Abstract

Climate changes show asymmetrical warming, and warming is typically greater at night than during the day. To understand how nocturnal warming (NW) affects the performance of maize (Zea mays L.), an open-field experiment with a free air temperature increase (FATI) facility was conducted for three seasons during 2014 to 2016 at Luancheng eco-agro-experimental station on the North China Plain (NCP). Three nocturnal warming scenarios were set up: the entire growing period (T1, from V4 to maturity), only the vegetative stages (T2, from V4 to a week presilking) and the reproductive stages (T3, from a week presilking to R6). The treatment without NW was the control. Maize lodged seriously in 2015 due to heavy rainfall combined with strong winds, and the experiment failed. The results from 2014 and 2016 were analyzed in this study. During the experimental duration, the average nocturnal temperature was increased by approximately 3.6 and 3.3 °C at 150 cm height and 2.0 and 1.7 °C at the soil surface during the vegetative stages. The corresponding increases were 2.1 and 2.5 °C and 0.7 and 1.2 °C at the soil surface during the reproductive stages in 2014 and 2016, respectively, as compared with that of the CK treatment. NW during the whole growth period significantly decreased maize yield for the two seasons. Treatment T2 had a smaller impact on maize yield than T1 and T3. The silking stage was delayed by 2 days in 2014 and 2016 under T1. As a result, presilking duration and VT-R1 interval were prolonged by 1–2 days; and the postsilking duration were shortened by 1–3 days under T1. The soil moisture in the warmed plots was slightly lower than that in the control plots in the 2014 and during the stages before the earlier grain-filling stages in 2016, but NW decreased soil water content greatly at the later grain-filling stages in 2016, which caused the fast green leaf senescence and exacerbated the negative effects of NW on maize yield. NW for the whole growth duration (T1) significantly decreased seed weight and harvest index. NW increased leaf nighttime respiration rate in both seasons. No significant effects of NW on ear leaf net photosynthesis, leaf area, and specific leaf weight at early grain-filling stage were observed, irrespective of the warming stage and season. The results suggested that reproductive stages were more sensitive to NW compared to vegetative stages under the growing conditions of NCP. The negative effects of NW were worsened in dry seasons. The reduction in maize yield with nocturnal warming was driven by the reduction in the aboveground carbon allocation from shoot to grain during postanthesis stage.

Highlights

  • The global mean air temperature is predicted to increase by approximately 1.0–1.7 ◦C by 2050 [1]

  • The effective grain filling period was shortened by 2–3 days by nocturnal warming (NW) (Table 1), which induced a decrease in the seed weight, and this might be one of the reasons that caused the yield reduction under NW

  • The reduction of the yield under NW was mainly related to the reduction in the seed weight and harvest index (HI), and these negative effects were more serious under dry soil water conditions

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Summary

Introduction

The global mean air temperature is predicted to increase by approximately 1.0–1.7 ◦C by 2050 [1]. Since the temperature is a key factor in regulating crop development and growth, future climatic warming will affect the global grain production substantially [3,4,5,6]. Crop production is experiencing increases in both the frequency and the intensity of nocturnal warming (NW). NW threatens the sustainability of crop production both currently and in the future. Many studies have indicated that decreased crop yields generally occur as a result of NW. A one-centigrade degree increase in the nighttime temperature can produce a drastic decrease in crop production [3]. It has become important to assess the effects of NW on crop production

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