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Effects of soil pH on the growth, soil nutrient composition, and rhizosphere microbiome of Ageratina adenophora

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Ageratina adenophora is an invasive weed species found in many countries. Methods to control the spread of this weed have been largely unsuccessful. Soil pH is the most important soil factor affecting the availability of nutrients for plant and impacting its growth. Understanding the mechanisms of the influence of soil pH on the growth of A. adenophora may help to develop effective control measures. In this study, we artificially changed the soil pH in pot experiments for A. adenophora. We studied the effects of acidic (pH 5.5), weakly acidic (pH 6.5), neutral (pH 7.2), and alkaline (pH 9.0) soils on the growth, availability of soil nutrients, activity of antioxidant enzymes, levels of redox markers in the leaves, and the structure and diversity of the rhizosphere microbiome. Soil with a pH 7.2 had a higher (47.8%) below-ground height versus soils of pH 5.5 at day 10; plant had a higher (11.3%) above-ground height in pH 7.2 soils than pH 9.0 soils at day 90; no differences in the fresh and dry weights of its above- and belowground parts, plant heights, and root lengths were observed in plants growing in acid, alkaline, or neutral pH soil were observed at day 180. Correspondingly, the antioxidant enzymes SOD (superoxide dismutase), POD (peroxidase), CAT (catalase) and redox markers GSH (glutathione) and MDA (malondialdehyde) were measured in the leaves. Significant differences existed in the activities of CAT and the levels of GSH between those growing in acidic and alkaline soils and those in neutral pH soil at day 90; however, only lower (36.8%) CAT activities in those grown at pH 5.5 than those grown at pH 7.2 were found at day 180. Similarly, significant differences in available P (16.89 vs 3.04 mg Kg−1) and total K (3.67 vs 0.96 mg Kg−1), total P (0.37 vs 0.25 g Kg−1) and total N (0.45 vs 1.09 g Kg−1) concentrations were found between the rhizosphere soils of A. adenophora grown at pH 9.0 and 7.2 at day 90; no such differences were seen at day 180. High throughput analyses of the 16S rRNA and ITS fragments showed that the rhizosphere microbiome diversity and composition under different soil pH conditions changed over 180 days. The rhizosphere microbiomes differed in diversity, phylum, and generic composition and population interactions under acid and alkaline conditions versus those grown in neutral soils. Soil pH had a greater impact on the diversity and composition of the prokaryotic rhizosphere communities than those of the fungal communities. A. adenophora responded successfully to pH stress by changing the diversity and composition of the rhizosphere microbiome to maintain a balanced nutrient supply to support its normal growth. The unusual pH tolerance of A. adenophora may be one crucial reason for its successful invasion. Our results suggest that attempts use soil pH to control its invasion by changing the soil pH (for example, using lime) will fail.
Title: Effects of soil pH on the growth, soil nutrient composition, and rhizosphere microbiome of Ageratina adenophora
Description:
Ageratina adenophora is an invasive weed species found in many countries.
Methods to control the spread of this weed have been largely unsuccessful.
Soil pH is the most important soil factor affecting the availability of nutrients for plant and impacting its growth.
Understanding the mechanisms of the influence of soil pH on the growth of A.
adenophora may help to develop effective control measures.
In this study, we artificially changed the soil pH in pot experiments for A.
adenophora.
We studied the effects of acidic (pH 5.
5), weakly acidic (pH 6.
5), neutral (pH 7.
2), and alkaline (pH 9.
0) soils on the growth, availability of soil nutrients, activity of antioxidant enzymes, levels of redox markers in the leaves, and the structure and diversity of the rhizosphere microbiome.
Soil with a pH 7.
2 had a higher (47.
8%) below-ground height versus soils of pH 5.
5 at day 10; plant had a higher (11.
3%) above-ground height in pH 7.
2 soils than pH 9.
0 soils at day 90; no differences in the fresh and dry weights of its above- and belowground parts, plant heights, and root lengths were observed in plants growing in acid, alkaline, or neutral pH soil were observed at day 180.
Correspondingly, the antioxidant enzymes SOD (superoxide dismutase), POD (peroxidase), CAT (catalase) and redox markers GSH (glutathione) and MDA (malondialdehyde) were measured in the leaves.
Significant differences existed in the activities of CAT and the levels of GSH between those growing in acidic and alkaline soils and those in neutral pH soil at day 90; however, only lower (36.
8%) CAT activities in those grown at pH 5.
5 than those grown at pH 7.
2 were found at day 180.
Similarly, significant differences in available P (16.
89 vs 3.
04 mg Kg−1) and total K (3.
67 vs 0.
96 mg Kg−1), total P (0.
37 vs 0.
25 g Kg−1) and total N (0.
45 vs 1.
09 g Kg−1) concentrations were found between the rhizosphere soils of A.
adenophora grown at pH 9.
0 and 7.
2 at day 90; no such differences were seen at day 180.
High throughput analyses of the 16S rRNA and ITS fragments showed that the rhizosphere microbiome diversity and composition under different soil pH conditions changed over 180 days.
The rhizosphere microbiomes differed in diversity, phylum, and generic composition and population interactions under acid and alkaline conditions versus those grown in neutral soils.
Soil pH had a greater impact on the diversity and composition of the prokaryotic rhizosphere communities than those of the fungal communities.
A.
adenophora responded successfully to pH stress by changing the diversity and composition of the rhizosphere microbiome to maintain a balanced nutrient supply to support its normal growth.
The unusual pH tolerance of A.
adenophora may be one crucial reason for its successful invasion.
Our results suggest that attempts use soil pH to control its invasion by changing the soil pH (for example, using lime) will fail.

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