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spelling paper:paper_13645072_v124_n1_p155_DellaMonica2023-06-08T16:11:46Z Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability P mineralization P solubilization P solubilizing fungi pH phosphatase acid phosphatase alkaline phosphatase aluminum calcium iron phosphatase phosphatidylcholine phosphorus phytate fungal protein phosphatase phosphate biomineralization enzyme activity fungus inoculation metabolism microbial activity nutrient availability pH phosphatase phosphorus cycle solubilization Article fungal development fungus growth mineralization nonhuman Penicillium purpurogenum pH phosphorus cycle rock solubilization Talaromyces Talaromyces diversus Talaromyces flavus Talaromyces helicus chemistry enzymology genetics metabolism microbiology Penicillium pH soil Talaromyces Fungi Penicillium purpurogenum Talaromyces flavus Fungal Proteins Hydrogen-Ion Concentration Penicillium Phosphates Phosphoric Monoester Hydrolases Soil Soil Microbiology Talaromyces Aims: The aim of this work is to analyse the effect of pH, fungal identity and P chemical nature on microbial development and phosphatase release, discussing solubilization and mineralization processes in P cycling. Methods and Results: P solubilizing fungi (Talaromyces flavus, T. helicus L, T. helicus N, T. diversus and Penicillium purpurogenum) were grown under three pH conditions (6, 6·5 and 8·5) and with different inorganic (calcium, iron, aluminium and rock) and organic (lecithin and phytate) P sources. P solubilization, mineralization, growth and phosphatase production were recorded. Acid and neutral environments maximized fungal development and P recycling. P chemical nature changed the phosphatases release pattern depending on the fungal identity. Acid phosphatase activity was higher than alkaline phosphatases, regardless of pH or sample times. Alkaline phosphatases were affected by a combination of those factors. Conclusions: P chemical nature and pH modify fungal growth, P mineralization and solubilization processes. The underlying fungal identity-dependent metabolism governs the capacity and efficiency of P solubilization and mineralization. P solubilization and mineralization processes are interrelated and simultaneously present in soil fungi. Significance and Impact of the study: This study constitutes a reference work to improve the selection of fungal bioinoculants in different environmental conditions, highlighting their role in P cycling. © 2017 The Society for Applied Microbiology 2018 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_13645072_v124_n1_p155_DellaMonica http://hdl.handle.net/20.500.12110/paper_13645072_v124_n1_p155_DellaMonica
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic P mineralization
P solubilization
P solubilizing fungi
pH
phosphatase
acid phosphatase
alkaline phosphatase
aluminum
calcium
iron
phosphatase
phosphatidylcholine
phosphorus
phytate
fungal protein
phosphatase
phosphate
biomineralization
enzyme activity
fungus
inoculation
metabolism
microbial activity
nutrient availability
pH
phosphatase
phosphorus cycle
solubilization
Article
fungal development
fungus growth
mineralization
nonhuman
Penicillium purpurogenum
pH
phosphorus cycle
rock
solubilization
Talaromyces
Talaromyces diversus
Talaromyces flavus
Talaromyces helicus
chemistry
enzymology
genetics
metabolism
microbiology
Penicillium
pH
soil
Talaromyces
Fungi
Penicillium purpurogenum
Talaromyces flavus
Fungal Proteins
Hydrogen-Ion Concentration
Penicillium
Phosphates
Phosphoric Monoester Hydrolases
Soil
Soil Microbiology
Talaromyces
spellingShingle P mineralization
P solubilization
P solubilizing fungi
pH
phosphatase
acid phosphatase
alkaline phosphatase
aluminum
calcium
iron
phosphatase
phosphatidylcholine
phosphorus
phytate
fungal protein
phosphatase
phosphate
biomineralization
enzyme activity
fungus
inoculation
metabolism
microbial activity
nutrient availability
pH
phosphatase
phosphorus cycle
solubilization
Article
fungal development
fungus growth
mineralization
nonhuman
Penicillium purpurogenum
pH
phosphorus cycle
rock
solubilization
Talaromyces
Talaromyces diversus
Talaromyces flavus
Talaromyces helicus
chemistry
enzymology
genetics
metabolism
microbiology
Penicillium
pH
soil
Talaromyces
Fungi
Penicillium purpurogenum
Talaromyces flavus
Fungal Proteins
Hydrogen-Ion Concentration
Penicillium
Phosphates
Phosphoric Monoester Hydrolases
Soil
Soil Microbiology
Talaromyces
Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
topic_facet P mineralization
P solubilization
P solubilizing fungi
pH
phosphatase
acid phosphatase
alkaline phosphatase
aluminum
calcium
iron
phosphatase
phosphatidylcholine
phosphorus
phytate
fungal protein
phosphatase
phosphate
biomineralization
enzyme activity
fungus
inoculation
metabolism
microbial activity
nutrient availability
pH
phosphatase
phosphorus cycle
solubilization
Article
fungal development
fungus growth
mineralization
nonhuman
Penicillium purpurogenum
pH
phosphorus cycle
rock
solubilization
Talaromyces
Talaromyces diversus
Talaromyces flavus
Talaromyces helicus
chemistry
enzymology
genetics
metabolism
microbiology
Penicillium
pH
soil
Talaromyces
Fungi
Penicillium purpurogenum
Talaromyces flavus
Fungal Proteins
Hydrogen-Ion Concentration
Penicillium
Phosphates
Phosphoric Monoester Hydrolases
Soil
Soil Microbiology
Talaromyces
description Aims: The aim of this work is to analyse the effect of pH, fungal identity and P chemical nature on microbial development and phosphatase release, discussing solubilization and mineralization processes in P cycling. Methods and Results: P solubilizing fungi (Talaromyces flavus, T. helicus L, T. helicus N, T. diversus and Penicillium purpurogenum) were grown under three pH conditions (6, 6·5 and 8·5) and with different inorganic (calcium, iron, aluminium and rock) and organic (lecithin and phytate) P sources. P solubilization, mineralization, growth and phosphatase production were recorded. Acid and neutral environments maximized fungal development and P recycling. P chemical nature changed the phosphatases release pattern depending on the fungal identity. Acid phosphatase activity was higher than alkaline phosphatases, regardless of pH or sample times. Alkaline phosphatases were affected by a combination of those factors. Conclusions: P chemical nature and pH modify fungal growth, P mineralization and solubilization processes. The underlying fungal identity-dependent metabolism governs the capacity and efficiency of P solubilization and mineralization. P solubilization and mineralization processes are interrelated and simultaneously present in soil fungi. Significance and Impact of the study: This study constitutes a reference work to improve the selection of fungal bioinoculants in different environmental conditions, highlighting their role in P cycling. © 2017 The Society for Applied Microbiology
title Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
title_short Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
title_full Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
title_fullStr Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
title_full_unstemmed Fungal extracellular phosphatases: their role in P cycling under different pH and P sources availability
title_sort fungal extracellular phosphatases: their role in p cycling under different ph and p sources availability
publishDate 2018
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_13645072_v124_n1_p155_DellaMonica
http://hdl.handle.net/20.500.12110/paper_13645072_v124_n1_p155_DellaMonica
_version_ 1768545941981233152