Name: microbes in streams, lakes, and rivers
Uploaded: 2026-03-12T13:57:36.000Z
Duration: 1 min 24 s
Channel: JoVE

K12 Standards

Alabama Course of Study Science

9-12

Environmental Science

Unity and Diversity

9-12.EVS.2.3.b

Freshwater Microbial Ecology

Die mikrobielle Ökologie des Süßwassers wird durch die Verfügbarkeit von organischem Kohlenstoff, Nährstoffen, Sauerstoff und Licht geprägt.Nahe der Oberfläche nutzen Phytoplankton Sonnenlicht, um Kohlendioxid in organischen Kohlenstoff umzuwandeln.In flachen Gewässern tragen Diatomeen zur organischen Kohlenstoffproduktion bei, während heterotrophe Mikroben diesen organischen Kohlenstoff abbauen, Kohlendioxid freisetzen und Nährstoffe zurück ins Wasser zurückführen.Biofilme auf untergetauchten Oberflächen fangen organische Substanz aus dem Wasser ein, wo Bakterien, Pilze und Protisten zusammenarbeiten, um sie abzubauen und Kohlendioxid freizusetzen.Die benthischen Zonen erhalten typischerweise Kohlenstoff aus Laubstreu und untergetauchtem organischem Material, das von heterotrophen Mikroben abgebaut wird.Diese Mikroben setzen gelösten organischen Kohlenstoff wieder ins Wasser frei und unterstützen so nahegelegene mikrobielle Gemeinschaften.Städtischer und landwirtschaftlicher Abfluss kann organische Abfälle ins Süßwasser einführen, was zu Eutrophierung führt.Dies fördert cyanobakterielle Blüten an der Oberfläche und anschließende Sauerstoffmangel, da heterotrophe Mikroben überschüssige Biomasse zersetzen und so die Gesamtstruktur der mikrobiellen Gemeinschaft beeinflussen.

süßwassermikrobielle Ökologie

Süßwassersysteme wie Bäche, Flüsse und Seen weisen besondere physikalische und biologische Merkmale auf, die ihre mikrobiellen Gemeinschaften beeinflussen. Diese Umgebungen werden grob in lotische Systeme unterteilt – solche mit fließenden Gewässern wie Bächen und den meisten Flüssen – und lentische Systeme, zu denen stehende oder langsam fließende Gewässer wie Seen, Teiche und Sümpfe gehören.In lentischen Systemen treibt Phytoplankton die Primärproduktion an und erzeugt autochthonen organischen Kohlenstoff. Im Gegensatz dazu erleben lotische Systeme Turbulenzen, wenig Licht und schnelle Vermischung, was das Planktonwachstum einschränkt. Diese fließenden Gewässer sind stattdessen auf allochthone Kohlenstoffeinträge – sowohl gelöste als auch partikel – aus der umliegenden Vegetation und menschlichen Aktivitäten angewiesen, was die mikrobielle Besiedlung unterstützt.Bäche und Flüsse unterstützen oft lebendige benthische mikrobielle Gemeinschaften, wobei Biofilme sowohl photosynthetische Organismen als auch Heterotrophe enthalten. Diese Biofilme spielen eine entscheidende Rolle beim Nährstoffrecycling und der Zersetzung organischer Substanz. Allerdings können Störungen durch städtischen Abfluss oder landwirtschaftliche Aktivitäten dieses Gleichgewicht stören, was zu einem reduzierten Sauerstoffgehalt, bekannt als Sauerstoffabsenkung, und potenzieller Anoxie führt. Punktverschmutzung, wie Abwassereinleitungen, und diffuse Verschmutzungen wie Abfluss von Bauernhöfen können mikrobielle Dynamiken verändern und die Wasserqualität verringern.Seen unterscheiden sich erheblich durch ihre lentische Natur. Ihre mikrobielle Struktur wird durch Tiefe, Nährstoffverfügbarkeit und thermische Schichtung beeinflusst. Flache Seen können benthische Autotrophe in der gesamten Wassersäule unterstützen, während tiefere Seen im Sommer deutliche thermische Schichten entwickeln. Das obere Epilimnion ist sauerstoffreich und produktiv, während das tiefere Hypolimnion aufgrund begrenzter Mischung und Atmung, die die Sauerstoffdiffusion übertrifft, oft anoxisch wird. Saisonale Umschläge im Herbst und Frühling können die Nährstoffe umverteilen, was zu vorübergehenden Blüten führt.Tropische Seen, obwohl sie im Sommer den gemäßigten Seen ähneln, erleben das ganze Jahr über Wärme und regenbedingte Dynamiken. Dies fördert kontinuierliche Produktivität und häufige Blüten, insbesondere bei stickstofffixierenden Cyanobakterien. Auch Seen variieren im Nährstoffgehalt, von nährstoffarmen oligotrophen Systemen, die das ganze Jahr über sauerstoffhaltig bleiben, bis hin zu nährstoffreichen eutrophen Seen, die große cyanobakterielle Populationen unterstützen. Diese Mikroben gedeihen in alkalisch, warmem Wasser und können eukaryotische Algen verdrängen, wobei sie manchmal Toxine produzieren und die Wasserqualität verändern.

Süßwassermikrobielle Ökologie

Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. ...

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Education

Lehre

JoVE Core

Microbiology

Mikrobiologie

Unit

Einheit

Microbial Ecology

Mikrobielle Ökologie

KEY TERMS AND CONCEPTS

ZENTRALE BEGRIFFE UND KONZEPTE

microbes in streams, lakes, and rivers

Freshwater microbes live in streams, rivers, lakes, ponds, and marshes, but their communities change with water movement, light, depth, and nutrients. These systems are often grouped into lotic waters, which flow, and lentic waters, which are still or slow-moving. The physical setting shapes where microbes grow and how they get energy.

In lentic systems, phytoplankton are the main producers. They make autochthonous organic carbon, which means carbon made within the water body. In lotic systems, rapid mixing, low light, and turbulence limit plankton growth. These flowing waters depend more on allochthonous carbon, which is material that comes from outside the water, such as vegetation and human activity.

Streams and rivers often have active benthic microbial communities on the bottom. Their biofilms include photosynthetic organisms and heterotrophs, which must obtain energy from organic matter. These biofilms help recycle nutrients and break down organic matter. Urban runoff or agricultural activity can disturb this balance and lower oxygen levels, a pattern called oxygen sag, which can lead to anoxia, or very low oxygen.

Pollution also changes freshwater microbes. Point source pollution, such as wastewater discharge, and nonpoint source pollution, such as farm runoff, can shift microbial communities and reduce water quality. Lakes show another set of patterns because depth and thermal stratification, or layering by temperature, strongly affect them. Shallow lakes may support benthic autotrophs through much of the water column, while deeper lakes form separate layers in summer.

In deep lakes, the upper epilimnion is oxygen-rich and productive. The lower hypolimnion often becomes anoxic because mixing is limited and respiration uses oxygen faster than it can diffuse downward. Seasonal overturn in autumn and spring can move nutrients through the water and trigger short-lived blooms. Tropical lakes also support frequent blooms, but they stay warm year-round and respond strongly to rainfall, especially when nitrogen-fixing cyanobacteria grow.

Lakes also vary in nutrient level. Oligotrophic lakes are nutrient-poor and usually stay oxygenated throughout the year. Eutrophic lakes are nutrient-rich and can support large cyanobacterial populations. These microbes do well in warm, alkaline water and may outcompete eukaryotic algae. Some can also produce toxins and change water quality.

Microbes in Streams, Lakes, and Rivers

introduction to microbial ecology

Microbial Communities in Soil and Extremes

Microbial ecology looks at how microorganisms live, interact, and adapt in different ecosystems. It also shows how these tiny organisms help shape nutrient cycling, energy flow, and environmental balance. An ecosystem includes living parts and non-living parts, and microbes respond to both. Microorganisms can form populations, which are groups of the same species living together at the same time. When populations from different species live and interact in the same place, they form a microbial...

ecological niche

Microbial Niches in Ecosystems

Microbial niches describe how microorganisms survive, grow, and interact in an ecosystem. A niche includes how a microbe gets resources, reproduces, and relates to other species in its environment. This idea helps explain microbial community dynamics, biogeography, and ecosystem function. A microorganism’s fundamental niche is the full range of conditions where it could survive, grow, and reproduce. These conditions include both biotic factors, such as living interactions, and abiotic factors,...

methods to assess microbial populations

Measuring Microbes in Samples

Measuring microbes in a sample helps scientists study health, ecology, and industry. Microbial counts can show how many cells are present, how diverse they are, and what they may be doing. To do this, researchers use both culture-based and molecular methods. A viable plate count is a classic culture method for estimating living microbes. The sample is first diluted step by step, then spread on nutrient agar plates. Each viable cell can grow into a visible colony, so the colonies can be counted.

methods to assess microbial communities

Measuring Microbial Diversity and Activity

Microbial communities include bacteria, archaea, and eukaryotic microorganisms. They live in many ecosystems and affect important environmental and biological processes. Scientists study these communities by looking at how many species are present, how many individuals each species has, and how evenly the species are spread out. Species richness is the number of different species in a sample. Species abundance is the relative amount of each species. Species evenness describes how uniformly the...

the winogradsky column

Microbial Layers Inside a Winogradsky Column

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microenvironments

Microbial Niches in Tiny Habitats

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microbial mats

Microbial Mats and Oxygen Gradients

Microbial mats are layered communities of microbes that grow in response to changes in light, oxygen, and nutrients. These ecosystems are highly organized, and different microorganisms live at different depths. Biofilms are the early stage of this growth and are only a few millimeters thick. Mature microbial mats can grow to centimeter scale and show clear vertical structure. This layered arrangement lets microbes fill separate niches within a very small space. In cyanobacterial mats from hot...

microbial interactions: mutualism

Mutualistic Partnerships in Nature

Mutualistic partnerships in nature show how two or more organisms can benefit from living together. These symbiotic relationships can be obligate, meaning the partners depend on each other, or facultative, meaning the association is helpful but not required. Mutualism helps support many ecosystem functions across land and water. One common example is the partnership between plant roots and mycorrhizal fungi, such as Rhizophagus species. The fungal hyphae grow into the root hairs and epidermis,...

microbial interactions: cooperation

Microbial Cooperation in Soil and Hosts

Microbial cooperation describes helpful interactions between different species. In these partnerships, microbes work together for one or mutual benefit. These interactions can shape ecosystems and evolution. They also play major roles in symbiosis and disease. One clear example involves the Gram-negative bacterium Xenorhabdus nematophila and the parasitic nematode Steinernema carpocapsae. Juvenile nematodes carry the bacteria in the soil and need an insect host to mature. When the nematode...

microbial interactions: predation

How Microbes Hunt and Defend

Microbial predation is a form of interaction in which one microorganism kills and eats another to gain nutrients and energy. It includes both bacterial predators and protozoan predators. This process helps shape microbial communities and affects how nutrients move through the environment. Some bacterial predators attack from the outside, while others enter the prey cell. Epibiotic predators, such as Vampirococcus, attach to the surface of a prey cell and release hydrolytic enzymes. These...

microbial interactions: competition

Microbial Competition and Niche Partitioning

Microbial competition shapes how bacteria and other microbes share space and resources. In shared environments, they compete for nutrients, space, or light. The strength of this competition depends on the environment, including nutrient levels, space limits, and how many microbial species are present. These interactions help determine the structure, function, and resilience of microbial communities. Microbial competition is usually grouped into exploitative competition and interference...

microbial interactions: parasitism

Microbial Parasites and Host Dependence

Microbial parasites depend on a host for nutrients and shelter, and this dependence often harms the host. In parasitism, only the parasite benefits. This is different from mutualism, where both organisms gain from the relationship. Microbial parasites are classified by where they live in or on the host. Ectoparasites stay on the host’s surface, such as the skin or outer tissues, and take in nutrients from outside. Endoparasites live inside the host’s body and invade tissues or organs.

microbe-plant interactions

How Plant Microbes Affect Growth

Plant microbes can help, harm, or simply live alongside their hosts. These microbe-plant interactions shape plant growth, health, and ecosystem function. The plant microbiome includes bacteria, fungi, archaea, protists, and viruses, and these organisms may live on the plant surface, inside plant tissues, or in symbiosis throughout the plant. Some of the most important beneficial partnerships involve mycorrhizal fungi. These fungi form close connections with roots and are grouped as arbuscular...

microbes and the carbon cycle

How Microbes Move Carbon Through Earth

Microbes move carbon through Earth’s major reservoirs and help drive the carbon cycle. Carbon shifts among the biosphere, lithosphere, atmosphere, and hydrosphere, where it supports life and helps regulate climate. It commonly cycles as carbon dioxide (CO2), the oxidized form of carbon, but methane (CH4) and organic compounds also matter. Photosynthetic microbes take in atmospheric CO2 and turn it into organic carbon. Cyanobacteria are especially important because they carry out oxygenic...

microbes and methanogenesis

How Microbes Produce Methane

Methane production in anaerobic ecosystems depends on methanogenic archaea and the microbes that work with them. This process happens where oxygen is absent, such as wetlands, sediments, and animal gastrointestinal tracts. In these anoxic habitats, aerobic respiration cannot run, so microbes use other pathways to break down organic matter. Anaerobic decomposition starts when cellulolytic bacteria, or cellulose-digesting bacteria, hydrolyze dead organic material into simple sugars. Other...

microbes and the nitrogen cycle

Microbial Steps in the Nitrogen Cycle

Microbes drive the nitrogen cycle by changing nitrogen into forms that plants and other organisms can use. This biogeochemical cycle keeps nitrogenous compounds balanced in ecosystems. It also supports plant growth and microbial growth. Nitrogen fixation begins the cycle by converting inert atmospheric nitrogen gas, N2, into ammonia, NH3. This step depends on nitrogenase enzymes. Free-living diazotrophs do this on their own. Aerobic bacteria such as Azotobacter spp. and anaerobic bacteria such...

microbes and the sulfur cycle

Sulfur Cycling Through Microbial Reactions

Sulfur cycling depends on microbial reactions that move sulfur through rocks, water, soil, and the air. In Earth systems, sulfur shifts among inorganic forms such as sulfate, elemental sulfur, and sulfide. These changes happen through both abiotic processes and biological activity in oxic and anoxic environments. Sulfate is the most oxidized form of sulfur. It is stored mainly in rocks, marine sediments, and ocean water, where it acts as a long-term reservoir in the global sulfur cycle. In...

microbes and other elemental cycles

Microbes Driving Iron and Manganese Cycles

Microbes drive iron and manganese cycling in aquatic environments by changing these metals between reduced and oxidized forms. These reactions are especially important along redox gradients, where oxygen levels shift across stratified water layers. The microbes use these metals for energy, growth, and structural needs. In oxygen-rich surface waters, iron is usually present as insoluble ferric iron, Fe(III). Some bacteria release siderophores, which are small organic molecules that bind ferric...

marine microbial ecology

Microbial Life in the Ocean

Marine microbial life is shaped by salinity, low nutrients, and changing oxygen levels. These physical and chemical limits influence which microbes can survive and how they function. They also affect how ocean microbes help drive nutrient and carbon cycling. Small cell size is common in these environments because it gives microbes a larger surface-to-volume ratio. That helps them take up nutrients more efficiently when nutrients are scarce. In estuaries, where salinity changes often,...

deep sea microbial ecology

Deep Sea Microbes and Extreme Conditions

Deep sea microbes live in one of Earth’s harshest environments. The deep ocean is far below the sunlit photic zone, which usually reaches the upper 100 to 200 meters of open water. Below that layer, the bathypelagic and abyssal zones stretch from about 1,000 to 6,000 meters, and hadal trenches go even deeper. This region is dark, cold, and highly pressurized. Temperatures are usually around 2 to 3°C, although hydrothermal vents can be slightly warmer. Pressure rises by about 1 atmosphere for...

freshwater microbial ecology

Freshwater microbes live in streams, rivers, lakes, ponds, and marshes, but their communities change with water movement, light, depth, and nutrients. These systems are often grouped into lotic waters, which flow, and lentic waters, which are still or slow-moving. The physical setting shapes where microbes grow and how they get energy. In lentic systems, phytoplankton are the main producers. They make autochthonous organic carbon, which means carbon made within the water body. In lotic...

soil microbial ecology

How Soil Microbes Cycle Nutrients

Soil microbes drive nutrient cycling, organic matter turnover, and ecosystem stability. A gram of soil can contain thousands of bacterial and archaeal taxa, but their shared job is what helps sustain land ecosystems. Their activity changes the way carbon, nitrogen, and other nutrients move through soil. Soil is a patchwork of minerals, organic matter, water, and air. Microbes live in tiny microhabitats shaped by pore size, moisture, oxygen, and nutrients. Sandy soils drain fast and tend to...

key terms and concepts

Explore how water flow, depth, nutrients, and pollution shape freshwater microbes in streams, rivers, lakes, and cyanobacteria blooms.

Microbes in Streams, Lakes, and Rivers | JoVE K12

JoVE Core Microbiology provides an engaging introduction to the microbial world and its influence on health, industry, and the environment. This comprehensive collection covers key concepts such as microbial structure, metabolism, genetics, and ecology. It introduces essential laboratory techniques and microscopy methods through visually engaging animations. Corresponding scientist-in-action videos bridge classroom concepts with real-world research and applications.

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Microbes in Streams, Lakes, and Rivers

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