Studies of the impact of traditional agroforestry practices on soil nutrien
t status in the Amazon Basin have largely been limited to upland sites, man
y of which are oligotrophic. However, rural population density in Amazonia
is highest on the floodplains of the major rivers and shifting cultivation
has been practiced on the floodplains for millennia. We established a slash
-and-burn cultivation plot and an untreated forest plot in tidal floodplain
successional forest in the Islands of Abaetetuba, Para, Brazil, and sample
d soils (0-10 cm) during four phases of the agroforest cycle (n = 9 in each
plot for each sampling period): (1) prior to clearing, (2) following burni
ng, (3) harvest one (rice at four months), and (4) harvest two (sugar cane
at 15 months). During the course of this pilot experiment, background tempo
ral variability in SOC, total N and available mineral nutrient pools (P, K,
Ca, Mg) exceeded treatment effects, suggesting that soil nutrient pools in
this environment are well-buffered against the effects of shifting cultiva
tion. These results contrast markedly with those reported for Amazonian upl
and sites where nutrient pulses and declines associated with the agroforest
cycle have been demonstrated and may restrict the potential for low-input,
continuous cultivation. Physical limitations imposed by flooding and fluvi
al erosion, rather than nutrient constraints, restrict the potential of agr
icultural intensification in the tidal floodplains.