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Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis
Soil organic carbon (SOC) dynamics after slash-burn agriculture are poorly understood in African tropical forest, though recent studies have revealed C4 grass invasion as a forest understory influences SOC dynamics after deforestation. This study aimed to quantify the relative SOC contribution of C4...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6614393/ https://www.ncbi.nlm.nih.gov/pubmed/31285565 http://dx.doi.org/10.1038/s41598-019-46406-2 |
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author | Sugihara, Soh Shibata, Makoto Mvondo Ze, Antoine D. Tanaka, Haruo Kosaki, Takashi Funakawa, Shinya |
author_facet | Sugihara, Soh Shibata, Makoto Mvondo Ze, Antoine D. Tanaka, Haruo Kosaki, Takashi Funakawa, Shinya |
author_sort | Sugihara, Soh |
collection | PubMed |
description | Soil organic carbon (SOC) dynamics after slash-burn agriculture are poorly understood in African tropical forest, though recent studies have revealed C4 grass invasion as a forest understory influences SOC dynamics after deforestation. This study aimed to quantify the relative SOC contribution of C4 and C3 plants separately through the sequential fallow periods of forest (cropland, or 4–7, 20–30, or >50 years of fallow forest) in the tropical forest of eastern Cameroon. We evaluated the SOC stock and natural (13)C abundance for each layer. The SOC stock was largest in 4–7 years fallow forest (136.6 ± 8.8 Mg C ha(−1); 100 cm depth, and C4:C3 = 58:42), and decreased with increasing fallow period. SOC from C4 plants was larger in the 4–7 and 20–30 years fallow forests (57.2–60.4 ± 5.8 Mg C ha(−1); 100 cm depth), while it clearly decreased in >50 years fallow forest (35.0 ± 4.1 Mg C ha(−1); 100 cm depth), resulting in the smallest SOC in this mature forest (106.4 ± 12.9 Mg C ha(−1); 100 cm depth). These findings indicate that C4 grass understories contributed to the SOC restoration during early fallow succession in the tropical forest of eastern Cameroon. |
format | Online Article Text |
id | pubmed-6614393 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-66143932019-07-17 Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis Sugihara, Soh Shibata, Makoto Mvondo Ze, Antoine D. Tanaka, Haruo Kosaki, Takashi Funakawa, Shinya Sci Rep Article Soil organic carbon (SOC) dynamics after slash-burn agriculture are poorly understood in African tropical forest, though recent studies have revealed C4 grass invasion as a forest understory influences SOC dynamics after deforestation. This study aimed to quantify the relative SOC contribution of C4 and C3 plants separately through the sequential fallow periods of forest (cropland, or 4–7, 20–30, or >50 years of fallow forest) in the tropical forest of eastern Cameroon. We evaluated the SOC stock and natural (13)C abundance for each layer. The SOC stock was largest in 4–7 years fallow forest (136.6 ± 8.8 Mg C ha(−1); 100 cm depth, and C4:C3 = 58:42), and decreased with increasing fallow period. SOC from C4 plants was larger in the 4–7 and 20–30 years fallow forests (57.2–60.4 ± 5.8 Mg C ha(−1); 100 cm depth), while it clearly decreased in >50 years fallow forest (35.0 ± 4.1 Mg C ha(−1); 100 cm depth), resulting in the smallest SOC in this mature forest (106.4 ± 12.9 Mg C ha(−1); 100 cm depth). These findings indicate that C4 grass understories contributed to the SOC restoration during early fallow succession in the tropical forest of eastern Cameroon. Nature Publishing Group UK 2019-07-08 /pmc/articles/PMC6614393/ /pubmed/31285565 http://dx.doi.org/10.1038/s41598-019-46406-2 Text en © The Author(s) 2019 Open Access This 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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Sugihara, Soh Shibata, Makoto Mvondo Ze, Antoine D. Tanaka, Haruo Kosaki, Takashi Funakawa, Shinya Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title | Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title_full | Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title_fullStr | Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title_full_unstemmed | Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title_short | Forest understories controlled the soil organic carbon stock during the fallow period in African tropical forest: a (13)C analysis |
title_sort | forest understories controlled the soil organic carbon stock during the fallow period in african tropical forest: a (13)c analysis |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6614393/ https://www.ncbi.nlm.nih.gov/pubmed/31285565 http://dx.doi.org/10.1038/s41598-019-46406-2 |
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