Language: En Journal: New Phytol Journal subject: BOTANICA Year: 2018 Document type: Article Affiliation country: United States Country of publication: United kingdom

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Trees / Tropical Climate / Forests / Carbon Cycle Country/Region as subject: America central / Panama Language: En Journal: New Phytol Journal subject: BOTANICA Year: 2018 Document type: Article Affiliation country: United States Country of publication: United kingdom