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Leaf decomposition and fine fuels in floodplain forests of the Rio Negro in the Brazilian Amazon

Published online by Cambridge University Press:  07 August 2013

Aline Ramos dos Santos
Affiliation:
INPA – National Institute for Amazon Research, Environmental Dynamics Department, Avenida André Araujo 2936, 69067-095 Manaus, Amazonas, Brazil
Bruce Walker Nelson*
Affiliation:
INPA – National Institute for Amazon Research, Environmental Dynamics Department, Avenida André Araujo 2936, 69067-095 Manaus, Amazonas, Brazil
*
1Corresponding author. Email: [email protected]

Abstract:

Despite being inundated for up to 9 mo of the year, black-water floodplain forests in the Brazilian Amazon are susceptible to fire. Post-fire tree mortality is higher and fire spreads further in the floodplain, compared with adjacent upland forest. To understand these differences between the two forest types, we compared how leaf decomposition and fine-fuel loads change with inundation and soil texture. Litterbags containing leaves of Clitoria fairchildiana were placed on upland forest floor and submerged at two depths in a backwater of the Rio Negro. We used 80 bags per treatment and retrieved subsets every ~16 d from which the contents were cleaned, dried, weighed and discarded. Over the 81-d experiment, upland leaves decomposed two to three times faster than submerged leaves. Fine-fuel biomass (litter + root mat) was measured at 28 upland forest sites and 29 floodplain forest sites of the middle Rio Negro. Floodplain forests held about twice the fine fuel (25.9 ± 10.6 Mg ha−1) of uplands (10.9 ± 2.3 Mg ha−1). Upland soils had more sand but a carpet of fine apogeotropic tree roots was more common and thicker in floodplains. We infer that slow decomposition of submerged leaves leads to high tree mortality from fire in black-water floodplains by (1) increasing fire intensity due to high fine-litter fuel load and (2) making tree roots more vulnerable to burning because they form a peat-like mat to absorb nutrients from the thick litter.

Type
Short Communication
Copyright
Copyright © Cambridge University Press 2013 

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