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Freshwater Biology

Freshwater biology is the scientific biological study of freshwater ecosystems and is a branch of limnology. This field seeks to understand the relationships between living organisms in their physical environment. These physical environments may include rivers, lakes, streams, ponds, lakes, reservoirs, or wetlands.^[1] Knowledge from this discipline is also widely used in industrial processes to make use of biological processes involved with sewage treatment^[2] and water purification. Water presence and flow is an essential aspect to species distribution and influences when and where species interact in freshwater environments.^[1]

In the UK the Freshwater Biological Association based near Windermere in Cumbria was one of the early institutions to research the biology of freshwater and promote the concepts of trophism in lakes and demonstrated the process of migration from oligotrophic water through mesotrophic to marsh.^[3]

Freshwater biology is also used to study the effects of climate change and increased human impact on both aquatic systems and wider ecosystems.^[4] Freshwater organisms, vertebrates especially, appear to be at a higher extinction risk from climate change than terrestrial or marine organisms. ^[5]

Freshwater Habitats

Freshwater habitats support a wide variety of organisms with habitats including rivers, streams, lakes, ponds, and wetlands^[6].

Running Water - Rivers and Streams

Running water is a type of a freshwater habitat that mainly consists of rivers and streams. Running, fast-moving waters have a higher oxygen content, allowing different species to thrive and making pollution easier to combat^[6]. Running water is an open system, meaning it is not isolate and exchanges matter and energy with other systems^[6]. Being an open system, a lot of organic matter found in running water is from land runoff or further sediment upstream and this matter is an important source of food for many species. Flowing bodies of water begin at the headwaters, which include springs, lakes, and snowmelt,  and travel to their mouths, typically another moving water channel or the ocean^[7]. The characteristics of the streams and rivers change throughout their journey from the source to the mouth. For example, the water at the source is clearer, has a higher oxygen content, lower temperatures, and heterotrophs common species. In the middle, the width usually expands and the species diversity increases due to temperature and oxygen content changes, including aquatic green plants and algae. The water at the mouth has a lower oxygen concentration and is murkier due to the sediment that has been collected and traveled along the length of the river or stream. This increased sediment decreases the amount of light that is able to penetrate the water and there is less diversity of flora and the lower oxygen lowers the diversity of fauna^[7].

The riparian zone is the area along a riverbank or streambank that is home to vital, high moisture plants. These plants create a buffer between the land and the running water system, protecting it from pollution and flooding. Additionally, these plants provide a large habitat for many wetland species, a large number of which are endangered or threatened. Lastly, riparian plants shade the water from sunlight, reducing the heat stress on the water and aquatic life, while also providing nutrients in the form of organic matter^[6].

Standing Water - Lakes and Ponds

Standing water is a type of freshwater habitat that mainly consists of lakes and ponds. This habitat has limited species diversity because they are isolated from one another and other water systems, unlike running water (cite ucmp). Standing water experiences the process of stratification, which is when water is layered due to the oxygen content(cite textbook). Stratification does not occur in running water because of the fast moving water that mixes water with varying oxygen content together. The topmost layer has the most amount of oxygen and as depth increases, the oxygen decreases (cite textbook). Stratification can be physically felt in the temperature of the water, as the uppermost layer of water is warmer than deeper water because it has been heated by the sun.

Standing water can be divided into three zones based on depth and distance from shore. The littoral zone is the uppermost layer and the warmest water found in lakes and ponds, as the sun directly heats is (cite ucmp). This zone hosts the most biodiversity in standing water, with a wide variety of organisms found here, vital to the health of the ecosystem and an important aspect of the diet of organisms in the habitat, like algae, aquatic plants, clams, insects, fish, crustaceans, and amphibians (cite ucmp). The limnetic zone is found below the littoral zone. This zone has lower temperatures, is fairly well-lit, and is occupied by a smaller variety of organisms, including phytoplankton, zooplankton, and fish (cite ucmp). The plankton found in this zone play a crucial role in the food web of the habitat and support the diet of many important organisms. The deepest zone is the profundal zone, with very little light, colder temperatures, and higher density than the previous layers (cite ucmp). When plankton die they fall into this layer and provide nutrients to the fauna that live in this layer. These fauna are called heterotrophs, meaning they eat dead organisms and use oxygen for cellular respiration, resulting in lower oxygen content in the profundal zone (cite ucmp).

The thermocline is the transitionary zone between the warm, surface water and the deeper water at a cooler temperature (cite textbook). The limited mixing and movement of water that occurs in standing water occurs at the thermocline. The mixing of the layers of water in standing water mostly comes from seasonal overturn. During the fall and spring, there is a mixing of layers usually due to wind that circulates oxygen and creates a more uniform temperature throughout the water system (cite ucmp). The shore zone is the transitional zone between the water systems and land, similar to the riparian zone seen in running water systems (cite textbook). This area functions in much the same way as the riparian zone, the plants protecting the water from pollution, flooding, and heat stress, while also providing nutrients and habitats for aquatic and wetland species.

Wetlands

Wetlands are a specific type of standing water habitats that include marshes, swamps, and bogs. Due to the waterlogged and submerged nature of the land, the anaerobic conditions of wetlands are unique and support the highest species diversity of all ecosystems (cite ucmp). Wetlands slow the decomposition of organic matter, creating layers of rich organic material that provides important nutrients for species in the system. The fauna that reside in wetlands are called hydrophytes, meaning they are adapted to very moist and humid conditions (cite ucmp). Wetlands are the home to a large number of bird, amphibian, insect, reptile, grass, and tree species that cannot inhabit any other system, making them at risk to endangerment, as wetlands are being destroyed for urban development and agriculture (cite textbook). Wetlands help combat pollution and climate change, as they filter pollutants and store a large amount of carbon from the biosphere in their moist soil and still water, despite the small amount of land they occupy. Additionally, wetlands provide flood and storm protection, as the system can absorb large amounts of excess water (cite textbook). Wetlands ability to absorb water also assists groundwater recharge, which is very important for human water use, as usable freshwater sources are dwindling. Wetlands are not only freshwater habitats and systems, as there are salt marshes and bogs that support different species (cite ucmp).

Freshwater Organisms

Freshwater organisms are generally divided into the categories of benthic and pelagic organisms, as these are the two zones of life found in the freshwater biome. Freshwater organism can include invertebrates, insects, fish, amphibians, mammals, birds, aquatic plants, and planktons^[7].

Threats

The most common cause of water pollution is stormwater runoff from developed areas, like pavement and rooftops (cite textbook). Stormwater runoff is moving rain and snowmelt that has not been absorbed (cite textbook). The impervious surfaces used in domestic and urban construction replace soil that used to absorb stormwater, increasing the amount of runoff traveling farther distances. This excess runoff can collect pollutants as it eventually makes its way into streams, rivers, lakes, wetlands, and even aquifers, polluting important freshwater ecosystems and usable water (cite textbook). Additionally, increased flooding and erosion can be caused by the increased stormwater runoff

Rivers and Streams

Rivers and streams drain water that falls on upland areas, and this moving water dissolves pollutants at a faster rate than standing water (cite textbook). However, due to the high production and placement of pollutants in these moving waters, the waters become polluted faster than the pollutant dilution rate, leading to over polluted rivers and streams. All three of the major contributors to pollution - industry, agriculture, and cities - are commonly found along moving waters, adding to the over-pollution of rivers and streams (cite textbook). Just the knowledge that fast moving waters can dilute pollutants has encouraged even more pollution, further adding to the pollution issue. Another issue contributing to the destruction of rivers and streams is the physical alteration of these moving waters, mainly in the form of dams, diversion of water, channel alteration, and land development (cite textbook). These alterations affect water temperature, water flow patterns, and increase sediment, destroying important habitat conditions for many aquatic organisms and reducing water quality (cite textbook).

An area of contention regarding the pollution of streams and rivers is the concept that the pollution upstream affects the people downstream (cite textbook). A factory’s waste upstream may contaminate someone’s drinking water downstream. This especially becomes an issue with bodies of moving water that border multiple countries or states, as what one country or state does upstream can drastically affect what the downstream country or state is able to do (cite textbook).

Lakes and Ponds

Lakes and ponds experience much of the same pollution as rivers and streams, but are polluted at a quicker rate due to slower moving waters, no water flow outlets, and amount of water (cite textbook). Standing water circulates much less than moving waters, with the deeper water layers only moving during seasonal changes twice a year (cite textbook). Lakes and ponds are basins into which running water usually flows and accumulates, meaning that the pollutants also accumulate with no outlet. Lakes and ponds contain less water than most rivers and streams, meaning smaller lakes and ponds are polluted at faster rates.

Eutrophication is the process of abundant plant growth, a dominating threat to standing waters (cite textbook). If chemical nutrients for aquatic plant growth that were previously limited become available, plant populations will increase rapidly. This excessive plant population growth decreases the oxygen content of the water and other aquatic life suffocates. Human waste often contains these chemical nutrients, like phosphorus in fertilizers, and in combination with the poor water circulation in standing waters, causes pollution and organism depletion (cite textbook). Much of the pollution issues that affect ponds and lakes also affect wetlands, as the water circulation of wetlands is also slow.

Groundwater

Surface water is where groundwater is being expressed, with wetlands being the largest examples of the water table being near or at the surface. The water found in freshwater habitats are the combination of surface flow, precipitation, and groundwater expression. This relationship between groundwater and surface water means that groundwater pollution affects surface freshwater pollution as well.

According to an Environmental Protection Agency survey, about a quarter of the United States’ usable groundwater is contaminated. Groundwater is the only source of drinking water for about half of the United States^[8]. As human populations increase and industrialize, the demand for groundwater is increasing, but the pollution of groundwater is also increasing. The pollution of groundwater is easy to achieve due to the slow circulation of water, even slower than that of lakes and ponds. The water must navigate through small holes in the aquifer rock, moving on average only a couple of inches each day (cite textbook). The rate of groundwater recharge is the time it takes for groundwater to replenish itself and extremely slow, leading to water shortages, as humans remove water from aquifers faster than the rate of recharge (cite textbook). Due to such slow circulation of water, groundwater can remain polluted for decades, as the natural purification processes are so slow.

Notes:

• Freshwater biology is the scientific study of the biology of freshwater organisms, their interactions, and habitats.
• Freshwater biome (textbook as source p. 120-121)
• Freshwater habitats support a wide variety of organisms with habitats including rivers, streams, lakes, ponds, and wetlands.
  • Running waters - rivers and streams
    • Running, fast-moving waters have a higher oxygen content, allowing different species to thrive and making pollution easier to combat
    • Open ecosystem (a system that is not isolated in that it exchanges matter and/or energy with other systems) and a lot of organic matter found in running water is from land runoff or further upstream. This matter is an important source of food for many species
    • Riparian zone - the area along a riverbank or streambank that is home to vital, high moisture plants. These plants create a buffer between the land and the running water system, protecting it from pollution and flooding. Additionally, these plants provide a large habitat for many wetland species, a large number of which are endangered or threatened. Lastly, riparian plants shade the water from sunlight, reducing the heat stress on the water and aquatic life, while also providing nutrients in the form of organic matter.
  • Standing waters - lakes and ponds
    • Stratification of water - layering of the water based on the oxygen content due to the slower motion of the water in standing water systems. The topmost layer has the most amount of oxygen and as depth increases, the oxygen decreases. Additionally, stratification is felt in the temperature of the water, as the water on top is the warmest, heated from the sun, and temperature decreases in the lower layers.
    • Thermocline - the boundary between the warm water on the surface and the deeper water at a cooler temperature.
    • The mixing of the layers of water in standing water mostly comes from seasonal overturn in the spring and fall.
    • Shore zone - the transitional zone between the water systems and land, similar to the riparian zone seen in running water systems. This area functions in much the same way as the riparian zone, the plants protecting the water from pollution, flooding, and heat stress, while also providing nutrients and habitats for aquatic and wetland species.
  • Estuaries - transitional ecosystems between the ocean and freshwater biomes
    • Large fluctuations in the salinity of the system
    • The flowing rivers provide estuaries with important nutrients, which are suspended in the water with oxygen due to the shallow water and tides. This in conjunction with available light allows for increased photosynthetic activity, creating a habitat that can support a large amount of organisms
    • Examples of organisms that reside in estuaries include:
      • Oysters, reefs, sponges, barnacles, fish
      • A single oyster reef has been found to support more than 300 species of organisms
  • Freshwater systems have two zones of life:
    • The bottom-dwelling benthic organisms
      • Crawling or burrowing invertebrates, various insects - crayfish, freshwater mussels
    • The swimming pelagic creatures
      • Fish (both bottom and shallow dwellers), amphibians (require water to reproduce), turtles, water mammals (otters, beavers, muskrats)
    • Freshwater plants
      • Algae, grasses, water lilies
      • Cattails, reeds, willows, river birches all occur along the riparian zone
  • Wetlands - marshes and swamps
    • Due to the waterlogged and submerged nature of the land, the anaerobic conditions of wetlands are unique and support a high diversity of organisms. Wetlands slow the decomposition of organic matter, creating layers of rich organic material that provides important nutrients for species in the system. Wetlands are the home to a large number of bird, amphibian, insect, reptile, grass, reed, and tree species that cannot inhabitat any other system, making them at risk to endangerment, as wetlands are being destroyed for urban development and agriculture.
    • Wetlands help combat pollution and climate change, as they filter pollutants and store a large amount of carbon in the biosphere, despite the small amount of land they occupy. Additionally, wetlands provide flood and storm protection, as the system can absorb large amounts of excess water. This also contributes to groundwater recharge, which is very important for human water use, as usable freshwater sources are dwindling.
• Pollution threats to freshwater systems (textbook as source p. 416-419)
  • According to the EPA, stormwater runoff from pavement and rooftops is the most common cause of water pollution. Stormwater runoff is rain and snowmelt. The impervious surfaces used in domestic and urban construction replace soil that used to absorb stormwater. This excess runoff can collect pollutants as it eventually makes its way into streams, rivers, lakes, wetlands, and even aquifers, polluting important freshwater ecosystems and usable water. Additionally, increased flooding and erosion can be caused by the increased stormwater runoff.
  • Rivers and Streams
    • Rivers and streams drain water that falls on upland areas, and this moving water decomposes pollutants at a faster rate than standing water. However, due to the high production placement of pollutants in these moving waters, they become polluted faster than they can dilute the pollutants, leading to over polluted rivers and streams. All three of the major contributors to pollution - industry, agriculture, and cities - are commonly found along moving waters, adding to the over-pollution of rivers and streams. Just the knowledge that fast moving waters can dilute pollutants has encouraged even more pollution, further adding to the pollution issue.
    • An area of contention regarding the pollution of streams and rivers is the concept that the pollution upstream affects the people downstream. A factory’s waste upstream may contaminate someone’s drinking water downstream. This especially becomes an issue with bodies of moving water that border multiple countries or states, as what one country or state does upstream can drastically affect what the downstream country or state is able to do.
    • Another issue contributing to the destruction of rivers and streams is the physical alteration of these moving waters, mainly in the form of dams, diversion of water, channel alteration, and land development. These alterations affect water temperature, water flow patterns, and increase sediment pollution, destroying important habitat conditions for many aquatic organisms and reducing water quality.
  • Lakes
    • Lakes and ponds experience much of the same pollution as rivers and streams, but are polluted at a quicker rate due to slower moving waters, no water flow outlets, and amount of water. Standing water circulates much less than moving waters, with the deeper water layers only moving during seasonal changes twice a year. Lakes and ponds are basins into which water usually flows and accumulates, meaning that the pollutants also accumulate with no outlet. Lakes and ponds contain less water than most rivers and streams, meaning smaller lakes and ponds are polluted at faster rates. Even if the lakes are large, they are still susceptible to quick pollution, as seen with the Great Lakes because they are used for many industries and dumping grounds for industrial waste and sewage. Eutrophication is the process of abundant plant growth and while an issue to all freshwater systems, a dominating threat to standing waters. If chemical nutrients for aquatic plant growth that were previously limited become available, plant populations will increase rapidly. This excessive plant population growth decreases the oxygen content of the water and other aquatic life suffocates. Human waste often contains these chemical nutrients, like phosphorus in fertilizers, and in combination with the poor water circulation in standing waters, causes pollution and organism depletion. Much of the pollution issues that affect ponds and lakes also affect wetlands, as the water circulation of wetlands is also slow.
  • Groundwater
    • Surface water is where groundwater is being expressed, with wetlands being the largest examples of the water table being near or at the surface. The water found in freshwater habitats are the combination of surface flow, precipitation, and groundwater expression. This relationship between groundwater and surface water means that groundwater pollution affects surface freshwater pollution as well. [diagram to explain this relationship]
    • According to an Environmental Protection Agency survey, about 25% of the United States’ usable groundwater is contaminated. Groundwater is the only source of drinking water for about half of the United States.
    • As human populations increase and industrialize, the demand for groundwater is increasing, but the pollution of groundwater is also increasing. The pollution of groundwater is easy to achieve rapidly due to the slow circulation of water, even slower than that of lakes and ponds. The water must navigate through pores in the aquifer rock, moving on average only a couple of inches each day. This slow movement is the rate of groundwater recharge, leading to water shortages, as humans remove water from aquifers faster than the rate of recharge. Due to such slow circulation of water, groundwater can remain polluted for decades, as the natural purification processes are so slow.
    • There are nine main contributors to groundwater pollution. Under the category of unintentional surficial percolation are landfills, waste disposal ponds, spills, and agriculture and land use. These pollutants are the result of a downward infiltration of rainwater that has passed through the aforementioned sites of pollutants. The only intentional surficial percolation is deep-well injection, which involves pumping waste into aquifers. Unintentional underground leakage includes septic tanks, buried wastes, and underground storage tanks, as pollutants from these sources leak into aquifer supplies. The last category is unintentional over-pumping that results in saltwater intrusion in the groundwater supply, making the water undrinkable and unusable for agricultural purposes.
• Freshwater biome (UC Museum of Paleontology as source)
  • Ponds and Lakes
    • Have limited species diversity because they are isolated from one another and other water systems
    • Divided into three zones determined by depth and distance from shore
      • Littoral zone - the top layer, the warmest as it is directly heated by the sun. There is a diverse community of species, like algae, rooted and floating aquatic plants, grazing snails, clams, insects, insect eggs and larvae, fishes, crustaceans, and amphibians. These organisms provide nutrients and food to other species, such as turtles, ducks, and snakes.
      • Limnetic zone - the next layer below the littoral zone, still well-lit and is occupied by phytoplankton, zooplankton, and fish. Plankton play a crucial role in the food web and support many important organisms.
      • Profundal zone - the deepest layer with very little light and is much colder and denser than the two previous layers. When plankton die they fall into this layer and provide nutrients to the fauna that live in this layer. These fauna are called heterotrophs, meaning they eat dead organisms and use oxygen for cellular respiration.
      • In between top and bottom layers, there is a narrow zone called the thermocline where the temperature of the water changes rapidly, especially during summer and winter temperature changes.
    • During the fall and spring, there is a mixing of layers usually due to wind that circulates oxygen and creates a more uniform temperature throughout the water system.
  • Streams and Rivers
    • Bodies of flowing water in one direction, get their starts at headwaters, which include springs, lakes, and snowmelt, and travel to their mouths, which are usually another water channel or the ocean.
    • The characteristics of the streams and rivers change throughout their journey from the source to the mouth. For example, the temperature is usually cooler at the source than the mouth. The water at the source is clearer, has a higher oxygen content, and heterotrophs and fish like trout are possible species. In the middle, the width usually expands and the species diversity increases, including aquatic green plants and algae. The water at the mouth has a lower oxygen concentration and is murkier due to the sediment that has been collected and traveled along the length of the river or stream. This increased sediment decreases the amount of light that is able to penetrate the water and there is less diversity of flora and the lower oxygen lowers the diversity of fauna.
  • Wetlands
    • Areas of standing water - marshes, swamps, and bogs are all considered wetlands.
    • The fauna that reside in wetlands are called hydrophytes, meaning they are adapted to very moist and humid conditions. For example, pond lilies, cattails, sedges, tamarack, cypress, gum, and black spruce.
    • Wetlands have the highest species diversity of all ecosystems. Some types of species include amphibians, reptiles, birds, and furbearers.
    • Wetlands are not only freshwater systems, as there are salt marshes and bogs that support different species.
• Freshwater Organisms
  • Freshwater organisms are generally divided into the categories of benthic and pelagic organisms and can include invertebrates, insects, fish, amphibians, mammals, birds, aquatic plants, and planktons.