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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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Phosphorus fractions in earthworm casts and soils ofagroforestry systesms, pasture, and secondary forest in <strong>the</strong>Central <strong>Amazon</strong> <strong>Basin</strong>Christienne N. Kuczak*, Erick C. M. Fernandes, Johannes Lehmann, and Marco RondonCornell University*address of primary author: 610 Bradfield Hall, Ithaca, NY 14853 U.S.A.; email: cnk4@cornell.eduPhosphorus is limiting to agricultural production throughout <strong>the</strong> tropics and 96%of land in <strong>the</strong> <strong>Amazon</strong> basin has been reported to be P-limited (Dem<strong>at</strong>ê and Dem<strong>at</strong>ê1997). Because P dynamics can be gre<strong>at</strong>ly affected by veget<strong>at</strong>ion cover and nutrientcycling (Solomon et. al 2002), we investig<strong>at</strong>ed <strong>the</strong> effects of tree species and earthworms(Family Glossoscolecidae) on P in soils and earthworm casts. Soils and earthworm castsbene<strong>at</strong>h <strong>the</strong> agroforestry species Theobroma grandiflorum, Bactris gasipaes, Eugeniastipit<strong>at</strong>a, and Bertholletia excelsa, <strong>the</strong> pasture grass Brachiaria sp., and <strong>the</strong> secondaryforest species Vismia sp. and Cecropia sp. were sequentially extracted using amodific<strong>at</strong>ion of <strong>the</strong> Hedley fraction<strong>at</strong>ion (Hedley 1982; Tiessen and Moir 1993).Earthworm casts had significantly more total P, inorganic P, and organic P than soils.Soils and casts bene<strong>at</strong>h agroforestry species had significantly more total P, inorganic P,and organic P than soils and casts bene<strong>at</strong>h Brachiaria sp. and <strong>the</strong> secondary forestspecies; and soils and casts bene<strong>at</strong>h Brachiaria sp. had significantly more total P,inorganic P, and organic P than soils and casts bene<strong>at</strong>h secondary forest species. Thesoils and casts bene<strong>at</strong>h <strong>the</strong> agroforestry species had significantly more P in <strong>the</strong> resinfraction than soils and casts bene<strong>at</strong>h <strong>the</strong> secondary forest species. The gre<strong>at</strong>est total Pwas in earthworm casts bene<strong>at</strong>h Eugenia sp. <strong>with</strong> a mean of 251 µg cm -3 and in soilsbene<strong>at</strong>h Bertholettia sp. <strong>with</strong> a mean of 89 µg cm -3 . Secondary forests had <strong>the</strong> least totalP in both casts and soils <strong>with</strong> a mean of 11 µg cm -3 and 41 µg cm -3 , respectively. Giventh<strong>at</strong> bulk density of earthworm casts was 1.47 g cm 3 and <strong>the</strong> bulk density of soil was 0.96g cm -3 , casts contained 1.87 to 2.97 times more total P (g cm 3 ) than soils. Within <strong>the</strong>system studied, earthworm casts can contribute from 61 kg ha -1 in secondary forest to 140kg ha -1 bene<strong>at</strong>h Eugenia sp. It was shown th<strong>at</strong> earthworm casts and veget<strong>at</strong>ion covercontributes gre<strong>at</strong>ly to P dynamics in agroforestry systems, pasture, and secondary forestin <strong>the</strong> Central <strong>Amazon</strong> <strong>Basin</strong>.

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