This MCQ module is based on: Patterns of Biodiversity
Patterns of Biodiversity
This assessment will be based on: Patterns of Biodiversity
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Patterns of Biodiversity
The diversity of plants and animals is not uniform throughout the world but shows a rather uneven distribution. For many groups of animals or plants there are interesting patterns in that distribution, and this part examines the two best-established ones.
Latitudinal gradients
The most well-known pattern is the latitudinal gradient in diversity. In general, species diversity decreases as we move away from the equator towards the poles. With very few exceptions, the tropics — the latitudinal range of 23.5° N to 23.5° S — harbour more species than temperate or polar areas.
| Place | Latitude | Species of birds |
|---|---|---|
| Colombia | Near the equator | Nearly 1,400 |
| India | Much of its land area in tropical latitudes | More than 1,200 |
| New York | 41° N | 105 |
| Greenland | 71° N | 56 |
The same gradient appears in plants. A forest in a tropical region like Ecuador has up to 10 times as many species of vascular plants as a forest of equal area in a temperate region like the Midwest of the USA.
The richest place of all
The largely tropical Amazonian rain forest in South America has the greatest biodiversity on Earth. It is home to:
- more than 40,000 species of plants;
- 3,000 of fishes;
- 1,300 of birds;
- 427 of mammals;
- 427 of amphibians;
- 378 of reptiles;
- and more than 1,25,000 invertebrates.
Scientists estimate that in these rain forests there might be at least two million insect species waiting to be discovered and named.
Why are the tropics so rich? Three hypotheses
What is so special about the tropics that might account for their greater biological diversity? Ecologists and evolutionary biologists have proposed various hypotheses; three are important.
(a) The tropics had more evolutionary time. Speciation is generally a function of time. Unlike temperate regions, which were subjected to frequent glaciations in the past, tropical latitudes have remained relatively undisturbed for millions of years, and thus had a long evolutionary time for species diversification.
(b) Tropical environments are less seasonal. They are relatively more constant and predictable than temperate ones, and such constant environments promote niche specialisation, which leads to greater species diversity.
(c) There is more solar energy available in the tropics, which contributes to higher productivity; this in turn might contribute indirectly to greater diversity.
Notice that the three are not rivals. Each supplies something the others do not: (a) explains why there has been time to accumulate species, (b) why narrow specialists can survive once they appear, and (c) why there is enough energy to support many populations at once. A complete explanation probably needs all three, which is why the chapter offers them together rather than choosing between them.
Species-area relationships
During his pioneering and extensive explorations in the wilderness of the South American jungles, the great German naturalist and geographer Alexander von Humboldt observed that within a region, species richness increased with increasing explored area — but only up to a limit.
In fact the relation between species richness and area, for a wide variety of taxa — angiosperm plants, birds, bats, freshwater fishes — turns out to be a rectangular hyperbola.
On a logarithmic scale, the relationship becomes a straight line, described by the equation:
\( \log S = \log C + Z \log A \)
| Symbol | Meaning |
|---|---|
| S | Species richness |
| A | Area |
| Z | Slope of the line (regression coefficient) |
| C | Y-intercept |
What Z turns out to be
Ecologists have discovered that the value of Z lies in the range of 0.1 to 0.2, regardless of the taxonomic group or the region. Whether it is the plants in Britain, birds in California or molluscs in New York state, the slopes of the regression line are amazingly similar.
But if you analyse species-area relationships among very large areas like entire continents, you find the slope of the line to be much steeper — with Z values in the range of 0.6 to 1.2. For example, for frugivorous (fruit-eating) birds and mammals in the tropical forests of different continents, the slope is found to be 1.15.
Within a region, Z is about 0.1 to 0.2. Across whole continents it rises to between 0.6 and 1.2 — and for frugivorous birds and mammals in tropical forests of different continents it is 1.15.
What a steep slope means numerically. Z is the exponent linking richness to area, so a slope of 1.15 means richness rises slightly faster than area itself: ten times the area holds more than ten times the species. A slope of 0.15 means ten times the area holds only about 1.4 times the species.
Why a single region gives a shallow slope. Expanding a study area within one region mostly adds more of the same. The species you find in a larger plot are largely the same species, plus a few rarer ones and a few from adjoining habitats. The regional pool is finite, so richness saturates — exactly Humboldt's observation that richness increases with explored area but only up to a limit.
Why continents give a steep slope. Each continent has had its own separate evolutionary history for tens of millions of years. Adding a second continent does not add more of the same species; it adds an entirely different set, because the species there are descended from different ancestors and are mostly endemic to that continent. There is no shared regional pool to saturate.
Why this matters for conservation. The steep continental slope says that the world's species are not interchangeable — a hectare of Amazon cannot be substituted by a hectare of African forest. And the shallow within-region slope has a sobering corollary read backwards: if losing area removes species slowly at first, then a reserve that preserves a fraction of a habitat preserves a good fraction of its species, but the last remnants are where the losses become steep.
🎯 Interactive: Explain the Pattern
Six observations about the distribution of diversity. Choose one to see which pattern or hypothesis accounts for it.
🎯 Competency-Based Questions
(a) The tropics had more evolutionary time. Speciation is generally a function of time, and unlike temperate regions subjected to frequent glaciations in the past, tropical latitudes have remained relatively undisturbed for millions of years, giving a long evolutionary time for species diversification. Test: compare the age of tropical and temperate lineages from fossil and molecular evidence; if the hypothesis holds, tropical clades should on average be older and temperate biotas should show signs of recent recolonisation after glacial retreat.
(b) Tropical environments are less seasonal, relatively more constant and predictable. Such constant environments promote niche specialisation, which leads to greater species diversity. Test: measure the breadth of diet, habitat and activity period of related species in tropical and temperate communities. The hypothesis predicts narrower niches and more overlap-free packing in the tropics.
(c) There is more solar energy available in the tropics, which contributes to higher productivity, and this in turn might contribute indirectly to greater diversity. Test: compare species richness against measured productivity across many sites at similar latitudes. If energy is the driver, richness should track productivity rather than latitude as such.
Why all three are offered together. They explain different things: (a) why there was time for species to appear, (b) why specialists can persist once they do, and (c) why enough resource exists to support many populations at once. None of them excludes the others, and the chapter presents them as hypotheses rather than conclusions because the question remains open.
What the slope is. The species-area relationship is a rectangular hyperbola on arithmetic axes, which becomes a straight line on a logarithmic scale, described by log S = log C + Z log A, where S is species richness, A is area, Z is the slope of the line, or regression coefficient, and C is the Y-intercept. Z therefore measures how fast species richness rises as area increases.
Its remarkable constancy within regions. Ecologists have found that Z lies in the range of 0.1 to 0.2 regardless of the taxonomic group or the region — plants in Britain, birds in California, molluscs in New York state all give amazingly similar slopes. That a single number should describe such different organisms in such different places suggests a general ecological rule rather than a local accident.
Its significance when the slope is steep. For very large areas such as entire continents, Z rises to between 0.6 and 1.2 — 1.15 for frugivorous birds and mammals in the tropical forests of different continents. A value near 1 means richness rises almost in proportion to area, because each continent contributes an almost entirely different set of species, having had its own separate evolutionary history. A shallow slope means additional area mostly adds more of the same species; a steep slope means it adds new ones.
Why it matters practically. Read backwards, the relationship predicts how many species will be lost when a habitat is reduced in area — which is the basis for estimating extinctions from deforestation, and for deciding how large a reserve must be to retain a given fraction of a region's species.
Why the curve flattens. The relation between species richness and area is a rectangular hyperbola, which rises steeply at first and then approaches a ceiling. The reason is that the number of species available in a region is finite. A small plot samples only some of them, so each addition of area finds several new ones. As the plot grows, most species in the regional pool have already been recorded, and further area adds only the rarest — so the gain per unit area falls steadily towards zero.
Why it does not flatten completely in practice. Expanding an area eventually crosses into a different habitat type, or a different region altogether, and then a fresh set of species appears. This is precisely why the slope becomes much steeper when very large areas such as entire continents are compared, with Z rising from 0.1–0.2 to 0.6–1.2.
What this implies for survey design.
(i) There is an efficient stopping point. Effort spent expanding a survey beyond the flattening of the curve buys very few additional species. Plotting a species-accumulation curve as the survey proceeds shows when that point has been reached.
(ii) Spread the effort rather than concentrating it. Several smaller plots in different habitats will record more species than one large plot of the same total area, because each plot begins again on the steep part of its own curve.
(iii) Never compare raw species counts from areas of different size. A larger sample will always yield more species. Comparisons must either use equal areas, or use the equation to standardise them.
What it reveals about biology: diversity is concentrated in small organisms. Among animals, insects are the most species-rich taxonomic group, making up more than 70 per cent of the total, so that out of every ten animals on the planet, seven are insects. Small body size means a single tree offers many separate niches — different leaves, bark, flowers, fruits, roots and stages of decay — where a mammal needs a territory. Short generation times also allow genetic divergence and reproductive isolation to accumulate faster.
What it reveals about our knowledge: the figures are not equally reliable. The mammal and amphibian counts are close to complete, because these animals are large, conspicuous and long studied. The invertebrate figure of 1,25,000 is a record of what has been found, and the estimate of at least two million insect species still awaiting discovery shows how far from complete it is. The uncertainty in our knowledge is concentrated exactly where the diversity is.
Why this is more than an academic gap. A large fraction of these species faces the threat of becoming extinct even before we discover them — nature's biological library is burning even before we have catalogued the titles of all the books stocked there. Undescribed species cannot be assessed, listed as threatened, or legally protected.
And a caution about using such figures. When comparing regions or arguing for conservation, remember that a low count may reflect low sampling effort rather than low diversity. This is the same difficulty that makes global estimates range from 7 million to 50 million species, and that leaves prokaryotes out of the count altogether.
The calculation. From log S = log C + Z log A, richness varies as S ∝ AZ. Reducing area to 90 per cent of the original gives
\( \dfrac{S_{new}}{S_{old}} = (0.90)^{0.15} \approx 0.984 \)
So about 1.6 per cent of the species would be expected to be lost — a small figure, and this is the reassuring part of the arithmetic. A shallow slope means that losing area removes species slowly at first.
Why the real loss is likely to be greater.
(i) Fragmentation, not just loss. A road does not merely remove 10 per cent of the area; it cuts the remainder in two. When large habitats are broken up into small fragments, mammals and birds requiring large territories, and animals with migratory habits, are badly affected, leading to population declines. The species-area equation assumes one continuous area of the new size, not two disconnected halves.
(ii) Which 10 per cent matters. The equation treats all area as equivalent. If the cleared strip includes a river, a salt lick, a breeding site or the only patch of a particular soil, the loss can be out of all proportion to the area — Ehrlich's point that loss of rivets on the wings is more serious than loss of rivets on the seats.
(iii) Endemism raises the stakes. In a biodiversity hotspot, species may be confined to that region and found nowhere else, so a local extinction is a global one.
(iv) Roads bring more than roads. Access enables logging, hunting, settlement and the introduction of alien species — each of which is an independent cause of biodiversity loss.
The honest conclusion. The species-area relationship gives a lower bound on the expected loss, and a useful one. It is not the whole answer, because it counts hectares and ignores their arrangement and their contents.
🧠 Assertion–Reason Questions
For each pair, decide whether both statements are true and whether the reason correctly explains the assertion.
Both A and R are true, and R is the correct explanation of A.
Speciation is generally a function of time, so an undisturbed region accumulates species while a repeatedly glaciated one keeps losing them and starting again. This is the first of the three hypotheses offered for tropical species richness.
Both A and R are true, and R is the correct explanation of A.
Within a region Z lies between 0.1 and 0.2, because extra area mostly adds more of the same species from a finite regional pool. Across continents Z rises to 0.6–1.2 — 1.15 for frugivorous birds and mammals in tropical forests of different continents — because there is no shared pool to saturate.
Both A and R are false, though A is nearly right for the wrong reason.
The relationship is a rectangular hyperbola; it becomes a straight line only when plotted on a logarithmic scale. And richness does not rise in direct proportion to area: Humboldt observed that it increases with increasing explored area but only up to a limit, and within a region the exponent Z is only 0.1 to 0.2, meaning ten times the area yields less than one and a half times the species.