Fluvial sedimentary deposits as carbon sinks: organic carbon pools and stabilization mechanisms across a Mediterranean catchment
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Abstract
Abstract. The role of fluvial sedimentary areas as organic carbon sinks remains largely unquantified. Little is known about mechanisms of organic carbon (OC) stabilization in alluvial sediments in semiarid and sub-humid catchments where those mechanisms are quite complex because sediments are often redistributed and exposed to a range of environmental conditions in intermittent and perennial fluvial courses within the same catchment. The main goal of this study was to evaluate the contribution of transport and depositional areas as sources or sinks of CO2 at the catchment scale. We used physical and chemical organic matter fractionation techniques and basal respiration rates in samples representative of the three phases of the erosion process within the catchment: (i) detachment, representing the main sediment sources from forests and agricultural upland soils, as well as fluvial lateral banks; (ii) transport, representing the main channel as suspended load and bedload; and (iii) depositional areas along the channel, downstream in alluvial wedges and in the reservoir at the outlet of the catchment, representative of medium and long-term residence deposits, respectively. Our results show that most of the sediments transported and deposited downstream come from agricultural upland soils and fluvial lateral bank sources, where the physico-chemical protection of OC is much lower than that of the forest soils, which are less sensitive to erosion. The protection of OC in forest soils and medium-term depositional areas (alluvial wedges) was mainly driven by physical stabilization mechanisms, while chemical protection of OC was observed in the fluvial lateral banks. However, in the remaining sediment sources, in sediments during transport, and after deposition in long-term deposits (the reservoir), both mechanisms are equally relevant. Mineralization of the most labile OC, intra-aggregate particulate organic matter (MPOM), was predominant during transport. Aggregate formation and OC accumulation, mainly associated with macroaggregates and occluded microaggregates within macroaggregates, were predominant in depositional areas, being more protected than the OC from the most eroding sources (agricultural soils and fluvial lateral banks). Both temporary and permanent sediment deposits in the catchment have an important role in erosive areas, compensating OC losses from the eroded sources and functioning as C sinks.
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Vegetation covers in almond crops reduce soil erosion by 51-95%.
“and reduce soil erosion by 51-95% (Durán Zuazo and Rodríguez Pleguezuelo, 2008;Martínez-Mena et al., 2019).”
From Almond farm profitability under agroecological management in south-eastern Spain: Accounting for externalities and opportunity costs (2020) · cites this paper as Martínez-Mena et al., 2019
The field sampling section (2.2; page unavailable) describes forest and agricultural soils, while section 3.4 discusses water erosion and organic-carbon stabilization. Searches for almond crops, vegetation cover, and a 51–95% erosion reduction found no passage addressing that claim. (LLM, conf=0.76)
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Cites
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Soil Erosion and Carbon Dynamics
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“Several authors have suggested that alluvial settings are important nonquantified OC sinks (Wisser et al., 2013; Hoffmann et al., 2013; Ran et al., 2014) with mechanisms of OC stabilization that can be quite complex in semiarid and subhumid areas.”
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“…lateral C fluxes are key to determine the fate of soil organic carbon (SOC) at the landscape scale. but, however However, current estimations of those fluxes (based on soil erosion and the associated SOC content), show high variation among studies (Quinton et al., 2010; Doetterl et al., 2012).”
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The effects of cultivation on the composition of organic-matter and structural stability of soils
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MethodSoil aggregation and the stabilization of organic carbon as affected by erosion and deposition
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“…microorganims protects the OC associated with these microaggregates Microbial induced processes of the microaggregates within larger aggregates protects the OC associated with these microaggregates by increasing its turnover time, and leads to long-term C sequestration (García-Franco et al., 2015).”
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“…or non-selective); iv) the connectivity and distance of travel between eroding sources and the streambed (Boix-Fayós et al., 2015; Wang et al., 2010); and v) the micro-environmental conditions under which the OC is stored in sedimentary settings (Van Hemelryck et al., 2011; Berhe and Kleber, 2013).”
BackgroundSoil organic matter and CO2 emission as affected by water erosion on field runoff plots
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“…reported how erosion enhances the release of easily mineralizable C encapsulated within aggregates in the mineralization process (Six et al., 2004; Polyakov and Lal, 2008; Van Hemelryck et al., 2010; Wang et al., 2014; Nie et al., 2018) and how that labile OC is also more easily transported…”
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“In fact, it is already known that soil aggregates physically protect OC from rapid decomposition by microorganisms (Razafimbelo et al., 2008; Six et al., 2000), and aggregate formation appears to be closely linked to soil C storage and stability (Barreto et al., 2009; Golchin et al., 1995, Salomé…”
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“…microorganims protects the OC associated with these microaggregates Microbial induced processes of the microaggregates within larger aggregates protects the OC associated with these microaggregates by increasing its turnover time, and leads to long-term C sequestration (García-Franco et al., 2015).”
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“…organic carbon (OC) depends on multiple factors: i) the nature of the soil organic matter being detached from different “sources” within a catchment (Nadeu et al., 2011; 2012; Kirkels et al., 2014); ii) its turnover rates during transport; iii) the type of erosion processes (selective or…”
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“…already known that soil aggregates physically protect OC from rapid decomposition by microorganisms (Razafimbelo et al., 2008; Six et al., 2000), and aggregate formation appears to be closely linked to soil C storage and stability (Barreto et al., 2009; Golchin et al., 1995, Salomé et al., 2010).”
BackgroundThermal stability of organic carbon in soil aggregates as affected by soil erosion and deposition
Nie, X., Li, Z., Huang, J., Liu, L., Xiao, H., Liu, C., & Zeng, G. (2017) · Soil and Tillage Research · doi:10.1016/j.still.2017.08.010 · Cited by 129 · cited 4× · see citing works
“Other authors have reported how erosion enhances the release of easily mineralizable C encapsulated within aggregates in the mineralization process (Six et al., 2004; Polyakov and Lal, 2008; Van Hemelryck et al., 2010; Wang et al., 2014; Nie et al., 2018) and how 15 that labile OC is also more easily transported in su…”
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“…(selective or non-selective); iv) the connectivity and distance of travel between eroding sources and the streambed (Boix-Fayós et al., 2015; Wang et al., 2010); and v) the micro-environmental conditions under which the OC is stored in sedimentary settings (Van Hemelryck et al., 2011;…”
BackgroundLiu, C., Li, Z., Chang, X., He, J., Nie, X., Liu, L., Xiao, H., Wang, D., Peng, H., & Zeng, G. (2017) · Agriculture Ecosystems & Environment · doi:10.1016/j.agee.2017.10.028 · Cited by 108 · cited 2× · see citing works
“…of OC induced by soil erosion, together with the identification of source materials contributing to the sediment OC dynamics within a catchment, are key to determine C budgets, to feed and develop prediction models, and to handle soil conservation strategies at catchment scales (Liu et al., 2018).”
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“…layers of the depositional areas, the relatively lower OC, microbial activitybasal respiration rate, and M POM Mpom were less favorable for aggregate formation and the process unfolded very slowly compared to the upper layers, which confirms the results reported by other authors (Xie et al., 2017).”
ResultThe effect of soil redistribution on soil organic carbon: an experimental study
Hemelryck, H. V., Fiener, P., Oost, K. V., Govers, G., & Merckx, R. (2010) · Biogeosciences · doi:10.5194/bg-7-3971-2010 · Cited by 103 · cited 1× · see citing works
“…in the min- Biogeosciences, 16, 1035–1051, 2019 www.biogeosciences.net/16/1035/2019/ eralization process (Six et al., 2004; Polyakov and Lal, 2008; Van Hemelryck et al., 2010; Wang et al., 2014; Nie et al., 2018) and how that labile OC is also more easily transported in suspension (Starr et al.,…”
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“…carbon (OC) depends on multiple factors: i) the nature of the soil organic matter being detached from different “sources” within a catchment (Nadeu et al., 2011; 2012; Kirkels et al., 2014); ii) its turnover rates during transport; iii) the type of erosion processes (selective or…”
BackgroundMethodInfluentialEvaluating the impact of soil redistribution on the in situ mineralization of soil organic carbon
Hemelryck, H. V., Govers, G., Oost, K. V., & Merckx, R. (2010) · Earth Surface Processes and Landforms · doi:10.1002/esp.2055 · Cited by 94 · cited 1× · see citing works
“…or non-selective); iv) the connectivity and distance of travel between eroding sources and the streambed (Boix-Fayós et al., 2015; Wang et al., 2010); and v) the micro-environmental conditions under which the OC is stored in sedimentary settings (Van Hemelryck et al., 2011; Berhe and Kleber, 2013).”
BackgroundErosion-induced massive organic carbon burial and carbon emission in the Yellow River basin, China
Ran, L., Lu, X., & Xin, Z. (2014) · Biogeosciences · doi:10.5194/bg-11-945-2014 · Cited by 90 · cited 1× · see citing works
“Several authors have suggested that alluvial settings are important, non-quantified OC sinks (Wisser et al., 2013; Hoffmann et al., 2013; Ran et al., 2014) with mechanisms of OC stabilization that can be quite complex in semiarid and sub-humid areas.”
Clercq, T. D., Heiling, M., Dercon, G., Resch, C., Aigner, M., Mayer, L., Mao, Y., Elsen, A., Steier, P., Leifeld, J., et al. (2015) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2015.05.011 · Cited by 87 · cited 2× · see citing works
“ii) The degree of microbial degradation index, as an indicator of the OC stability/decomposability, based on De Clercq et al. (2015). According to this, the OC associated with the free microaggregate and mineral fractions (OC-m and OC-min, 5 respectively) would represent the oldest OC, while the OC in the intra-aggreg…”
BackgroundGirolamo, A. M. D., Bouraoui, F., Buffagni, A., Pappagallo, G., & Porto, A. L. (2017) · River Research and Applications · doi:10.1002/rra.3165 · Cited by 66 · cited 1× · see citing works
“…that this percentage will increase worldwide in response to climate change and increased water extraction for human use (Shewe et al., 2014), because intermittent and ephemeral rivers will suffer more severe, sustained, and more frequent droughts (De Girolamo et al., 2017; Vadher et al., 2018).”
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Short Communication: Humans and the missing C-sink: erosion and burial of soil carbon through time
Hoffmann, T., Mudd, S. M., Oost, K. V., Verstraeten, G., Erkens, G., Lang, A., Middelkoop, H., Boyle, J., Kaplan, J. O., Willenbring, J. K., et al. (2013) · Earth Surface Dynamics · doi:10.5194/esurf-1-45-2013 · Cited by 58 · see citing works
Sediment flow paths and associated organic carbon dynamics across a Mediterranean catchment
Boix‐Fayos, C., Nadeu, E., Quiñonero, J. M., Martínez‐Mena, M., Almagro, M., & de Vente, J. (2015) · Hydrology and earth system sciences · doi:10.5194/hess-19-1209-2015 · Cited by 46 · cited 6× · see citing works
“This previous analysis was the background to the combination of the sediment cascade (Hoffman et al., 2013; Boix-Fayos et al., 2015) and the erosion cycle as the experimental approach (Fig.”
BackgroundMethodResultInfluentialTransport-distance specific SOC distribution: Does it skew erosion induced C fluxes?
Hu, Y., Berhe, A. A., Fogel, M. L., Heckrath, G. J., & Kuhn, N. J. (2016) · Biogeochemistry · doi:10.1007/s10533-016-0211-y · Cited by 46 · see citing works
Erosion-induced exposure of SOC to mineralization in aggregated sediment
Hu, Y., & Kuhn, N. J. (2015) · CATENA · doi:10.1016/j.catena.2015.10.024 · Cited by 38 · see citing works
Trigalet, S., Oost, K. V., Roisin, C., & van Wesemael, B. (2014) · Agriculture Ecosystems & Environment · doi:10.1016/j.agee.2014.06.011 · Cited by 27 · see citing works
Effects of gravel on grassland soil carbon and nitrogen in the arid regions of the Tibetan Plateau
Wang, X., Liu, G., & Liu, S. (2011) · Geoderma · doi:10.1016/j.geoderma.2011.07.028 · Cited by 26 · cited 2× · see citing works
“Other authors (Sodhi et al. 2009; Wang et al., 2011) also reported a higher OC content in macroaggregates than in 15 microaggregates in soils, which means that organic matter could be the major binding agent in such soils (Oades and Waters, 1991).”
BackgroundVadher, A. N., Millett, J., Stubbington, R., & Wood, P. J. (2018) · Hydrobiologia · doi:10.1007/s10750-018-3544-9 · Cited by 22 · cited 1× · see citing works
“…that this percentage will increase worldwide in response to climate change and increased water extraction for human use (Shewe et al., 2014), because intermittent and ephemeral rivers will suffer more severe, sustained, and more frequent droughts (De Girolamo et al., 2017; Vadher et al., 2018).”
BackgroundRitchie, J. C., & Rasmussen, P. E. (2000) · Land Degradation and Development · doi:10.1002/(sici)1099-145x(200001/02)11:1 · Cited by 12 · see citing works
Pérez‐Cutillas, P., Cataldo, M. F., Zema, D. A., de Vente, J., & Boix‐Fayos, C. (2018) · Bosque (Valdivia) · doi:10.4067/s0717-92002018000100119 · Cited by 12 · see citing works
A modified siphon sampler for shallow water
Diehl, T. H. (2008) · Scientific investigations report · doi:10.3133/sir20075282 · Cited by 10 · see citing works
Flagged first, then by citations
1 of the 65 references couldn’t be matched to a known paper.
Research works printed but not linked: 1
- Paul, E. A., Morris, S. J., and Boehm, S.: The determination of soil C pool sizes and turnover rates: biophysical fractionation and tracers, in: Assessment Methods for Soil Carbon (Advances in Soil Science),edited by: Lal, R., Kimble, J. M., Follett, R. F., and Stewart, B. A., CRC Press LLC, Boca Raton, FL, USA, 193-206, 2001.
Cited by
Sorted by citations
Agriculture, Forestry and Other Land Uses (AFOLU)
Change, I. P. O. C. (2023) · Cambridge University Press eBooks · doi:10.1017/9781009157926.009 · Cited by 287 · see citing works
De Leijster, V., Verburg, R. W., Santos, M. J., Wassen, M. J., Martínez-Mena, M., de Vente, J., & Verweij, P. A. (2020) · Agricultural Systems · doi:10.1016/j.agsy.2020.102878 · Cited by 52 · see citing works
The fate of carbon in check dam sediments
Yao, Y., Song, J., & Wei, X. (2021) · Earth-Science Reviews · doi:10.1016/j.earscirev.2021.103889 · Cited by 41 · see citing works
Boix‐Fayos, C., Boerboom, L. G. J., Janssen, R., Martínez‐Mena, M., Almagro, M., Pérez‐Cutillas, P., Eekhout, J., Castillo, V. M., & de Vente, J. (2020) · Ecosystem Services · doi:10.1016/j.ecoser.2020.101136 · Cited by 36 · see citing works
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The occurrence and distribution characteristics of microbial necromass carbon in lake sediments
Liu, Y., Nie, X., Ran, F., Wang, S., Liao, S., Zeng, A., & Li, Z. (2024) · CATENA · doi:10.1016/j.catena.2024.107944 · Cited by 8 · see citing works
Downey, A. R., Riddell, J. L., Padilla, I., & Vesper, D. J. (2022) · Environmental Earth Sciences · doi:10.1007/s12665-022-10720-2 · Cited by 8 · see citing works
“Sedimentary deposits within fluvial systems are a known carbon sink, storing organic carbon introduced from upland areas (Martínez-Mena et al. 2019).”
BackgroundLei, K., Bucka, F. B., Just, C., van Grinsven, S., Floßmann, S., Dannenmann, M., Völkel, J., & Kögel‐Knabner, I. (2025) · Biogeochemistry · doi:10.1007/s10533-025-01213-y · Cited by 6 · see citing works
“This results in higher SOM accumulation through inundation and sedimentation in the subsoil (Martinez-Mena et al. 2019; Mayer et al. 2018), leading to significantly higher OC and TN stocks (Table S.4).”
Upadhayay, H. R., Granger, S. J., Zhang, Y., Amorim, F. F., Cilione, L., Micale, M., & Collins, A. L. (2021) · Biogeochemistry · doi:10.1007/s10533-021-00825-4 · Cited by 4 · see citing works
Halifa‐Marín, A., Pérez‐Cutillas, P., Almagro, M., & Boix‐Fayos, C. (2019) · Cuadernos de Investigación Geográfica · doi:10.18172/cig.3690 · Cited by 2 · see citing works
Lei, K., Bucka, F. B., van Grinsven, S., Floßmann, S., Völkel, J., & Kögel‐Knabner, I. (2023) · SSRN Electronic Journal · doi:10.2139/ssrn.4611678
- Authors
- Martínez-Mena, M., Almagro, M., García-Franco, N., de Vente, J., García, E., & Boix-Fayos, C.
- Affiliations
- University of the Basque Country (ES)
- Technical University of Munich (DE)
- Consejo Superior de Investigaciones Científicas (ES)
- Corresponding author
- Almagro, María
- García-Franco, Noelia
- García, Eloisa
- Venue
- Biogeosciences
- Publisher
- Copernicus GmbH
- Published
- 2019-03-15
- Volume
- 16
- Issue
- 5
- Pages
- 1035-1051
- ISSN
- 1726-4170 (ISSN-L)
- 1726-4189
- OpenAlex
- W2894875741
- Cited by
- 14
- References
- 65
- Citations by year
- 2025: 1 · 2024: 1 · 2023: 3 · 2022: 1 · 2021: 2 · 2020: 4 · 2019: 2
- FWCI
- 1.79
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Biogeosciences (publishedVersion, cc-by)
- Communities in ADDI (Universidad del Pais Vasco) (submittedVersion, other-oa)
- LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas) (submittedVersion, cc-by-nc-sa)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
- Hispana (submittedVersion, cc-by-nc-sa)
- mediaTUM (Technical University of Munich) (submittedVersion, other-oa)
- Biogeosciences (European Geosciences Union) (submittedVersion, cc-by)
- Topics
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil erosion and sediment transport
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Physical Sciences › Environmental Science › Ecology › Hydrology and Sediment Transport Processes
- Keywords
- organic carbon stabilization, carbon sink, alluvial deposits, soil organic carbon, sediment transport, organic matter fractionation, basal respiration, soil aggregates, mineral-associated organic carbon, forest soils, reservoir sediments, Mediterranean catchments
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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