Leaf flushing during the dry season: The paradox of Asian monsoon forests

Aim: Most deciduous species of dry monsoon forests in Thailand and India form new leaves 1-2 months before the first monsoon rains, during the hottest and driest part of the year around the spring equinox. Here we identify the proximate causes of this characteristic and counterintuitive 'spring...

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Main Authors: Stephen Elliott, Patrick J. Baker, Rolf Borchert
Format: Journal
Published: 2018
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spelling th-cmuir.6653943832-614862018-09-11T08:57:24Z Leaf flushing during the dry season: The paradox of Asian monsoon forests Stephen Elliott Patrick J. Baker Rolf Borchert Agricultural and Biological Sciences Environmental Science Aim: Most deciduous species of dry monsoon forests in Thailand and India form new leaves 1-2 months before the first monsoon rains, during the hottest and driest part of the year around the spring equinox. Here we identify the proximate causes of this characteristic and counterintuitive 'spring-flushing' of monsoon forest trees. Location: Trees of 20 species were observed in semi-deciduous dry monsoon forests of northern Thailand with a 5-6-month-long severe dry season and annual rainfall of 800-1500 mm. They were growing on dry ridges (dipterocarp-oak forest) or in moist gullies (mixed deciduous-evergreen forest) at 680-750 m altitude near Chiang Mai and in a dry lowland stand of Shorea siamensis in Utahai Thani province. Methods: Two novel methods were developed to analyse temporal and spatial variation in vegetative dry-season phenology indicative of differences in root access to subsoil water reserves. Results: Evergreen and leaf exchanging species at cool, moist sites leafed soon after partial leaf shedding in January-February. Drought-resistant dipterocarp species were evergreen at moist sites, deciduous at dry sites, and trees leafed soon after leaf shedding whenever subsoil water was available. Synchronous spring flushing of deciduous species around the spring equinox, as induced by increasing daylength, was common in Thailand's dipterocarp-oak forest and appears to be prevalent in Indian dry monsoon forests of the Deccan peninsula with its deep, water-storing soils. Main conclusions: In all observed species leafing during the dry season relied on subsoil water reserves, which buffer trees against prolonged climatic drought. Implicitly, rainfall periodicity, i.e. climate, is not the principal determinant of vegetative tree phenology. The establishment of new foliage before the summer rains is likely to optimize photosynthetic gain in dry monsoon forests with a relatively short, wet growing season. © 2006 The Authors Journal compilation © 2006 Blackwell Publishing Ltd. 2018-09-11T08:54:02Z 2018-09-11T08:54:02Z 2006-01-01 Journal 14668238 1466822X 2-s2.0-33646161246 10.1111/j.1466-8238.2006.00213.x https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=33646161246&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/61486
institution Chiang Mai University
building Chiang Mai University Library
country Thailand
collection CMU Intellectual Repository
topic Agricultural and Biological Sciences
Environmental Science
spellingShingle Agricultural and Biological Sciences
Environmental Science
Stephen Elliott
Patrick J. Baker
Rolf Borchert
Leaf flushing during the dry season: The paradox of Asian monsoon forests
description Aim: Most deciduous species of dry monsoon forests in Thailand and India form new leaves 1-2 months before the first monsoon rains, during the hottest and driest part of the year around the spring equinox. Here we identify the proximate causes of this characteristic and counterintuitive 'spring-flushing' of monsoon forest trees. Location: Trees of 20 species were observed in semi-deciduous dry monsoon forests of northern Thailand with a 5-6-month-long severe dry season and annual rainfall of 800-1500 mm. They were growing on dry ridges (dipterocarp-oak forest) or in moist gullies (mixed deciduous-evergreen forest) at 680-750 m altitude near Chiang Mai and in a dry lowland stand of Shorea siamensis in Utahai Thani province. Methods: Two novel methods were developed to analyse temporal and spatial variation in vegetative dry-season phenology indicative of differences in root access to subsoil water reserves. Results: Evergreen and leaf exchanging species at cool, moist sites leafed soon after partial leaf shedding in January-February. Drought-resistant dipterocarp species were evergreen at moist sites, deciduous at dry sites, and trees leafed soon after leaf shedding whenever subsoil water was available. Synchronous spring flushing of deciduous species around the spring equinox, as induced by increasing daylength, was common in Thailand's dipterocarp-oak forest and appears to be prevalent in Indian dry monsoon forests of the Deccan peninsula with its deep, water-storing soils. Main conclusions: In all observed species leafing during the dry season relied on subsoil water reserves, which buffer trees against prolonged climatic drought. Implicitly, rainfall periodicity, i.e. climate, is not the principal determinant of vegetative tree phenology. The establishment of new foliage before the summer rains is likely to optimize photosynthetic gain in dry monsoon forests with a relatively short, wet growing season. © 2006 The Authors Journal compilation © 2006 Blackwell Publishing Ltd.
format Journal
author Stephen Elliott
Patrick J. Baker
Rolf Borchert
author_facet Stephen Elliott
Patrick J. Baker
Rolf Borchert
author_sort Stephen Elliott
title Leaf flushing during the dry season: The paradox of Asian monsoon forests
title_short Leaf flushing during the dry season: The paradox of Asian monsoon forests
title_full Leaf flushing during the dry season: The paradox of Asian monsoon forests
title_fullStr Leaf flushing during the dry season: The paradox of Asian monsoon forests
title_full_unstemmed Leaf flushing during the dry season: The paradox of Asian monsoon forests
title_sort leaf flushing during the dry season: the paradox of asian monsoon forests
publishDate 2018
url https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=33646161246&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/61486
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