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Seasonal patterns of leaf gas exchange and water relations in dry rain forest trees of contrasting leaf phenology

机译:叶片物候相反的干旱雨林树木叶片气体交换和水关系的季节性模式

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摘要

Diurnal and seasonal patterns of leaf gas exchange and water relations were examined in tree species of contrasting leaf phenology growing in a seasonally dry tropical rain forest in north-eastern Australia. Two drought-deciduous species, Brachychiton australis (Schott and Endl.) A. Terracc. and Cochlospermum gillivraei Benth., and two evergreen species, Alphitonia excelsa (Fenzal) Benth. and Austromyrtus bidwillii (Benth.) Burret. were studied. The deciduous species had higher specific leaf areas and maximum photosynthetic rates per leaf dry mass in the wet season than the evergreens. During the transition from wet season to dry season, total canopy area was reduced by 70-90% in the deciduous species and stomatal conductance (g(s)) and assimilation rate (A) were markedly lower in the remaining leaves. Deciduous species maintained daytime leaf water potentials (Psi(L)) at close to or above wet season values by a combination of stomatal regulation and reduction in leaf area. Thus, the timing of leaf drop in deciduous species was not associated with large negative values of daytime Psi(L) (greater than -1.6 MPa) or predawn Psi(L) (greater than -1.0 MPa). The deciduous species appeared sensitive to small perturbations in soil and leaf water status that signalled the onset of drought. The evergreen species were less sensitive to the onset of drought and g(s) values were not significantly lower during the transitional period. In the dry season, the evergreen species maintained their canopies despite increasing water-stress; however, unlike Eucalyptus species from northern Australian savannas, A and g(s) were significantly lower than wet season values.
机译:在澳大利亚东北部一个季节性干燥的热带雨林中生长的具有相反叶片物候的树种中,研究了叶片气体交换和水关系的昼夜和季节性模式。两种干旱落叶树种,澳大利亚短枝曲霉(Schott and Endl。)和Cochlospermum gillivraei Benth。,以及两个常绿物种,卓越的Alphitonia(Fenzal)Benth。和Austromyrtus bidwillii(Benth。)Burret。被研究了。与常绿植物相比,在湿季,落叶树种具有更高的比叶面积和最大的光合速率。从湿季到旱季的过渡期间,落叶树种的总冠层面积减少了70-90%,其余叶片的气孔导度(g(s))和同化率(A)明显降低。通过结合气孔调节和减少叶片面积,落叶树种将白天的叶片水势(Psi(L))维持在接近或高于湿季的水平。因此,落叶树种叶片掉落的时机与白天的Psi(L)(大于-1.6 MPa)或黎明前的Psi(L)(大于-1.0 MPa)较大的负值无关。落叶树种对土壤和叶片水分状况的小扰动敏感,这预示着干旱的开始。常绿树种对干旱的发生不那么敏感,并且在过渡期的g(s)值也没有明显降低。在干旱季节,尽管水分压力增加,常绿树种仍保持其冠层。但是,与澳大利亚北部大草原的桉树种类不同,A和g(s)明显低于雨季的值。

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