Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/61486
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dc.contributor.authorStephen Elliotten_US
dc.contributor.authorPatrick J. Bakeren_US
dc.contributor.authorRolf Borcherten_US
dc.date.accessioned2018-09-11T08:54:02Z-
dc.date.available2018-09-11T08:54:02Z-
dc.date.issued2006-01-01en_US
dc.identifier.issn14668238en_US
dc.identifier.issn1466822Xen_US
dc.identifier.other2-s2.0-33646161246en_US
dc.identifier.other10.1111/j.1466-8238.2006.00213.xen_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=33646161246&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/61486-
dc.description.abstractAim: 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.en_US
dc.subjectAgricultural and Biological Sciencesen_US
dc.subjectEnvironmental Scienceen_US
dc.titleLeaf flushing during the dry season: The paradox of Asian monsoon forestsen_US
dc.typeJournalen_US
article.title.sourcetitleGlobal Ecology and Biogeographyen_US
article.volume15en_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsMonash Universityen_US
article.stream.affiliationsUniversity of Kansas Lawrenceen_US
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