Patterns of Biodiversity
Environment & Ecology › Biodiversity Basics and Classification · Topic 6.2
Patterns of biodiversity are the regular ways in which the number of species changes across space. The best known is the latitudinal gradient: species richness is highest in the tropics and falls towards the poles, with Colombia having over 1,400 bird species and New York around 105. Reasons offered include more solar energy and productivity in the tropics, stable climate over long periods, larger area of tropical regions and long evolutionary time, since temperate areas were hit by glaciation. Altitudinal gradient is similar, with diversity falling as height increases. The species-area relationship, found by Alexander von Humboldt, shows that species number rises with area in a rectangular hyperbola on a linear scale and as a straight line on a log scale, written log S = log C + Z log A, with Z usually between 0.1 and 0.2 for small regions and 0.6 to 1.2 for very large areas.
5 min read · UPSC Prelims · Environment & Ecology · Biodiversity Basics and Classification
At a Glance
- Richest region Tropics
- Trend Falls towards poles
- Species-area Humboldt
- Z value 0.1 to 0.2 typical
- Island theory MacArthur and Wilson
- Exam link UPSC Prelims, Environment & Ecology: Biodiversity Basics and Classification
Where Does It Fit?
This topic follows the definition and types of biodiversity. It explains how species numbers vary across the globe, before the classifications and hotspots that use these patterns. Previous topic: Definition and Types of Biodiversity (Genetic, Species, Ecosystem). Next topic: Bio-Geographical Classification of the World.
What Are the Main Patterns and Their Causes?
| Pattern | Description and reasons |
|---|---|
| Latitudinal gradient | Diversity falls from the equator to the poles. Tropical rainforests such as the Amazon hold the most species. India with tropical areas has over 1,200 bird species, against about 105 for New York |
| Reason: time | Tropics were relatively undisturbed by glaciation, giving more time for species to evolve |
| Reason: climate stability | Seasons are less variable, favouring specialisation and narrow niches |
| Reason: energy and productivity | More solar energy supports higher productivity and more species |
| Reason: area | The tropical belt is the largest biome by area |
| Altitudinal gradient | Diversity usually falls as elevation rises because of cooler temperature, thinner air and less area |
| Species-area relationship | Larger areas hold more species. On a log scale it is a straight line: log S = log C + Z log A |
What Do the Species-Area Curve and Island Theory Tell Us?
- S, A, C, Z: S is species richness, A is area, C is the Y-intercept, Z is the slope of the line (regression coefficient)
- Z values: 0.1 to 0.2 for areas of different sizes within a region, irrespective of taxon or region
- Large areas: For very large areas such as whole continents, the slope is steeper, with Z from 0.6 to 1.2
- Alexander von Humboldt: observed in South American forests that species richness increases with area up to a limit
- Island biogeography: MacArthur and Wilson (1967) proposed that the number of species on an island is a balance between immigration and extinction rates
- Island size and distance: large islands near the mainland hold more species than small, far islands
- Implication: habitat loss lowers species, with the area reduced by 90 percent causing loss of about half the species
- Conservation use: reserve design needs large, connected areas
What Else Should You Remember?
- Rapoport’s rule: species ranges are narrower in the tropics than at high latitudes
- Species-energy hypothesis: diversity follows available energy
- Mid-domain effect: species ranges overlap most in the middle of a bounded area
- Hotspots: regions of high endemism and threat; see Biodiversity Hotspots
- Longitudinal pattern: less marked than latitudinal pattern
- Depth gradient: marine diversity varies with depth, often highest at mid depths
- Coral triangle: highest marine diversity
- Amazon: about 40,000 plant species, 1,300 birds, 427 mammals, 378 reptiles and over 3,000 fish
- Western Ghats: a hotspot with high endemism in amphibians and plants
- Himalaya: shows an altitudinal gradient with mid elevation peaks
- Edge effect: more species at habitat boundaries
- Ecotone: transition zone between ecosystems
- Habitat fragmentation: breaks areas into smaller pieces, cutting species
- Extinction debt: species lost over time after habitat loss
- Wallace line: a faunal boundary between Asia and Australia
- Alfred Russel Wallace: a founder of biogeography
- Link to previous: see Definition and Types of Biodiversity (Genetic, Species, Ecosystem)
- Link to next: see Bio-Geographical Classification of the World
- Link to threats: see Threats to Biodiversity and Conservation Strategies macro
- Caution: the latitudinal gradient has exceptions, such as high diversity of some groups in temperate zones
- Marine pattern: shallow tropical seas such as coral reefs also show high diversity, while polar seas are less rich
- Island examples: the Andaman and Nicobar Islands and Lakshadweep show the theory of island biogeography
- Practical value: the species-area rule helps estimate species lost when a forest is cut
- Number tip: remember Z of about 0.1 to 0.2, and that it is the same for different taxa
- Exam hint: state the five reasons for the tropical richness: time, stability, energy, area and less glaciation
- Tropical regions: cover the largest area of any climate belt and hold most of the world’s species, which is why conservation attention concentrates there
Why Does It Matter for the Exam?
- Gradients: latitude, altitude
- Law: species-area
- Z value: 0.1 to 0.2
- Current affairs link: habitat fragmentation and linear projects
- Common errors: saying diversity rises towards the poles or confusing slope Z with intercept C
As an analytical point, these patterns explain why tropical forests and large intact areas are conservation priorities. The species-area rule also warns that shrinking habitat eventually costs species in a predictable way.
Why Is This Topic Important?
- Gradient Tropics richest
- Area Bigger holds more
- Islands Balance of arrival and loss
What Came Next?
The next topic covers the bio-geographical classification of the world. Next topic: Bio-Geographical Classification of the World.
Key People and Terms
- Latitudinal gradient Diversity change with latitude
- Species-area curve Species rise with area
- Z Slope of the line
- Island biogeography Theory on island species
- Ecotone Transition zone
- Extinction debt Delayed species loss
Exam Corner
Points to Remember
- Richest: tropics.
- Species-area by Humboldt.
- Z is 0.1 to 0.2.
- Island theory by MacArthur and Wilson.
- Diversity falls with altitude.
Do Not Confuse With
- C and Z Intercept versus slope
- Ecotone and edge effect Transition zone versus its richer biota
- Latitudinal and altitudinal gradient Poleward versus upward decline
Memory Hook
Warm, old, stable and big: that is why the tropics are rich.
Mains Angle
Questions ask for causes and the curve. These points help.
- Patterns Gradients
- Causes Reasons
- Use Reserve design
A Question You May Face
An original practice question, not a past paper question.
“Explain the latitudinal gradient in species diversity and the species-area relationship, and discuss their relevance for conservation.”
How to Answer
- Gradient Latitude.
- Causes Reasons.
- Curve Species-area.
- Use Reserves.
GS Relevance
Frequently Asked Questions
What is the latitudinal gradient of biodiversity?
The latitudinal gradient is the pattern in which the number of species is highest near the equator and decreases towards the poles. For example, the tropical forests of the Amazon hold far more species of trees, birds and insects than the forests of high-latitude regions. This is one of the oldest patterns recognised in ecology.
Why are the tropics richer in species?
The tropics have a stable climate, high solar energy that supports productivity, a large area, and a long unbroken evolutionary history because they escaped the glaciations that wiped out temperate life. These factors allowed more species to evolve, survive and specialise in narrow niches.
What is the species-area relationship?
The species-area relationship states that the number of species increases with the size of the area explored, in the form of a rectangular hyperbola. On a logarithmic scale it becomes a straight line described by log S equals log C plus Z log A, where Z is the slope, usually 0.1 to 0.2.
What is the theory of island biogeography?
The theory of island biogeography, proposed by MacArthur and Wilson in 1967, says that the number of species on an island is a dynamic balance between the rate at which new species arrive and the rate at which resident species go extinct. Large islands near the mainland have more species than small, distant ones.
How does altitude affect species diversity?
Species diversity generally declines with increasing altitude because temperature falls, the air becomes thinner, the growing season shortens and the area available becomes smaller. In mountains such as the Himalaya, many groups show highest diversity at low or mid elevations and fewest species near the snowline.
PYQ Practice — Statement Analysis
1 Species diversity generally decreases from the equator to the poles.
The latitudinal gradient.
2 The species-area relationship was described by Charles Darwin.
By Alexander von Humboldt.
3 The slope Z of the species-area line is typically 0.1 to 0.2.
For regions of different sizes.
4 Large, distant islands hold fewer species than small islands near the mainland.
Large and near ones hold more.
Past Mains Questions on This Topic
This topic comes under Biodiversity Basics and Classification. UPSC Mains questions asked on the matching syllabus topic, year-wise with marks:
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