The Tropical Rain Forest

"... the most complex ecosystem on earth ... the tropical rain forest is one thousand times more biologically complex than the tropical reef system, the second most complex system on earth, with one million times greater biodiversity than our own ecosystem here."
- Mike Robinson, Director of National Zoo
 

In this lesson, we wish to ask:

  • How can the most productive forests in the world occur on soils of extremely low fertility?
  • Why is biological diversity concentrated in the tropics?
  • What are the consequences if humid tropical forests are almost totally destroyed? 

Jump to: [Introduction] [Climate and Geography] [Nutrient Cycling and Productivity] [Biodiversity] [Human Use and Sustainability] [Summary]

 
11/06/2008 Format for printing

Introduction

In previous lectures we focused on general principles of ecosystems, emphasizing the processes of biogeochemical cycling and energy transfers. In the next lectures we will look at one ecosystem in detail, the tropical forest. There are several reasons for this. Ecosystems may all function according to the same basic principles, but they most certainly don't all look the same and it is important to have some understanding and appreciation of this diversity. Second, it is important to learn about the "specifics" of ecosystems as well as the "generalities". Finally, we can use this examination of the tropical forest to help tie together some of the material that has been presented in the ecology and evolution sections of the course. 

Today we will examine the most productive and diverse ecosystem found on land: the tropical rain forest. These ecosystems are also, and perhaps more accurately, called humid tropical forests. These ecosystems are also changing rapidly, as Figure 1 illustrates in terms of the past and present distribution of tropical forests on earth.


Figure 1: Present and original extent of humid tropical forest

Climate and Geography

Certain ranges of temperature and rainfall characterize the places where tropical rainforests occur: 


Figure 2: Vegetation and latitude in Africa

Temperatures generally fall between 23 - 27 deg C, with a greater daily than monthly range. In other words, there is no strong seasonality of temperature (unlike what we experience in Michigan).

Rainfall tends to be highest near the equator, where the sun's evaporative power causes high evapotranspiration, and rising air cools and then sheds its moisture. Precipitation tapers off as one moves away from the equator, and dry belts are found at 25-30 deg of latitude. Local variation can also be great due to trade winds, ocean currents, land masses, and mountain ranges. 

Evergreen forests are replaced by deciduous forests as precipitation becomes seasonal. Wherever dry periods are several months or longer in duration, leaves are shed as the dry season takes hold, providing a winter-like visual appearance. Leaves re-appear in anticipation of or with the onset of the rains. (A dry month is one where evapotranspiration exceeds precipitation.) The growing season is thus shortened, and so forest productivity is less than in the evergreen forests of the more humid tropics. At lower annual rainfall (ca. 1500 mm), forest gives way to savanna as can be seen in the vegetation map of Africa in Figure 2. 

Boundaries between ecosystems or biomes are often gradual, and they can be sensitive to changing conditions. A prolonged period of wetness or drought, or human intervention, can cause dramatic changes because of the transitional nature of environmental conditions near the boundaries between biomes. 

Humid tropical forests appear superficially similar everywhere, but in fact they differ widely in species composition and ecosystem attributes. In the coterminous United States, botanists recognize 135 natural plant formations based on dominant species, and driven by latitude and climate. This system is called the Holdridge system (Figure 3) and it is widely used for conservation purposes. However, its use is far from feasible in tropics. Instead, the future in classifying tropical rainforest plant formations may lie in remote sensing, where large areas can be mapped relatively quickly. 


Figure 3: Holdridge vegetation classification system

Nutrient Cycling and the Productivity of Humid Tropical Forests


Figure 4: Tropical tree with thin topsoil and deep, unweathered rocks
 
The first Europeans to view humid tropical forests were stunned by the luxuriant growth, giant trees with huge buttresses, thick vines, plants growing on plants (epiphytes), and so forth. Such luxurious growth signals high productivity, and modern scientific measurements confirm this. If one measures the photosynthesis, or captures the litterfall of leaves, branches, fruit and other plant parts to the forest floor, one finds the production of tropical evergreen forests to be roughly double that of temperate forests. 

It would be natural to infer that tropical soils are very fertile in order to support this high productivity. But, as we have seen in other instances, or general inferences about what makes sense are often incorrect -- we must look more closely at the system and analyze how it functions. In fact the soils are very thin and the rock below them highly weathered (Figure 4). 

You already know that ecosystems are open with respect to nutrient cycling, meaning that inputs and outputs are significant. (Remember that the entire Globe is closed with respect to nutrient cycling, because the inputs and outputs to Earth as a whole are extremely small.) What makes humid tropical forests so productive is the combination of high temperatures, light, and rainfall year-round (good growing conditions), coupled with especially efficient nutrient recycling. 
 

What is the evidence for this claim?

First, analysis of soils of tropical regions shows them to be virtually devoid of soluble minerals. Rocks weather rapidly due to high temperatures and abundant moisture, and millennia of rapid weathering and torrential rains to wash away nutrients from the soils have left the soils very low in nutrient stocks. 

This is supported by the analysis of stream water draining tropical regions, which likewise reveals a scarcity of dissolved nutrients. Most tropical soils are clays with little soluble mineral content, and moderate to strong acidity which interferes with the ability of roots to take up nutrients. Only about 20% of the humid tropics has soils that can support agriculture, and most of this area is already in use. 
 

If the nutrients aren't in the soils, where do they come from?

 


Figure 5: Nutrient budget in a tropical forest

Figure 5 shows a budget accounting that indicates nutrients are found mainly in living plant biomass and in the layer of decomposing litter; there is little nutrient content of the deeper soil, as there is in temperate-zone ecosystems. This suggests that plants are intercepting and taking up nutrients the moment they are released by decomposition. 

There are many organisms that are players in this decomposition process: termites, bacteria, fungi, various invertebrates. Of particular importance are micorrhizal fungi which invade the roots of trees to obtain nourishment. As we learned in the lecture on Microbes, these fungi gain carbon nourishment from the tree and they benefit the tree by providing a vastly expanded nutrient gathering network in the soils. In some circumstances tree roots even grow upward toward the soil surface, permeating the litter layer. 

Isotope experiments have shown the importance of roots in nutrient uptake. For example, one study in the Amazon rain forest, which used Ca-45 and P-35, found that more than 99% of the nutrients added to the system (in the form of isotopes) were retained in root mats. More commonly, about 60 - 80% of nutrients are retained by the roots, and thus made available to the tree. The remaining 20 - 40% needed by the tree must be made up by fresh inputs, either from rainfall or rock weathering. 

What happens when the forest is harvested for timber or other plant products, or the forest is burned? In all these cases nutrients will be lost from the ecosystem, but the outputs cannot exceed inputs for very long because the stock of nutrient capital in the system will be depleted. When forests are burned, or the cut timber is removed as in logging, the nutrients that were in the tree biomass are either washed out in the case of burning or simply removed from the system. Because there was only a small stock of nutrients in the soil and most of the nutrients were in the biomass, there is little nutrient stock remaining to support regrowth. This is why slash and burn agriculture does not work for more than a few years after burning, and why the land is made very infertile and growing new vegetation is difficult. We can't simply "regrow" tropical forests once they are burned -- once they are lost they are gone forever (or at least for 1000s of years, and even then the species that regrow will be different from the original forest species). 

Table 1 shows 7 tropical forests, arranged roughly from least to most fertile soils. Note the range of above-ground biomass is about twofold. Yet the nutrient stocks vary by several orders of magnitude (an "order of magnitude" is equal to one power of ten, so that 100 is one order of magnitude greater than 10, and 1000 is two orders of magnitude greater than 10). The greatest above-ground productivity is in the Ivory Coast forest, on soils of intermediate fertility. This reinforces the point that you cannot guess the fertility of the soils of a tropical forest by looking at the trees. 

Look next at the root biomass, which correlates pretty well with the soil fertility. Root biomass is highest where soil quality is poorest, and vice-versa. There is also a "causal" explanation for this correlation; when soil nutrients are high, the tree does not need to spend as much energy in building roots to forage in the soil for new nutrient sources. Competition for nutrients presumably is very strong at the Venezuelan sites with low soil fertility and high root biomass, whereas competition for light presumably is most important in the Ivory Coast forest. At the Venezuelan sites we also see a well developed surface root mat infiltrating the litter. We also see tougher, more slowly decaying leaves at the poor fertility sites. This is because leaves are held longer under poor growth conditions (their turnover time is longer), and because they are exposed to herbivores longer they must be better protected (meaning they need to be tough and unpalatable). This causes slow decomposition of the leaves once they are dropped to the forest floor, and further retards the forest's productivity.

Biodiversity

Tropical forests, covering 7% of the earth's surface area, contain perhaps 50% of the world's species. What causes this prodigious concentration of biological diversity? 

Until ten years ago, if you had asked any biologist how many species of plants and animals lived on earth, the answer probably would have been "about 2 million." This would include the nearly 1.5 million described species, and allowed for another half million un-described species. 

 


Figure 6: Breeding bird species of North and Central America
 

Then, in 1982, Smithsonian biologist Terry Erwin developed a technique to fumigate the crowns of individually selected forest trees with biodegradable pyrethrin (the same chemical in mosquito coils). A huge number of previously unknown spiders, insects, and other invertebrates came tumbling down onto tarps spread on the forest floor. Based on the high proportion of undescribed species, and the expectation that each tree species contains many host-specific species (species that live only in that host tree), our estimates of biological diversity have been drastically altered. One commonly hears the figures of 5 to 30 million species, but the truth is we don't know. In fact, we know more about the stars in the sky than we do about the species on earth. We are certain that tropical forests contain a great many species, and most of these are unknown to science. 

We also know that the tropics are highly diverse based on evidence from well-studied groups, including the vertebrates and flowering plants. Whenever one compares the number of species along a latitudinal gradient (Figure 6), one observes a trend of increasing numbers of species towards the equator. 

Why are tropical forests so diverse? We only have partial answers. One class of answers centers around the spectacular specialization we observe in tropical forests. Tropical species exhibit highly specialized ecological roles. However, this begs the question of how these species became so specialized and diverse, and here we turn to an evolutionary perspective. 

First, let's examine two examples of the high degree of specialization found in tropical forests. The forests themselves are multi-layered. A temperate forest usually has two or three main layers. In an undisturbed forest the trees are fairly similar in height, there usually is some ground vegetation, and in between there may or may not be a shade-adapted middle layer. But tropical forests are vertically more complex (Figure 7). As many as perhaps five layers exist, although the distinctness of layers is arguable. 


Figure 7: "Layers" in a Dipterocarp Forest


Figure 8: Arboreal versus ground-dwelling mammals, day and night 

 


Figure 9: Bird guilds and ecological specialization (light bars for the tropics, dark bars for the temperate zone)

We also see evidence of great ecological specialization, as illustrated for mammals living in trees and on the ground which are active at day versus at night (Figure 8). The term "guild" is used much as it is in human society, to describe a collection of individuals who make a living in the same way. Human examples include cobblers, brewers, and professors. In the animal kingdom we use the word guild to indicate a finer sub-division than trophic level. As Figure 9 illustrates for birds, there are more guilds in the tropics than in the temperate zone, and more species per guild. 

Let's now turn to the deeper question of how this greater specialization came about. Although we don't fully understand why more species are formed in one place than another, we do know that geographical isolation of small populations for a long time promotes species formation (refer back to the Lecture on The Process of Speciation). This is because those isolated populations become independent genetic and hence independent evolutionary units. If the gene pool is small and the environment is unique, evolutionary specialization is likely. 

It also seems likely that the forests of the tropics have gone through many cycles of fragmentation and reunion, due to the same global climate changes that gave us repeated bouts of glaciations at higher latitudes. These repeated episodes of forest retreat and advance would provide numerous opportunities for forest-dwelling species to be isolated into separate small populations. This in turn allows genetic change and evolutionary specialization to occur. 

The reasoning goes as follows. The border between forest and non-forest in present-day tropical South America closely follows the line of 1500 mm annual precipitation.
 

Figure 10: Contemporary pattern of rainfall in South America

During periods of glaciation, the earth's average temperature was cooler, and this would result in less evaporation and thus less rainfall. During these dry periods, the area receiving more than 1500 mm of rainfall would be reduced and fragmented. 

During wetter periods associated with interglacials (time during the glacial retreats), forests would expand and rejoin. If the dry periods correspond roughly to periods of glacial advance, they would have lasted 50 to 100 thousand years, which likely is sufficient time for evolutionary divergence. This process has happened over and over, in conjunction with the many cycles of glaciation that the earth has experienced in the last several million years. Therefore the Milankovitch cycles , which drive much of the glacial activity, may have acted as a "species pump", causing the process of speciation to be more active in the tropics and resulting in more species found there today. 

Now, we must also remember that this idea is speculation because we cannot demonstrate the process in experiments and we can't go back in a time machine to observe the process directly. However, the process does correspond well to what we know about the causes of species formation, and how climate influences the distribution of dominant vegetation.

Some other factors probably contribute to the rich specialization of tropical rain forests. Two of the favored candidate factors are high year-round productivity, and the lack of any need to adapt to harsh environment conditions. In addition, specialization may favor further specialization, in a kind of runaway cycle. 
 

Human Use and Sustainability

Tropical forests once covered 15-20% of earth's land surface. About half of this is now replaced by cropland, pasture, tree plantations, secondary forest, or wasteland. We are in a race between human destruction and human discovery. Some say we have less than 50 years before we'll hit bottom, with perhaps only 5-10% of tropical forests remaining. 

Why are we rapidly converting these lush, productive, and biologically diverse ecosystems to timber production and agriculture? Clearly, this is to meet the needs for food and land of the rapidly growing number of peasant farmers in tropical countries. Equally clearly, there is a need to meet this demand. The question is, are we doing so in a sensible way? Ecosystem science gives us a basis to evaluate this aspect of change now occurring on a global scale, using the criteria of productivity and ecological sustainability. 

The two primary categories of disruption that result from the conversion of tropical rainforests to agricultural land concern nutrient and water cycles.

1. Disruption of nutrient cycles.

Traditional slash and burn agriculture releases the nutrients held in above ground biomass to produce a high yield from a small area right after the burning. Afterwards, such areas are left fallow (unused) for years to decades because the nutrients have been mostly lost from the system, as described earlier in this lecture. This traditional land use is not really "sustainable" because the majority of the land is fallow at any one time and new areas of forests must be cut and burned. 

Alternatives to this agricultural system are highly debatable. There have been some spectacularly unsuccessful efforts to adapt modern agriculture from the temperate zone to tropical conditions. Without fertilizers, crop yields decline each year as the remaining nutrients in the soil are further depleted. Mechanization and fertilizers usually produce high yields, but the rate of soil erosion and degradation indicate that these practices are not sustainable into the future. High-tech agriculture also is costly and requires a level of technological sophistication that is inconsistent with the low-tech needs of rural agriculture. As a consequence, many people regard such efforts with great skepticism. However, research continues, and solutions would benefit people and simultaneously relieve some of the pressures on remaining wildlands. 

2. Disruption of the water cycle

Not just nutrients are lost when the forest is removed. The water cycle itself is disrupted, and the initial consequence is increased erosion because there is no vegetation to act as a "buffer" to hold the water in the plants and soils.  Another likely consequence is a long-term and irreversible decline in available water in the region. Initially in this lecture, we emphasized how climate determined the type of ecosystem in any tropical area, and thus its productivity. Here we see that ecosystems influence climate in the form of a feedback through the water cycle. An area as vast as the Amazonian rain forest recycles a great deal of rainfall back into the atmosphere by transpiration. If the forest is removed, that precipitation will run off to the sea via river flow, as has been demonstrated in many experiments where forests are clear cut. Evaporation of sea water will of course return fresh water to the atmosphere, but it is very unlikely that the Amazon rain forest will receive much of the rainfall. The climate of the Amazon region will become drier, and it is questionable whether a humid tropical forest would ever be able to re-establish. 

This inference is supported by a computer model in which the Amazonian forest was replaced by grasslands due to land use change. Surface temperatures increased in the model, evapotranspiration declined, and precipitation also declined. It appears that a dry season would occur, sufficient to prevent the re-establishment of a humid forest.

Summary

  • Tropical rain forests are found in regions where temperatures and precipitation are high year-round  
  • High primary productivity in tropical rain forests is due to the combination of climate and efficient recycling of nutrients through plant biomass 
  • Tropical rain forests may contain 50% or more of the world's biodiversity. High biodiversity appears related to high ecological specialization of species. 
  • Periods of forest fragmentation in the past, driven by global changes in climate such as glacial cycles, may have led to high rates of speciation due to geographic isolation. 
  • Tropical rain forests are being converted to agricultural land, with associated erosion and disruptions of nutrient and water cycling. 

Review

Suggested Readings

Terborgh, John. 1992. Diversity and the Tropical Rainforest. New York: Scientific American Library. 242 pp.
 

All materials the Regents of the University of Michigan unless noted otherwise.