2005
DOI: 10.1098/rstb.2005.1711
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Tropical forests and the changing earth system

Abstract: Tropical forests are global epicentres of biodiversity and important modulators of the rate of climate change. Recent research on deforestation rates and ecological changes within intact forests, both areas of recent research and debate, are reviewed, and the implications for biodiversity (species loss) and climate change (via the global carbon cycle) addressed. Recent impacts have most likely been: (i) a large source of carbon to the atmosphere, and major loss of species, from deforestation and (ii) a large c… Show more

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Cited by 283 publications
(218 citation statements)
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“…The consequences of longer droughts and higher temperatures are potentially dramatic. For example, rapid forest collapse as a result of drought could convert the world's tropical forests from a net carbon sink into a large carbon source during this century 8,15 . Predicting how forests will respond to future climate changes hinges on a quantitative understanding of the physiological mechanisms governing drought stress at the species level.…”
mentioning
confidence: 99%
“…The consequences of longer droughts and higher temperatures are potentially dramatic. For example, rapid forest collapse as a result of drought could convert the world's tropical forests from a net carbon sink into a large carbon source during this century 8,15 . Predicting how forests will respond to future climate changes hinges on a quantitative understanding of the physiological mechanisms governing drought stress at the species level.…”
mentioning
confidence: 99%
“…They are important for recreation and human well being, and provide numerous ecosystem services, and are vital for the maintenance of the majority of biological diversity on Earth (Lacaze, 2000;Dirzo and Raven, 2003;Ozanne et al, 2003;Lewis, 2006). These roles need to be considered when we try to manage forests.…”
Section: Introductionmentioning
confidence: 99%
“…One important observation from a tropical forest network is the increase in biomass quantified over time on fixed-area permanent sample plots, which when scaled globally accounted for ∼60% (1.3 Pg C·y −1 ) of the residual terrestrial carbon sink (6,21). There have been broad discussions on potential causal agents driving this nonsteady-state behavior, and growth fertilization of tropical trees from increasing atmospheric CO 2 has been suggested as a parsimonious explanation for some of these observations (22). However, if patches that are rapidly losing carbon following disturbance demonstrate spatial and temporal clustering, they may be underrepresented in current sampling schemes (19,23).…”
mentioning
confidence: 99%