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Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape

Phosphorus (P) is an important macronutrient in arctic and subarctic tundra and its bioavailability is regulated by the mineralization of organic P. Temperature is likely to be an important control on P bioavailability, although effects may differ across contrasting plant communities with different...

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Autores principales: Vincent, Andrea G., Sundqvist, Maja K., Wardle, David A., Giesler, Reiner
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3968050/
https://www.ncbi.nlm.nih.gov/pubmed/24676035
http://dx.doi.org/10.1371/journal.pone.0092942
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author Vincent, Andrea G.
Sundqvist, Maja K.
Wardle, David A.
Giesler, Reiner
author_facet Vincent, Andrea G.
Sundqvist, Maja K.
Wardle, David A.
Giesler, Reiner
author_sort Vincent, Andrea G.
collection PubMed
description Phosphorus (P) is an important macronutrient in arctic and subarctic tundra and its bioavailability is regulated by the mineralization of organic P. Temperature is likely to be an important control on P bioavailability, although effects may differ across contrasting plant communities with different soil properties. We used an elevational gradient in northern Sweden that included both heath and meadow vegetation types at all elevations to study the effects of temperature, soil P sorption capacity and oxalate-extractable aluminium (Al(ox)) and iron (Fe(ox)) on the concentration of different soil P fractions. We hypothesized that the concentration of labile P fractions would decrease with increasing elevation (and thus declining temperature), but would be lower in meadow than in heath, given that N to P ratios in meadow foliage are higher. As expected, labile P in the form of Resin-P declined sharply with elevation for both vegetation types. Meadow soils did not have lower concentrations of Resin-P than heath soils, but they did have 2–fold and 1.5–fold higher concentrations of NaOH-extractable organic P and Residual P, respectively. Further, meadow soils had 3-fold higher concentrations of Al(ox) + Fe(ox) and a 20% higher P sorption index than did heath soils. Additionally, Resin-P expressed as a proportion of total soil P for the meadow was on average half that in the heath. Declining Resin-P concentrations with elevation were best explained by an associated 2.5–3.0°C decline in temperature. In contrast, the lower P availability in meadow relative to heath soils may be associated with impaired organic P mineralization, as indicated by a higher accumulation of organic P and P sorption capacity. Our results indicate that predicted temperature increases in the arctic over the next century may influence P availability and biogeochemistry, with consequences for key ecosystem processes limited by P, such as primary productivity.
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spelling pubmed-39680502014-04-01 Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape Vincent, Andrea G. Sundqvist, Maja K. Wardle, David A. Giesler, Reiner PLoS One Research Article Phosphorus (P) is an important macronutrient in arctic and subarctic tundra and its bioavailability is regulated by the mineralization of organic P. Temperature is likely to be an important control on P bioavailability, although effects may differ across contrasting plant communities with different soil properties. We used an elevational gradient in northern Sweden that included both heath and meadow vegetation types at all elevations to study the effects of temperature, soil P sorption capacity and oxalate-extractable aluminium (Al(ox)) and iron (Fe(ox)) on the concentration of different soil P fractions. We hypothesized that the concentration of labile P fractions would decrease with increasing elevation (and thus declining temperature), but would be lower in meadow than in heath, given that N to P ratios in meadow foliage are higher. As expected, labile P in the form of Resin-P declined sharply with elevation for both vegetation types. Meadow soils did not have lower concentrations of Resin-P than heath soils, but they did have 2–fold and 1.5–fold higher concentrations of NaOH-extractable organic P and Residual P, respectively. Further, meadow soils had 3-fold higher concentrations of Al(ox) + Fe(ox) and a 20% higher P sorption index than did heath soils. Additionally, Resin-P expressed as a proportion of total soil P for the meadow was on average half that in the heath. Declining Resin-P concentrations with elevation were best explained by an associated 2.5–3.0°C decline in temperature. In contrast, the lower P availability in meadow relative to heath soils may be associated with impaired organic P mineralization, as indicated by a higher accumulation of organic P and P sorption capacity. Our results indicate that predicted temperature increases in the arctic over the next century may influence P availability and biogeochemistry, with consequences for key ecosystem processes limited by P, such as primary productivity. Public Library of Science 2014-03-27 /pmc/articles/PMC3968050/ /pubmed/24676035 http://dx.doi.org/10.1371/journal.pone.0092942 Text en © 2014 Vincent et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Vincent, Andrea G.
Sundqvist, Maja K.
Wardle, David A.
Giesler, Reiner
Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title_full Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title_fullStr Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title_full_unstemmed Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title_short Bioavailable Soil Phosphorus Decreases with Increasing Elevation in a Subarctic Tundra Landscape
title_sort bioavailable soil phosphorus decreases with increasing elevation in a subarctic tundra landscape
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3968050/
https://www.ncbi.nlm.nih.gov/pubmed/24676035
http://dx.doi.org/10.1371/journal.pone.0092942
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