Abstract

In recent years, the alternating occurrence of high temperature and waterlogging disasters in South China has seriously reduced the yield of single cropping rice. Studying the changes in anatomical structure of the rice root system could provide theoretical basis for understanding the mechanisms of high temperature and waterlogging stress. To examine interactions between temperature and waterlogging stress, an experiment was set up in a growth chamber consisting of two temperatures (moderate, 30–34 °C and high, 35–38 °C) with three depths of flooding (0–5, 10 and 15 cm). Treatments commenced at the booting stage and lasted five days, after which all treatments were returned to a 0–5 cm flooding depth and the same temperature regime. Observations were made immediately after cessation of treatments, then after 5, 10 and 20 d to test the effect of treatments on subsequent root anatomical development. The low-stress control (0–5 cm, medium temperature) showed no change with time in aerenchyma area, thickness of the outer root, stele diameter, and the number nor diameter of xylem vessels. Root diameter and stele diameter under the high-stress control (0–5 cm, high temperature) were decreased by 29.09% and 15.28%, respectively, at the booting stage, whereas the high stress control (15 cm, high temperature) affected only the vessel diameter, reducing it by 14.11% compared with that in the low-stress control (0–5 cm, medium temperature). Compared to the high-stress control (0–5 cm, high temperature), the interaction of high temperature and waterlogging stress alleviated the inhibiting effect of the changes in the root system, especially after the end of the stress. We thought that waterlogging could reduce the damage of high temperature on rice root growth. Low water depth waterlogging has little effect on rice root system and aerenchyma area root diameter at 0, 5, 10 and 20 d after the stress ended, and the thickness of the outer root, stele diameter and the number and diameter of vessels at 0 d under M15 (15 cm, medium temperature) had no significant difference compared with M5 (0–5 cm, medium temperature). However, the increase in rice root diameter, stele diameter, thickness of the outer root cortex depth and vessel diameter were inhibited under high temperature stress at the booting stage. Root diameter and stele diameter under H5 (0–5 cm, high temperature) were decreased by 29.09% and 15.28%, respectively, at the booting stage, whereas H15 (15 cm, high temperature) affected only the vessel diameter, reducing it by 14.11% compared with that in the M5. Compared to H5, the interaction of high temperature and waterlogging stress alleviated the inhibiting effect of the changes in the root system, especially after the end of the stress. We thought that waterlogging could lighten the damage of high temperature on rice root growth.

Highlights

  • China is one of the major rice producers, accounting for 18.5% of the world’s total planting area and 27.7% of world rice production [1]

  • As stress ended for 10 days (19 August), temperature × water affected significantly the anatomical parameters of rice roots

  • We found that for 20analyzed days, the the root relationship diameter treated with H5root was decreased when the soil temperature was between 25–35 °C, the root diameter decreased with the increase of

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Summary

Introduction

China is one of the major rice producers, accounting for 18.5% of the world’s total planting area and 27.7% of world rice production [1]. Temperature and moisture are the main factors affecting rice production. The atmospheric temperature is expected to increase by. A high temperature (>35 ◦ C), especially during grain filling, can remarkably reduce grain development, quantity and quality [5]. High temperature can affect many processes of rice growth and development, including germination, seedling growth, leaf emergence, tillering, heading and filling [6,7,8,9,10,11]. The frequency of extremely high temperatures and heat waves in most of mainland China is likely to continue increasing in the 21st century [12]. High temperature and rainstorms have coincided frequently with the rice reproductive growth stage in Huanghuai and South China [14]

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