ArticlePlants (Basel, Switzerland)2023
Warm Temperature Increments Strengthen the Crosstalk between Roots and Soil in the Rhizosphere of Soybean Seedlings.
Article in Plants (Basel, Switzerland), 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed.
- Terracing influences soil microbial assembly in citrus orchards: stochastic processes dominate community dynamics in a karst sloping land.BMC microbiology · 2026Article
- Endophyte-mediated biosynthesis of biogenic nanoparticles: mechanisms and biomedical applications.Archives of microbiology · 2026Review
- Responses of vegetation-soil enzyme activities to climatic factors under different treatments in desertified areas.Frontiers in plant science · 2026Article
- SlATG8f coordinates ethylene signaling and chloroplast turnover to drive tomato fruit ripening.Plant cell reports · 2025Article
- Temperature-Dependent Root Responses to Water Deficit Modulate Biological Nitrogen Fixation and Rhizosphere Dynamics in Soybeans.Physiologia plantarumArticle
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Authors and funding
9 authors.
Funding
Abstract
The plant rhizosphere underlies the crosstalk between plant and soil and has a crucial role in plant growth and development under various environments. We examined the effect of temperature rise on the rhizosphere environment of soybean roots to clarify the rhizosphere crosstalk between roots and soil in response to warm temperature rises in a global warming background. The in situ results of root enzyme activity revealed that soybean roots secrete β-glucosidase, and enzyme spectrum imaging demonstrated different enzymatic activities under different temperature environments. The soil enzyme kinetics results showed that soil enzymatic activity increased with increasing temperature, and soybean rhizosphere soil enzymatic activity was higher than that of non-rhizosphere soil. Rhizosphere soil and non-rhizosphere soil showed that the dominant bacterial phylum in soybean rhizosphere soil was
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