common limiting nutrient (Grubb 1977, Vitousek 1984, Vitousek and Sanford 1986, Medina
and Cuevas 1994), but seedling growth and survival may be affected by simultaneous
limitations of several nutrients.
In Melastoma malabathricum mixtures of P plus Ca, micronutrients, Mg, K, and N
stimulated growth far beyond that provoked by P alone (Burslem et al. 1994, 1995). Particularly
important are the light-intensity–nutrient-availability interactions. Increasing light intensity
elevates nutrient demands, most notably in the case of N (Medina 1971). Increased nutrient
supply leads to higher maximum photosynthetic rates in seedlings of plants of different
successional status, irrespective of the light intensity of cultivation (Thompson et al. 1988,
1992, Riddoch et al. 1991b). High-light intensity may even negatively affect photosynthetic
performance under conditions of low-nutrient availability (Thompson et al. 1988).
Mycorrhizal symbiosis is widespread in tropical humid forests (Janos 1983, St John and
Uhl 1983, Hopkins et al. 1996). Most species develop VAM, but an important group
constituted by the Dipterocarpaceae and legumes of the subtribes Amherstieae and Detarieae
(Caesalpinioid), and such important genera as Aldina and Swartzia in the Papilionoid, are
ectomycorrhizal and can reach dominance over large areas in the humid tropics (Janos 1983,
Alexander and Ho
¨
gberg 1986, Alexander 1989). The occurrence of mycorrhiza is essential to
understand the nutrient balance of humid tropical forests. The widespread limitation of P
availability over vast tropical areas emphasizes the importance of this biological interaction,
which is considered to increase the capability of water and nutrient uptake, particularly P, by
higher plants. Went and Stark (1968) proposed the occurrence in tropical forests of a ‘‘closed’’
nutrient cycle mediated by mycorrhiza preventing or reducing nutrient leaching. It is now
generally accepted that predominance of mycorrhizal symbiosis (both ecto- and endomycor-
rhiza) in the majority of humid tropical forests is certainly associated to low P availability in
the soil (Newbery et al. 1988). The frequency and percentage of mycorrhizal infection is
inversely related to soil pH and available P (van Noordwijk and Hairiah 1986). In tropical
forests with a thick root mat, phosphate solutions sprayed on the soil surface are effectively
taken up by VAM, thereby preventing nutrient leaching in these forests (Jordan et al. 1979).
The improvement in nutrient supply brought about by mycorrhizal symbioses is related to
the increase of surface for nutrient absorption, by penetrating the soil beyond the zone of
nutrient depletion around the fine roots. In addition, some mycorrhizal fungi are capable of
using organic P sources directly or through previous digestion by extracellular phosphatases
(Alexander 1989).
Diversity of VAM is generally low to very low compared with the diversity of host
vascular plants in tropical forests, and little information exists about the differential efficiency
of VAM species in the process of nutrient uptake and the specific relationships between VAM
and host species. Lovelock et al. (2003) showed that VAM communities in a tropical forest at
La Selva, Costa Rica, are affected by host tree species and soil fertility. These observations
were confirmed by the analysis of VAM community diversity in plantations on relatively
fertile soils (Lovelock and Ewel 2005). In plots planted alone or in combination of Cedrela
odorata, Cordia alliodora, and Hyeronima alcorneoides they showed that host tree species and
host plant diversity had strong effects on the VAM fungal community. VAM fungal diversity
(Shannon-index) was positively correlated with ecosystem net primary productivity, whereas
evenness was correlated with P-use effciency. The authors concluded that in tropical forests
diversity of VAM fungi and ecosystem NPP are correlated.
Nutrient availability in a given soil may be markedly affected by root competition.
Particularly in forests growing on nutrient poor soils, fine roots tend to accumulate near
and above the soil surface, developing a root mat that can exert a strong competitive pressure
for water and nutrients (Stark and Jordan 1977, Jordan et al. 1979, Cuevas and Medina 1988).
Root trenching experiments in a tropical rain forest of the upper Orinoco basin resulted in
increased concentration of N and P in the trenched saplings, and also a marked increase in
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