Ashoka Trust for Research in Ecology and the Environment (ATREE), Bangalore 560064, Karnataka, India.
Manipal Academy of Higher Education (MAHE), Manipal 576104, Karnataka, India.
J Exp Bot. 2023 Sep 13;74(17):5273-5293. doi: 10.1093/jxb/erad207.
The interactive role of life-history traits and environmental factors on plant water relations is crucial for understanding the responses of species to climate change, but it remains poorly understood in secondary tropical montane forests (TMFs). In this study, we examined differences in sap flow between the pioneer species Symplocos racemosa and Eurya acuminata, and the late-successional species Castanopsis hystrix that co-occur in a biodiverse Eastern Himalayan secondary broadleaved TMF. The fast-growing pioneers had sap flux densities that were 1.6-2.1 times higher than the late-successional species, and exhibited characteristics of long-lived pioneer species. Significant radial and azimuthal variability in sap flow (V) between species was observed and could be attributed to the life-history trait and the access of the canopy to sunlight. Nocturnal V was 13.8% of the daily total and was attributable to stem recharge during the evening period (18.00-23.00 h) and to endogenous stomatal controls during the pre-dawn period (00.00-05.00 h). The shallow-rooted pioneer species both exhibited midday depression in V that was attributable to photosensitivity and diel moisture stress responses. In contrast, the deep-rooted late-successional species showed unaffected transpiration across the dry season, indicating their access to groundwater. Thus, our results suggest that secondary broadleaved TMFs, with a dominance of shallow-rooted pioneers, are more prone to the negative impacts of drier and warmer winters than primary forests, which are dominated by deep-rooted species. Our study provides an empirical understanding of how life-history traits coupled with microclimate can modulate plant water use in the widely distributed secondary TMFs in Eastern Himalaya, and highlights their vulnerability to warmer winters and reduced winter precipitation due to climate change.
生活史特征和环境因素对植物水分关系的相互作用对于理解物种对气候变化的响应至关重要,但在次生热带山地森林(TMFs)中仍知之甚少。在这项研究中,我们研究了在生物多样性丰富的东喜马拉雅山次生阔叶 TMF 中共存的先锋物种 Symplocos racemosa 和 Eurya acuminata 以及晚生种 Castanopsis hystrix 之间的 sap 流差异。快速生长的先驱者 sap 通量密度比晚生种高 1.6-2.1 倍,表现出长寿先锋种的特征。在物种之间观察到 sap 流(V)的显著径向和方位变化,并归因于生活史特征和树冠对阳光的获取。夜间 V 占日总量的 13.8%,归因于傍晚(18.00-23.00 h)期间茎的补给和黎明前(00.00-05.00 h)期间内源气孔控制。浅根先锋物种都表现出 V 的午间低谷,这归因于光敏感性和昼夜水分胁迫响应。相比之下,深根晚生种在旱季表现出不受影响的蒸腾作用,表明它们可以获得地下水。因此,我们的研究结果表明,以浅根先锋物种为主的次生阔叶林比以深根物种为主的原生林更容易受到更干燥和温暖的冬季的负面影响。我们的研究提供了对生活史特征与小气候如何调节东喜马拉雅山广泛分布的次生 TMF 中植物水分利用的经验理解,并强调了它们对更温暖的冬季和气候变化导致的冬季降水减少的脆弱性。