Ecosystems are intricate webs of life where living organisms interact with their physical surroundings, including biotic (living) and abiotic (non-living) factors. Abiotic factors are the environmental conditions and elements that shape ecosystems but do not possess life themselves. These factors play a critical role in determining the distribution, composition, and functioning of ecosystems. In this series of explanations, we will delve into various abiotic factors that influence ecosystems, shedding light on how each one impacts the natural world. From climate variables like temperature and rainfall to geological factors like soil composition and topography, and even human-induced elements like pollution, we will explore the wide-ranging effects of abiotic factors on the delicate balance of ecosystems. Understanding these abiotic factors is essential for ecological research, conservation efforts, and our broader mission to safeguard the health and stability of the natural world.
Water is one of the most essential abiotic factors that support life on Earth. Approximately 71% of Earth’s surface is covered by water. Saltwater in the world’s oceans and seas makes up about 97.5% of the planet’s water. The remaining 2.5% is freshwater, majorly locked in glaciers, ice caps, underground water, lakes, rivers, and atmospheric water vapour. Water significantly influences the structure and function of ecosystems.
- It provides a habitat for numerous aquatic species (fish, amphibians, phytoplankton, etc.) which are the foundation of aquatic food webs.
- Water bodies like oceans and lakes, help regulate temperature by absorbing heat during the day and releasing it slowly at night. This is due to the high heat capacity of water allowing it to absorb and store a significant amount of heat energy. The thermal regulation by water influences the nearby terrestrial ecosystems as well, thus impacting the entire ecosystem.
- Water is an active oxygen source for aquatic life which depends on the dissolved oxygen in the water for respiration.
- Water is undoubtedly essential for terrestrial organisms as well. All living forms rely on water for hydration and as a resource for their life cycles.
- Along with oxygen, water is also a carrier of essential nutrients and minerals. It transports nutrients from terrestrial areas to aquatic ecosystems, contributing to the fertility of aquatic habitats. It dissolves and transports gases, ions, and organic compounds necessary for life processes.
- Water is a powerful abiotic factor that shapes landscapes and influences the distribution of sediments. It sculpts geological features, creates river valleys, and can contribute to soil formation.
There is no doubt that due to the surge of water pollution, over-extraction, and alterations to natural watercourses, our ecosystem is getting negatively impacted. If left unchecked, such activities will ultimately lead to the depletion of water, the life source on earth.
Sunlight is the ultimate source of energy for life on Earth and plays a significant role in the sustenance of the ecosystem. Sunlight is essential for photosynthesis, the process by which photoautotrophs (green plants, algae, and some bacteria) convert sunlight into chemical energy. Through photosynthesis, these organisms produce glucose (sugar) and oxygen from carbon dioxide and water. This energy-rich glucose serves as the foundation of the food web, as it is consumed by herbivores, which are further preyed upon by carnivores. As a result, sunlight sustains entire ecosystems by providing the energy necessary for life processes. The intensity, duration, and quality of sunlight vary with certain parameters such as geographical location, time of day, and season which leads to diverse ecological niches. For example, shade-tolerant plants have adapted to lower levels in forests, while the sun-loving species thrive in deserts with abundant sunlight. Seasonal rhythms (mechanisms that enable an organism to survive changes in season) are also dependent upon sunlight. Sunlight influences the behaviour of diurnal (active during the day) and nocturnal (active at night) animals, as well as the timing of reproductive cycles, migration patterns, and hibernation.
3. Atmospheric gases
Atmospheric gases constitute the composition of gases present in the Earth’s atmosphere. These gases have a profound influence on the health, structure, and function of ecosystems, as they directly impact the respiration, photosynthesis, and behaviour of living organisms. The most abundant atmospheric gases include nitrogen (N2), oxygen (O2), carbon dioxide (CO2), and trace gases like argon (Ar), neon (Ne), methane (CH4), and ozone (O3).
- Nitrogen makes up about 78% of the atmosphere and is an extremely important element that maintains atmospheric stability by limiting the reactivity of other elements. Its primary function is to dilute oxygen and ensure that it’s breathable and suitable for life. It also acts as a significant nutrient for plant growth, supporting the foundation of terrestrial ecosystems. In industrial applications, nitrogen is used to create inert atmospheres, preventing combustion and oxidation.
- Oxygen is vital for the respiration of most organisms, which allows them to extract energy from organic compounds. Plants, in contrast, release oxygen as a byproduct of photosynthesis, which is a process where they convert carbon dioxide (Co2) and sunlight into energy-rich molecules.
- Carbon dioxide, while essential for photosynthesis, is also a greenhouse gas that regulates the Earth’s temperature, influencing climate patterns and, consequently, ecosystems. Changes in its concentration due to human activities, such as air pollution and burning fossil fuels, have led to concerns about global climate change (global warming).
- Methane (CH4)is produced by certain bacteria and is involved in microbial processes, while ozone (O3) can be beneficial or harmful depending on its location in the atmosphere. Ozone in the stratosphere protects life on Earth by absorbing harmful ultraviolet radiation, while ground-level ozone can damage plant tissues and harm ecosystems.
- Noble gases argon (Ar) and neon (Ne), account for about 0.93% and 0.0018% of Earth’s atmosphere respectively. Although they are present in small quantities, they have important applications in various industries. Argon is valued for its chemical inertness and is used in welding, lighting, cryogenic cooling, and scientific research. In contrast, neon is utilized for its colourful glow in illuminated signs, lighting displays, lasers, and as indicator lights in electronics.
Understanding the composition and dynamics of atmospheric gases is crucial for assessing air quality, predicting weather patterns, and studying climate change. Changes in atmospheric gas concentrations, driven by either natural processes or human activities, can negatively impact ecosystems. It can result in altered temperature, precipitation patterns, and lesser availability of essential gases like oxygen and carbon dioxide. Therefore, monitoring and managing their concentrations are essential components of environmental conservation efforts.
4. Atmospheric pressure
Atmospheric pressure refers to the force exerted by the weight of the air above a particular point on the Earth’s surface. This pressure varies with altitude and weather patterns and can significantly influence the distribution, behaviour, and adaptations of living organisms within ecosystems.
- As altitude increases, atmospheric pressure decreases due to the lower density of air at higher elevations. This reduction in pressure affects the availability of oxygen for respiration, which can be particularly challenging for organisms living at high altitudes, such as mountain-dwelling species. To adapt to reduced oxygen levels, these organisms may have evolved mechanisms such as increased lung capacity or more efficient oxygen utilization.
- Atmospheric pressure also plays a role in weather patterns, with changes in pressure influencing wind patterns and precipitation. Low-pressure systems often bring stormy weather and can lead to increased precipitation, while high-pressure systems are associated with fair weather and clear skies. These weather patterns, in turn, affect the availability of water resources in an ecosystem, which is critical for plant and animal life.
- Barometric pressure (a measure of atmospheric pressure) can serve as an indicator of imminent weather changes. Certain species of fish and birds can detect changes in barometric pressure and use this information to adjust their behaviours, such as feeding or migrating.
- Atmospheric pressure is an important abiotic factor in conservation efforts, especially for high-altitude ecosystems and species that are particularly sensitive to oxygen availability and pressure fluctuations. Understanding the variations in atmospheric pressure is essential for ecological research and predicting the impacts of climate change.
The physical features of the land surface, including its elevation, slope, relief, and geological formations all comprise its topography. The elevation of an area determines its climate, as higher altitudes are generally cooler due to changes in temperature with altitude (the lapse rate). This temperature variation can lead to the formation of distinct ecological zones at different elevations, known as altitudinal or elevational zonation. Each zone may host its unique plant and animal communities adapted to the specific environmental conditions. Steep slopes can influence water runoff and erosion, affecting soil composition and stability. This can lead to the creation of microhabitats, with different plant species adapted to the varying moisture and sunlight levels on different aspects of slopes (e.g., north-facing vs. south-facing slopes).
Geological formations, such as rock outcrops, cliffs, and caves, provide important habitats for various species. Moreover, topographical features like valleys and depressions can influence the accumulation of water, which helps in the creation of wetlands, ponds, and lakes. These aquatic ecosystems, in turn, support their own communities of plants and animals and contribute to the overall biodiversity of the region. Human activities can also significantly alter topography through processes like land grading, dam construction, and urban development. These alterations can disrupt natural topographical features and lead to water flow patterns, erosion, and local habitat loss.
6. Soil nutrients
Soil nutrients are essential elements and compounds present in the soil that provide nourishment for plants and, subsequently, for the entire food web within an ecosystem. These nutrients are crucial for plant growth and the overall health and functioning of terrestrial ecosystems. Soil nutrients include macronutrients (needed in larger quantities) like nitrogen (N), phosphorus (P), and potassium (K), as well as micronutrients (needed in smaller quantities) like iron (Fe), zinc (Zn), and copper (Cu). These nutrients affect the distribution and abundance of plant species within an ecosystem, as different plants have varying nutrient requirements. For example, some plants are adapted to thrive in nutrient-poor soils, while others require more fertile soils rich in nutrients. The availability of soil nutrients also influences the primary productivity of an ecosystem, which, in turn, affects the energy flow and sustenance of herbivores, carnivores, and decomposers in the food chain. Soil nutrients play a significant role in nutrient cycling within ecosystems. Decomposers (bacteria and fungi) break down organic matter (dead leaves, animal remains) releasing essential nutrients back into the soil. These nutrients are then taken up by plants, continuing the cycle. Balancing soil nutrient content is crucial for maintaining ecosystem health and biodiversity. Inadequate nutrients can limit plant growth, affecting herbivores and higher trophic levels. Human activities, such as agriculture, land development, and pollution can alter soil nutrient levels, often leading to nutrient imbalances, environmental degradation, and the disruption of aquatic ecosystems through processes like eutrophication.
7. Soil pH
Soil pH refers to the measurement of the acidity or alkalinity of the soil. It is a crucial determinant of the health of plant and microbial life within an ecosystem. Soil pH is measured on a scale from 0 to 14, with 7 being neutral. Soils with a pH below 7 are considered acidic, while those with a pH above 7 are alkaline. Some plant species (magnolia, ferns, hydrangeas, etc.) thrive in acidic soils, while others (lavender, geranium, legumes, etc.) prefer alkaline conditions. Soil pH influences nutrient availability; for example, acidic soils may have higher concentrations of aluminium and iron, which can be toxic to some plants, while alkaline soils can limit the availability of essential nutrients like iron and phosphorus. Microbes involved in decomposition, nutrient cycling, and nitrogen fixation are sensitive to pH levels. Acidic soils may inhibit microbial activity, affecting nutrient availability and organic matter decomposition. Soil pH affects the solubility of essential nutrients like nitrogen, phosphorus, and potassium. These nutrients become more or less available to plants depending on whether the soil is acidic or alkaline. Proper pH levels are essential for nutrient uptake by plants and the pH of the soil directly influences the types of plants that can grow in an area. Ultimately, it also impacts other animals that depend on these plants for food and habitat. Thus, any change in soil pH can lead to shifts in the composition and distribution of species in an ecosystem.
Acid rain, a form of pollution caused by emissions of sulfur and nitrogen oxides, can lower soil pH, making it more acidic. This can harm plants and aquatic life, disrupt nutrient cycling, and affect overall ecosystem health. Alterations in soil pH due to human activities, such as industrial pollution or agricultural practices, can have negative consequences on the functioning of biodiversity. Therefore, monitoring and regulating soil pH is essential for preserving the health and balance of ecoystems.
8. Soil texture
Soil texture means the composition and arrangement of mineral particles within the soil. It is an important characteristic that influences many aspects of an ecosystem, including plant growth, water retention, and the living organisms living in the soil. Soil texture is mainly determined by the relative proportions of three types of mineral particles: sand, silt, and clay, each with unique properties:
Sand particles are the largest, with a coarse texture. Sandy soils have good drainage and aeration but may struggle to retain water and nutrients. Plants that are adapted to sandy soils often have drought-resistant traits.
Silt particles are intermediate in size and feel smooth when rubbed between fingers. They come under the medium soil textural class. Silty soils have good water and nutrient retention capabilities but can become compacted easily. Many crops grow well in silty soils.
Clay particles are the smallest and have a fine, sticky, and dense texture. Clay soils have the highest water retention capacity and can hold water and nutrients effectively but they can become waterlogged and less aerated. Some plant species are adapted to clay soils, but they can pose challenges for root growth.
Soil particles with an equal proportion of sand, silt, and clay are called loam soil. Loamy soil has smaller pores than sand and a higher retention capacity for water and nutrients. Thus, it is considered ideal soil for plant growth.
Soil texture influences the distribution of plant species within an ecosystem, as different plants have varying preferences for soil types. It also affects the movement of water, with sandy soils allowing water to drain quickly, while clay soils can lead to waterlogged conditions. This, in turn, impacts the availability of moisture for plants and the types of aquatic organisms that can inhabit wetlands and water bodies associated with the ecosystem. Moreover, soil texture influences the burrowing activities of soil-dwelling organisms (earthworms, ants, and microorganisms) which play critical roles in nutrient cycling and soil structure.
9. Soil moisture content
Soil moisture content is the amount of water present in the soil at a specific point in time. It is a critical environmental variable which is essential for the survival and growth of plants, serving as a primary source of water for their root systems. Adequate soil moisture is crucial for photosynthesis, nutrient uptake, and other physiological processes in plants. The availability of soil moisture also affects many terrestrial animals ranging from insects to mammals, which depend on the water contained within the soil for drinking, nesting, and burrowing. For example, certain species of rodents (rats, squirrels, hamsters, etc.) dig burrows in damp soil to create underground homes and rely on soil moisture to maintain their habitat. Variations in soil moisture content are influenced by factors like climate, topography, and vegetation. Arid ecosystems have low soil moisture content due to limited rainfall, making it challenging for living organisms to thrive. Whereas in wetlands and rainforests, high soil moisture content creates favourable living conditions. Extreme fluctuations in soil moisture content can lead to drought stress, hinder plant growth, and disrupt the availability of water resources for both plants and animals.
Temperature plays a significant role in shaping the distribution, behaviour, and survival of living organisms within an ecosystem.
- Temperature directly affects the metabolic rates of organisms. In general, as temperature increases, metabolic processes in organisms become more active, and as it decreases, metabolic processes slow down. This influence extends to various aspects of an organism’s life, including growth, reproduction, and overall activity levels.
- As you move up or down in elevation within an ecosystem, temperatures can vary significantly. High elevations tend to be cooler, while lower elevations are warmer. This creates different microclimates and influences the types of species that can be found at different elevations.
- The Earth has various climate zones (e.g., polar, temperate, tropical) characterized by different temperature patterns. These climate zones determine the types of ecosystems and the plant and animal species that can inhabit them. Different species have varying temperature tolerances and preferences. The temperature range in which a species can thrive is known as its thermal niche. For example, some species are adapted to cold environments and can only survive at low temperatures, while others are adapted to warm or hot environments.
- Some organisms have evolved specific adaptations to deal with temperature extremes. For example, desert animals have mechanisms to cool themselves during the day and retain heat at night.
- Seasonal temperature fluctuations can impact the behaviour and life cycles of many organisms. For example, some plants require a period of cold temperatures (winter) to trigger flowering and fruit production (vernalization).
- In colder regions, many animals hibernate or migrate to warmer areas during the winter months. Extreme temperatures, whether hot or cold, can stress or even kill organisms that are not adapted to such conditions. For instance, heatwaves (extreme heat) can cause heat stress and dehydration in many species, while cold snaps (rapid fall in temperature) can lead to frostbite and freezing.
- Temperature is critical in aquatic ecosystems as well. Water temperature affects the solubility of gases (like oxygen), which is crucial for aquatic life. It also influences the distribution of species in oceans, lakes, and rivers.
- Urban areas often have higher temperatures due to the urban heat island effect. Urban areas are packed with building structures which retain heat and ultimately increase energy costs, air pollution, and illnesses. If left unchecked, global climate change can lead to overall temperature increases (global warming), disrupting ecosystems.
Rainfall is a crucial abiotic factor of the ecosystem, representing the amount and distribution of precipitation in a given area. It is one of the major sources of water availability on Earth, a fundamental requirement for all forms of life. Rainfall is measured by an instrument called a rain gauge. Plants depend on rainfall to provide the moisture necessary for photosynthesis, growth, and reproduction. The timing and amount of rainfall affect the types of vegetation found in an ecosystem. Regions experiencing higher rainfall support lush forests, while arid regions (areas lacking available water, such as deserts) have adapted to sparse vegetation. Rainfall patterns also affect animal behaviour and distribution. Many animals rely on access to water sources for drinking, and the availability of rainfall can determine the presence or absence of these water sources. Additionally, variations in rainfall can influence the breeding and migration patterns of animals. For example, certain species of frogs rely on heavy rainfall to trigger their mating and reproductive activities. Ecosystems are susceptible to changes in rainfall patterns, and precipitation alterations due to climate change can have significant ecological consequences. Prolonged droughts can lead to water scarcity, food shortages, and habitat loss, endangering both plant and animal species. Excessive rainfall and flooding can disrupt ecosystems, leading to soil erosion, water contamination, and the displacement of species.
Humidity is the amount of moisture or water vapour present in the air. It plays a significant role in influencing the conditions within an ecosystem.
- High humidity levels indicate a considerable amount of water vapour in the air, while low humidity indicates dry conditions with relatively little moisture.
- The humidity of an environment affects the rates of evaporation and transpiration in plants, which, in turn, influences the availability of water for both flora (plants) and fauna (animals). In regions with high humidity, plants may lose less water through transpiration, allowing them to thrive. On the other hand, low humidity can lead to rapid water loss in plants, which can be challenging for their survival.
- Humidity also affects the behaviour and physiology of animals. Many species are adapted to specific humidity levels, and deviations from these levels can stress or harm them. For example, amphibians (frogs, salamanders, etc.) have permeable skin that can easily lose moisture in dry, low-humidity environments, and make them vulnerable to desiccation (complete dehydration).
- Some insects, like termites, are highly sensitive to changes in humidity, as it affects their nest construction and respiratory systems.
- Humidity also influences weather patterns, cloud formation, and precipitation. High humidity levels can contribute to the formation of clouds, which may lead to rainfall. This, in turn, affects the availability of water resources in an ecosystem.
Salinity is the concentration of salt (primarily sodium chloride) dissolved in a water body. It helps in shaping the characteristics of aquatic ecosystems and influencing the distribution of organisms living in aquatic habitats. Salinity levels vary widely in different aquatic environments, from freshwater streams and lakes to brackish estuaries and full-strength marine environments. Both plants and animals have varying salinity tolerances, with some adapted to freshwater conditions, while others are specialized for life in saline or hypersaline waters. For example, many marine fish and invertebrates have evolved mechanisms to maintain a proper salt balance in their bodies, allowing them to live in saltwater environments. Salinity levels can fluctuate due to natural factors like rainfall, evaporation, and the mixing of freshwater and seawater. Human activities, such as agriculture and industrial runoff, can also change salinity levels in aquatic ecosystems. This may result in environmental stress and harm to sensitive species. High salinity can lead to reduced water quality and the loss of biodiversity, while low salinity can impact the growth of salt-tolerant species and disrupt ecosystem functioning.
Wind refers to the movement of air across a given area. Wind speed and direction vary widely across different regions and climates, resulting in significant ecological consequences.
- Wind patterns can determine the distribution of plant spores and pollen, as they are often carried by the wind to new locations for germination and reproduction.
- Wind can also influence the dispersal of small organisms, such as insects and microorganisms, which may be transported over long distances.
- Wind can affect the availability of moisture in an ecosystem through processes like evaporation and transpiration. Strong winds can lead to increased evaporation rates from bodies of water, making water sources more vulnerable to drying up. Wind can increase transpiration rates in plants, potentially leading to water stress for vegetation.
- In some ecosystems, particularly coastal areas, wind can influence the movement of ocean currents and the formation of dunes and sandbars. Coastal vegetation is often adapted to withstand strong winds and salt spray, which are common in these environments.
- Wind can also affect the behaviour of animals. For example, birds use wind patterns for migration, taking advantage of favourable winds to conserve energy during long journeys. In addition, some predators and prey rely on the wind to carry scents or sounds that help them locate food or avoid being detected.
Altitude is defined as the elevation or height above sea level at which a particular area or ecosystem is situated. It is a critical environmental variable that significantly influences the physical and biological characteristics of an ecosystem. As altitude increases, several key factors change, including temperature, atmospheric pressure, oxygen levels, and the availability of water. These changes, in turn, impact the distribution of species and the overall ecological dynamics of the area. One of the most significant effects of increasing altitude is a decrease in temperature. Generally, as one ascends in altitude, the temperature tends to drop and high-altitude areas experience colder and often more extreme weather conditions. This temperature variation directly affects the types of plant and animal species that can thrive in an ecosystem. For example, alpine and montane ecosystems (found on mountains) are adapted to the colder conditions. At higher altitudes, the atmospheric pressure decreases, leading to lower oxygen levels. This can pose challenges for organisms that require oxygen for respiration. To survive in such conditions, many high-altitude species have developed specialized adaptations, such as increased lung capacity or more efficient oxygen utilization. Altitude also influences precipitation patterns and water availability. Higher altitudes often receive more precipitation, but the cold temperatures can lead to reduced evaporation rates. This results in the formation of unique wetland ecosystems and the creation of glaciers and snowfields, which serve as critical water sources for downstream areas.
16. Natural calamities
Natural calamities include a wide range of natural disasters and extreme events, such as hurricanes, tornadoes, earthquakes, volcanic eruptions, floods, wildfires, and tsunamis. These calamities are powerful forces of nature that can have significant and often devastating impacts on ecosystems. Either way, they help shape an ecosystem’s dynamics, diversity, and resilience. Some examples are as follows:
- Wildfires, caused by factors like dry conditions, lightning strikes, or even human involvement can rapidly alter landscapes and destroy habitats. However, certain ecosystems (pine forests) are adapted to periodic wildfires and are even dependent on them for their regeneration processes.
- Floods can bring both benefits and challenges to ecosystems. While they can transport nutrients, create new habitats, and promote plant growth, excessive or frequent flooding can lead to serious consequences such as erosion, loss of soil fertility, and the displacement of species.
- Natural calamities can also affect the distribution of species by altering physical barriers and facilitating species movements. For instance, earthquakes can create new landforms, change watercourses, and lead to shifts in species distribution patterns.
- Volcanic eruptions, while initially destructive, can eventually enrich the soil with minerals and nutrients, creating fertile grounds for new vegetation.
These natural events are integral components of Earth’s dynamic systems, and ecosystems have evolved various strategies to adapt to and recover from such disturbances. However, human activities, including deforestation, urbanization, and climate change, can worsen the impacts of natural calamities and make ecosystems more vulnerable to their effects. Ultimately, recognizing the complex interconnectedness between natural calamities and ecosystems is essential for managing the long-term stability of Earth’s diverse habitats.
Pollution is the result of the introduction of harmful contaminants into the environment, often as a result of human activities. Polution-causing substances (pollutants) can have devastating effects on ecosystems, disrupting their balance and functioning. Pollution often results in the loss of biodiversity, since sensitive species cannot thrive in contaminated environments. Additionally, pollutants can disrupt critical ecological processes, such as nutrient cycling and decomposition. Pollutants come in various forms, including air pollution (emissions from vehicles, industrial processes, and agriculture), water pollution (contaminants from sewage, chemicals, and oil spills), and soil pollution (contaminated soil due to hazardous waste disposal or agricultural chemicals). Each type of pollution can impact ecosystems differently:
- Air pollution can lead to acid rain, which affects soil pH and water bodies, harming aquatic life and soil-dwelling organisms. It can also result in smog (smoke fog), reducing sunlight penetration and disrupting photosynthesis in plants, ultimately affecting the entire food web.
- Water pollution, whether from chemical runoff or sewage discharge, can contaminate aquatic ecosystems and make water bodies uninhabitable. Excessive nutrient pollution can lead to eutrophication, causing harmful algal blooms that deplete oxygen levels, suffocating fish and other aquatic organisms.
- Soil pollution can affect plant health, leading to reduced crop yields and the decline of soil-dwelling organisms crucial for nutrient cycling and soil structure maintenance. Pollutants like heavy metals can accumulate in the food chain, posing health risks to both wildlife and humans.
Mitigating pollution and its impacts on ecosystems is extremely important for conservation and environmental protection. Efforts including reduced emissions, implementing cleaner technologies, and enforcing environmental regulations can help minimize pollution’s negative effects.
In conclusion, abiotic factors are the often overlooked but vital components of ecosystems. From the air we breathe to the soils beneath our feet, these non-living elements play a significant role in sustaining life on Earth. Various abiotic factors such as water, temperature, sunlight, rainfall, humidity, wind, soil, etc., all exert their influence on ecosystems. Recognizing the impact of these abiotic factors highlights the interconnectedness of all life on Earth and their undeniable significance in life sustenance. In order to preserve the ecosystems for future generations, a comprehensive understanding of abiotic factors is necessary to ensure the continued well-being of the present habitats.