Vegetation Effects on Soil Organic Matter Chemistry of Aggregate Fractions in a Hawaiian Forest

We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow (Dicranopteris linearis) and fast-decomposing species (Cheirodendron trigynum) and surface (O), and subsurface (A-horizon)...

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Bibliographic Details
Published inEcosystems (New York) Vol. 14; no. 3; pp. 382 - 397
Main Authors Stewart, Catherine E, Neff, Jason C, Amatangelo, Kathryn L, Vitousek, Peter M
Format Journal Article
LanguageEnglish
Published New York Springer-Verlag 01.04.2011
Springer Science+Business Media
Springer
Springer Nature B.V
Subjects
Acid soils
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Biomarkers
Biomedical and Life Sciences
Carbon content
Cheirodendron
Cheirodendron trigynum
Chemical properties
Chemistry
chromatography
cutin
Decomposition
derivatization
Dicranopteris
Dicranopteris linearis
Ecology
Environmental Management
Forest soils
Forestry
forests
Fundamental and applied biological sciences. Psychology
Gas chromatography
General aspects
General forest ecology
Generalities. Production, biomass. Quality of wood and forest products. General forest ecology
Geochemistry
Geoecology/Natural Processes
Hydrology/Water Resources
inheritance (genetics)
Leaves
Life Sciences
Lignin
Lipids
Litter
Mass spectrometry
Microorganisms
Organic matter
Organic soils
physicochemical properties
plant biochemistry
plant litter
Plant Sciences
Plant tissues
Plants
Polysaccharides
Pyrolysis
rooting
Saccharides
Soil aggregates
Soil biochemistry
Soil chemistry
Soil organic matter
Soil structure
Soils
suberin
Synecology
Vegetation
Vegetation effects
Zoology
Hawaii
Polynesia
Oceania
soil organic chemistry
fern
Hawaii
soil organic carbon
decomposition
pyrolysis-gas chromatography/mass spectrometry
soil organic matter
Soil chemistry
Organic carbon
Pyrolysis
Forests
Organic matter
Decomposition
Vegetation effect
Pteridophyta
Organic chemistry
Gas chromatography
Soils
Ecosystem
Aggregate
Mass spectrometry
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Abstract We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow (Dicranopteris linearis) and fast-decomposing species (Cheirodendron trigynum) and surface (O), and subsurface (A-horizon) SOM beneath each species using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS), with and without derivatization. The live tissues of Dicranopteris had greater lignin content whereas Cheirodendron had a greater lipid, N-bearing, and polysaccharide component. Despite this difference in leaf chemistry, SOM chemistry was similar between soil aggregate fractions, but different between horizons. The O-horizon contained primarily lignin and polysaccharide biomarkers whereas the A-horizon contained polysaccharide, aromatic, and N-derived compounds, indicating considerable microbial processing of plant litter. The soils beneath Cheirodendron inherited a greater lipid signal composed of cutin and suberin biomarkers whereas the soils beneath Dicranopteris contained greater aromatic biomarker content, possibly derived from plant lignins. The soils beneath both species were more similar to root polysaccharides, lipids, and lignins than aboveground tissue. This study indicates that although plant-derived OM is processed vigorously, species-specific biomarkers and compound class differences persist into these soils and that differences in plant chemical properties may influence soil development even after considerable reworking of plant litter by microorganisms.
AbstractList We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow (Dicranopteris linearis) and fast-decomposing species (Cheirodendron trigynum) and surface (O), and subsurface (A-horizon) SOM beneath each species using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS), with and without derivatization. The live tissues of Dicranopteris had greater lignin content whereas Cheirodendron had a greater lipid, N-bearing, and polysaccharide component. Despite this difference in leaf chemistry, SOM chemistry was similar between soil aggregate fractions, but different between horizons. The O-horizon contained primarily lignin and polysaccharide biomarkers whereas the A-horizon contained polysaccharide, aromatic, and N-derived compounds, indicating considerable microbial processing of plant litter. The soils beneath Cheirodendron inherited a greater lipid signal composed of cutin and suberin biomarkers whereas the soils beneath Dicranopteris contained greater aromatic biomarker content, possibly derived from plant lignins. The soils beneath both species were more similar to root polysaccharides, lipids, and lignins than aboveground tissue. This study indicates that although plant-derived OM is processed vigorously, species-specific biomarkers and compound class differences persist into these soils and that differences in plant chemical properties may influence soil development even after considerable reworking of plant litter by microorganisms.
We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow ( Dicranopteris linearis ) and fast-decomposing species ( Cheirodendron trigynum ) and surface (O), and subsurface (A-horizon) SOM beneath each species using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS), with and without derivatization. The live tissues of Dicranopteris had greater lignin content whereas Cheirodendron had a greater lipid, N-bearing, and polysaccharide component . Despite this difference in leaf chemistry, SOM chemistry was similar between soil aggregate fractions, but different between horizons. The O-horizon contained primarily lignin and polysaccharide biomarkers whereas the A-horizon contained polysaccharide, aromatic, and N-derived compounds, indicating considerable microbial processing of plant litter. The soils beneath Cheirodendron inherited a greater lipid signal composed of cutin and suberin biomarkers whereas the soils beneath Dicranopteris contained greater aromatic biomarker content, possibly derived from plant lignins. The soils beneath both species were more similar to root polysaccharides, lipids, and lignins than aboveground tissue. This study indicates that although plant-derived OM is processed vigorously, species-specific biomarkers and compound class differences persist into these soils and that differences in plant chemical properties may influence soil development even after considerable reworking of plant litter by microorganisms.
We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow (Dicranopteris linearis) and fast-decomposing species (Cheirodendron trigynum) and surface (O), and subsurface (A-horizon) SOM beneath each species using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS), with and without derivatization. The live tissues of Dicranopteris had greater lignin content whereas Cheirodendron had a greater lipid, N-bearing, and polysaccharide component. Despite this difference in leaf chemistry, SOM chemistry was similar between soil aggregate fractions, but different between horizons. The O-horizon contained primarily lignin and polysaccharide biomarkers whereas the A-horizon contained polysaccharide, aromatic, and N-derived compounds, indicating considerable microbial processing of plant litter. The soils beneath Cheirodendron inherited a greater lipid signal composed of cutin and suberin biomarkers whereas the soils beneath Dicranopteris contained greater aromatic biomarker content, possibly derived from plant lignins. The soils beneath both species were more similar to root polysaccharides, lipids, and lignins than aboveground tissue. This study indicates that although plant-derived OM is processed vigorously, species-specific biomarkers and compound class differences persist into these soils and that differences in plant chemical properties may influence soil development even after considerable reworking of plant litter by microorganisms.[PUBLICATION ABSTRACT]
We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We characterized a slow (Dicranopteris linearis) and fast-decomposing species (Cheirodendron trigynum) and surface (O), and subsurface (A-horizon) SOM beneath each species using pyrolysis-gas chromatography/mass spectrometry (py-GC/MS), with and without derivatization. The live tissues of Dicranopteris had greater lignin content whereas Cheirodendron had a greater lipid, N-bearing, and polysaccharide component. Despite this difference in leaf chemistry, SOM chemistry was similar between soil aggregate fractions, but different between horizons. The O-horizon contained primarily lignin and polysaccharide biomarkers whereas the A-horizon contained polysaccharide, aromatic, and N-derived compounds, indicating considerable microbial processing of plant litter. The soils beneath Cheirodendron inherited a greater lipid signal composed of cutin and suberin biomarkers whereas the soils beneath Dicranopteris contained greater aromatic biomarker content, possibly derived from plant lignins. The soils beneath both species were more similar to root polysaccharides, lipids, and lignins than aboveground tissue. This study indicates that although plant-derived OM is processed vigorously, speciesspecific biomarkers and compound class differences persist into these soils and that differences in plant chemical properties may influence soil development even after considerable reworking of plant litter by microorganisms.
Audience Academic
Author Amatangelo, Kathryn L.
Neff, Jason C.
Vitousek, Peter M.
Stewart, Catherine E.
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– sequence: 2
  fullname: Neff, Jason C
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  fullname: Amatangelo, Kathryn L
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  fullname: Vitousek, Peter M
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Springer Science+Business Media, LLC 2011
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IsPeerReviewed true
IsScholarly true
Issue 3
Keywords soil organic chemistry
fern
Hawaii
soil organic carbon
decomposition
pyrolysis-gas chromatography/mass spectrometry
soil organic matter
Soil chemistry
Organic carbon
Pyrolysis
Forests
Organic matter
Decomposition
Vegetation effect
Pteridophyta
Organic chemistry
Gas chromatography
Soils
Ecosystem
Aggregate
Mass spectrometry
Language English
License CC BY 4.0
http://www.springer.com/tdm
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Notes http://handle.nal.usda.gov/10113/62134
http://dx.doi.org/10.1007/s10021-011-9417-y
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ObjectType-Feature-1
content type line 23
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PQPubID 55443
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springer_journals_10_1007_s10021_011_9417_y
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PublicationDate 2011-04-01
PublicationDateYYYYMMDD 2011-04-01
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  year: 2011
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PublicationDecade 2010
PublicationPlace New York
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PublicationTitle Ecosystems (New York)
PublicationTitleAbbrev Ecosystems
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Snippet We examined chemical changes from leaf tissue to soil organic matter (SOM) to determine the persistence of plant chemistry into soil aggregate fractions. We...
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SubjectTerms Acid soils
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Biomarkers
Biomedical and Life Sciences
Carbon content
Cheirodendron
Cheirodendron trigynum
Chemical properties
Chemistry
chromatography
cutin
Decomposition
derivatization
Dicranopteris
Dicranopteris linearis
Ecology
Environmental Management
Forest soils
Forestry
forests
Fundamental and applied biological sciences. Psychology
Gas chromatography
General aspects
General forest ecology
Generalities. Production, biomass. Quality of wood and forest products. General forest ecology
Geochemistry
Geoecology/Natural Processes
Hydrology/Water Resources
inheritance (genetics)
Leaves
Life Sciences
Lignin
Lipids
Litter
Mass spectrometry
Microorganisms
Organic matter
Organic soils
physicochemical properties
plant biochemistry
plant litter
Plant Sciences
Plant tissues
Plants
Polysaccharides
Pyrolysis
rooting
Saccharides
Soil aggregates
Soil biochemistry
Soil chemistry
Soil organic matter
Soil structure
Soils
suberin
Synecology
Vegetation
Vegetation effects
Zoology
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Title Vegetation Effects on Soil Organic Matter Chemistry of Aggregate Fractions in a Hawaiian Forest
URI https://www.jstor.org/stable/41507773
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