2016
DOI: 10.1007/s00468-016-1362-0
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Climate variability, tree increment patterns and ENSO-related carbon sequestration reduction of the tropical dry forest species Loxopterygium huasango of Southern Ecuador

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Cited by 25 publications
(15 citation statements)
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“…Most general circulation models (GCMs) predict an increase in annual precipitation in northwestern Peru and southern Ecuador, but a decrease in dry season precipitation, especially in the lowland forests. Previous studies suggest that marked drought events can engender strong negative impacts on the recruitment, survival and growth rates of TDF tree species (Castro, Sanchez-Azofeifa, & Sato, 2018;Maza-Villalobos, Poorter, & Martínez-Ramos, 2013;Spannl et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Most general circulation models (GCMs) predict an increase in annual precipitation in northwestern Peru and southern Ecuador, but a decrease in dry season precipitation, especially in the lowland forests. Previous studies suggest that marked drought events can engender strong negative impacts on the recruitment, survival and growth rates of TDF tree species (Castro, Sanchez-Azofeifa, & Sato, 2018;Maza-Villalobos, Poorter, & Martínez-Ramos, 2013;Spannl et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…The balance between CO 2 sink and source during drought is important because future drought in tropical regions may increase in frequency and severity because of global climate change [55]. These adverse weather conditions cause a reduction in tree growth, showing the serious impact of such climate extremes on carbon sequestration in dry tropical forest ecosystems [56]. Collectively, the results of the present study offer insights on photosynthesis and carbon assimilation dynamics in Z. serrata plantations, which could facilitate the assessment and management of plantation species under projected climate change.…”
Section: Seasonal Carbon Assimilationmentioning
confidence: 99%
“…The balance between CO 2 sink and source during drought is important because future drought in tropical regions may increase in frequency and severity because of global climate change (Grünzweig et al 2003). These adverse weather conditions cause a reduction in tree growth, showing the serious impact of such climate extremes on carbon sequestration in dry tropical forest ecosystems (Spannl et al 2016).…”
Section: Seasonal Carbon Assimilationmentioning
confidence: 99%