Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile

Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbat...

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Veröffentlicht in:Plant and soil 1998-04, Vol.201 (2), p.251-258
Hauptverfasser: Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources), Johnson, A.H, Thomas, S.M
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Johnson, A.H
Thomas, S.M
description Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P > 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P < 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.
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(New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources) ; Johnson, A.H ; Thomas, S.M</creator><creatorcontrib>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources) ; Johnson, A.H ; Thomas, S.M</creatorcontrib><description>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P &gt; 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P &lt; 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1023/A:1004375920790</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Kluwer Academic Publishers</publisher><subject>Acid soils ; Agronomy. Soil science and plant productions ; Air pollution ; AZOTE ; Biological and medical sciences ; BOSQUE SUBALPINO ; CARBON ; CARBONE ; CARBONO ; Cations ; Chemical, physicochemical, biochemical and biological properties ; CHILE ; CHILI ; Coniferous forests ; CUPRESSACEAE ; DISPONIBILIDAD DE NUTRIENTES ; DISPONIBILITE D'ELEMENT NUTRITIF ; Ecosystem studies ; FERTILIDAD DEL SUELO ; FERTILITE DU SOL ; Forest ecosystems ; FOREST SOILS ; Forest watersheds ; FORET SUBALPINE ; Fundamental and applied biological sciences. Psychology ; MATERIA ORGANICA DEL SUELO ; MATIERE ORGANIQUE DU SOL ; Mineral components. Ionic and exchange properties ; Montane environments ; Montane forests ; Moorlands ; NITROGEN ; NITROGENO ; NUTRIENT AVAILABILITY ; Nutrient status ; Old growth ; Old growth forests ; Organic carbon ; Organic soils ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Regression analysis ; Soil density ; SOIL FERTILITY ; Soil nutrients ; SOIL ORGANIC MATTER ; Soil pollution ; Soil profiles ; Soil science ; SOL DE FORET ; SUBALPINE FORESTS ; SUELO FORESTAL ; Temperate forests ; Vegetation</subject><ispartof>Plant and soil, 1998-04, Vol.201 (2), p.251-258</ispartof><rights>1998 Kluwer Academic Publishers</rights><rights>1998 INIST-CNRS</rights><rights>Kluwer Academic Publishers 1998</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c330t-25425a499aa998bf6637c8c632368ad8b5246fa02654ebaae64e1007ff248c203</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42948326$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42948326$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=2370648$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Zarin, D.J. (New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</creatorcontrib><creatorcontrib>Johnson, A.H</creatorcontrib><creatorcontrib>Thomas, S.M</creatorcontrib><title>Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile</title><title>Plant and soil</title><description>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P &gt; 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). 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Soil science and plant productions</subject><subject>Air pollution</subject><subject>AZOTE</subject><subject>Biological and medical sciences</subject><subject>BOSQUE SUBALPINO</subject><subject>CARBON</subject><subject>CARBONE</subject><subject>CARBONO</subject><subject>Cations</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>CHILE</subject><subject>CHILI</subject><subject>Coniferous forests</subject><subject>CUPRESSACEAE</subject><subject>DISPONIBILIDAD DE NUTRIENTES</subject><subject>DISPONIBILITE D'ELEMENT NUTRITIF</subject><subject>Ecosystem studies</subject><subject>FERTILIDAD DEL SUELO</subject><subject>FERTILITE DU SOL</subject><subject>Forest ecosystems</subject><subject>FOREST SOILS</subject><subject>Forest watersheds</subject><subject>FORET SUBALPINE</subject><subject>Fundamental and applied biological sciences. 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(New Hampshire Univ., Durham, NH (USA). Dept. of Natural Resources)</au><au>Johnson, A.H</au><au>Thomas, S.M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile</atitle><jtitle>Plant and soil</jtitle><date>1998-04-01</date><risdate>1998</risdate><volume>201</volume><issue>2</issue><spage>251</spage><epage>258</epage><pages>251-258</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Montane temperate forests of the Cordillera de Piuchué Ecosystem Study, Isla Chiloé, Chile, are unaffected by air pollution, timber exploitation and agricultural clearing, and the current floristic assemblage has been relatively stable for the past 7500 years. The apparent absence of major perturbation at this location makes it an appropriate baseline site for ecosystem analysis. We measured soil bulk density, pH, soil organic C (SOC), total N, and NH₄Cl-exchangeable cations (Ca⁺², Mg⁺², K⁺, Na⁺, Al⁺³) in 0-10 and 10-40 cm depth samples from 72 soil profiles representing three vegetation zones: Fitzroya cupressoides Forest, Pilgerodendron uvifera-Tepualia stipularis Forest, and Magellanic Moorland. Fitzroya and Pilgerodendron-Tepualia Forests were indistinguishable for all measured soil characteristics (P &gt; 0.05, Dunn's multiple comparison test on ranked data); these included very high median SOC concentrations (0-10 cm = 49.6%) and correspondingly low bulk density values (0-10 cm = 0.07). Moorland soil median values (0-10 cm) were significantly higher for bulk density (0.12) and lower for SOC (28.5%), but not for total N (Forests = 0.99%, Moorland = 0.95%), resulting in lower median C: N ratios for the moorland (Forests = 44.7; Moorland = 30.3). Across both depths and all three vegetation zones regression analysis indicated that SOC was an excellent predictor (R²= 0.93, P &lt; 0.001) of ∑ (exchangeable Ca⁺² + Mg⁺² + K⁺ + Na⁺).Comparison with other old growth montane environments indicates that the Fitzroya and Pilgerodendron-Tepualia soil profiles are characterized by C:N ratios typical of other relatively unpolluted conifer forest soils (33.0-49.3). Soil profiles of representative polluted montane conifer forests have lower C:N ratios (16.2-23.5).Organic horizons from representative polluted montane conifer forests also retain fewer exchangeable base cations per unit SOC than are retained by organic horizons from the Cordillera de Piuchué forests.</abstract><cop>Dordrecht</cop><pub>Kluwer Academic Publishers</pub><doi>10.1023/A:1004375920790</doi><tpages>8</tpages></addata></record>
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source SpringerNature Journals; JSTOR Archive Collection A-Z Listing
subjects Acid soils
Agronomy. Soil science and plant productions
Air pollution
AZOTE
Biological and medical sciences
BOSQUE SUBALPINO
CARBON
CARBONE
CARBONO
Cations
Chemical, physicochemical, biochemical and biological properties
CHILE
CHILI
Coniferous forests
CUPRESSACEAE
DISPONIBILIDAD DE NUTRIENTES
DISPONIBILITE D'ELEMENT NUTRITIF
Ecosystem studies
FERTILIDAD DEL SUELO
FERTILITE DU SOL
Forest ecosystems
FOREST SOILS
Forest watersheds
FORET SUBALPINE
Fundamental and applied biological sciences. Psychology
MATERIA ORGANICA DEL SUELO
MATIERE ORGANIQUE DU SOL
Mineral components. Ionic and exchange properties
Montane environments
Montane forests
Moorlands
NITROGEN
NITROGENO
NUTRIENT AVAILABILITY
Nutrient status
Old growth
Old growth forests
Organic carbon
Organic soils
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Regression analysis
Soil density
SOIL FERTILITY
Soil nutrients
SOIL ORGANIC MATTER
Soil pollution
Soil profiles
Soil science
SOL DE FORET
SUBALPINE FORESTS
SUELO FORESTAL
Temperate forests
Vegetation
title Soil organic carbon and nutrient status in old-growth montane coniferous forest watersheds, Isla Chiloe, Chile
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