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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

The hydroclimatic and ecophysiological basis of cloud forest distributions under current and projected climates

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Author(s):
Oliveira, Rafael S. [1, 2] ; Eller, Cleiton B. [1] ; Bittencourt, Paulo R. L. [1] ; Mulligan, Mark [3]
Total Authors: 4
Affiliation:
[1] Univ Estadual Campinas UNICAMP, Inst Biol, Dept Biol Vegetal, Campinas, SP - Brazil
[2] Univ Western Australia, Fac Nat & Agr Sci, Sch Plant Biol, Nedlands, WA 6009 - Australia
[3] Kings Coll London, Dept Geog, London WC2R 2LS - England
Total Affiliations: 3
Document type: Review article
Source: ANNALS OF BOTANY; v. 113, n. 6, p. 909-920, MAY 2014.
Web of Science Citations: 45
Abstract

Tropical montane cloud forests (TMCFs) are characterized by a unique set of biological and hydroclimatic features, including frequent and/or persistent fog, cool temperatures, and high biodiversity and endemism. These forests are one of the most vulnerable ecosystems to climate change given their small geographic range, high endemism and dependence on a rare microclimatic envelope. The frequency of atmospheric water deficits for some TMCFs is likely to increase in the future, but the consequences for the integrity and distribution of these ecosystems are uncertain. In order to investigate plant and ecosystem responses to climate change, we need to know how TMCF species function in response to current climate, which factors shape function and ecology most and how these will change into the future. This review focuses on recent advances in ecophysiological research of TMCF plants to establish a link between TMCF hydrometeorological conditions and vegetation distribution, functioning and survival. The hydraulic characteristics of TMCF trees are discussed, together with the prevalence and ecological consequences of foliar uptake of fog water (FWU) in TMCFs, a key process that allows efficient acquisition of water during cloud immersion periods, minimizing water deficits and favouring survival of species prone to drought-induced hydraulic failure. Fog occurrence is the single most important microclimatic feature affecting the distribution and function of TMCF plants. Plants in TMCFs are very vulnerable to drought (possessing a small hydraulic safety margin), and the presence of fog and FWU minimizes the occurrence of tree water deficits and thus favours the survival of TMCF trees where such deficits may occur. Characterizing the interplay between microclimatic dynamics and plant water relations is key to foster more realistic projections about climate change effects on TMCF functioning and distribution. (AU)

FAPESP's process: 11/52072-0 - Soil-plant-atmosphere interactions in a changing tropical landscape
Grantee:Rafael Silva Oliveira
Support Opportunities: Research Grants - Research Partnership for Technological Innovation - PITE
FAPESP's process: 10/17204-0 - Climate change in Brazilian mountains: functional responses of native plants from campos rupestres and campos de altitude to extreme droughts
Grantee:Rafael Silva Oliveira
Support Opportunities: Regular Research Grants