Correction to: Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities

George, T. S.; Giles, Courtney D.; Condron, Leo M.; Gama-Rodrigues, Antônio Carlos; Jaisi, Deb P.; Lang, Friederike; Neal, Andrew L.; Stutter, Marc; Almeida, Danilo Silva; Bol, Roland; Celi, Leo Anthony; Cotner, James B.; Feng, Gu; Goll, Daniel S.; Hallama, Moritz; Krueger, Jeffrey; Plassard, Claude; Rosling, Anna; Darch, Tegan; Fraser, Tandra D.; Giesler, Reiner; Richardson, Alan; Tamburini, F.; Shand, C. A.; Lumsdon, David G.; Zhang, H.; Blackwell, Martin; Wearing, Catherine; Mezeli, Malika M.; Almås, Åsgeir R.; Audette, Yuki; Bertrand, Isabelle; Beyhaut, Elena; Boitt, Gustavo; Bradshaw, N.; Brearley, Charles A.; Bruulsema, Tom W.; Ciais, Philippe; Cozzolino, Vincenza; Durán, Paola; Mora, Marı́a de la Luz; Menezes, Alexandre B. de; Dodd, Rosalind; Dunfield, Kari E.; Engl, Christoph; Frazão, Joaquim José; Garland, Gina; Jiménez, José; Graça, Jessica; Granger, Steven J.; Harrison, A. F.; Heuck, Christine; Hou, Enqing; Johnes, Penny J; Kaiser, Klaus; Kjær, Helle Astrid; Klumpp, Erwin; Lamb, Angela L.; Macintosh, Katrina A.; Mackay, Eleanor B.; McGrath, John W.; McIntyre, Catherine; McLaren, Timothy I.; Mészáros, Éva; Missong, Anna; Mooshammer, Maria; Negrón, C. P.; Nelson, Lee-Ann; Pfahler, Verena; Poblete-Grant, Patricia; Randall, M.; Seguel, Alex; Seth, Kritarth; Smith, Andrew; Smits, Mark M.; Sobarzo, J. A.; Spohn, Marie; Tawaraya, Keitaro; Tibbett, Mark; Voroney, Paul; Wallander, Håkan; Wang, L.; Wasaki, Jun; Haygarth, Philip M.

doi:10.1007/s11104-017-3488-2

Cited by 11 publications

(4 citation statements)

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“…These results generally agree with the previous study of Siddique and Robinson and Song et al [43,44] who observed that long-term crop cultivation without any fertilizer input resulted in a decreased labile P content in the soil. The changes in labile and moderately labile P pools could be due to the organic P mineralization that allows the inorganic P to be utilized by the ectomycorrhizal fungi [45,46]. The changes might also because of the elevated SOM contents in the soil with HNPK additions which could affect P-sorption sites, either by creating a cover over iron and aluminum sorption spots to cease the added or the applied P from fixation/adsorption or by modifying the mineral surface charges that also reduce the sorption sites, eventually increasing the soil phosphorus [47].…”

Section: Relationship Of Soil Properties and P Fractions With Npk Addmentioning

confidence: 99%

Long-Term Mineral Fertilization Improved the Grain Yield and Phosphorus Use Efficiency by Changing Soil P Fractions in Ferralic Cambisol

et al. 2019

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Elevated mineral fertilization may change the composition and increase the availability of soil phosphorus (P) in subtropical paddy soils and thus affect long-term plant growth. However, an understanding of the response of soil P fractions to long-term nitrogen, phosphorus and potassium (NPK) additions remains elusive. This study aimed to explore the responses of soil P-fractions and their mobility to different long-term chemical fertilization rates under a double rice cropping system. The rates of nitrogen (N), phosphorus (P), and potassium (K) in the low NPK treatment (LNPK) were 90, 45, and 75 kg ha −1 year −1 , respectively, and in the high NPK treatment (HNPK), they were 180, 90, and 150 kg ha −1 year −1 , respectively. The results showed that the concentrations of soil organic matter (SOM), total P, Olsen P, total N, and mineral N were remarkably increased under HNPK by 17.46%, 162.66%, 721.16%, 104.42%, and 414.46%, respectively, compared with those under control (CT). Compared to the CT P fractions, HNPK increased the labile P fractions (i.e., NaHCO 3 -Pi and NaHCO 3 -Po) by 322.25% and 83.53% and the moderately labile P fractions (i.e., NaOH-Pi, NaOH-Po and HCl. dil. Pi) by 163.54%, 183.78%, and 3167.25% respectively, while the non-labile P was decreased by the HNPK addition. P uptake and grain yield were increased by LNPK and HNPK by 10.02% and 35.20%, respectively, compared with CT. P use efficiency indices were also higher under HNPK than under LNPK. There was a strong positive relationship between grain yield and P use efficiency (R 2 = 0.97). A redundancy analysis (RDA) showed a strong correlation between soil chemical properties and the labile and moderately labile P pools. Structural equation modeling (SEM) revealed that SOM, mineral N, and available P strongly control the labile P pool. In conclusion, NPK additions under the paddy soils significantly influences the soil P fractions. The soil P dynamics Agronomy 2019, 9, 784 2 of 15 and the mechanisms governing the interactions between plants and soil nutrients are clearly explained in this study.

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Section: Relationship Of Soil Properties and P Fractions With Npk Addmentioning

confidence: 99%

Long-Term Mineral Fertilization Improved the Grain Yield and Phosphorus Use Efficiency by Changing Soil P Fractions in Ferralic Cambisol

et al. 2019

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“…They are synthesized in terrestrial ecosystems by plants and strongly complexed in soils, where they accumulate to form the dominant component of organic phosphorus (P o ) ( Menezes-Blackburn et al, 2013 ). The survey of global P storage suggested that the potential of the use of monoester P (mostly inositol phosphates) ( George et al, 2018 ) is greater for grasslands than for arable soils ( Menezes-Blackburn et al, 2018 ). However, due to the lack of active substances that hydrolyze phytate, it is not easy for plants to obtain P from them ( Gerke, 2015 ).…”

Section: Introductionmentioning

confidence: 99%

In-depth characterization of phytase-producing plant growth promotion bacteria isolated in alpine grassland of Qinghai-Tibetan Plateau

Yang

et al. 2023

Front. Microbiol.

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The use of plant growth promoting bacteria (PGPB) express phytase (myo-inositol hexakisphosphate phosphohydrolase) capable of hydrolyzing inositol phosphate in soil was a sustainable approach to supply available phosphorus (P) to plants. A total of 73 bacterial isolates with extracellular phytase activity were selected from seven dominant grass species rhizosphere in alpine grassland of Qinghai-Tibetan Plateau. Then, the plant growth promoting (PGP) traits of candidate bacteria were screened by qualitative and quantitative methods, including organic/inorganic Phosphorus solubilization (P. solubilization), plant hormones (PHs) production, nitrogen fixation, 1-aminocyclopropane-1-carboxylic acid (ACC) deaminase activity and antimicrobial activity. Further experiment were conducted to test their growth promoting effect on Lolium perenne L. under P-limitation. Our results indicated that these bacteria as members of phyla Proteobacteria (90.41%) and Actinobacteria (9.59%) were related to 16 different genera. The isolates of Pseudomonas species showed the highest isolates number (36) and average values of phytase activity (0.267 ± 0.012 U mL–1), and showed a multiple of PGP traits, which was a great candidate for PGPBs. In addition, six strains were positive in phytase gene (β-propeller phytase, bpp) amplification, which significantly increased the shoot length, shoot/root fresh weight, root average diameter and root system phytase activity of Lolium perenne L. under P-limitation, and the expression of phytase gene (bppP) in root system were verified by qPCR. Finally, the PHY101 gene encoding phytase from Pseudomonas mandelii GS10-1 was cloned, sequenced, and recombinantly expressed in Escherichia coli. Biochemical characterization demonstrated that the recombinant phytase PHY101 revealed the highest activity at pH 6 and 40°C temperature. In particular, more than 60% of activity was retained at a low temperature of 15°C. This study demonstrates the opportunity for commercialization of the phytase-producing PGPB to developing localized microbial inoculants and engineering rhizobacteria for sustainable use in alpine grasslands.

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“…Soil phosphatase, pivotal in mineralizing soil organic P, is also influenced by N input (George et al, 2018;Cao et al, 2022;Ma et al, 2023). We found that N input significantly increased ALP activity and the abundance of the phoD gene in yellow soil, while the response was less pronounced for acid phosphatase (ACP) and phoC abundance (Figure 5).…”

Section: Relationship Between Changes In Soil Available P and Plant R...mentioning

confidence: 89%

Influences of nitrogen input forms and levels on phosphorus availability in karst grassland soils

Zhou,

Yang,

Zhao

et al. 2024

Front. Sustain. Food Syst.

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The availability of soil phosphorus (P), a crucial nutrient influencing plant productivity and ecosystem function, is impacted by continuously increasing nitrogen (N) enrichment, which changes the soil P cycle. The effect of varying forms of N input on soil P dynamics in P-limited karst grassland ecosystems remains unclear. To address this knowledge gap, we conducted a greenhouse experiment to explore the effects of various forms of N addition [Ca(NO3)2, NH4Cl, NH4NO3, Urea] on soil P fractions in these ecosystems, applying two levels (N1: 50 mg N kg−1soil, N2: 100 mg N kg−1soil) of N input in two soils (yellow soil, limestone soil). Results indicated that P fractions in both soil types were significantly affected by N additions, with yellow soil demonstrating a higher sensitivity to these additions, and this effect was strongly modulated by the form and level of N added. High N addition, rather than low N, significantly affect the P fractions in both soil types. Specially, except for Ca(NO3)2, high N addition significantly increased the available P in both soils, following the order: Urea and NH4NO3 > NH4Cl > Ca(NO3)2, and decreased NaHCO3-Pi in both soils. High N addition also significantly reduced NaOH-Po and C.HCl-Po fractions in yellow soil. Additionally, the response of root biomass and alkaline phosphatase activity in both soils to N input paralleled the trends observed in the available P fractions. Notably, changes in soil available P were strongly correlated with plant root biomass and soil alkaline phosphatase activity. Our study highlights that the N addition form significantly influences soil P availability, which is closely tied to plant root biomass and alkaline phosphatase activity. This finding underscores the importance of considering N input form to boost soil fertility and promote sustainable agriculture.

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Correction to: Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities

Cited by 11 publications

References 0 publications

Long-Term Mineral Fertilization Improved the Grain Yield and Phosphorus Use Efficiency by Changing Soil P Fractions in Ferralic Cambisol

Long-Term Mineral Fertilization Improved the Grain Yield and Phosphorus Use Efficiency by Changing Soil P Fractions in Ferralic Cambisol

In-depth characterization of phytase-producing plant growth promotion bacteria isolated in alpine grassland of Qinghai-Tibetan Plateau

Influences of nitrogen input forms and levels on phosphorus availability in karst grassland soils

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