N and P in New Zealand Soil Chronosequences and Relationships with Foliar N and P
The growth of forest species in soil development chronosequences becomes increasingly phosphorus (P)-limited with time, as P is weathered, eroded and leached from soil. Foliar nitrogen (N) concentrations also tend to decrease with soil age when vegetation may be limited in both N and P. Here we repo...
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description | The growth of forest species in soil development chronosequences becomes increasingly phosphorus (P)-limited with time, as P is weathered, eroded and leached from soil. Foliar nitrogen (N) concentrations also tend to decrease with soil age when vegetation may be limited in both N and P. Here we report on soil development in temperate rain forests along three New Zealand chronosequences that have minimal pollution and disturbance from human activities, at Franz Josef, Waitutu and Central Volcanic Plateau, and on factors influencing soil net N mineralization (aerobic; 56 days) and foliar N and P concentrations. Except in very young soils (< 500 years), at least 85% of total-P in mineral soil (0-10 cm) was transformed to organic-P. In each chronosequence, total-P declined with time, and foliar N:P ratios (mass) generally increased from 8 to 15-18, suggesting P was more limiting than N in the oldest soils of the chronosequence. There was a negative relationship between net N mineralization and C:N ratio for mineral soil. For the FH (organic) layer, net N mineralization had the strongest relationships with total-N concentration (positively) and C:organic-P ratio (negatively); however, relationships varied with forest group, suggesting that other factors were also important. Foliar P of kamahi (Weinmannia racemosa Linn. f.), a dominant canopy species, was related to soil organic-P, suggesting mineralization was an important process for tree nutrition. Foliar N was positively related to N concentration in the FH layer, but was not significantly related to any measured property in mineral soil, possibly because of the wide range of soils. The consistent declines in both soil and foliar P across the contrasting chronosequences strongly suggest that vegetation becomes progressively P-limited during long-term ecosystem development. |
doi_str_mv | 10.1007/s10533-004-7790-8 |
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L. ; Ross, D. J. ; Coomes, D. A. ; Richardson, S. J. ; Smale, M. C. ; Dahlgren, R. A.</creator><creatorcontrib>Parfitt, R. L. ; Ross, D. J. ; Coomes, D. A. ; Richardson, S. J. ; Smale, M. C. ; Dahlgren, R. A.</creatorcontrib><description>The growth of forest species in soil development chronosequences becomes increasingly phosphorus (P)-limited with time, as P is weathered, eroded and leached from soil. Foliar nitrogen (N) concentrations also tend to decrease with soil age when vegetation may be limited in both N and P. Here we report on soil development in temperate rain forests along three New Zealand chronosequences that have minimal pollution and disturbance from human activities, at Franz Josef, Waitutu and Central Volcanic Plateau, and on factors influencing soil net N mineralization (aerobic; 56 days) and foliar N and P concentrations. Except in very young soils (&lt 500 years), at least 85% of total-P in mineral soil (0-10 cm) was transformed to organic-P. In each chronosequence, total-P declined with time, and foliar N:P ratios (mass) generally increased from 8 to 15-18, suggesting P was more limiting than N in the oldest soils of the chronosequence. There was a negative relationship between net N mineralization and C:N ratio for mineral soil. For the FH (organic) layer, net N mineralization had the strongest relationships with total-N concentration (positively) and C:organic-P ratio (negatively); however, relationships varied with forest group, suggesting that other factors were also important. Foliar P of kamahi (Weinmannia racemosa Linn. f.), a dominant canopy species, was related to soil organic-P, suggesting mineralization was an important process for tree nutrition. Foliar N was positively related to N concentration in the FH layer, but was not significantly related to any measured property in mineral soil, possibly because of the wide range of soils. The consistent declines in both soil and foliar P across the contrasting chronosequences strongly suggest that vegetation becomes progressively P-limited during long-term ecosystem development.</description><identifier>ISSN: 0168-2563</identifier><identifier>EISSN: 1573-515X</identifier><identifier>DOI: 10.1007/s10533-004-7790-8</identifier><identifier>CODEN: BIOGEP</identifier><language>eng</language><publisher>Heidelberg: Springer</publisher><subject>Alluvial soils ; Animal and plant ecology ; Animal, plant and microbial ecology ; Biological and medical sciences ; Chronosequences ; Earth sciences ; Earth, ocean, space ; Ecological succession ; Exact sciences and technology ; Forest soils ; Fundamental and applied biological sciences. 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Here we report on soil development in temperate rain forests along three New Zealand chronosequences that have minimal pollution and disturbance from human activities, at Franz Josef, Waitutu and Central Volcanic Plateau, and on factors influencing soil net N mineralization (aerobic; 56 days) and foliar N and P concentrations. Except in very young soils (&lt 500 years), at least 85% of total-P in mineral soil (0-10 cm) was transformed to organic-P. In each chronosequence, total-P declined with time, and foliar N:P ratios (mass) generally increased from 8 to 15-18, suggesting P was more limiting than N in the oldest soils of the chronosequence. There was a negative relationship between net N mineralization and C:N ratio for mineral soil. For the FH (organic) layer, net N mineralization had the strongest relationships with total-N concentration (positively) and C:organic-P ratio (negatively); however, relationships varied with forest group, suggesting that other factors were also important. Foliar P of kamahi (Weinmannia racemosa Linn. f.), a dominant canopy species, was related to soil organic-P, suggesting mineralization was an important process for tree nutrition. Foliar N was positively related to N concentration in the FH layer, but was not significantly related to any measured property in mineral soil, possibly because of the wide range of soils. The consistent declines in both soil and foliar P across the contrasting chronosequences strongly suggest that vegetation becomes progressively P-limited during long-term ecosystem development.</description><subject>Alluvial soils</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Chronosequences</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Ecological succession</subject><subject>Exact sciences and technology</subject><subject>Forest soils</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Geochemistry</subject><subject>Mineral soils</subject><subject>Mineralization</subject><subject>Nitrogen</subject><subject>Old growth forests</subject><subject>Organic soils</subject><subject>Rainforests</subject><subject>Soil and rock geochemistry</subject><subject>Soil ecology</subject><subject>Soil plant interactions</subject><subject>Soils</subject><subject>Surficial geology</subject><subject>Synecology</subject><subject>Temperate rain forests</subject><subject>Terrestrial ecosystems</subject><subject>Vegetation</subject><subject>Volcanic soils</subject><subject>Weinmannia</subject><issn>0168-2563</issn><issn>1573-515X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpdkU9LAzEQxYMoWKsfwIMQBL2tTjbJZnOUYlUo9T-IlxCzCU3Zbmqypfjt3bVFwdPAzO89Hm8QOiZwQQDEZSLAKc0AWCaEhKzcQQPCBc044W-7aACkKLOcF3QfHaQ0BwApgA7Q4xTrpsIP2Dd4atf43eq6XzwHX-PRLIYmJPu5so2x6Yd8srVufWjSzC8TXvt2hseh9jrirdMh2nO6TvZoO4fodXz9MrrNJvc3d6OrSWYo521mhCsqAjkTwjFdGGGrUhgjS8EYF5WTheWO6FxTYyg4RkomnKxYYT-MJGVFh-h847uMoQuYWrXwydi6i2_DKqmcEMJZUXbg6T9wHlax6bIpwbrygNEeIhvIxJBStE4to1_o-KUIqL5htWlYdbjqG1a95mxrrJPRtYu6MT79CUUuc0mg40423Dy1If7ecwDO8-4L33UHgwI</recordid><startdate>20050801</startdate><enddate>20050801</enddate><creator>Parfitt, R. 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L.</au><au>Ross, D. J.</au><au>Coomes, D. A.</au><au>Richardson, S. J.</au><au>Smale, M. C.</au><au>Dahlgren, R. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>N and P in New Zealand Soil Chronosequences and Relationships with Foliar N and P</atitle><jtitle>Biogeochemistry</jtitle><date>2005-08-01</date><risdate>2005</risdate><volume>75</volume><issue>2</issue><spage>305</spage><epage>328</epage><pages>305-328</pages><issn>0168-2563</issn><eissn>1573-515X</eissn><coden>BIOGEP</coden><abstract>The growth of forest species in soil development chronosequences becomes increasingly phosphorus (P)-limited with time, as P is weathered, eroded and leached from soil. Foliar nitrogen (N) concentrations also tend to decrease with soil age when vegetation may be limited in both N and P. Here we report on soil development in temperate rain forests along three New Zealand chronosequences that have minimal pollution and disturbance from human activities, at Franz Josef, Waitutu and Central Volcanic Plateau, and on factors influencing soil net N mineralization (aerobic; 56 days) and foliar N and P concentrations. Except in very young soils (&lt 500 years), at least 85% of total-P in mineral soil (0-10 cm) was transformed to organic-P. In each chronosequence, total-P declined with time, and foliar N:P ratios (mass) generally increased from 8 to 15-18, suggesting P was more limiting than N in the oldest soils of the chronosequence. There was a negative relationship between net N mineralization and C:N ratio for mineral soil. For the FH (organic) layer, net N mineralization had the strongest relationships with total-N concentration (positively) and C:organic-P ratio (negatively); however, relationships varied with forest group, suggesting that other factors were also important. Foliar P of kamahi (Weinmannia racemosa Linn. f.), a dominant canopy species, was related to soil organic-P, suggesting mineralization was an important process for tree nutrition. Foliar N was positively related to N concentration in the FH layer, but was not significantly related to any measured property in mineral soil, possibly because of the wide range of soils. The consistent declines in both soil and foliar P across the contrasting chronosequences strongly suggest that vegetation becomes progressively P-limited during long-term ecosystem development.</abstract><cop>Heidelberg</cop><pub>Springer</pub><doi>10.1007/s10533-004-7790-8</doi><tpages>24</tpages></addata></record> |
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subjects | Alluvial soils Animal and plant ecology Animal, plant and microbial ecology Biological and medical sciences Chronosequences Earth sciences Earth, ocean, space Ecological succession Exact sciences and technology Forest soils Fundamental and applied biological sciences. Psychology Geochemistry Mineral soils Mineralization Nitrogen Old growth forests Organic soils Rainforests Soil and rock geochemistry Soil ecology Soil plant interactions Soils Surficial geology Synecology Temperate rain forests Terrestrial ecosystems Vegetation Volcanic soils Weinmannia |
title | N and P in New Zealand Soil Chronosequences and Relationships with Foliar N and P |
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