4.2 Article

Annual Rainfall and Seasonality Predict Pan-tropical Patterns of Liana Density and Basal Area

期刊

BIOTROPICA
卷 42, 期 3, 页码 309-317

出版社

WILEY
DOI: 10.1111/j.1744-7429.2009.00589.x

关键词

abundance; climate; liana communities; tropical forest

类别

资金

  1. NCEAS
  2. NSF [EF-0553768]
  3. University of California
  4. Santa Barbara
  5. State of California
  6. HSBC Climate Partnership
  7. NSF, National Science Foundation of China
  8. Wageningen University
  9. Department of Science and Technology of the Government of India
  10. World Wildlife Fund (Brazil)
  11. USAID
  12. Organization for Tropical Studies, British Ecological Society
  13. CONACyT (Mexico)
  14. European Commission
  15. Fondo Mexicano para la Conservacion de la Naturaleza
  16. BOLFOR
  17. PAPIIT-UNAM
  18. Center for Tropical Forest Science
  19. Smithsonian Tropical Research Institute
  20. University of Wisconsin-Milwaukee Graduate School
  21. International Cooperative Biodiversity Groups
  22. Bioresources Development and Conservation Programme-Cameroon
  23. Ministry of Environment and Forests-Cameroon
  24. Centre National de la Recherche Scientifique
  25. UNESCO
  26. University of Miami
  27. Pontificia Universidad Catolica del Ecuador
  28. REPSOL-YPF
  29. Andrew W. Mellon Foundation
  30. Division Of Environmental Biology
  31. Direct For Biological Sciences [0743457, 0845071, 1019436, GRANTS:13865627] Funding Source: National Science Foundation

向作者/读者索取更多资源

We test the hypotheses proposed by Gentry and Schnitzer that liana density and basal area in tropical forests vary negatively with mean annual precipitation (MAP) and positively with seasonality. Previous studies correlating liana abundance with these climatic variables have produced conflicting results, warranting a new analysis of drivers of liana abundance based on a different dataset. We compiled a pan-tropical dataset containing 28,953 lianas (>= 2.5 cm diam.) from studies conducted at 13 Neotropical and 11 Paleotropical dry to wet lowland tropical forests. The ranges in MAP and dry season length (DSL) (number of months with mean rainfall < 100 mm) represented by these datasets were 860-7250 mm/yr and 0-7 mo, respectively. Pan-tropically, liana density and basal area decreased significantly with increasing annual rainfall and increased with increasing DSL, supporting the hypotheses of Gentry and Schnitzer. Our results suggest that much of the variation in liana density and basal area in the tropics can be accounted for by the relatively simple metrics of MAP and DSL.

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