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Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material
Sustainable forest management requires understanding of ecosystem phosphorus (P) cycling. Lang et al. (2017) [Biogeochemistry, https://doi.org/10.1007/s10533-017-0375-0] introduced the concept of P-acquiring vs. P-recycling nutrition strategies for European beech (Fagus sylvatica L.) forests on sili...
Autores principales: | , , , , , , , , , , , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer International Publishing
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8860963/ https://www.ncbi.nlm.nih.gov/pubmed/35221401 http://dx.doi.org/10.1007/s10533-021-00884-7 |
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author | Prietzel, Jörg Krüger, Jaane Kaiser, Klaus Amelung, Wulf Bauke, Sara L. Dippold, Michaela A. Kandeler, Ellen Klysubun, Wantana Lewandowski, Hans Löppmann, Sebastian Luster, Jörg Marhan, Sven Puhlmann, Heike Schmitt, Marius Siegenthaler, Maja B. Siemens, Jan Spielvogel, Sandra Willbold, Sabine Wolff, Jan Lang, Friederike |
author_facet | Prietzel, Jörg Krüger, Jaane Kaiser, Klaus Amelung, Wulf Bauke, Sara L. Dippold, Michaela A. Kandeler, Ellen Klysubun, Wantana Lewandowski, Hans Löppmann, Sebastian Luster, Jörg Marhan, Sven Puhlmann, Heike Schmitt, Marius Siegenthaler, Maja B. Siemens, Jan Spielvogel, Sandra Willbold, Sabine Wolff, Jan Lang, Friederike |
author_sort | Prietzel, Jörg |
collection | PubMed |
description | Sustainable forest management requires understanding of ecosystem phosphorus (P) cycling. Lang et al. (2017) [Biogeochemistry, https://doi.org/10.1007/s10533-017-0375-0] introduced the concept of P-acquiring vs. P-recycling nutrition strategies for European beech (Fagus sylvatica L.) forests on silicate parent material, and demonstrated a change from P-acquiring to P-recycling nutrition from P-rich to P-poor sites. The present study extends this silicate rock-based assessment to forest sites with soils formed from carbonate bedrock. For all sites, it presents a large set of general soil and bedrock chemistry data. It thoroughly describes the soil P status and generates a comprehensive concept on forest ecosystem P nutrition covering the majority of Central European forest soils. For this purpose, an Ecosystem P Nutrition Index (ENI(P)) was developed, which enabled the comparison of forest P nutrition strategies at the carbonate sites in our study among each other and also with those of the silicate sites investigated by Lang et al. (2017). The P status of forest soils on carbonate substrates was characterized by low soil P stocks and a large fraction of organic Ca-bound P (probably largely Ca phytate) during early stages of pedogenesis. Soil P stocks, particularly those in the mineral soil and of inorganic P forms, including Al- and Fe-bound P, became more abundant with progressing pedogenesis and accumulation of carbonate rock dissolution residue. Phosphorus-rich impure, silicate-enriched carbonate bedrock promoted the accumulation of dissolution residue and supported larger soil P stocks, mainly bound to Fe and Al minerals. In carbonate-derived soils, only low P amounts were bioavailable during early stages of pedogenesis, and, similar to P-poor silicate sites, P nutrition of beech forests depended on tight (re)cycling of P bound in forest floor soil organic matter (SOM). In contrast to P-poor silicate sites, where the ecosystem P nutrition strategy is direct biotic recycling of SOM-bound organic P, recycling during early stages of pedogenesis on carbonate substrates also involves the dissolution of stable Ca-P(org) precipitates formed from phosphate released during SOM decomposition. In contrast to silicate sites, progressing pedogenesis and accumulation of P-enriched carbonate bedrock dissolution residue at the carbonate sites promote again P-acquiring mechanisms for ecosystem P nutrition. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10533-021-00884-7. |
format | Online Article Text |
id | pubmed-8860963 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Springer International Publishing |
record_format | MEDLINE/PubMed |
spelling | pubmed-88609632022-02-23 Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material Prietzel, Jörg Krüger, Jaane Kaiser, Klaus Amelung, Wulf Bauke, Sara L. Dippold, Michaela A. Kandeler, Ellen Klysubun, Wantana Lewandowski, Hans Löppmann, Sebastian Luster, Jörg Marhan, Sven Puhlmann, Heike Schmitt, Marius Siegenthaler, Maja B. Siemens, Jan Spielvogel, Sandra Willbold, Sabine Wolff, Jan Lang, Friederike Biogeochemistry Article Sustainable forest management requires understanding of ecosystem phosphorus (P) cycling. Lang et al. (2017) [Biogeochemistry, https://doi.org/10.1007/s10533-017-0375-0] introduced the concept of P-acquiring vs. P-recycling nutrition strategies for European beech (Fagus sylvatica L.) forests on silicate parent material, and demonstrated a change from P-acquiring to P-recycling nutrition from P-rich to P-poor sites. The present study extends this silicate rock-based assessment to forest sites with soils formed from carbonate bedrock. For all sites, it presents a large set of general soil and bedrock chemistry data. It thoroughly describes the soil P status and generates a comprehensive concept on forest ecosystem P nutrition covering the majority of Central European forest soils. For this purpose, an Ecosystem P Nutrition Index (ENI(P)) was developed, which enabled the comparison of forest P nutrition strategies at the carbonate sites in our study among each other and also with those of the silicate sites investigated by Lang et al. (2017). The P status of forest soils on carbonate substrates was characterized by low soil P stocks and a large fraction of organic Ca-bound P (probably largely Ca phytate) during early stages of pedogenesis. Soil P stocks, particularly those in the mineral soil and of inorganic P forms, including Al- and Fe-bound P, became more abundant with progressing pedogenesis and accumulation of carbonate rock dissolution residue. Phosphorus-rich impure, silicate-enriched carbonate bedrock promoted the accumulation of dissolution residue and supported larger soil P stocks, mainly bound to Fe and Al minerals. In carbonate-derived soils, only low P amounts were bioavailable during early stages of pedogenesis, and, similar to P-poor silicate sites, P nutrition of beech forests depended on tight (re)cycling of P bound in forest floor soil organic matter (SOM). In contrast to P-poor silicate sites, where the ecosystem P nutrition strategy is direct biotic recycling of SOM-bound organic P, recycling during early stages of pedogenesis on carbonate substrates also involves the dissolution of stable Ca-P(org) precipitates formed from phosphate released during SOM decomposition. In contrast to silicate sites, progressing pedogenesis and accumulation of P-enriched carbonate bedrock dissolution residue at the carbonate sites promote again P-acquiring mechanisms for ecosystem P nutrition. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10533-021-00884-7. Springer International Publishing 2022-02-02 2022 /pmc/articles/PMC8860963/ /pubmed/35221401 http://dx.doi.org/10.1007/s10533-021-00884-7 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Prietzel, Jörg Krüger, Jaane Kaiser, Klaus Amelung, Wulf Bauke, Sara L. Dippold, Michaela A. Kandeler, Ellen Klysubun, Wantana Lewandowski, Hans Löppmann, Sebastian Luster, Jörg Marhan, Sven Puhlmann, Heike Schmitt, Marius Siegenthaler, Maja B. Siemens, Jan Spielvogel, Sandra Willbold, Sabine Wolff, Jan Lang, Friederike Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title | Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title_full | Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title_fullStr | Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title_full_unstemmed | Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title_short | Soil phosphorus status and P nutrition strategies of European beech forests on carbonate compared to silicate parent material |
title_sort | soil phosphorus status and p nutrition strategies of european beech forests on carbonate compared to silicate parent material |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8860963/ https://www.ncbi.nlm.nih.gov/pubmed/35221401 http://dx.doi.org/10.1007/s10533-021-00884-7 |
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