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Changing enzymatic activities and mycorrhizal infections in a chronosequence of secondary and mature forests of eastern Amazonia
Cláudio José Reis de Carvalho1, Eric A. Davidson2, Tereza Primo dos
Santos3, Fábio Carneiro Dutra4, Bruno de Oliveira Serrão4
1Embrapa Amazônia Oriental; 2The Woods Hole Research Center, 3Instituto de Pesquisa Ambiental da Amazônia, 4Bolsista ITI/DTI, CNPQ-LBA
Amazônia Oriental The Woods Hole Research Center
The availability of N and P may limit rates of regrowth of secondary forests in Amazonia.
Age (years)
0 20 40 60 80 100
Bio
mas
s (M
g.ha
-1)
0
50
100
150
200
250
300
Primary forest
Losses of a 7-year-fallow Losses of a 7-year-fallow vegetation after burning vegetation after burning
(31 t/ha DM)(31 t/ha DM)
Losses in kg/ha and in Losses in kg/ha and in % of biomass% of biomass
Carbon 14378 (98%) Nitrogen 205 (96%) Potassium 39 (48%) Phosphorus 4 (47%) Calcium 107 (35%) Magnesium 18 (40%) Sulfur 14 (76%) Sodium 6 (30%)
Carbon 14378 (98%) Nitrogen 205 (96%) Potassium 39 (48%) Phosphorus 4 (47%) Calcium 107 (35%) Magnesium 18 (40%) Sulfur 14 (76%) Sodium 6 (30%)
Hölscher 1995
Losses of a 7-year-fallow Losses of a 7-year-fallow vegetation after burning vegetation after burning
(31 t/ha DM)(31 t/ha DM)
Losses in kg/ha and in Losses in kg/ha and in % of biomass% of biomass
Carbon 14378 (98%) Nitrogen 205 (96%) Potassium 39 (48%) Phosphorus 4 (47%) Calcium 107 (35%) Magnesium 18 (40%) Sulfur 14 (76%) Sodium 6 (30%)
Carbon 14378 (98%) Nitrogen 205 (96%) Potassium 39 (48%) Phosphorus 4 (47%) Calcium 107 (35%) Magnesium 18 (40%) Sulfur 14 (76%) Sodium 6 (30%)
Hölscher 1995
The highly weathered soils are nutrient poor, and numerous cycles of slash and burn can further impoverish nutrient stocks and lead to site degradation.
Site pHH20 Corg
(Mg.ha-1)
Norg
(Mg.ha-1)
PMehlich
(kg.ha-1)
Porg
(kg.ha-1)
Ptotal
(kg.ha-1)
Primary forest 4.36 (0.35) 47.4 (9.8) 3.42 (0.35) 6.81 (0.58) 247.84 (12.59) 715.63 (99.17)
Secondary forests
3 years 5.25 (0.16) 39.0 (7.2) 2.37 (0.75) 5.49 (1.28) 171.25 (78.49) 875.49 (224.27)
6 years 5.10 (0.24) 43.0 (4.4) 2.56 (0.55) 8.24 (1.44) 231.92 (33.00) 862.23 (147.35)
10 years 5.32 (0.16) 33.6 (6.3) 2.24 (0.88) 6.43 (1.56) 132.88 (48.54) 568.90 (134.58)
20 years 4.89 (0.41) 38.2 (6.3) 2.51 (0.54) 11.92 (7.67) 246.00 (107.92)
679.49 (185.03)
40 years 4.92 (0.25) 34.1 (8.1) 1.92 (0.68) 4.83 (0.37) 146.87 (25.42) 703.45 (45.57)
70 years 4.88 (0.29) 38.0 (6.7) 2.66 (1.02) 5.61 (0.40) 170.60 (71.01) 739.79 (71.79)
The mineralization of N and P from soil and litter by enzymatic activity and the acquisition of nutrients by mycorrhizae could be important for the recuperation of nutrient cycles during secondary forest succession.
These processes were studied in a secondary forest chronosequence (5, 8, 12, 22, 42, and 72 years), a recently abandoned black pepper plantation, and a remnant mature forest in the municipality of São Francisco do Pará.
• At the end of the rainy season (May), samples of soil and roots were
collected from the litter-soil interface and at 0-5, 5-15, and 15-30 cm
depths in mineral soil.
• Available P, total N, extractable NH4+ and NO3
-, urease and acid
phosphatase activity, and concentrations of total and readily extractable
glomalin were measured.
• The number of fungal spores and infections of mycorrhizae (VAM) were
counted in roots.
The number of spores and mycorrhizal infections decreased with increasing age of the forest, whereas the activity of acid phosphatase increased with forest age.
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
Sp
ore
s (N
º. 3
0g
-1)
0
20
40
60
80
100
Surface0-5cm5-15cm15-30cm
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
Infe
ctio
ns (
Nº.
cm
-1)
0
10
20
30
40
Surface0-5cm5-15cm15-30cm
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
g 4
-Nitr
ophe
nol.g
-1.h
-1
0
5000
10000
15000
20000
25000
Surface0-5 cm5-15 cm15-30 cm
The concentration of total and readily extractable glomalin tended to increase with forest
age.
E E
xtr.
Glo
ma
lin (
mg
.g-1
)
0
1
2
3
4
5
6
7
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
To
tal G
lom
alin
(m
g.g
-1)
0
2
4
6
8
10
12
14
Surface0-5cm5-15cm15-30cm
The concentration of NH4+ and NO3
- tended to increase with forest age, and
were significantly higher in the mature forest soil.
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
g N
-NH
4.g
-1.h
-1
0
20
40
60
80
100
120
140
160
180
Surface0-5cm5-15cm15-30cm
Site/Age (years)
Pimental 5 8 12 22 42 72 Floresta
NH
4-N
(m
g.kg
-1)
0
200
400
600
800
Surface0-5 cm5-15 cm 15-30 cm
Site/Age (years)
Pepper 5 8 12 22 42 72 Forest
NO
3-N
(m
g.k
g-1)
0
20
40
60
80
Surface0-5cm5-15cm15-30cm
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
25003 anos
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
2500Pimental
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
250010 anos
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
250040 anos
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
2500
70 anos
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
25006 anos
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
2500
Floresta primária
2001 / 2002
fev abr jun ago out dez fev abr
Litte
r (k
g.ha
-1)
0
500
1000
1500
2000
2500
20 anos
Site/Age (years)
Pepper 3 6 10 20 40 70 Forest
Bio
mas
s (M
g.ha
-1)
0
2
4
6
8
10
12
14Fine litter
Woody litter
Litterfall and decomposition
Site/Age (years)
Pepper 3 6 10 20 40 70 Forest
C/N
rat
io
10
12
14
16
18
20
22
24
The results indicate that some, but not all, of these indicators of nutrient mineralization and acquisition become similar to the mature forest within 8 years of secondary forest succession.