Chen Siluo, Ten Tusscher Kirsten H W J, Sasidharan Rashmi, Dekker Stefan C, de Boer Hugo J
Computational Developmental Biology, Department of Biology Utrecht University Utrecht The Netherlands.
Centre for Complex System Studies Utrecht University Utrecht The Netherlands.
Plant Environ Interact. 2023 Jun 30;4(4):175-187. doi: 10.1002/pei3.10117. eCollection 2023 Aug.
Drought and flooding occur at opposite ends of the soil moisture spectrum yet their resulting stress responses in plants share many similarities. Drought limits root water uptake to which plants respond with stomatal closure and reduced leaf gas exchange. Flooding limits root metabolism due to soil oxygen deficiency, which also limits root water uptake and leaf gas exchange. As drought and flooding can occur consecutively in the same system and resulting plant stress responses share similar mechanisms, a single theoretical framework that integrates plant responses over a continuum of soil water conditions from drought to flooding is attractive. Based on a review of recent literature, we integrated the main plant eco-physiological mechanisms in a single theoretical framework with a focus on plant water transport, plant oxygen dynamics, and leaf gas exchange. We used theory from the soil-plant-atmosphere continuum modeling as "backbone" for our framework, and subsequently incorporated interactions between processes that regulate plant water and oxygen status, abscisic acid and ethylene levels, and the resulting acclimation strategies in response to drought, waterlogging, and complete submergence. Our theoretical framework provides a basis for the development of mathematical models to describe plant responses to the soil moisture continuum from drought to flooding.
干旱和洪涝出现在土壤水分范围的两端,但它们在植物中引发的应激反应却有许多相似之处。干旱限制根系对水分的吸收,对此植物会通过气孔关闭和减少叶片气体交换来做出反应。洪涝由于土壤缺氧限制根系代谢,这也会限制根系对水分的吸收和叶片气体交换。由于干旱和洪涝可能在同一系统中相继发生,且由此产生的植物应激反应具有相似的机制,因此一个整合植物在从干旱到洪涝的连续土壤水分条件下反应的单一理论框架很有吸引力。基于对近期文献的综述,我们将主要的植物生态生理机制整合到一个单一的理论框架中,重点关注植物水分运输、植物氧气动态和叶片气体交换。我们将土壤-植物-大气连续体建模的理论用作我们框架的“主干”,随后纳入了调节植物水分和氧气状态、脱落酸和乙烯水平的过程之间的相互作用,以及由此产生的应对干旱、涝渍和完全淹没的适应策略。我们的理论框架为开发数学模型以描述植物对从干旱到洪涝的土壤水分连续体的反应提供了基础。