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Amazon Basin forest pyrogenic carbon stocks: First estimate of deep storage
被引:30
|作者:
Koele, Nina
[1
]
Bird, Michael
[2
,3
]
Haig, Jordahna
[2
,3
]
Marimon-Junior, Ben Hur
[1
]
Marimon, Beatriz Schwantes
[1
]
Phillips, Oliver L.
[4
]
de Oliveira, Edmar A.
[1
]
Quesada, C. A.
[5
]
Feldpausch, Ted R.
[1
,6
]
机构:
[1] Univ Estado Mato Grosso UNEMAT, Lab Ecol Vegetal, Caixa Postal 08, BR-78690000 Nova Xavantina, MT, Brazil
[2] James Cook Univ, Coll Sci Technol & Engn, Cairns, Qld 4870, Australia
[3] James Cook Univ, Ctr Trop Environm & Sustainabil Sci, Cairns, Qld 4870, Australia
[4] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
[5] Natl Inst Res Amazonia INPA, CP 2223, BR-69080971 Manaus, Amazonas, Brazil
[6] Univ Exeter, Geog, Coll Life & Environm Sci, Rennes Dr, Exeter EX4 4RJ, Devon, England
来源:
关键词:
Deep mineral soil horizons;
Soil organic carbon;
Pyrogenic carbon stability;
SCALE SPATIAL VARIABILITY;
SOIL ORGANIC-MATTER;
BLACK CARBON;
VEGETATION CHANGES;
BRAZILIAN AMAZON;
CHARCOAL RECORDS;
HOLOCENE;
FIRE;
RESIDUES;
QUANTIFICATION;
D O I:
10.1016/j.geoderma.2017.07.029
中图分类号:
S15 [土壤学];
学科分类号:
0903 ;
090301 ;
摘要:
Amazon 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.
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页码:237 / 243
页数:7
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