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8/2/2019 Decomposition of Leaf Litter of Four Tree Species in A
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Decomposition of leaf litter of four tree species in a subtropicalevergreen broad-leaved forest, Okinawa Island, Japan
Laode Alhamd, Syoko Arakaki, Akio Hagihara*
Laboratory of Ecology and Systematics, University of the Ryukyus, Okinawa 903-0213, Japan
Received 13 January 2003; received in revised form 16 September 2003; accepted 20 February 2004
Abstract
The leaf litter decomposition of four indigenous tree species, such as Castanopsis sieboldii, Schima wallichii, Elaeocarpus
japonicus, and Daphniphyllum teijsmannii, was monthly monitored using the litterbag technique over a 12-month period in a
subtropical evergreen broad-leaved forest of Okinawa Island, Japan. The decomposition rate constant (k) was 1.19 0.19 for D.teijsmannii, 1.09 0.07 for C. sieboldii, 0.94 0.05 for E. japonicus, and 0.66 0.05 (S.E.) yr1 for S. wallichii. Thedecomposition rate constant was significantly lower in S. wallichii than the other three species (P < 0.01). It might be attributed
to the low number of micro-fauna. The fastest rate of decomposition of the leaf litter of D. teijsmannii can be attributed to
collembola whose number was almost twice compared to the number of collembola observed in the other species leaf litters. The
remaining carbon of leaf litter decreased with increasing incubation time and its concentration was ca. 50% over one year. The
remaining nitrogen ofC. sieboldii, E. Japonicus, and D. teijsmannii showed three phases: leaching, net gain, and net loss, while
S. wallichii showed two phases without net loss phase. The leaf litter of D. teijsmannii, which had the highest initial N
concentration of 0.97%, showed the highest decomposition rate constant. Concerning the other species of leaf litters, however,
their initial N concentration did not reflect on their decomposition rate constant. The critical value of C/N ratio ranged from 31
for D. teijsmannii to 33 for C. sieboldii.
# 2004 Elsevier B.V. All rights reserved.
Keywords: Decomposition rate constant; Leaf litter decomposition; Litterbag; Micro-fauna; Subtropical rain forest
1. Introduction
Decomposition of leaf litter, by which organicmatter and nutrients are returned to the forest soils,
is a primary mechanism and has received considerable
attention for sustainable soil fertility (Moretto et al.,
2001; Xuluc-Tolosa et al., 2003). The rate of litter
decomposition has been associated with the carbon
and nitrogen content (Fog, 1988; Kemp et al., 2003;
Meentemeyer, 1978; Swift et al., 1979). Complexes of
bacteria, fungi, and soil organisms have also an
important role in decomposing leaf litter. Themicro-fauna, which can move freely through the
litterbag net, have been shown to cause an increase
in weight loss (Berg et al., 1980; Berg and Staaf,
1981). The successional changes of soil organisms
have been demonstrated during the decomposition
process of various litters using the litterbag method
(Berg and Soderstrom, 1979). The roles of soil organ-
isms on nutrient cycle may be changed during decom-
position processes of litter (Hasegawa and Takeda,
1995; Warren and Zou, 2002).
Forest Ecology and Management 202 (2004) 111
* Corresponding author. Tel.: 81-98-895-8546;fax: 81-98-895-8546.E-mail address: [email protected] (A. Hagihara).
0378-1127/$ see front matter # 2004 Elsevier B.V. All rights reserved.doi:10.1016/j.foreco.2004.02.062
8/2/2019 Decomposition of Leaf Litter of Four Tree Species in A
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Okinawan forests that are identified as subtropical
evergreen broad-leaved forests have high woody species
diversity including Castanopsis sieboldii (Makino)
Hatusima ex Yamazaki et Mashiba (Ito, 1997). InOkinawa, temperature and precipitation are high and
strong winds commonly occur together with a heavy
rain. These factors potentially contribute to the high
degree of nutrient supply through decomposition of
litters. However, studies on leaf litter decomposition
in subtropical rain forests in Okinawa, which are sub-
stantial to be performed for comprehending ecological
processes in the forests, have not yet been conducted.
The aims of this study were to determine the
remaining mass of leaf litter after decomposition, to
examine monthly changes in carbon (C), nitrogen (N),
and C/N ratio in decomposing leaves after the incuba-
tion, and to observe the number of micro-fauna in
process of the decomposition over one year.
2. Materials and methods
2.1. Study site
This study was carried out in a subtropical ever-
green broad-leaved forest in the northern part of
Okinawa Island, Japan (2684503000N and12880500000E). A general map of the study site is
shown in Fig. 1. Tanaka (1999) reported that trees
having DBH ! 4.5 cm in this area were mostlyoccupied by C. sieboldii (Makino) Hatusima ex Yama-
zaki et Mashiba, Elaeocarpus japonicus Sieb. et
Zucc., and Schima wallichii (DC.) Korthals, whose
percentages in number were 40%, 14%, and 10%,
respectively, and the other species were less than 6%.
Altitude and terrain-slope of the study area were
250 m above sea level and 24.58, respectively. The pH
of the soil was 4.35. Air moisture just above the forestfloor was approximately 90%. Monthly temperature
and rainfall distribution during the study period are
presented in Fig. 2. Mean monthly temperature ranged
from 16.4 8C to 28.2 8C and mean annual air tem-
perature was 22.9 8C. Annual rainfall was 2197 mm.
2.2. Litter decomposition
The leaf litter decomposition experiment was car-
ried out during a 12-month period from May 1999 to
May 2000. Four tree species were used in the experi-
ment: C. sieboldii, S. wallichii, E. japonicus, and
Daphniphyllum teijsmannii Zoll. ex Kurz. The decom-
position rates were evaluated using 25 cm 28 cmlitterbags with 2-mm mesh size constructed from
nylon net with 2-mm mesh size.
From March to April 1999, leaf litters were col-
lected in the study site by applying litterfall traps.
Collected leaf litter samples were immediately trans-
ported to the Laboratory of the University of the
Ryukyus, separated according to species, selected
in a wide range of leaf size, shape, and texture,
cleaned, and then air-dried to a constant weight at
a room temperature. Ten grams (12 replicates) of
each leaf litter type was weighed. All samples of leaf
litter were placed in litterbags. The top of the filled
litterbags was sealed and a plastic tag with an ID
number was wired to each litterbag. A total of 48
leaf litterbags were placed on the flat surface area in
May 1999 by utilizing metal pins to prevent move-
ment and to ensure a suitable contact between litter-
bags and organic soil layers. One litterbag from each
of theleaf littertypeswas retainedin the laboratoryto
determine the initial weight and chemical composi-
tion.
At monthly intervals from June 1999 to May 2000,
one litterbag was randomly retrieved from each leaflitter type. Each bag was placed into a separate poly-
ethylene bag and directly transferred to the laboratory.
Extraneous materials, including roots, were carefully
brushed off from the litterbags. Leaf residues were
oven-dried at 85 8C for 24 h and then weighed.
2.3. Chemical analysis
The leaf litter samples of each bag were milled to
determine the chemical contents (Janke & Kunkel
Gmbh & Co. KG, Type A 10 S11). A sample of10 mg was analyzed with an automatic gas chromato-
graph N.C.-Analyzer (Sumigraph, Model NC-80) to
determine the total concentration of carbon (C) and
nitrogen (N). Four replicates of each litterbag were
performed.
Remaining C and N after a given month incubation
were calculated by the following formula:
Remaining % LtCt
L0C0 100; (1)
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where Lt is the mass of dry matter after a given
month, L0 is the initial mass of dry matter, Ct is the
concentration of C or N after a given month incuba-
tion, and C0 is the initial concentration of C or N in
litter.
2.4. Micro-fauna abundance
The abundance of micro-fauna in each litterbag
was extracted at a constant temperature (358
C)for three days by a modified Tullgren funnel and
collected in 90% ethanol. Then identification and
counting of these micro-fauna were performed
under a binocular microscope with a magnification
of 20.
2.5. Exponential decay model
The process of decomposing mass of leaf litter was
described using a single exponential decay model
(Olson, 1963), as follows:
Lt
L0 expkt; (2)
where L0 is the initial mass of dry matter,Lt is the mass
of dry matter after a given month incubation t, and kis
the decomposition rate constant.
2.6. Statistical analysis
The t-test was used for detecting a significantdifference in the decomposition rate constant among
the different species of leaf litter.
3. Results
3.1. Remaining mass
The loss of mass from decomposing leaf litter in
litterbags is described in Fig. 3. The remaining mass
Fig. 1. Map showing the study site (closed circle) in the northern part of Okinawa Island, Japan.
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after 12 months incubation on the forest floor was
54%, 46%, 59%, and 61% to the initial mass for C.
sieboldii, S. wallichii, E. japonicus, and D. teijsman-
nii, respectively. The decay process was well-approxi-
mated by the exponential decay model given by
Eq. (2). As given in Table 1, the values of the decom-
position rate constant (k) were 1.19 0.19 for D.teijsmannii, 1.09 0.07 for C. sieboldii, 0.94 0.05for E. japonicus, and 0.66 0.05 (S.E.) yr1 for S.wallichii. The k-value for S. wallichii was significantly
low, as compared with the other species (P < 0.01).
3.2. Remaining C and N
The changes of remaining carbon followed a similar
pattern in all species, declining with increasing incu-
bation time during the process of decomposition, as
shown in Fig. 4. The carbon sharply decreased in the
first 2 months, reaching 3.2 g (71%) of C. sieboldii,
3.7 g (72%) of S. wallichii, 2.9 g (57%) ofE. japoni-
cus, and 2.8 g (54% of the initial C content) of D.
teijsmannii. During the later months, the decreasing
rate of carbon was comparatively low.
The remaining nitrogen decreased more slowly thancarbon during this study (Fig. 4). The nitrogen change
ofC. sieboldii showed a three-phase pattern: leaching
from the 1st to the 2nd month, net gain from the 3rd to
the 9th month, and net loss from the 10th to the 12th
month. On the other hand, the nitrogen change of S.
wallichii showed two phases: leaching from the 1st to
the 2nd month and net gain from the 3rd up to the 12th
month. The nitrogen change ofE. japonicus had three
phases: leaching in the first two months, net gain from
the 3rd to the 9th month, and net loss from the 10th to
Fig. 2. Monthly temperature and rainfall at the study site, from January 1999 to December 2000. The data were collected from the weather
station (Nago City, Okinawa) nearest to the study area.
Table 1
Annual decomposition rate constant (k) and 95% breakdown period of the four selected tree species during a 12-month period
Tree species k S.E. (yr1) n r2 95% breakdownperiod (year)
Castanopsis sieboldii 1.09 0.07 a,b 13 0.76 2.7Schima wallichii 0.66 0.05 c 13 0.86 4.5Elaeocarpus japonicus 0.94 0.05 b 13 0.84 3.2
Daphniphyllum teijsmannii 1.19 0.19 a 13 0.87 2.5
Values followed by different letters (a and b) in the same column are signi ficantly different (P < 0.01).
4 L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111
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the end of this study. The nitrogen change of D. teijs-
mannii had also three phases: leaching in the first one
month, net gain from the 2nd to the 7th month, and net
loss starting in the 8th and continuing to the 12th month.
3.3. Changes in C/N ratio
Fig. 5 shows the changes of C/N ratio in decom-
posing leaves of four tree species. The four species
showed a similar trend of C/N ratio, which decreased
progressively to the end of experiment. The C/N ratio
ofC. sieboldii sharply decreased with increasing N in
the 1st month (Fig. 4), gradually decreased until the
9th month, and then tended to 29 at the 12th month
incubation. The C/N ratio of S. wallichii decreased in
the first month and then slowly decreased to 29 at the
12th month. The C/N ratio of E. japonicus abruptly
decreased in the first three months, slowly decreaseduntil the 9th month, tended to increase until the 10th
month, and decreased again to 25. The C/N ratio ofD.
teijsmannii sharply decreased from the 1st to the 3rd
month and then slowly decreased down to 26.
3.4. Changes in faunal abundance
The number of micro-fauna in all litterbags was
counted. Both acari and collembola were the predo-
minant orders among 21 orders observed in the
Fig. 3. Percentage of remaining mass to initial mass in process of decomposition from May 1999 to May 2000. (a) C. sieboldii; (b) S.
wallichii; (c) E. japonicus; (d) D. teijsmannii. For the decomposition rate constant (k), see Table 1.
L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111 5
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litterbags. They contributed 82% and 14% of the total
micro-fauna for C. sieboldii, 67% and 28% for S.
wallichii, 73% and 21% for E.japonicus, and 59% and
35% for D. teijsmannii, respectively.
The densities of micro-fauna, in terms of the num-ber of individuals per gram of leaf litter residue, are
summarized in Table 2. The density of micro-fauna for
C. sieboldii had three peaks at 4, 7, and 11 months
after the incubation. The maximum value appeared in
the third peak with 72 individuals per gram of leaf
litter residue. On the other hand, the density for S.
wallichii showed a short-fluctuation pattern, in which
the peak of micro-fauna was reached at 5 months after
the incubation (37 individuals per gram of the residue
of leaf litter). The density for E. japonicus peaked at
11 months after the incubation with 138 individuals
per gram of the residue of leaf litter, which was
especially larger than those for the other three species.
The abundance of micro-fauna for D. teijsmannii
showed a similar trend to C. sieboldii and had threepeaks concentrating at 4, 7, and 10 months after the
incubation. The highest abundance arose at 10 months
after the incubation (113 individuals per gram of the
residue of leaf litter).
4. Discussion
The remaining mass of leaf litter decreased with
increasing incubation time (Fig. 3). It seems that
Fig. 4. Changes of the remaining carbon (*) and remaining nitrogen (*) of decomposing leaf litter after the incubation from May 1999 to
May 2000. Values are represented as mean S.E. (n 4). (a) C. sieboldii; (b) S. wallichii; (c) E. japonicus; (d), D. teijsmannii.
6 L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111
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there exist two stages in decomposition during this
study. Therate of decreasein all species was higherin
the first half than in the second half of decomposition
phase. Berg (1986) and Takeda (1995) also con-
cluded that the decomposition of leaf litter was
divided into two phases. In the first phase, the solublesubstances and non-lignified carbohydrates, e.g.
cellulose and hemicellulose, are decomposed by
saprotrophic fungi, while in the second decomposi-
tion phase, primarily lignin and lignified cellulose
remain. In addition, decomposing leaf litter is influ-
enced by the internal physicochemical properties of
the substrate and by the environmental factors under
which decomposition takes place (Gillon et al.,
1994). The estimated leaf decomposition of 95%
was faster in D. teijsmanii (2.5 years) than in C.
sieboldii (2.7 years), E. japonicus (3.2 years), and S.
wallichii (4.5 years) (Table 1). Since the full decom-
position of the leaf litters was longer than one year,
there is still a great need of conducting this investiga-
tion more than one year in this area. Kira and Shidei
(1967) reported that the duration for the 95% break-down of leaf litterwas 0.3 year afterdecomposition in
a tropical rain forest and 23.3 years in a subalpine
spruce forest.
Several studies have demonstrated that there are
significant contributions of soil micro-fauna on the
decomposition processes (Singh and Shekhar, 1989;
Tian et al., 1992). In the present study, the decom-
position rate constant k was significantly lower in S.
wallichii than the other three species (P < 0.01)
(Table 1). It may be attributed to the low number of
Fig. 5. Changes of the C/N ratio of decomposing leaf litter after the incubation from May 1999 to May 2000. Values are represented as mean
S.E. (n 4). (a) C. sieboldii; (b) S. wallichii; (c) E. japonicus; (d) D. teijsmannii.
L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111 7
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micro-fauna. The fastest rate of decomposition of the
leaf litter of D. teijsmannii can be attributed to col-
lembola whose number was almost twice compared to
the number of collembola observed in the other spe-cies leaf litters (Table 2). The highest k-value D.
teijsmannii was not significantly different from the
k-value of C. siebolldii. The result of both species
could be related to the similar abundance of micro-
fauna, which most likely influenced the decomposi-
tion of the leaf litters. The values of the decomposition
rate constant (Table 1), except the value ofS. wallichii,
were rather comparable to the mean value of 0.93 yr1
in temperate forests, but were much lower than the
mean value of 1.85 yr1 in tropical forests summar-
ized by Takeda (1996).
The remaining carbon of each species showed a
similar trend to the remaining mass, which decreased
with increasing incubation time (Fig. 4). It is sug-
gested that carbon content after monthly incubation
may be a factor in decomposition rate of leaf litter. In
addition, the mean C concentration of each leaf litter
type was ca. 50% over one year (Fig. 6).
The nutrient content of the leaves also affects therate of decomposition. Generally high levels of nutri-
ents, notably nitrogen, are expected to be able to
accelerate the decomposition process. Several studies
have shown a positive correlation between initial N
concentration and the decomposition rate constant
(Melillo et al., 1982; Vogt et al., 1991; Corteaux
et al., 1995; Mfilinge et al., 2002). In this study, the
leaf litter of D. teijsmannii, which had the highest
initial N concentration of 0.97% (Fig. 6), showed the
highest decomposition rate constant. Concerning the
other species, however, their initial N concentration
did not reflect on their decomposition rate constant
(Table 1).
Gosz et al. (1973) and Staff and Berg (1982) noticed
that nitrogen dynamics in decomposing leaf litter
Table 2
Numbers of micro-fauna colonizing in the residual of leaf litter of the four selected tree species in process of decomposition
Micro-fauna (g1
) Incubation time (month) Total (%)
2 3 4 5 6 7 8 9 10 11 12
Castanopsis sieboldiiAcari 19 28 52 44 34 61 26 24 57 66 33 444 (82)
Collembola 3 11 10 9 2 4 3 2 8 5 18 75 (14)
Others 1 2 3 2 2 2 2 1 2 1 4 22 (4)
Total 23 41 65 55 38 67 31 27 67 72 55 541
Schima wallichii
Acari 10 11 25 24 15 23 22 17 21 14 15 197 (67)
Collembola 3 4 7 12 4 4 6 6 11 13 13 83 (28)
Others 3 4 1 1 1 1 1 1 1 1 1 16 (5)
Total 16 19 33 37 20 28 29 24 33 28 29 296
Elaeocarpus japonicus
Acari 16 24 23 19 34 30 9 16 23 124 12 330 (73)Collembola 1 6 3 4 5 3 8 4 14 13 34 95 (21)
Others 7 1 1 1 2 6 2 2 2 1 1 26 (6)
Total 24 31 27 24 41 39 19 22 39 138 47 451
Daphniphyllum teijsmannii
Acari 8 2 27 23 1 38 2 21 69 40 42 273 (59)
Collembola 1 1 8 7 0 6 0 11 39 41 51 165 (35)
Others 1 2 3 3 0 2 1 0 5 2 8 27 (6)
Total 10 5 38 33 1 46 3 32 113 83 101 465
8 L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111
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showed three sequential phases: firstly, the initial
release phase in which leaching predominates; sec-
ondly, the net gain phase in which nitrogen is imported
into the residual material through the activity of
microorganisms, and thirdly, the net loss phase in
which an absolute decrease in the nutrient mass of
decomposing leaf litter occurs. In this study, nitrogenchanges of leaf litter after monthly incubation showed
two or three phases, such as leaching, net gain, and net
loss, in all species. Only two phases, i.e. without net
loss, were found in S. wallichii, but three phases
were observed in C. sieboldii, E. japonicus, and
D. teijsmannii (Fig. 4).
The C/N ratio of C. sieboldii was initially 57 and
then decreased to 52 by the end of the leaching phase
(second month) (Fig. 5). During the net gain phase, the
ratio further decreased from 52 to 33 (sixth month),
which might be recognized as a critical value of C/N
ratio for C. sieboldii. As shown in Fig. 7, the critical
value of S. wallichii reached 32 at 9 months after the
incubation, while those of E. japonicus and D. teijs-
mannii were 32 at 6 months and 31 at 9 months after
the incubation, respectively. The critical values
obtained in all species were achieved when the rangeof N concentration was 1.41.7% (Fig. 6). The present
critical values were a little bit lower than the respec-
tive values of 38 and 34 of Dipterocarpus baudii
leaves reported by Yamashita and Takeda (1998) in
two types of litterbags, 0.5 mm and 2.0 mm in mesh
size.
Acari and collembola were more dominant than the
other orders (Table 2). The number of acari of C.
sieboldii leaf litter was greater than those of the other
leaf litters for a 11-month collection, suggesting that a
Fig. 6. Changes of carbon (*) and nitrogen (*) concentrations after the incubation from May 1999 to May 2000. Values are represented as
mean S.E. (n 4). (a) C. sieboldii; (b) S. wallichii; (c) E. japonicus; (d) D. teijsmannii.
L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111 9
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rapid weight loss in C. sieboldii leaves might be
attributed to the presence of acari. On the other hand,
the low density of micro-fauna might not enhance the
decomposing rate of S. wallichii leaves (Table 1).
Acknowledgements
We are thankful to Prof. T. Shinzato and Dr. T.
Enoki, Subtropical Field Science Center at Yona,
University of the Ryukyus, for their help. We also
thank Prof. M. Tsuchiya for his suggestion in operat-
ing the N.C.-Analyzer. Thanks are due to Mr. B.
Tanaka for their invaluable cooperation in the field
works and Mr. B. Ranjeet for his correction of English.
We also thank two anonymous reviewers provided
many helpful comments on the manuscript. This study
was supported in part by Nippon Life Insurance
Foundation and a Grant-in-Aid for Scientific Research
(No. 12794001) from the Japanese Ministry of Educa-
tion, Culture, Sports, Science and Technology.
References
Berg, B., 1986. Nutrient release from litter and humus in coniferousforest soilsa mini review. Scan. J. For. Res. 1, 359369.
Berg, B., Lohm, U., Lundkvist, H., Wiren, A., 1980. In fluence of
soil animals on decomposition of Scots pine needle litter. Ecol.
Bull. 32, 401409.
Berg, B., Soderstrom, B., 1979. Fungal biomass and nitrogen in
decomposing Scot pine needle litter. Soil Biol. Biochem. 11,
339341.
Berg, B., Staaf, H., 1981. Leaching, accumulation and release
of nitrogen in decomposing forest litter. Ecol. Bull. 33, 163
178.
Corteaux, M.M., Bottner, P., Berg, B., 1995. Litter decomposition,
climate and litter quality. Tree 10, 6366.
Fig. 7. C/N dynamics in process of decomposing leaf litter from May 1999 to May 2000. The numbers show the months after incubation. The
straight line is a critical value. (a) C. sieboldii; (b) S. wallichii; (c) E. japonicus; (d) D. teijsmannii.
10 L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111
8/2/2019 Decomposition of Leaf Litter of Four Tree Species in A
11/11
Fog, K., 1988. The effect of added nitrogen on the rate of
decomposition of organic matter. Biol. Rev. 63, 433462.
Gillon, D., Joffre, R., Ibrahima, A., 1994. Initial litter properties
and decay rate: a microcosm experiment on Mediterranean
species. Can. J. Bot. 72, 946954.Gosz, J.R., Likens, G.E., Bormann, F.H., 1973. Nutrient release
from decomposing leaf and branch litter in the Hubbard Brook
Forest, New Hampshire. Ecol. Monogr. 43, 173191.
Hasegawa, M., Takeda, H., 1995. Changes in feeding attributes of
four collembolan populations during the decomposition process
of pine needles. Pedobiologia 39, 155169.
Ito, Y., 1997. Diversity of forest tree species in Yanbaru, the
northern part of Okinawa Island. Plant Ecol. 133, 125133.
Kemp, P.R., Reynolds, J.F., Virginia, R.A., Whitford, W.J., 2003.
Decomposition of leaf and root litter of Chihuahuan desert
shrubs: effect of three years of summer drought. J. Arid Env.
53, 2139.
Kira, T., Shidei, T., 1967. Primary production and turnover of
organic matter in different forest ecosystems of the western
pacific. Jpn. J. Ecol. 17, 7087.
Meentemeyer, V., 1978. Macroclimate and lignin control of litter
decomposition rates. Ecology 59, 465472.
Melillo, J.M., Aber, J.D., Muratore, J.E., 1982. Nitrogen and lignin
control of hardwood leaf litter decomposition dynamics.
Ecology 63, 621626.
Mfilinge, P.L., Atta, N., Tsuchiya, M., 2002. Nutrient dynamics and
leaf litter decomposition in a subtropical mangrove forest at
Oura Bay, Okinawa. Jpn. Trees 16, 172180.
Moretto, A.S., Distel, R.A., Didone, N.G., 2001. Decomposition
and nutrient dynamic of leaf litter and roots from palatable and
unpalatable grasses in a semi-arid grassland. Appl. Soil Ecol.
18, 3137.Olson, J.S., 1963. Energy storage and the balance of producers and
decomposers in ecological systems. Ecology 44, 322331.
Singh, K.P., Shekhar, C., 1989. Concentration and release pattern of
nutrients (N, P, K) during decomposition of maize and wheat
roots in a seasonally dry tropical region. Soil Biol. Biochem.
21, 8185.
Staff, H., Berg, B., 1982. Accumulation and release of plant
nutrients in decomposing. Scot pine needle litter. Long-term
decomposition in Scot pine forest II. Can. J. Bot. 60, 1561
1568.
Swift, M.J., Heal, O.W., Anderson, J.M., 1979. Decomposition interrestrial ecosystems. Studies in Ecology, vol. 5. University of
California Press, Berkeley, CA.
Takeda, H., 1995. A 5 year study of litter decomposition processes
in a Chamaecyparis obtusa. Endl. For. Ecol. Res. 10, 95104.
Takeda, H., 1996. Templates for the organization of soil animals
communities in tropical forests. In: Turner, I.M., Diong, C.H.,
Lim, S.S.L., Ng, P.K.L. (Eds.), Biodiversity and the Dynamics
of Ecosystems. DIWPA SERIES, Singapore, pp. 217226.
Tanaka, B., 1999. Structure and Biodiversity of Trees in a Broad-
leaved Forest, Okinawa. Bachelor Thesis. Faculty of Science,
University of the Ryukyus, 70 pp. (in Japanese).
Tian, G., Kang, B.T., Brussaard, L., 1992. Biological effects of
plant residues with contrasting chemical compositions under
humid tropical conditions-decomposition and nutrient release.
Soil Biol. Biochem. 24, 10511060.
Vogt, K.A., Vogt, D.J., Bloomfield, J., 1991. Input of organic matter
to the soil by tree roots. In: Mc Michael, B.L., Persson, H.
(Eds.), Plant Roots and Their Environment. Proceedings ISSR
Symposium on Developments in Agricultural and Managed
Forest Ecology, Uppasala, Sweden. Elsevier, Amsterdam,
pp. 171190.
Warren, M.W., Zou, X., 2002. Soil macrofauna and litter nutrients
in three tropical tree plantations on a disturbed site in Puerto
Rico. For. Ecol. Manage. 170, 161171.
Xuluc-Tolosa, F.J., Vester, H.F.M., Ram rez-Marcial, N., Castella-
nos-Albores, J., Lawrence, D., 2003. Leaf litter decomposition
of tree species in three successional phases of tropical drysecondary forest in Campeche, Mexico. For. Ecol. Manage.
174, 401412.
Yamashita, T., Takeda, H., 1998. Decomposition and nutrient
dynamics of leaf litter in litter bags of two mesh sizes set in two
dipterocarp forest sites in Peninsular Malaysia. Pedobiologia
42, 1121.
L. Alhamd et al. / Forest Ecology and Management 202 (2004) 111 11