Abstract

Roots have long been proposed as a major avenue of research to improve crop adaptation to water limitations. The simple assumption is that deeper and more profuse root systems could tap extra water from the soil profile and alleviate drought effects. However, after decades of research, success in breeding cultivars with improved root systems is lagging behind. Here, we attempt to analyze the possible reasons for this, and re-focus on what root traits might provide the most promising avenues for drought adaptation. We approach the root system from the angle of water extraction, using data from a lysimetric system that allows monitoring and comparing plant water use over the entire crop life cycle and yield, and analyze whether and how differences in water extraction lead to improved yield across different crops. The main message from that analysis is that water extraction during reproduction and grain filling is critical and comes from a number of traits that influence the rate at which plant use the available water before and during stress. Roots may have an effect on this, not from the traditionally thought density or depth, but rather from their hydraulic characteristics. Plants can indeed control water use by controlling leaf area development and this is a “long term” control. Plants also control water losses by controlling stomata opening under high vapor pressure deficit (VPD) conditions, in a transient manner. Both processes (leaf development and stomata opening) are mostly controlled by hydraulic processes. The role of roots in drought adaptation could be there, along with the soil, in setting an hydraulic environment that allow plants to use water in a way that allow maximizing water use for these critical stages.

Highlights

  • Agriculture production worldwide is often limited by water deficits and the case is very acute in semi-arid tropics of Asia and Africa where populations are large, dense, and depend on subsistence agriculture

  • This can be interpreted in different ways: (i) root depth and/or root length density (RLD) are not akin to water extraction; (ii) deep or profuse rooting would have no effect in shallow soil, in soil where there is no water at depth, or under conditions of mild water stress; (iii) root and shoot growth are closely coordinated and deeper rooting might lead to faster soil water depletion, which would be a problem for crops depending on stored soil moisture; (iv) capturing deep layer water is a one-time benefit since any rainfall/irrigation event would wet the profile from the top in progressive drought stress conditions

  • Especially root length density and root depth, have long been seen as critical trait to harness in order to improve crop adaptation to water stress

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Summary

Introduction

Agriculture production worldwide is often limited by water deficits and the case is very acute in semi-arid tropics of Asia and Africa where populations are large, dense, and depend on subsistence agriculture. The end of this section is a transition in which we discuss the linkage between some of these traits related to the plant water budget and the plant hydraulic characteristics. There is evidence that some of the traits related to the plant water budget are ruled by hydraulic mechanisms, e.g. the control of leaf expansion (Reymond et al, 2003; Simonneau et al, 2009), or the transpiration response to high vapor pressure deficit (VPD) (Sinclair et al, 2008), and some of these are determined by differences in the root hydraulics (Parent et al, 2010). The last section deals with possible root characteristics that can influence root hydraulics (Maurel et al, 2010) and eventually can alter the different traits related to the water budget. We review the role of aquaporins in influencing hydraulic conductance of plant tissues, focusing here on their role in root tissues (e.g. Ehlert et al, 2009; Thompson et al, 2007)

Current views
Limits to deep and profuse rooting
The need for 3-D methods to capture root architecture in situ
Description of the lysimetric method
The importance of water access at key times – link to water saving traits
Looking at roots through the angle of their hydraulic characteristics
Findings
Conclusion
Full Text
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