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dc.contributor.authorKoele, N
dc.contributor.authorBird, M
dc.contributor.authorHaig, J
dc.contributor.authorMarimon-Junior, BH
dc.contributor.authorMarimon, BS
dc.contributor.authorPhillips, OL
dc.contributor.authorde Oliveira, EA
dc.contributor.authorQuesada, CA
dc.contributor.authorFeldpausch, TR
dc.date.accessioned2017-08-21T10:20:12Z
dc.date.issued2017-11-15
dc.description.abstractAmazon Basin forest soils contain considerable soil organic carbon stocks; however, the contribution of soil pyrogenic carbon (PyC) to the total is unknown. PyC is derived from local fires (historical and modern) and external inputs via aeolian deposition. To establish an initial estimate of PyC stocks in non-terra preta forest with no known history of fire, to assess site and vertical variability, as well as to determine optimal sampling design, we sampled 37 one hectare forest plots in the Amazon Basin and analysed PyC via hydrogen pyrolysis of three individual samples per plot and of bulked samples to 200 cm depth. Using our data and published total organic carbon stocks, we present the first field-based estimate of total PyC stock for the Amazon Basin of 1.10 Pg over 0–30 cm soil depth, and 2.76 Pg over 0–100 cm soil depth. This is up to 20 times higher than previously assumed. Three individual samples per 1 ha are sufficient to capture the site variability of PyC in our plots. PyC showed significant, large-scale variability among plots. To capture 50% of the PyC in 200 cm soil profiles, soil must be sampled to a depth of at least 71 cm. PyC represents a significant (11%) portion of total organic carbon in soil profiles 0–200 cm depth. This finding highlights the potentially important role that historical fire has played in modifying soil C stocks. Our data suggest that PyC is an important carbon pool for long-term storage, involved in millennial scale biogeochemical cycling, particularly in the subsurface soil.en_GB
dc.description.sponsorshipWe gratefully acknowledge financial support for NK, TRF, BSM, BHMJ, and EAO from the Coordination of Improvement of Personnel in Higher Education, Brazil (CAPES) through a Science without Borders grant to TRF (PVE 177/2012). Research was also supported by the College of Life and Environmental Science, University of Exeter and NERC (NE/N011570/1). The National Council of Science and Technology, Brazil (CNPq) provided a productivity grant for BHMJ and BSM, and support to the projects PELD (403725/2012-7) and PPBio (457602/2012-0). Wen_GB
dc.identifier.citationVol. 306, pp. 237 - 243en_GB
dc.identifier.doi10.1016/j.geoderma.2017.07.029
dc.identifier.urihttp://hdl.handle.net/10871/29002
dc.language.isoenen_GB
dc.publisherElsevieren_GB
dc.rights© 2017 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/BY/4.0/)en_GB
dc.subjectDeep mineral soil horizonsen_GB
dc.subjectSoil organic carbonen_GB
dc.subjectPyrogenic carbon stabilityen_GB
dc.titleAmazon Basin forest pyrogenic carbon stocks: First estimate of deep storageen_GB
dc.typeArticleen_GB
dc.date.available2017-08-21T10:20:12Z
dc.identifier.issn0016-7061
dc.descriptionThis is the final version of the article. Available from the publisher via the DOI in this record.en_GB
dc.identifier.journalGeodermaen_GB


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