Integrated transcriptome and metabolome analysis reveals the divergent evolution of low-P tolerance in cultivated and Tibetan wild barley

被引:1
|
作者
Zhang, Junhao [1 ]
Sun, Wenyue [1 ]
Zhao, Huifang [1 ]
Liang, Qiyu [1 ]
Zhang, Guoping [1 ,2 ]
Cai, Shengguan [1 ,2 ]
机构
[1] Zhejiang Univ, Inst Crop Sci, Hangzhou 310058, Peoples R China
[2] Zhejiang Univ, Zhongyuan Inst, Zhengzhou 450000, Peoples R China
关键词
Cultivated barley ( Hordeum vulgare L.); Metabolome; Low -P tolerance; Transcriptome; Tibetan wild barley(Hordeum spontaneum L.); PHOSPHATE-STARVATION; ACID-PHOSPHATASE; PHOSPHORUS AVAILABILITY; LIPID-COMPOSITION; PLASMA-MEMBRANES; PLANT-GROWTH; RICE; TRANSPORTER; RESPONSES; BIOSYNTHESIS;
D O I
10.1016/j.envexpbot.2023.105641
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Most arable lands in the world are quite low in available phosphorus (P), becoming an important factor restricting crop yield. However, the genotypic difference of low-P tolerance in barley is rarely understood at molecular level. In this study, low-P responses of three barley genotypes were explored by physiological, transcriptomic and metabolomic analysis. The results showed that low-P-tolerant genotypes Zaoaibai (cultivar) and X130 (Tibetan wild accession) showed less growth inhibition compared to low-P-sensitive Salooni2 under low-P stress. Omics analysis showed that many genes involved in Pi acquisition and transport were more upregulated in Zaoaibai, which had relatively higher concentrations of shoot P and glucose-6-phosphate, indicating that enhancement of P acquisition, P translocation and P availability contributed to low-P tolerance in Zaoaibai. On the other hand, the genes and metabolites involved in biosynthesis of Pi-free lipids were highly expressed and more abundant in X130, suggesting that remodeling of membrane lipids by replacing phospholipids with Pi-free lipids is an important strategy for X130 in its adaptation to low-P stress. The divergent evolution of low-P tolerance in Zaoaibai and X130 could be driven by diverse ecological factors in Eastern China (low soil P) and Tibet Plateau (high soil P and low temperature), respectively.
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页数:14
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