Articles | Volume 23, issue 6
https://doi.org/10.5194/bg-23-2155-2026
https://doi.org/10.5194/bg-23-2155-2026
Research article
 | 
30 Mar 2026
Research article |  | 30 Mar 2026

Characterisation and quantification of organic carbon burial using a multiproxy approach in saltmarshes from Aotearoa New Zealand

Olga Albot, Joshua Ratcliffe, Richard Levy, Sebastian Naeher, Daniel J. King, Catherine Ginnane, Jocelyn Turnbull, Mary Jill Ira Banta, Christopher Wood, Jenny Dahl, Jannine Cooper, and Andy Phillips
Publisher's note: on 2 April 2026 the country of affiliation 7 was corrected from USA to New Zealand.

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Cited articles

Albot, O., Ratcliffe, J., Levy, R., Naeher, S., King, D., Ginnane, C., Jocelyn, T., Banta, M. J. I., Wood, C., Dahl, J., Cooper, J., and Phillips, A.: Characterisation and quantification of organic carbon burial using a multiproxy approach in saltmarshes from Aotearoa New Zealand, Zenodo [data set], https://doi.org/10.5281/zenodo.17790165, 2026. 
Alongi, D. M.: Coastal ecosystem processes, CRC Press, 1st ed., ISBN 978-0367400798, 1997. 
Antler, G., Mills, J. V., Hutchings, A. M., Redeker, K. R., and Turchyn, A. V.: The sedimentary carbon-sulfur-iron interplay–A lesson from East Anglian salt marsh sediments, Front. Earth Sci., 7, 140, https://doi.org/10.3389/feart.2019.00140, 2019. 
Appleby, P. G.: Dating recent sediments by 210Pb: problems and solutions, Seminar on dating of sediment and determination of sedimentation rate, Helsinki, Finland, 1–3 April 1997, paper presentation, https://inis.iaea.org/records/vtsmx-fvz88 (last access: 18 November 2024), 1997. 
Arias-Ortiz, A., Masqué, P., Garcia-Orellana, J., Serrano, O., Mazarrasa, I., Marbà, N., Lovelock, C. E., Lavery, P. S., and Duarte, C. M.: Reviews and syntheses: 210Pb-derived sediment and carbon accumulation rates in vegetated coastal ecosystems – setting the record straight, Biogeosciences, 15, 6791–6818, https://doi.org/10.5194/bg-15-6791-2018, 2018. 
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Short summary
Saltmarshes store carbon in their soils, contributing to climate change mitigation. We analysed five sites across New Zealand and found that carbon storage and accumulation rates vary widely with geomorphic setting, land use history and sediment inputs. Plant material was a major source of carbon in the soil and has been preserved in basal sediments for several centuries. These results improve national blue carbon estimates and highlight the role of saltmarshes as natural climate solutions.
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