Articles | Volume 12, issue 8
https://doi.org/10.5194/bg-12-2471-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-2471-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Apr 2015
Research article |
| 29 Apr 2015
Large fluxes and rapid turnover of mineral-associated carbon across topographic gradients in a humid tropical forest: insights from paired 14C analysis
S. J Hall
Department of Environmental Science, Policy, and Management, University of California-Berkeley, Berkeley, USA
now at: Global Change and Sustainability Center, University of Utah, Salt Lake City, USA
G. McNicol
Department of Environmental Science, Policy, and Management, University of California-Berkeley, Berkeley, USA
T. Natake
Department of Environmental Science, Policy, and Management, University of California-Berkeley, Berkeley, USA
W. L. Silver
Department of Environmental Science, Policy, and Management, University of California-Berkeley, Berkeley, USA
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Cited
34 citations as recorded by crossref.
- From pools to flow: The PROMISE framework for new insights on soil carbon cycling in a changing world B. Waring et al. 10.1111/gcb.15365
- Development of energetic and enzymatic limitations on microbial carbon cycling in soils H. Naughton et al. 10.1007/s10533-021-00781-z
- Reductive release of Fe mineral-associated organic matter accelerated by oxalic acid Y. Ding et al. 10.1016/j.scitotenv.2020.142937
- Conceptualizing soil organic matter into particulate and mineral‐associated forms to address global change in the 21st century J. Lavallee et al. 10.1111/gcb.14859
- Carbon Sequestration Potential Promoted by Oxalate Extractable Iron Oxides through Organic Fertilization X. Huang et al. 10.2136/sssaj2017.02.0068
- Temperature response of permafrost soil carbon is attenuated by mineral protection N. Gentsch et al. 10.1111/gcb.14316
- Decadal-scale litter manipulation alters the biochemical and physical character of tropical forest soil carbon D. Cusack et al. 10.1016/j.soilbio.2018.06.005
- Nutrient limitation of soil microbial processes in tropical forests T. Camenzind et al. 10.1002/ecm.1279
- Small altitudinal change and rhizosphere affect the SOM light fractions but not the heavy fraction in European beech forest soil M. De Feudis et al. 10.1016/j.catena.2019.104091
- Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw F. Liu et al. 10.1038/s41467-022-32681-7
- Elevated moisture stimulates carbon loss from mineral soils by releasing protected organic matter W. Huang & S. Hall 10.1038/s41467-017-01998-z
- Where and Why Do Particulate Organic Matter (Pom) and Mineral-Associated Organic Matter (Maom) Differ Among Diverse Soils? W. Yu et al. 10.2139/ssrn.4062834
- Straw type and returning amount affects SOC fractions and Fe/Al oxides in a rice-wheat rotation system L. Dong et al. 10.1016/j.apsoil.2022.104736
- The C:N:P:S stoichiometry of soil organic matter E. Tipping et al. 10.1007/s10533-016-0247-z
- An optical method for carbon dioxide isotopes and mole fractions in small gas samples: Tracing microbial respiration from soil, litter, and lignin S. Hall et al. 10.1002/rcm.7973
- Where and why do particulate organic matter (POM) and mineral-associated organic matter (MAOM) differ among diverse soils? W. Yu et al. 10.1016/j.soilbio.2022.108756
- The Millennial model: in search of measurable pools and transformations for modeling soil carbon in the new century R. Abramoff et al. 10.1007/s10533-017-0409-7
- Distinct storage mechanisms of soil organic carbon in coniferous forest and evergreen broadleaf forest in tropical China F. Su et al. 10.1016/j.jenvman.2021.113142
- Short organic carbon turnover time and narrow 14C age spectra in early Holocene wetland paleosols L. Vetter et al. 10.1002/2016GC006526
- Impacts of Lithology and Slope Position on Arbuscular Mycorrhizal Fungi Communities in a Karst Forest Soil J. Zhao et al. 10.3390/jof9121133
- The downhill positions exhibit higher microbial network complexity and ecosystem multifunctionality compared to the upper slopes D. Xiao et al. 10.1016/j.foreco.2024.121744
- Order from disorder: do soil organic matter composition and turnover co-vary with iron phase crystallinity? S. Hall et al. 10.1007/s10533-018-0476-4
- Variation of soil carbon accumulation across a topographic gradient in a humid subtropical mountain forest Q. Tian et al. 10.1007/s10533-020-00679-2
- Reconciling multiple impacts of nitrogen enrichment on soil carbon: plant, microbial and geochemical controls C. Ye et al. 10.1111/ele.13083
- Beyond bulk: Density fractions explain heterogeneity in global soil carbon abundance and persistence K. Heckman et al. 10.1111/gcb.16023
- Simulating measurable ecosystem carbon and nitrogen dynamics with the mechanistically defined MEMS 2.0 model Y. Zhang et al. 10.5194/bg-18-3147-2021
- Iron addition to soil specifically stabilized lignin S. Hall et al. 10.1016/j.soilbio.2016.04.010
- Modeling the Effects of Global Change on Ecosystem Processes in a Tropical Rainforest A. Russell & W. Parton 10.3390/f11020213
- Mineral and Climatic Controls Over Soil Organic Matter Stability Across the Tibetan Alpine Permafrost Region K. Fang et al. 10.1029/2021GB007118
- Increased interactions between iron oxides and organic carbon under acid deposition drive large increases in soil organic carbon in a tropical forest in southern China J. Chen et al. 10.1007/s10533-022-00897-w
- Predicting Gross Nitrogen Mineralization and Potentially Mineralizable Nitrogen using Soil Organic Matter Properties W. Osterholz et al. 10.2136/sssaj2017.02.0055
- Persistent soil carbon enhanced in Mollisols by well-managed grasslands but not annual grain or dairy forage cropping systems Y. Rui et al. 10.1073/pnas.2118931119
- Reducing conditions, reactive metals, and their interactions can explain spatial patterns of surface soil carbon in a humid tropical forest S. Hall & W. Silver 10.1007/s10533-015-0120-5
- Stable and radioactive carbon in forest soils of Chhattisgarh, Central India: Implications for tropical soil carbon dynamics and stable carbon isotope evolution A. Laskar et al. 10.1016/j.jseaes.2016.03.021
32 citations as recorded by crossref.
- From pools to flow: The PROMISE framework for new insights on soil carbon cycling in a changing world B. Waring et al. 10.1111/gcb.15365
- Development of energetic and enzymatic limitations on microbial carbon cycling in soils H. Naughton et al. 10.1007/s10533-021-00781-z
- Reductive release of Fe mineral-associated organic matter accelerated by oxalic acid Y. Ding et al. 10.1016/j.scitotenv.2020.142937
- Conceptualizing soil organic matter into particulate and mineral‐associated forms to address global change in the 21st century J. Lavallee et al. 10.1111/gcb.14859
- Carbon Sequestration Potential Promoted by Oxalate Extractable Iron Oxides through Organic Fertilization X. Huang et al. 10.2136/sssaj2017.02.0068
- Temperature response of permafrost soil carbon is attenuated by mineral protection N. Gentsch et al. 10.1111/gcb.14316
- Decadal-scale litter manipulation alters the biochemical and physical character of tropical forest soil carbon D. Cusack et al. 10.1016/j.soilbio.2018.06.005
- Nutrient limitation of soil microbial processes in tropical forests T. Camenzind et al. 10.1002/ecm.1279
- Small altitudinal change and rhizosphere affect the SOM light fractions but not the heavy fraction in European beech forest soil M. De Feudis et al. 10.1016/j.catena.2019.104091
- Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw F. Liu et al. 10.1038/s41467-022-32681-7
- Elevated moisture stimulates carbon loss from mineral soils by releasing protected organic matter W. Huang & S. Hall 10.1038/s41467-017-01998-z
- Where and Why Do Particulate Organic Matter (Pom) and Mineral-Associated Organic Matter (Maom) Differ Among Diverse Soils? W. Yu et al. 10.2139/ssrn.4062834
- Straw type and returning amount affects SOC fractions and Fe/Al oxides in a rice-wheat rotation system L. Dong et al. 10.1016/j.apsoil.2022.104736
- The C:N:P:S stoichiometry of soil organic matter E. Tipping et al. 10.1007/s10533-016-0247-z
- An optical method for carbon dioxide isotopes and mole fractions in small gas samples: Tracing microbial respiration from soil, litter, and lignin S. Hall et al. 10.1002/rcm.7973
- Where and why do particulate organic matter (POM) and mineral-associated organic matter (MAOM) differ among diverse soils? W. Yu et al. 10.1016/j.soilbio.2022.108756
- The Millennial model: in search of measurable pools and transformations for modeling soil carbon in the new century R. Abramoff et al. 10.1007/s10533-017-0409-7
- Distinct storage mechanisms of soil organic carbon in coniferous forest and evergreen broadleaf forest in tropical China F. Su et al. 10.1016/j.jenvman.2021.113142
- Short organic carbon turnover time and narrow 14C age spectra in early Holocene wetland paleosols L. Vetter et al. 10.1002/2016GC006526
- Impacts of Lithology and Slope Position on Arbuscular Mycorrhizal Fungi Communities in a Karst Forest Soil J. Zhao et al. 10.3390/jof9121133
- The downhill positions exhibit higher microbial network complexity and ecosystem multifunctionality compared to the upper slopes D. Xiao et al. 10.1016/j.foreco.2024.121744
- Order from disorder: do soil organic matter composition and turnover co-vary with iron phase crystallinity? S. Hall et al. 10.1007/s10533-018-0476-4
- Variation of soil carbon accumulation across a topographic gradient in a humid subtropical mountain forest Q. Tian et al. 10.1007/s10533-020-00679-2
- Reconciling multiple impacts of nitrogen enrichment on soil carbon: plant, microbial and geochemical controls C. Ye et al. 10.1111/ele.13083
- Beyond bulk: Density fractions explain heterogeneity in global soil carbon abundance and persistence K. Heckman et al. 10.1111/gcb.16023
- Simulating measurable ecosystem carbon and nitrogen dynamics with the mechanistically defined MEMS 2.0 model Y. Zhang et al. 10.5194/bg-18-3147-2021
- Iron addition to soil specifically stabilized lignin S. Hall et al. 10.1016/j.soilbio.2016.04.010
- Modeling the Effects of Global Change on Ecosystem Processes in a Tropical Rainforest A. Russell & W. Parton 10.3390/f11020213
- Mineral and Climatic Controls Over Soil Organic Matter Stability Across the Tibetan Alpine Permafrost Region K. Fang et al. 10.1029/2021GB007118
- Increased interactions between iron oxides and organic carbon under acid deposition drive large increases in soil organic carbon in a tropical forest in southern China J. Chen et al. 10.1007/s10533-022-00897-w
- Predicting Gross Nitrogen Mineralization and Potentially Mineralizable Nitrogen using Soil Organic Matter Properties W. Osterholz et al. 10.2136/sssaj2017.02.0055
- Persistent soil carbon enhanced in Mollisols by well-managed grasslands but not annual grain or dairy forage cropping systems Y. Rui et al. 10.1073/pnas.2118931119
2 citations as recorded by crossref.
- Reducing conditions, reactive metals, and their interactions can explain spatial patterns of surface soil carbon in a humid tropical forest S. Hall & W. Silver 10.1007/s10533-015-0120-5
- Stable and radioactive carbon in forest soils of Chhattisgarh, Central India: Implications for tropical soil carbon dynamics and stable carbon isotope evolution A. Laskar et al. 10.1016/j.jseaes.2016.03.021
Saved (final revised paper)
Latest update: 25 Apr 2024
Short summary
We used measurements of radiocarbon to model the decomposition of organic matter associated with minerals in tropical rainforest soils, using contemporary and archived samples. Most organic matter decomposed over 11 to 26 years, while a smaller portion decomposed over centuries. Rates were similar among soils with strongly differing physical and chemical properties, but declined with a proxy for oxygen limitation. Previous models based on one time point may underestimate decomposition rates.
We used measurements of radiocarbon to model the decomposition of organic matter associated with...
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