Differential temperature responses of diurnal and nocturnal leaf respiration in four alpine herbaceous species

Tianyu Zheng*, Huixing Kang, Yuan Yu, Tong Guo, Xinran Ke, Owen K. Atkin, Yanhong Tang

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

1 Citation (Scopus)

Abstract

Current estimates of diel respiratory carbon release depend on accurate predictions of the temperature sensitivity (Q10) of leaf respiration during the day and night. Such predictions typically rely on measurements of the Q10 of respiration in the light (RL) and dark (RD) made during the day, and assuming that the Q10 of nocturnal respiration (RN) equals that of RD. Using RD as a surrogate for RN, however, creates errors in estimates of diel respiration whenever the Q10 of RD and RN differ. Using measurements made on field-grown, high-altitude alpine plants, our study investigated whether the Q10 of leaf respiration differs between the day and night. We characterised diurnal RL and RD from 15 to 35 °C, and RN from 10 to 25 °C at night, in four common herbaceous species widely distributed in alpine meadows on the Qinghai-Tibetan Plateau. We measured leaf temperature every second for 24 h over a period of 18 days. By combining leaf temperature with respiratory physiological measurements, we calculated leaf carbon loss to assess the consequences of differences in temperature response of leaf respiration between day and night. RN exhibited a higher Q10 than RL and RD by about one third. Although there were no significant differences in Q10 between RL and RD, light inhibition of leaf respiration (i.e. 100 % - RL / RD) was at its lowest at a moderate leaf temperature (22−25 °C). G. straminea and S. pulchra showed lower levels of inhibition than L. sagitta and L. virgaurea. Respiratory carbon loss (Closs_day) based on RN exceeded Closs_day based on RL by up to 47 %, which varied considerably between the species. These results suggest that the temperature sensitivity (Q10) of leaf respiration differs significantly between day and night, a finding that needs to be taken into account when modelling the diel rates of respiratory carbon loss in plants, especially at high altitudes and some high latitudes with a large diurnal variation and low mean temperature. Therefore, considering that neither RN nor RD can accurately represent RL, we strongly recommend that the observations of RL should be prioritized when estimating daytime leaf carbon loss.

Original languageEnglish
Article number110385
JournalAgricultural and Forest Meteorology
Volume362
DOIs
Publication statusPublished - 1 Mar 2025

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