Environment & Ecology · UPSC Notes
Terrestrial & Aquatic Biomes — UPSC Environment Notes
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Types of Ecosystems and Tropical Evergreen Forests
Ecosystems are divided into terrestrial and aquatic types. Terrestrial ecosystems are further classified into biomes, with the Tropical Evergreen Forest being the most productive. Located near the equator, these forests are characterized by high temperatures, heavy rainfall, and immense biodiversity.
Types of Ecosystems
Ecosystems are broadly categorized into two major divisions:
1. Terrestrial Ecosystem: A land-based community of organisms where biotic and abiotic components interact (e.g., forests, grasslands, deserts).
2. Aquatic Ecosystem: Includes water-based environments, further divided into Marine (oceans) and Freshwater (rivers, lakes) environments.
Biomes
To study terrestrial ecosystems efficiently, we divide them into Biomes. A Biome is a major community of plants and animals that share similar life forms and adapt to similar environmental conditions.
Tropical Evergreen Forest Biome
This biome is the most biologically diverse and productive region on Earth.
1. Distribution
Found between 5 degrees and 10 degrees North and South of the equator.
Major Regions: Amazon Basin (South America), Congo Basin (Africa), and the Indo-Malaysian region (Java, Sumatra, Borneo, Malaysia).
2. Climate
Temperature: Consistently warm and frost-free throughout the year, with a monthly average around 27 degrees Celsius.
Precipitation: Mostly wet throughout the year. Cloudiness and heavy rain help moderate the daily high temperatures.
3. Plant and Animal Species
Flora: Tall, tightly spaced evergreen trees are dominant. Woody vines and climbers (epiphytes) are common. The forest floor is usually dark and shaded by a thick canopy of tree crowns.
Fauna: Includes herbivores like sloths and tapirs; carnivores like jaguars; and various species like monkeys, toucans, and parrots.
4. Productivity
The productivity of this biome is the highest in the world.
It accounts for approximately 40 percent of the total global biological productivity.
| Feature | Details |
|---|---|
| Latitudinal Extent | 5 degrees to 10 degrees N & S of Equator |
| Average Temperature | Around 27 degrees Celsius |
| Global Productivity | Accounts for 40% of world's total |
| Key Flora | Tall evergreen trees, Woody vines, Canopy layers |
| Key Fauna | Jaguars, Sloths, Monkeys, Toucans |
Prelims tips
- Tropical Evergreen forests are found in the equatorial belt (5-10 degrees N/S).
- These forests have a multi-layered structure with a dense canopy that limits sunlight to the forest floor.
- They are the most productive biomes, contributing 40% to global biological productivity.
- Major regions include the Amazon (Selvas), Congo, and Indo-Malaysian archipelago.
- The climate is characterized by high humidity and consistent warmth (no winter season).
Mains points
- The high productivity of Tropical Evergreen forests makes them a critical 'carbon sink,' helping regulate the global climate by absorbing vast amounts of CO2.
- Deforestation in the Amazon and Congo basins poses a severe threat to global biodiversity and indigenous communities residing in these biomes.
- The dense canopy structure creates unique micro-environments at different heights, allowing a vast array of niche-specific species to coexist.
- Soil in these forests is often nutrient-poor because the high rainfall causes rapid leaching, and nutrients are quickly re-absorbed by the dense root systems.
Monsoon Deciduous Forests
Monsoon Deciduous Forests, also known as Tropical Deciduous forests, are found in regions with distinct wet and dry seasons. The trees shed their leaves during the dry period to conserve water. This biome is highly significant as it supports the world's largest human population and intensive agriculture.
Distribution and Location
These forests are found in the tropical regions between 5 degrees and 30 degrees latitude on both sides of the equator.
Key Regions: They are most well-developed in India, Burma (Myanmar), Thailand, Laos, Cambodia, parts of Vietnam, South China, and Northern Australia.
Climate Characteristics
The environment of this biome is defined by a rhythmic cycle of seasons:
Seasons: Characterized by distinct tropical rainy seasons and prolonged dry seasons.
Temperature: Summers are hot, with average temperatures ranging from 27 degrees to 30 degrees Celsius.
Rainfall: The average annual precipitation is approximately 1500mm, mostly concentrated in the monsoon months.
Plant and Animal Species
Flora: The trees are deciduous, meaning they shed their leaves during the dry period to survive drought conditions. While biodiversity is high, there are fewer plant species compared to the evergreen forest biome. Major species include Sal, Teak, and Bamboo.
Fauna: This biome supports large mammals such as rhinos, elephants, tigers, and wild buffalo. It is also home to a vast variety of bird species.
Human Interaction and Economy
This biome is unique because it supports the largest human population in the world.
Agriculture: The primary economic activity is farming. The fertile plains and seasonal rains are ideal for growing major crops like Rice, Sugarcane, and Jute.
Impact: Due to the high population density, large areas of these forests have been cleared for human settlements and intensive cultivation.
| Feature | Details |
|---|---|
| Latitudinal Extent | 5 degrees to 30 degrees N & S |
| Average Annual Rainfall | Approx. 1500mm |
| Survival Strategy | Deciduous nature (shedding leaves in dry season) |
| Economic Importance | Intensive Agriculture (Rice, Sugarcane, Jute) |
| Commercial Timber | Teak and Sal |
Prelims tips
- Monsoon Deciduous forests are the most widespread forests in India.
- The primary reason for shedding leaves is to reduce transpiration and conserve water during the dry season.
- This biome supports the highest human population density globally.
- Teak and Sal are commercially very important timber species found here.
- The rainfall range (around 1500mm) places them between Evergreen forests (>2000mm) and Thorn forests (<750mm).
Mains points
- The monsoon deciduous biome is a critical region for global food security, as the seasonal rains dictate the agricultural calendar for billions of people.
- Deforestation and land-use changes in this biome have led to increased human-wildlife conflict, particularly involving elephants and tigers in South and Southeast Asia.
- Unlike evergreen forests, the open canopy of deciduous forests during the dry season allows more sunlight to reach the ground, often resulting in a thicker undergrowth of shrubs and grasses.
- The sustainable management of teak and sal forests is vital for the timber industry, providing a balance between economic gain and ecological preservation.
Savanna Biome (Sudan Type Climate)
The Savanna biome is a transitional zone between lush equatorial forests and hot deserts. It is characterized by an 'open park-like' appearance with tall grasses and widely spaced trees, supporting the world's largest concentration of grazing mammals.
Distribution and Regional Names
The Savanna climate is a transitional zone found between the equatorial forests and the hot deserts. It is best developed in Sudan, which is why it is often called the 'Sudan Climate'.
Africa: Extends from West African Sudan to East Africa and Southern Africa.
South America: Known as Llanos in the Orinoco basin (Venezuela/Colombia) and Campos in the Brazilian Highlands.
Australia: Found in Northern Australia.
Climate: The Land of Extremes
Seasons: It has highly distinct wet and dry seasons. Unlike the Monsoon climate, the rainy season is not as long or reliable.
Temperature: The annual average temperature stays above 18 degrees Celsius. The diurnal range (daily difference) is high, with hot days and cold nights.
Plant Adaptation: Park-like Appearance
Because soil moisture is insufficient to support a dense forest, trees are spaced widely apart.
Vegetation Structure: It has an 'open park-like' appearance where tall grasses form a dense lower layer between scattered trees.
Key Species: Famous trees include the Baobab (the 'bottle tree' that stores water), various Palms, and Eucalyptus (in Australia).
Animal Life: The Big Game Country
African Savanna: Hosts the world's largest number of grazing animals (herbivores) like Zebra, Giraffes, Elephants, and African Buffalo.
Australian Savanna: Dominated by Kangaroos.
Human Interaction
The economy is largely tribal and varies by region:
Masai: Located in East Africa, they are primarily pastoralists (cattle herders).
Hausa: Located in Northern Nigeria, they are settled farmers.
Agriculture: Generally underdeveloped due to the extreme dry season and poor soil quality.
| Parameter | Details |
|---|---|
| Alternative Name | Sudan Type Climate |
| South American Names | Llanos (Orinoco) and Campos (Brazil) |
| Vegetation Style | Parkland (scattered trees and tall grass) |
| Characteristic Tree | Baobab (stores water) |
| Human Tribes | Masai (Pastoralists) and Hausa (Farmers) |
Prelims tips
- Savanna is often called 'Big Game Country' due to the concentration of large wild animals.
- Llanos and Campos are the tropical grassland names specifically used in South America.
- The Baobab tree is a 'succulent' tree that survives the dry season by storing water in its thick trunk.
- Unlike Temperate grasslands (Steppes), Savanna is a TROPICAL grassland.
- Masai tribes are famous pastoralists of the East African Savanna.
Mains points
- The Savanna serves as a vital ecological buffer between the expanding Sahara Desert and the shrinking tropical rainforests of Africa.
- Human activities like overgrazing and frequent bushfires for clearing land are accelerating soil erosion and desertification in the Sudan region.
- The biome's tourism potential (safaris) is a major economic driver for East African nations, though it requires a delicate balance between conservation and commercialization.
- Understanding the water-storage adaptations of Savanna flora (like the Baobab) is essential for developing drought-resistant agricultural strategies in semi-arid regions.
Desert Biome
Hot deserts are typically located on the western margins of continents between 15 and 30 degrees latitude. Characterized by extreme temperatures and very low rainfall (below 30 cm), life here depends on specialized adaptations like water-storing tissues in plants (xerophytes) and heat-regulating features in animals.
Distribution of Hot Deserts
Major hot deserts are found on the western coasts of continents between 15 degrees and 30 degrees North and South latitudes.
Africa: Sahara (largest), Kalahari, and Namib Deserts.
Asia: Arabian, Iranian, and Thar (India/Pakistan) Deserts.
Australia: Great Australian Desert.
Americas: Atacama (driest - South America), and the Mohave, Sonoran, and Mexican deserts in North America.
Climate: Extreme Heat and Scanty Rain
Temperature: Average summer temperatures are around 30 degrees Celsius, but extremes can reach up to 58 degrees Celsius (e.g., Al Azizia, Libya).
Diurnal Range: There is a very high difference between day and night temperatures.
Precipitation: Rainfall is very low, usually below 30 cm annually.
Adaptations: Surviving the Heat
1. Plants (Xerophytes)
Plants in deserts are called Xerophytes. They have specialized features to conserve water, such as:
Thick, fleshy stems to store water.
Spines instead of leaves to reduce water loss through transpiration.
Long root systems to reach deep groundwater.
2. Animals
Common animals include arthropods, reptiles, and small mammals like rodents, foxes, and rabbits.
Adaptation Example: The black-tailed jackrabbit has extra-long ears filled with blood vessels that help radiate excess body heat into the air.
Human Inhabitants
Desert populations are often categorized by their lifestyle:
Primitive Hunters/Collectors: Bushmen (Kalahari) and Bindibu (Australia).
Nomadic Herdsmen: Tuaregs (Sahara), Bedouins (Arabia), and Gobi Mongols.
Others: Caravan traders, settled cultivators near oases, and mining settlers (e.g., copper mining in Atacama).
| Continent | Major Desert Name |
|---|---|
| Africa | Sahara, Kalahari, Namib |
| Asia | Arabian, Thar, Iranian, Gobi (Cold) |
| Australia | Great Australian Desert |
| North America | Mohave, Sonoran |
| South America | Atacama (Peruvian) |
Prelims tips
- Most hot deserts are on the WESTERN margins of continents due to cold ocean currents and off-shore trade winds.
- Xerophytes are plants specifically adapted to dry environments.
- The Atacama Desert is the driest place on Earth.
- High diurnal range means the difference between the day's highest and the night's lowest temperature is very large.
- The Tuaregs (Sahara) and Bedouins (Arabia) are key nomadic tribes associated with this biome.
Mains points
- The location of deserts at 15-30 degrees latitude is primarily due to the presence of subtropical high-pressure belts where air descends, inhibiting cloud formation.
- Desertification is a major global threat, often caused by overgrazing and climate change, turning semi-arid lands into unproductive deserts.
- Indigenous knowledge of tribes like the Bedouins or Bushmen is vital for sustainable survival and biodiversity conservation in extreme arid environments.
- Modern technology, such as solar power and drip irrigation, is transforming desert economies, turning high-sunlight areas into energy and agricultural hubs.
Mediterranean Biome
The Mediterranean biome is unique for its 'Winter Rain and Dry Summer' climate. Found on the western margins of continents between 30 and 40 degrees latitude, it is world-famous for citrus fruits, viticulture (winemaking), and drought-resistant sclerophyllous vegetation.
Distribution and Locations
This biome is found between 30 degrees and 40 degrees latitudes in both hemispheres, typically on the western parts of continents.
Europe/Africa/Asia: Lands bordering the Mediterranean Sea (Southern Europe, North Africa, Western Turkey, Syria, Israel, Lebanon).
North America: Central and Southern California (USA).
South America: Central Chile.
Australia: Coastal zones of Western and Southern Australia.
Africa: The southwestern tip (Cape region).
Climate: Dry Summers and Wet Winters
Unique Feature: Unlike most biomes, the maximum rainfall occurs in winter. Summers are warm and dry.
Temperature: Winters are cool (5-10 degrees Celsius), while summers range from 20-27 degrees Celsius.
Precipitation: Average annual rainfall is between 370mm and 650mm.
Plant Adaptations: Sclerophylls
Plants here are called Sclerophylls. They have small, hard, or thick leathery leaves designed to resist water loss (transpiration) during the long, dry summers.
Trees: Holm oaks, olive trees, laurels, carob, junipers, and cypresses.
Aromatic Herbs: Rosemary, thyme, sage, and oregano.
Animal Life
The biome supports a variety of mammals and birds adapted to hilly and shrubby terrains.
Common Species: Wild goats, sheep, cattle, mouflon (wild sheep), lynx, and wild boar.
Human and Economic Significance
Known as the 'Orchard of the World' for its massive fruit production.
Agriculture: Citrus fruit cultivation (lemons, oranges), cereal production, and olive oil industry.
Viticulture: World-renowned for grapes and winemaking.
Industry: Engineering, mining, and agricultural processing.
| Region | Local Vegetation Name |
|---|---|
| France | Maquis |
| Italy | Macchia |
| California (USA) | Chaparral |
| Chile | Matorral |
| South Africa | Fynbos |
Prelims tips
- Rainfall in winter is the 'Gold Standard' identifier for the Mediterranean climate.
- Trees have 'sclerophyllous' features (hard, waxy leaves) to survive drought.
- This biome is the largest producer of Citrus fruits and Grapes (Viticulture) globally.
- It is found on the WESTERN margins of continents.
- Local names like Chaparral (USA) and Maquis (France) are frequently asked in exams.
Mains points
- The Mediterranean biome is highly susceptible to wildfires during the dry summer months, which is a natural part of the ecosystem but has been worsened by climate change.
- Intensive agriculture and tourism in the Mediterranean basin put immense pressure on limited freshwater resources, especially during the dry summers.
- Transhumance (seasonal movement of livestock) was historically a key cultural and economic practice in the European Mediterranean regions.
- The unique timing of the growing season (starting with winter rains) requires specialized agricultural techniques compared to temperate or tropical biomes.
Temperate Grassland Biome
Temperate grasslands are located in the interiors of continents in the Northern Hemisphere and on the margins in the Southern Hemisphere. Known as the 'Granaries of the World,' they are characterized by perennial treeless grasses and have been extensively converted for mechanized wheat and maize cultivation.
Global Distribution and Local Names
Temperate grasslands are found across the globe but are known by specific regional names:
Eurasia: Known as Steppes (stretching from the Black Sea to China).
North America: Known as Prairies (between the Rockies and the Great Lakes).
Argentina & Uruguay: Known as Pampas.
South Africa: Known as Velds (between Drakensberg mountains and Kalahari Desert).
Australia: Known as Downs (Murray–Darling basin).
Climate: Continental vs. Maritime
Northern Hemisphere: Characterized by a Continental Climate with extreme summer and winter temperatures due to their interior location.
Southern Hemisphere: Features a moderate climate because these grasslands are located closer to the sea (maritime influence).
Precipitation: In both hemispheres, rainfall is light to moderate and is received mostly during the summer.
Vegetation and Animal Species
Flora: The natural vegetation consists of treeless grasslands. These grasses are perennial and belong to the family Gramineae. Unlike tropical Savanna grasses, these are shorter and more nutrient-dense.
Fauna: Major species include antelopes, wild asses, horses, and wolves. In Australia, unique species like kangaroos, emus, and dingoes are dominant.
Human and Economic Significance
These grasslands are often referred to as the 'Granaries of the World'.
Agriculture: The flat, fertile land is ideal for extensive, mechanized wheat cultivation.
Crops: Wheat is the primary crop, while maize is grown in the warmer, wetter sections.
Pastoralism: They serve as vast grazing grounds for livestock (cattle and sheep), supporting large-scale dairy and meat industries.
| Region | Local Name |
|---|---|
| Eurasia | Steppes |
| North America | Prairies |
| Argentina (South America) | Pampas |
| South Africa | Velds |
| Australia | Downs |
| Hungary | Puszta |
| New Zealand | Canterbury |
Prelims tips
- Temperate grasslands are known as 'Granaries of the World' due to extensive mechanized wheat farming.
- Unlike Savannas (Tropical Grasslands), Temperate Grasslands are largely treeless and have shorter, more nutritious grass.
- Chernozem (Black Soil) is typically found in these regions, making them highly fertile.
- In the Northern Hemisphere, they experience a Continental climate (huge temperature range).
- Pampas (Argentina) are famous for high-quality alfalfa grass used for commercial cattle rearing.
Mains points
- The transformation of temperate grasslands into agricultural heartlands represents one of the most significant land-use changes in history, ensuring global calorie supplies but reducing natural biodiversity.
- Mechanized farming in the Prairies and Steppes has led to environmental challenges like soil erosion (e.g., the 1930s Dust Bowl in the USA), necessitating sustainable soil conservation practices.
- The moderating marine influence in Southern Hemisphere grasslands (Pampas, Velds, Downs) allows for year-round agricultural activity compared to the harsher winters of the Northern Steppes.
- Extensive livestock ranching in these biomes contributes significantly to international trade in meat and wool, especially from nations like Australia and Argentina.
Taiga Biome (Boreal Forest)
The Taiga, also known as the Boreal Forest, is the world's largest terrestrial biome. Located in the high latitudes of the Northern Hemisphere, it is characterized by long, freezing winters and is the primary source of the world's softwood timber.
Distribution and Location
The Taiga is located in the sub-arctic region of the Northern Hemisphere, just south of the Arctic Circle.
Regions: It spans across Alaska (USA), Canada, Scandinavia (Northern Europe), and Siberia (Russia).
Alternative Name: It is widely known as the Boreal Forest Biome.
Climate: Harsh and Cold
Temperature: It has the lowest annual average temperatures among forest biomes, ranging from -5 to 5 degrees Celsius. Winters are long and extremely cold, while summers are very short and only mildly warm.
Precipitation: Rainfall and snowfall are generally low throughout the year.
Plant Species: The Softwood Treasury
The biome is dominated by evergreen coniferous trees, which are the world's richest source of softwood. These trees are cone-shaped to allow snow to slide off easily.
Major Conifers: Pine (White, Red, Scots), Fir (Douglas, Balsam), Spruce, and Larch.
Deciduous Members: Some cold-hardy deciduous trees like Alder, Birch, and Poplar are also found.
Animal Adaptations
Animals are highly adapted to survive extreme cold through thick fur or hibernation.
Fauna: Common animals include Moose, Lynx, Bears, and Siberian Tigers.
Birds: Most bird species are migratory, flying south to escape the freezing, harsh winters.
Human and Economic Interaction
Due to the harsh climate, the human impact is centered on resource extraction rather than settlement.
Economy: Lumbering (logging for timber and paper pulp) is the most significant economic activity.
Agriculture: Very little agriculture exists as the growing season is too short and the soil is often acidic (Podzols).
Indigenous Activities: Groups like the Siberian Samoyeds and Yakuts engage in traditional hunting, trapping, and fishing.
| Feature | Taiga (Boreal Forest) | Tundra |
|---|---|---|
| Vegetation | Dense Coniferous Forests | Mosses, Lichens, no trees |
| Soil | Acidic (Podzols) | Permafrost (Frozen ground) |
| Location | Sub-arctic (South of Arctic Circle) | Arctic (North of Arctic Circle) |
| Economic Activity | Commercial Logging | Nomadic Herding/Mining |
Prelims tips
- Taiga is the world's largest land biome.
- The wood obtained from Taiga is 'Softwood', which is used for making paper, matches, and furniture.
- Larch is a unique 'deciduous' conifer found in the Taiga (it sheds needles in winter).
- Podzol is the characteristic grey, acidic, and nutrient-poor soil of this biome.
- Taiga is found only in the NORTHERN Hemisphere; there is no equivalent land belt in the Southern Hemisphere.
Mains points
- The Taiga is a massive carbon storehouse; however, rising global temperatures are causing forest fires and pest infestations, threatening to turn this sink into a carbon source.
- The lumbering industry in the Taiga is highly mechanized and organized, providing the backbone for the global paper and pulp market, particularly in Canada and Russia.
- Climate change is causing the 'treeline' to shift northward, as Taiga species begin to encroach upon the warming Tundra regions.
- Conservation of the Taiga is essential for the preservation of iconic large mammals like the Siberian Tiger and for maintaining the global oxygen-carbon balance.
Temperate Deciduous Biome
Temperate deciduous forests are known for their distinct four seasons and broadleaf trees that shed their leaves in winter. Found in the mid-latitudes, this biome receives moderate rainfall and is characterized by fertile soil and a rich layer of organic matter.
Global Distribution
This biome is primarily found in the mid-latitudes of the Northern Hemisphere.
Regions: Eastern United States and Canada, most of Europe, and parts of East Asia (China and Japan).
Climate: The Land of Four Seasons
The region is exposed to both warm and cold air masses, resulting in a well-defined seasonal cycle.
Seasons: It experiences four distinct seasons: Spring, Summer, Autumn, and Winter.
Temperature: The average yearly temperature is approximately 10°C.
Precipitation: Receives 750 to 1,500 mm of precipitation, which is spread fairly evenly throughout the year.
Plant and Animal Species
Flora: Dominated by tall, broadleaf trees. These trees create a dense canopy during the summer but shed their leaves completely in the winter to conserve water and survive the cold.
Key Tree Species: Beech, Oak, Maple, Mulberry, Willow, and Cherry.
Vegetation Structure: The canopy is continuous in summer, but the lower layers of shrubs and small trees are generally weakly developed compared to tropical forests.
Fauna: Common animals include deer, bears, squirrels, and various bird species, many of which migrate or hibernate during the winter months.
| Feature | Temperate Deciduous | Tropical Evergreen |
|---|---|---|
| Leaf Habit | Shed leaves annually in winter. | Maintain leaves year-round. |
| Seasons | Four distinct seasons. | Consistently warm and wet. |
| Biodiversity | Moderate. | Extremely high. |
| Soil Fertility | High (rich in leaf litter/humus). | Low (nutrients leached by heavy rain). |
Prelims tips
- Temperate deciduous forests are found in mid-latitude regions with moderate rainfall.
- The shedding of leaves is a response to the physiological drought of winter (frozen water).
- This biome has very fertile soil due to the slow decomposition of thick leaf litter.
- Oak and Maple are classic indicator species for this biome.
- Precipitation is distributed evenly throughout the year, unlike the Monsoon Deciduous forests.
Mains points
- The vibrant autumn colors of the temperate deciduous biome are a significant driver of seasonal tourism (leaf-peeping) in regions like New England, USA.
- This biome has historically faced extensive clearing for agriculture and urban development due to its moderate climate and fertile soils.
- The accumulation of leaf litter on the forest floor supports a rich community of decomposers and contributes to the high organic content of the soil.
- Current climate trends are shifting the timing of bud-burst in spring and leaf-fall in autumn, potentially disrupting the synchronized life cycles of insects and birds.
Tundra Biome
Tundra, meaning 'deserted land,' is characterized by extreme polar climates, a lack of trees, and a permanently frozen subsoil called permafrost. It exists in the highest latitudes of the Northern Hemisphere and on high mountain peaks.
What is Tundra?
The word Tundra comes from the Finnish word for 'deserted land.' It represents regions with the most extreme arctic climates and minimal vegetation.
Classification:
1. Arctic Tundra: Found in the high latitudes of the Northern Hemisphere.
2. Alpine Tundra: Found at high altitudes on mountains across the world (even in tropical areas) where trees cannot grow.
Distribution
Primarily found north of the Arctic Circle in the Northern Hemisphere.
Regions: Greenland's coastal strip, the barren lands of Northern Canada and Alaska, and the Arctic coastal regions of Eurasia (Siberia).
Climate: Extreme Cold
Temperature: Mean annual temperature is very low. The warmest month (June) rarely exceeds 10°C. Mid-winter temperatures can drop to -35°C or lower.
Seasons: Long, dark, and harsh winters with brief, cool summers.
Precipitation: Mostly in the form of snow, which is often redistributed by strong winds during snowstorms.
Plant and Animal Species
Flora: Trees are absent. Vegetation is dwarf and grows during the brief summer. Major species include mosses, lichens, grasses, and low shrubs.
Fauna: Animals are adapted to the cold with thick fur or fat layers. Species include Reindeer (Caribou), Polar Bears, Arctic Foxes, Musk-ox, Arctic Hares, Seals, and Lemmings.
Human Interaction
Life is challenging and mostly confined to coastal areas.
Livelihood: People are often semi-nomadic, traditionally engaging in hunting and fishing.
Tribes: Famous indigenous groups include the Eskimos (Inuit) of North America, Lapps (Sami) of Scandinavia, and Samoyeds of Siberia.
Modern Changes: The discovery of minerals (like oil and gas) has led to new permanent settlements and infrastructure.
| Feature | Details |
|---|---|
| Meaning | Deserted land (Finnish origin) |
| Warmest Temp. | Rarely exceeds 10 degrees Celsius |
| Vegetation Type | Treeless; Mosses, Lichens, Sedges |
| Soil Condition | Permafrost (Permanently frozen soil) |
| Human Groups | Inuit (Eskimos), Lapps, Samoyeds |
Prelims tips
- Tundra is a treeless biome; any trees found near the boundary are stunted (Krummholz).
- Permafrost is a defining characteristic where subsoil remains frozen throughout the year.
- Alpine Tundra is different from Arctic Tundra as it occurs due to altitude, not latitude.
- Lichens are a primary food source for many Tundra herbivores like Reindeer.
- Vegetation has a very short growing season (usually 50-60 days).
Mains points
- The Tundra is highly sensitive to climate change; as temperatures rise, the melting permafrost releases large amounts of methane, a potent greenhouse gas.
- Indigenous communities in the Tundra have developed unique cultural and physiological adaptations to survive one of the harshest environments on Earth.
- The fragility of the Tundra ecosystem means that human activities like oil drilling and mining can have long-lasting negative impacts on the slow-growing vegetation.
- The 'greening of the Arctic' is a phenomenon where shrubs and Taiga species are moving into Tundra regions due to global warming, altering local food webs.
Aquatic Ecosystems
Aquatic ecosystems are classified based on salt concentration (salinity) and water movement (mobility). The presence of specific life forms depends on factors like sunlight penetration (photic zone), temperature, and nutrient levels.
Characteristics of Aquatic Systems
Aquatic systems have distinct zones with unique plants, animals, and microorganisms. The variations in life forms are primarily driven by:
Physical Factors: Temperature, sunlight (Photic zone), and Mud/Silt.
Chemical Factors: Salinity, dissolved nutrients, and inorganic contents.
Classification Based on Salinity
1. Freshwater Ecosystem: Contains very low salt content, consistently less than 5 ppt (parts per thousand).
Examples: Rivers, Ponds, Lakes, and Streams.
2. Marine Ecosystem: Contains high salt content, usually above 35 ppt.
Examples: Shallow seas and open oceans.
3. Brackish Water Ecosystem: These are transition zones where freshwater mixes with seawater. Salt content ranges between 5 and 35 ppt.
Examples: Estuaries, Mangrove swamps, and salt marshes.
Classification Based on Water Mobility
1. Lotic Ecosystem (Flowing): In this type, the water moves or flows continuously in one direction.
Examples: Rivers and Streams.
2. Lentic Ecosystem (Still): In this type, the water remains relatively still and does not flow.
Examples: Lakes and Ponds.
| Type | Salinity Level | Water Movement | Examples |
|---|---|---|---|
| Freshwater | < 5 ppt | Lotic or Lentic | Rivers, Lakes |
| Brackish | 5 - 35 ppt | Variable | Estuaries, Mangroves |
| Marine | > 35 ppt | Tides/Currents | Oceans, Seas |
Prelims tips
- Salinity measurement: ppt stands for 'parts per thousand'.
- Freshwater < 5 ppt; Marine > 35 ppt; Brackish is in between (5-35 ppt).
- Remember: Lotic = 'L' for 'Lehrein' (waves/flow) or 'Low-tick' (moving); Lentic = 'L' for 'Lazy' or 'Lake' (still).
- Estuaries and Mangroves are the most productive brackish water ecosystems.
- The Photic zone is the upper layer of water where sunlight penetrates, allowing photosynthesis.
Mains points
- Aquatic ecosystems provide essential services such as water purification, flood control, and carbon sequestration (especially in mangroves and seagrasses).
- Anthropogenic factors like chemical runoff from agriculture and industrial waste are causing 'Eutrophication' in lentic systems, leading to oxygen depletion and fish kills.
- Brackish water ecosystems like estuaries are vital 'nurseries' for many marine species, serving as a buffer between terrestrial and marine environments.
- Climate change-induced sea-level rise is increasing the salinity of freshwater and brackish systems, threatening local biodiversity and human water supplies.
Pond Ecosystem (Lentic Freshwater)
A pond is a lentic (still-water) ecosystem characterized by its shallow depth, allowing light to reach most parts. It features distinct vertical zones (Surface, Photic, and Aphotic) and a diverse range of plant life adapted to various water depths and surface conditions.
Characteristics of a Pond
A pond ecosystem is a type of lentic (still-water) aquatic ecosystem. These can be man-made or natural.
Temporality: Some ponds are temporary (monsoon season only), while larger ones (lakes/tanks) sustain an ecosystem year-round.
Depth: Defined by shallow depth, allowing light to often reach the bottom, which supports specialized aquatic life.
Zones in a Pond Ecosystem
Surface Zone: The topmost layer where light is abundant. It supports floating plants like duckweed.
Photic Zone: The area with sufficient light penetration for photosynthesis. It is rich in algae and submerged plants.
Aphotic Zone: The deep, dark bottom layer where light cannot reach. Organic matter (detritus) accumulates here, and life is limited to decomposers.
Flora of the Pond Ecosystem
The plants in a pond are categorized by how they interact with water and air:
1. Algae: Primary producers and the base of the food chain.
2. Emergent Plants: Roots are underwater, but stems/leaves are exposed to air. Found near edges.
Examples: Cattails, Bulrushes, Reeds.
3. Submerged Plants: Grow completely underwater, usually anchored to the bottom.
Examples: Water milfoil, Pondweeds.
4. Floating Plants: Float on the surface without being anchored.
Examples: Duckweed, Water hyacinth.
5. Riparian Plants: Grow along the damp edges/banks; not necessarily aquatic but part of the pond boundary.
Examples: Willows, Alders.
| Plant Type | Position | Common Examples |
|---|---|---|
| Emergent | Roots in water, leaves in air | Cattails, Reeds |
| Submerged | Entirely underwater | Water milfoil, Pondweeds |
| Floating | Surface of water, unanchored | Duckweed, Water hyacinth |
| Riparian | Along the water edge/bank | Willows, Cottonwoods |
Prelims tips
- Ponds are Lentic (Still water) systems.
- The Photic zone is where NPP (Net Primary Productivity) is highest due to photosynthesis.
- Emergent plants like Cattails are found in the Littoral zone (near the shore).
- Aphotic zones are characterized by decomposition and accumulation of organic waste (detritus).
- Water Hyacinth is an invasive species often called the 'Terror of Bengal'.
Mains points
- Pond ecosystems play a vital role in local hydrology, acting as a buffer for heavy rains and a sanctuary for migratory birds and amphibians.
- The classification of plants (emergent, submerged, floating) shows the adaptation of species to vary oxygen and sunlight availability at different depths.
- Human activities, such as excess fertilizer runoff, lead to algal blooms in ponds, rapidly turning a healthy pond into a dead zone through the process of eutrophication.
- Conservation of riparian vegetation is crucial as it prevents soil erosion from the banks and filters pollutants before they enter the pond water.
Marine Ecosystem
The marine ecosystem is the largest aquatic system on Earth, categorized by depth and light penetration. It features a vertical layering of life—from the sunlit surface to the bioluminescent deep—and supports specialized communities ranging from microscopic plankton to active swimming nekton.
Zonation in the Marine Ecosystem
The ocean is divided into zones based on depth and light availability:
1. Pelagic Zone (Open Ocean)
This refers to the open water column, not in contact with the shore or sea floor. It is vertically subdivided:
Epipelagic (Sunlit Zone): Surface to approx. 200m. Sunlight is abundant, allowing for photosynthesis.
Mesopelagic (Twilight Zone): 200m to 1,000m. Light is very faint. It holds nearly 90% of global fish biomass.
Bathypelagic (Midnight Zone): 1,000m to 4,000m. It is completely lightless. The only light comes from bioluminescence (light produced by organisms).
Abyssopelagic (Abyssal Zone): 4,000m to 6,000m. Pitch-black, high pressure, and near-freezing. Life here relies on detritus (falling organic waste).
2. Benthic Zone (Sea Floor)
Encompasses the entire sediment surface and the water layer immediately above it, from the shoreline to the deepest trenches.
Marine Organisms Communities
1. Plankton Community
Organisms that drift with water currents. They are the foundation of the marine food web.
Phytoplankton (Algae): Microscopic photosynthetic organisms. They lack roots/stems but produce the majority of the world's oxygen.
Zooplankton: Minute animals (crustaceans, larvae). They are Primary Consumers (eat algae) or Secondary Consumers (eat other zooplankton). They link producers to larger predators.
2. Nekton Community
Active swimmers that can move independently of water currents.
Pelagic Fish: Live in open waters, away from the shore or bottom.
Reef Fish: Associated specifically with coral reef structures.
Demersal Fish: Found living on or near the very bottom of the ocean.
| Zone | Depth Range | Light Condition | Key Feature |
|---|---|---|---|
| Epipelagic | 0 - 200m | Sunlit | Photosynthesis occurs here |
| Mesopelagic | 200 - 1000m | Twilight | 90% of global fish biomass |
| Bathypelagic | 1000 - 4000m | Dark | Bioluminescent life only |
| Abyssopelagic | 4000 - 6000m | Pitch Black | Extreme pressure, relies on detritus |
Prelims tips
- Epipelagic is the ONLY zone where photosynthesis takes place.
- Bioluminescence is the primary light source in the Bathypelagic zone.
- Zooplankton act as the 'bridge' in the food chain between producers and fish.
- Benthic organisms live on the floor; Pelagic organisms live in the open water column.
- Marine salinity is typically around 35 ppt (parts per thousand).
Mains points
- Ocean zonation determines the distribution of biodiversity; the Mesopelagic zone, despite having less light, is a critical carbon storage area due to the vertical migration of fish.
- The Abyssopelagic zone remains one of the least explored frontiers on Earth, yet it is highly vulnerable to deep-sea mining and climate-induced changes in detritus flow.
- Phytoplankton in the Epipelagic zone are responsible for roughly 50% of the world's oxygen production, making ocean health vital for terrestrial life survival.
- Overfishing of pelagic species disrupts the entire marine food web, causing cascading effects that can lead to the collapse of local benthic and reef communities.
