Microbial Processes Associated with Roots of Bulbous Rush Coated with Iron Plaques

Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives...

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Published inMicrobial ecology Vol. 46; no. 3; pp. 302 - 311
Main Authors K sel, K., Chabbi, A., Trinkwalter, T.
Format Journal Article
LanguageEnglish
Published New York, NY Springer-Verlag New York Inc 01.11.2003
Springer
Springer Nature B.V
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Abstract Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 106Fe(III) reducers and 107Fe(II) oxidizers g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}$were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}\ {\rm d}^{-1}$and 3.6 mmol g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}\ {\rm d}^{-1}$under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
AbstractList Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 10(6) Fe(III) reducers and 10(7) Fe(II) oxidizers g (fresh wt root)(-1) were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g (fresh wt root) (-1) d(-1) and 3.6 mmol g (fresh wt root)(-1) d(-1) under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2 and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2 levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 10(6) Fe(III) reducers and 10(7) Fe(II) oxidizers g (fresh wt root)(-1) were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g (fresh wt root) (-1) d(-1) and 3.6 mmol g (fresh wt root)(-1) d(-1) under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2 and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2 levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 10(6) Fe(III) reducers and 10(7) Fe(II) oxidizers g (fresh wt root)(-1) were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g (fresh wt root) (-1) d(-1) and 3.6 mmol g (fresh wt root)(-1) d(-1) under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2 and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2 levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 10 super(6) Fe(III) reducers and 10 super(7) Fe(II) oxidizers g (fresh wt root) super(-1) were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g (fresh wt root) super(-1) d super(-1) and 3.6 mmol g (fresh wt root) super(-1) d super(-1) under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO sub(2) and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO sub(2) levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 106 Fe(III) reducers and 107 Fe(II) oxidizers g (fresh wt root)−1 were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g (fresh wt root) −1 d−1 and 3.6 mmol g (fresh wt root)−1 d−1 under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2 and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2 levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron plaques, and it has been suggested that microbial processes under the iron plaques might be supportive for Juncus plant growth. The objectives of this work were to enumerate the microbes involved in the turnover of iron and organic root exudates in the rhizoplane, to investigate the effect of oxygen and pH on the utilization of these exudates by the rhizobacteria, and to study the ability of the root-colonizing microbiota to reduce sulfate. Enumeration studies done at pH 3 demonstrated that 106Fe(III) reducers and 107Fe(II) oxidizers g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}$were associated with Juncus roots. When roots were incubated in goethite-containing medium without and with supplemental glucose, Fe(II) was formed at rates approximating 1.1 mmol g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}\ {\rm d}^{-1}$and 3.6 mmol g$(\text{fresh}\ {\rm wt}\ \text{root})^{-1}\ {\rm d}^{-1}$under anoxic conditions, respectively. These results suggest that a rapid microbially mediated cycling of iron occurs in the rhizosphere of Juncus roots under changing redox conditions. Most-probable-number estimates of aerobes and anaerobes capable of consuming root exudates at pH 3 were similar in the rhizosphere sediment and in Juncus roots, but numbers of aerobes were significantly higher than those of anaerobes. At pH 3, supplemental organic exudates were primarily subject to aerobic oxidation to CO2and not subject to fermentation. However, at pH 4.5, root exudates were also rapidly utilized under anoxic conditions. Root-associated sulfate reduction was not observed at pH 3 to 4.5 but was observed at pH 4.9. The pH increased during all root-incubation studies both under oxic and anoxic conditions. Thus, as result of the microbial turnover of organic root exudates, pH and CO2levels might be elevated at the root surface and favor Juncus plants to colonize acidic habitats.
Author T. Trinkwalter
A. Chabbi
K. Küsel
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Issue 3
Keywords Biotope
Monocotyledones
Oxygen
Exudate
Root
Growth
Iron
Freshwater environment
Plant
Juncaceae
Juncus
Angiospermae
Coal
Turnover
Lakes
pH
Spermatophyta
Pioneer species
Language English
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PublicationTitle Microbial ecology
PublicationTitleAlternate Microb Ecol
PublicationYear 2003
Publisher Springer-Verlag New York Inc
Springer
Springer Nature B.V
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References 16347168 - Appl Environ Microbiol. 1986 Oct;52(4):751-7
12123477 - Environ Microbiol. 2002 Jul;4(7):414-21
11229928 - Appl Environ Microbiol. 2001 Mar;67(3):1328-34
11849360 - J Appl Microbiol. 2002;92(2):315-21
10347074 - Appl Environ Microbiol. 1999 Jun;65(6):2758-61
10427060 - Appl Environ Microbiol. 1999 Aug;65(8):3633-40
18961462 - Talanta. 1974 Apr;21(4):314-8
9406396 - Appl Environ Microbiol. 1997 Dec;63(12):4784-92
11080381 - Microb Ecol. 2000 Aug;40(3):238-249
16348395 - Appl Environ Microbiol. 1991 Jan;57(1):207-11
16535147 - Appl Environ Microbiol. 1995 Oct;61(10):3667-75
10508065 - Appl Environ Microbiol. 1999 Oct;65(10):4393-8
References_xml – reference: 9406396 - Appl Environ Microbiol. 1997 Dec;63(12):4784-92
– reference: 10427060 - Appl Environ Microbiol. 1999 Aug;65(8):3633-40
– reference: 18961462 - Talanta. 1974 Apr;21(4):314-8
– reference: 10347074 - Appl Environ Microbiol. 1999 Jun;65(6):2758-61
– reference: 16347168 - Appl Environ Microbiol. 1986 Oct;52(4):751-7
– reference: 10508065 - Appl Environ Microbiol. 1999 Oct;65(10):4393-8
– reference: 11229928 - Appl Environ Microbiol. 2001 Mar;67(3):1328-34
– reference: 12123477 - Environ Microbiol. 2002 Jul;4(7):414-21
– reference: 16535147 - Appl Environ Microbiol. 1995 Oct;61(10):3667-75
– reference: 16348395 - Appl Environ Microbiol. 1991 Jan;57(1):207-11
– reference: 11080381 - Microb Ecol. 2000 Aug;40(3):238-249
– reference: 11849360 - J Appl Microbiol. 2002;92(2):315-21
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Snippet Bulbous rush (Juncus bulbosus) is a pioneer species in acidic, iron-rich, coal mining lakes in the eastern part of Germany. Juncus roots are coated with iron...
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SubjectTerms Aerobes
Aerobic bacteria
Anaerobes
Anaerobic conditions
Animal, plant and microbial ecology
Anoxia
Anoxic conditions
Anoxic sediments
Aquatic plants
Biological and medical sciences
Carbon dioxide
Carbon Dioxide - analysis
Coal
Coal mining
Enumeration
Exudates
Exudation
Fermentation
Freshwater
Fundamental and applied biological sciences. Psychology
Goethite
Hydrogen-Ion Concentration
Iron
Iron - metabolism
Juncus bulbosus
Magnoliopsida - growth & development
Magnoliopsida - microbiology
Microbial ecology
Microbial flora
Microbiota
Microflora of plants
Microorganisms
Mining
Oxidation
Oxidation-Reduction
Oxides
Oxidizing agents
pH effects
Plant growth
Plant roots
Plant Roots - microbiology
Plaques
Rhizoplane
Rhizosphere
Root exudates
Roots
Sediments
Soil ecology
Soil Microbiology
Sulfate reduction
Sulfates
Sulphate reduction
Various environments (extraatmospheric space, air, water)
Title Microbial Processes Associated with Roots of Bulbous Rush Coated with Iron Plaques
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