Microorganisms Promote Soil Phosphorus Bioavailability at the Beginning of Pedogenesis

ABSTRACT The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio‐P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier forelan...

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Published inGlobal change biology Vol. 31; no. 8; pp. e70419 - n/a
Main Authors Xu, Mingyang, Wu, Yanhong, Bing, Haijan, Luo, Chaoyi, Zhu, He, He, Junbo
Format Journal Article
LanguageEnglish
Published England Blackwell Publishing Ltd 01.08.2025
Subjects
Accumulation
Bacteria - metabolism
beginning of pedogenesis
Bioavailability
Biological Availability
China
Ecological succession
Ecosystem
glacier foreland
Glaciers
Microbial activity
microbial communities
Microbiomes
Microbiota
Microorganisms
Mineralization
nutrient cycling
Organic phosphorus
Phosphorus
Phosphorus - metabolism
phosphorus bioavailability
phosphorus cycling genes (PCGs)
Phytase
Polar environments
Polar regions
Soil - chemistry
Soil formation
Soil Microbiology
Soil microorganisms
Solubilization
China
phosphorus cycling genes (PCGs)
beginning of pedogenesis
microbial communities
glacier foreland
nutrient cycling
phosphorus bioavailability
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Abstract ABSTRACT The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio‐P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co‐occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust. The results showed that bacteria were dominant at all stages. Microbial diversity and evenness increased gradually, whereas the topological properties of the microbial network initially increased and then decreased. Community assembly is mainly driven by deterministic processes under environmental pressures. At the beginning of pedogenesis, microorganisms adapt to scarce Bio‐P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3‐Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization. Tight cooperative network structures within microbial communities and dominant microbial taxa were the major factors accelerating Bio‐P. Thus, it can be concluded that microorganisms promote Bio‐P accumulation at the beginning of pedogenesis by regulating PCGs and typical microbial community construction. These findings provide new insights into the mechanisms by which microbial communities regulate phosphorus dynamics during pedogenesis, particularly on newly exposed land resulting from global change in alpine and polar regions. At the beginning of pedogenesis, microorganisms promote the enhancement of phosphorus bioavailability. Microbial community assembly is closely associated with phosphorus‐cycling genes and phosphorus bioavailability. Microorganisms adapt to scarce Bio‐P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3‐Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization.
AbstractList The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio‐P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co‐occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust. The results showed that bacteria were dominant at all stages. Microbial diversity and evenness increased gradually, whereas the topological properties of the microbial network initially increased and then decreased. Community assembly is mainly driven by deterministic processes under environmental pressures. At the beginning of pedogenesis, microorganisms adapt to scarce Bio‐P conditions by enhancing the functional potential of key PCGs (e.g., pqqE , gcd , phoD , and 3‐Phytase ), which mediate mineral phosphorus solubilization and organic phosphorus mineralization. Tight cooperative network structures within microbial communities and dominant microbial taxa were the major factors accelerating Bio‐P. Thus, it can be concluded that microorganisms promote Bio‐P accumulation at the beginning of pedogenesis by regulating PCGs and typical microbial community construction. These findings provide new insights into the mechanisms by which microbial communities regulate phosphorus dynamics during pedogenesis, particularly on newly exposed land resulting from global change in alpine and polar regions.
ABSTRACT The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio‐P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co‐occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust. The results showed that bacteria were dominant at all stages. Microbial diversity and evenness increased gradually, whereas the topological properties of the microbial network initially increased and then decreased. Community assembly is mainly driven by deterministic processes under environmental pressures. At the beginning of pedogenesis, microorganisms adapt to scarce Bio‐P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3‐Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization. Tight cooperative network structures within microbial communities and dominant microbial taxa were the major factors accelerating Bio‐P. Thus, it can be concluded that microorganisms promote Bio‐P accumulation at the beginning of pedogenesis by regulating PCGs and typical microbial community construction. These findings provide new insights into the mechanisms by which microbial communities regulate phosphorus dynamics during pedogenesis, particularly on newly exposed land resulting from global change in alpine and polar regions. At the beginning of pedogenesis, microorganisms promote the enhancement of phosphorus bioavailability. Microbial community assembly is closely associated with phosphorus‐cycling genes and phosphorus bioavailability. Microorganisms adapt to scarce Bio‐P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3‐Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization.
The rapid accumulation of bioavailable phosphorus (Bio-P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio-P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co-occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust. The results showed that bacteria were dominant at all stages. Microbial diversity and evenness increased gradually, whereas the topological properties of the microbial network initially increased and then decreased. Community assembly is mainly driven by deterministic processes under environmental pressures. At the beginning of pedogenesis, microorganisms adapt to scarce Bio-P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3-Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization. Tight cooperative network structures within microbial communities and dominant microbial taxa were the major factors accelerating Bio-P. Thus, it can be concluded that microorganisms promote Bio-P accumulation at the beginning of pedogenesis by regulating PCGs and typical microbial community construction. These findings provide new insights into the mechanisms by which microbial communities regulate phosphorus dynamics during pedogenesis, particularly on newly exposed land resulting from global change in alpine and polar regions.The rapid accumulation of bioavailable phosphorus (Bio-P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland. However, the role of microorganisms in Bio-P accumulation during early pedogenesis remains unclear. Using the Hailuogou Glacier foreland on Gongga Mountain as a natural laboratory, microbial community assembly, co-occurrence networks, and phosphorus cycling genes (PCGs) were examined across four successional stages, from bare land to moss crust. The results showed that bacteria were dominant at all stages. Microbial diversity and evenness increased gradually, whereas the topological properties of the microbial network initially increased and then decreased. Community assembly is mainly driven by deterministic processes under environmental pressures. At the beginning of pedogenesis, microorganisms adapt to scarce Bio-P conditions by enhancing the functional potential of key PCGs (e.g., pqqE, gcd, phoD, and 3-Phytase), which mediate mineral phosphorus solubilization and organic phosphorus mineralization. Tight cooperative network structures within microbial communities and dominant microbial taxa were the major factors accelerating Bio-P. Thus, it can be concluded that microorganisms promote Bio-P accumulation at the beginning of pedogenesis by regulating PCGs and typical microbial community construction. These findings provide new insights into the mechanisms by which microbial communities regulate phosphorus dynamics during pedogenesis, particularly on newly exposed land resulting from global change in alpine and polar regions.
Author Xu, Mingyang
Bing, Haijan
He, Junbo
Luo, Chaoyi
Wu, Yanhong
Zhu, He
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Issue 8
Keywords phosphorus cycling genes (PCGs)
beginning of pedogenesis
microbial communities
glacier foreland
nutrient cycling
phosphorus bioavailability
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This study was supported by the National Natural Science Foundation of China (Nos, 42271064 and 42107281), the Central Government‐Guided Local Science and Technology Development Project (2024ZYD0038), the International Partnership Program of the Chinese Academy of Sciences (131551KYSB20190028) and the Science and Technology Research Program of the institute of Mountain Hazards and Environment, Chinese Academy of Sciences (IMHE‐ZDRW‐06).
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e_1_2_9_10_1
e_1_2_9_56_1
e_1_2_9_33_1
e_1_2_9_90_1
e_1_2_9_71_1
e_1_2_9_103_1
e_1_2_9_107_1
e_1_2_9_122_1
e_1_2_9_14_1
e_1_2_9_37_1
e_1_2_9_18_1
e_1_2_9_41_1
e_1_2_9_64_1
e_1_2_9_87_1
e_1_2_9_22_1
e_1_2_9_45_1
e_1_2_9_68_1
e_1_2_9_83_1
e_1_2_9_6_1
e_1_2_9_119_1
e_1_2_9_60_1
e_1_2_9_2_1
e_1_2_9_111_1
e_1_2_9_115_1
e_1_2_9_26_1
e_1_2_9_49_1
e_1_2_9_30_1
e_1_2_9_53_1
e_1_2_9_99_1
e_1_2_9_72_1
e_1_2_9_11_1
e_1_2_9_34_1
e_1_2_9_57_1
e_1_2_9_95_1
e_1_2_9_76_1
e_1_2_9_91_1
e_1_2_9_102_1
e_1_2_9_106_1
e_1_2_9_15_1
e_1_2_9_38_1
e_1_2_9_121_1
e_1_2_9_19_1
e_1_2_9_42_1
e_1_2_9_88_1
e_1_2_9_61_1
e_1_2_9_46_1
e_1_2_9_84_1
Csardi G. (e_1_2_9_21_1) 2005; 1695
e_1_2_9_23_1
e_1_2_9_65_1
e_1_2_9_80_1
e_1_2_9_5_1
e_1_2_9_114_1
e_1_2_9_118_1
e_1_2_9_9_1
e_1_2_9_27_1
e_1_2_9_69_1
e_1_2_9_110_1
e_1_2_9_31_1
e_1_2_9_50_1
e_1_2_9_73_1
e_1_2_9_35_1
e_1_2_9_77_1
e_1_2_9_96_1
e_1_2_9_12_1
e_1_2_9_54_1
e_1_2_9_92_1
e_1_2_9_109_1
e_1_2_9_101_1
e_1_2_9_105_1
e_1_2_9_124_1
e_1_2_9_39_1
e_1_2_9_16_1
e_1_2_9_58_1
e_1_2_9_20_1
e_1_2_9_62_1
e_1_2_9_89_1
e_1_2_9_24_1
e_1_2_9_43_1
e_1_2_9_66_1
e_1_2_9_85_1
e_1_2_9_8_1
e_1_2_9_81_1
e_1_2_9_4_1
e_1_2_9_113_1
e_1_2_9_117_1
e_1_2_9_28_1
e_1_2_9_47_1
e_1_2_9_74_1
e_1_2_9_51_1
e_1_2_9_78_1
e_1_2_9_13_1
e_1_2_9_32_1
e_1_2_9_55_1
e_1_2_9_97_1
e_1_2_9_93_1
e_1_2_9_108_1
e_1_2_9_70_1
e_1_2_9_100_1
e_1_2_9_123_1
e_1_2_9_104_1
Zhong X. (e_1_2_9_120_1) 1999; 28
e_1_2_9_17_1
e_1_2_9_36_1
e_1_2_9_59_1
e_1_2_9_63_1
e_1_2_9_40_1
e_1_2_9_67_1
e_1_2_9_44_1
e_1_2_9_86_1
e_1_2_9_7_1
e_1_2_9_82_1
e_1_2_9_3_1
e_1_2_9_112_1
e_1_2_9_116_1
e_1_2_9_25_1
e_1_2_9_48_1
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Snippet ABSTRACT The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier...
The rapid accumulation of bioavailable phosphorus (Bio‐P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland....
The rapid accumulation of bioavailable phosphorus (Bio-P) promotes ecosystem development at the beginning of pedogenesis in the Hailuogou Glacier foreland....
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StartPage e70419
SubjectTerms Accumulation
Bacteria - metabolism
beginning of pedogenesis
Bioavailability
Biological Availability
China
Ecological succession
Ecosystem
glacier foreland
Glaciers
Microbial activity
microbial communities
Microbiomes
Microbiota
Microorganisms
Mineralization
nutrient cycling
Organic phosphorus
Phosphorus
Phosphorus - metabolism
phosphorus bioavailability
phosphorus cycling genes (PCGs)
Phytase
Polar environments
Polar regions
Soil - chemistry
Soil formation
Soil Microbiology
Soil microorganisms
Solubilization
Title Microorganisms Promote Soil Phosphorus Bioavailability at the Beginning of Pedogenesis
URI https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fgcb.70419
https://www.ncbi.nlm.nih.gov/pubmed/40792352
https://www.proquest.com/docview/3244167913
https://www.proquest.com/docview/3238720163
Volume 31
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