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丛枝菌根和胞外酶对干旱条件下高粱氮素获取的贡献

Contribution of arbuscular mycorrhiza and exoenzymes to nitrogen acquisition of sorghum under drought.

作者信息

Munene Rosepiah, Mustafa Osman, Loftus Sara, Banfield Callum C, Rötter Reimund P, Bore Ezekiel K, Mweu Benard, Mganga Kevin Z, Otieno Dennis O, Ahmed Mutez A, Dippold Michaela A

机构信息

Biogeochemistry of Agroecosystems, Department of Crop Sciences, University of Goettingen, Goettingen, Germany.

Geo-Biosphere Interactions, Department of Geosciences, University of Tuebingen, Tuebingen, Germany.

出版信息

Front Plant Sci. 2025 Apr 15;16:1514416. doi: 10.3389/fpls.2025.1514416. eCollection 2025.

Abstract

INTRODUCTION

For low-fertile and degraded soils of sub-Saharan Africa, nitrogen (N) is often the most growth-limiting factor restricting crop yields. The often-suggested exploitation of advantageous rhizosphere traits such as enzyme secretion and/or the symbiosis with arbuscular mycorrhizal fungi (AMF) remains to be validated as a potential strategy to overcome N limitation, especially when N deficiency co-occurs with further abiotic stresses such as water scarcity.

METHODS

Three sorghum genotypes were cultivated in soil mesocosms with a root-exclusion compartment, where only AMF could scavenge for nutrients under drought and optimal conditions. Plant carbon (C) investment into the rhizosphere and N uptake were tracked by N application coupled with CO labeling.

RESULTS

Under drought, uptake of mineral N by AMF from the root-exclusion compartment increased 4-12 times compared to well-watered conditions. In addition, water stress enhanced below-ground allocation of recently assimilated C into microbial biomass. Drought reduced the enzymatic potential (Vmax) of chitinase while increasing leucine aminopeptidase (LAP) activity. This suggests that N acquisition via protein mineralization in soil was relatively enhanced compared to that of chitin following moisture limitation. LAP substrate affinity (Km) was reduced by drought compared to that of chitinase with genotype-specific shifts in the rhizosphere enzyme systems observed.

CONCLUSION

Our findings suggest that below-ground C allocation activated AMF symbiosis and its associated microbiome. This not only led to a shift in enzyme-driven exploitation of distinct organic N sources but also induced a strong increase in AMF-based mineral N acquisition from the mycosphere. This trait plasticity in response to drought may be harnessed to stabilize food production from low-fertile soil under the increasingly negative impacts of droughts due to climate change.

摘要

引言

在撒哈拉以南非洲地区肥力较低且退化的土壤中,氮(N)常常是限制作物产量的最主要生长限制因素。人们常提出利用诸如酶分泌和/或与丛枝菌根真菌(AMF)共生等有利的根际特性作为克服氮限制的潜在策略,但仍有待验证,尤其是当氮缺乏与水资源短缺等其他非生物胁迫同时发生时。

方法

在带有根系隔离区的土壤中型生态系统中种植三种高粱基因型,在干旱和最佳条件下,只有AMF能够在该隔离区获取养分。通过施氮结合CO标记追踪植物碳(C)向根际的投入和氮吸收情况。

结果

在干旱条件下,与充分浇水的条件相比,AMF从根系隔离区吸收的矿质氮增加了4至12倍。此外,水分胁迫增强了新同化碳向微生物生物量的地下分配。干旱降低了几丁质酶的酶活性(Vmax),同时增加了亮氨酸氨肽酶(LAP)的活性。这表明在水分受限的情况下,通过土壤中蛋白质矿化获取氮相对于几丁质而言相对增强。与几丁质酶相比,干旱降低了LAP的底物亲和力(Km),且在根际酶系统中观察到基因型特异性变化。

结论

我们的研究结果表明,地下碳分配激活了AMF共生及其相关微生物群落。这不仅导致了酶驱动的对不同有机氮源利用的转变,还促使基于AMF的从菌根圈获取矿质氮的能力大幅增加。这种对干旱的性状可塑性可用于在气候变化导致干旱负面影响日益增加的情况下,稳定低肥力土壤的粮食生产。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5205/12037375/d3b834003427/fpls-16-1514416-g002.jpg

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