influence of tree species on canopy soil nutrient status in a tropical lowland wet forest in Costa Rica
The canopy is host to a large percentage of the flora and fauna in tropical wet forests and is distinct from the forest floor in plant richness, soil type and microclimate. In this study, we examined the influence of tree species and season on soil nutrient cycling processes in canopy soils of four...
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| Veröffentlicht in: | Plant and soil 2009-05, Vol.318 (1-2), p.47-61 |
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| creator | Cardelús, Catherine L Mack, Michelle C Woods, Carrie DeMarco, Jennie Treseder, Kathleen K |
| description | The canopy is host to a large percentage of the flora and fauna in tropical wet forests and is distinct from the forest floor in plant richness, soil type and microclimate. In this study, we examined the influence of tree species and season on soil nutrient cycling processes in canopy soils of four tree species common to Costa Rican wet forests. We also compared the canopy soils to the associated forest floor mineral soils. Both tree species and season had strong effects on canopy soil nutrients and processes. Canopy soils from trees with high litter lignin concentrations had higher net N-mineralization rates and higher dissolved inorganic N concentrations than those with low lignin concentrations. During the dry season, net N-immobilization occurred and dissolved organic and inorganic N and available P concentrations were significantly higher than during the wet season. Overall, canopy soils had higher N levels and higher fungi + bacteria richness than forest floor mineral soils. The differences in canopy soil properties observed among tree species indicates that these species have distinct N cycles that reflect differences in both soil origin and biological controls. |
| doi_str_mv | 10.1007/s11104-008-9816-9 |
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In this study, we examined the influence of tree species and season on soil nutrient cycling processes in canopy soils of four tree species common to Costa Rican wet forests. We also compared the canopy soils to the associated forest floor mineral soils. Both tree species and season had strong effects on canopy soil nutrients and processes. Canopy soils from trees with high litter lignin concentrations had higher net N-mineralization rates and higher dissolved inorganic N concentrations than those with low lignin concentrations. During the dry season, net N-immobilization occurred and dissolved organic and inorganic N and available P concentrations were significantly higher than during the wet season. Overall, canopy soils had higher N levels and higher fungi + bacteria richness than forest floor mineral soils. The differences in canopy soil properties observed among tree species indicates that these species have distinct N cycles that reflect differences in both soil origin and biological controls.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-008-9816-9</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Dordrecht : Springer Netherlands</publisher><subject>Acid soils ; Agronomy. Soil science and plant productions ; Animal, plant and microbial ecology ; Biological and medical sciences ; Biomedical and Life Sciences ; Canopies ; Canopy soil ; Discriminant function analysis ; Dry season ; Dry seasons ; Ecology ; Flora ; Forest canopy ; Forest floor ; Forest litter ; Forest soils ; Forests ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Life Sciences ; Microclimate ; Mineral soils ; Mineralization ; Minerals ; Nutrient cycles ; Nutrient status ; Organic soil ; Organic soils ; Plant Physiology ; Plant Sciences ; Plant species ; Rainy season ; Rainy seasons ; Regular Article ; Seasons ; Soil microorganisms ; Soil nutrients ; Soil properties ; Soil science ; Soil Science & Conservation ; Soil types ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. 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In this study, we examined the influence of tree species and season on soil nutrient cycling processes in canopy soils of four tree species common to Costa Rican wet forests. We also compared the canopy soils to the associated forest floor mineral soils. Both tree species and season had strong effects on canopy soil nutrients and processes. Canopy soils from trees with high litter lignin concentrations had higher net N-mineralization rates and higher dissolved inorganic N concentrations than those with low lignin concentrations. During the dry season, net N-immobilization occurred and dissolved organic and inorganic N and available P concentrations were significantly higher than during the wet season. Overall, canopy soils had higher N levels and higher fungi + bacteria richness than forest floor mineral soils. The differences in canopy soil properties observed among tree species indicates that these species have distinct N cycles that reflect differences in both soil origin and biological controls.</description><subject>Acid soils</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Biomedical and Life Sciences</subject><subject>Canopies</subject><subject>Canopy soil</subject><subject>Discriminant function analysis</subject><subject>Dry season</subject><subject>Dry seasons</subject><subject>Ecology</subject><subject>Flora</subject><subject>Forest canopy</subject><subject>Forest floor</subject><subject>Forest litter</subject><subject>Forest soils</subject><subject>Forests</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Life Sciences</subject><subject>Microclimate</subject><subject>Mineral soils</subject><subject>Mineralization</subject><subject>Minerals</subject><subject>Nutrient cycles</subject><subject>Nutrient status</subject><subject>Organic soil</subject><subject>Organic soils</subject><subject>Plant Physiology</subject><subject>Plant Sciences</subject><subject>Plant species</subject><subject>Rainy season</subject><subject>Rainy seasons</subject><subject>Regular Article</subject><subject>Seasons</subject><subject>Soil microorganisms</subject><subject>Soil nutrients</subject><subject>Soil properties</subject><subject>Soil science</subject><subject>Soil Science & Conservation</subject><subject>Soil types</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. 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Soil science and plant productions</topic><topic>Animal, plant and microbial ecology</topic><topic>Biological and medical sciences</topic><topic>Biomedical and Life Sciences</topic><topic>Canopies</topic><topic>Canopy soil</topic><topic>Discriminant function analysis</topic><topic>Dry season</topic><topic>Dry seasons</topic><topic>Ecology</topic><topic>Flora</topic><topic>Forest canopy</topic><topic>Forest floor</topic><topic>Forest litter</topic><topic>Forest soils</topic><topic>Forests</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. 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In this study, we examined the influence of tree species and season on soil nutrient cycling processes in canopy soils of four tree species common to Costa Rican wet forests. We also compared the canopy soils to the associated forest floor mineral soils. Both tree species and season had strong effects on canopy soil nutrients and processes. Canopy soils from trees with high litter lignin concentrations had higher net N-mineralization rates and higher dissolved inorganic N concentrations than those with low lignin concentrations. During the dry season, net N-immobilization occurred and dissolved organic and inorganic N and available P concentrations were significantly higher than during the wet season. Overall, canopy soils had higher N levels and higher fungi + bacteria richness than forest floor mineral soils. The differences in canopy soil properties observed among tree species indicates that these species have distinct N cycles that reflect differences in both soil origin and biological controls.</abstract><cop>Dordrecht</cop><pub>Dordrecht : Springer Netherlands</pub><doi>10.1007/s11104-008-9816-9</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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| ispartof | Plant and soil, 2009-05, Vol.318 (1-2), p.47-61 |
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| source | Jstor Complete Legacy; SpringerLink Journals - AutoHoldings |
| subjects | Acid soils Agronomy. Soil science and plant productions Animal, plant and microbial ecology Biological and medical sciences Biomedical and Life Sciences Canopies Canopy soil Discriminant function analysis Dry season Dry seasons Ecology Flora Forest canopy Forest floor Forest litter Forest soils Forests Fundamental and applied biological sciences. Psychology General agronomy. Plant production Life Sciences Microclimate Mineral soils Mineralization Minerals Nutrient cycles Nutrient status Organic soil Organic soils Plant Physiology Plant Sciences Plant species Rainy season Rainy seasons Regular Article Seasons Soil microorganisms Soil nutrients Soil properties Soil science Soil Science & Conservation Soil types Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Soils Studies Trees Tropical forests tropical rain forests |
| title | influence of tree species on canopy soil nutrient status in a tropical lowland wet forest in Costa Rica |
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