Name: how chemolithotrophs make atp
Uploaded: 2025-06-12T09:35:21.000Z
Duration: 1 min 15 s
Channel: JoVE

I chemiolitotrofi ottengono energia ossidando composti inorganici come idrogeno gassoso, ammoniaca, solfuri e ferro ferroso. Gli elettroni di queste molecole entrano nella catena di trasporto degli elettroni, guidando la produzione di ATP attraverso la fosforilazione ossidativa tramite ATP sintasi. I donatori inorganici rilasciano meno energia rispetto alle molecole organiche. Di conseguenza, un minor numero di protoni viene pompato attraverso la membrana, con conseguente minore produzione di ATP. L'ossigeno è l'accettore di elettroni più comune, ma i chemiolitotrofi possono anche utilizzare nitrato, solfato o anidride carbonica in condizioni anaerobiche. La maggior parte dei chemiolitotrofi sono autotrofi e utilizzano la loro energia per fissare l'anidride carbonica e sintetizzare molecole organiche. Alcuni di essi si basano sul flusso inverso di elettroni per generare potenza riducente sotto forma di NADH. Ciò si verifica quando il donatore di elettroni ha un potenziale redox più elevato rispetto al NAD+. In questi casi, l'energia della forza motrice del protone viene utilizzata per spingere gli elettroni contro il gradiente per ridurre il NAD+ a NADH.

vie di conservazione dell’energia

Metabolism of Chemolithotrophs

I chemiolitotrofi sono microrganismi che ottengono energia ossidando molecole inorganiche come l&#8217;idrogeno molecolare (H_2), l&#8217;ammoniaca (NH_3), i composti ridotti dello zolfo (H_2S, S^2-) e il ferro ferroso (Fe^2+). A differenza degli organismi eterotrofi che si basano sul carbonio organico, i chemiolitotrofi trasferiscono elettroni da questi donatori inorganici alla catena di trasporto degli elettroni (ETC), generando una forza proton-motrice (PMF) che guida la sintesi di ATP attraverso la fosforilazione ossidativa. Tuttavia, visto che i donatori elettronici inorganici generalmente forniscono meno energia rispetto alle molecole organiche, i chemiolitotrofi devono ossidare grandi quantit&#224; di materiale inorganico per sostenere la crescita.
L&#8217;efficienza della produzione di energia nei chemiolitotrofi dipende dal potenziale redox dei loro donatori e accettori di elettroni. L&#8217;ossigeno (O_2) &#232; l&#8217;accettore finale di elettroni pi&#249; comunemente utilizzato, poich&#233; possiede un potenziale redox altamente positivo, massimizzando cos&#236; la resa energetica. Tuttavia, alcuni chemiolitotrofi possono utilizzare accettori alternativi come il nitrato (NO_3^-), il solfato (SO_4^2-) o l&#8217;anidride carbonica (CO_2) in condizioni anaerobiche. Dato che le molecole inorganiche forniscono meno energia rispetto ai substrati organici, le catene di trasporto degli elettroni nei chemiolitotrofi spesso pompano meno protoni attraverso la membrana, portando a una produzione di ATP inferiore rispetto agli organismi eterotrofi.
La maggior parte dei chemiolitotrofi &#232; autotrofa, il che significa che utilizza l&#8217;ATP e il potere riducente per fissare la CO_2 e sintetizzare molecole organiche per la crescita. Tuttavia, alcuni donatori inorganici di elettroni, come il Fe^2+ e il NO_2^-, possiedono potenziali redox pi&#249; elevati rispetto alla coppia NAD^+/NADH, rendendo termodinamicamente sfavorevole la riduzione diretta del NAD^+ a NADH. Per superare
questo ostacolo, molti chemiolitotrofi usano il flusso elettronico inverso, un processo che consuma energia e forza gli elettroni a fluire contro il gradiente termodinamico per produrre NADH per le reazioni biosintetiche.
I chemiolitotrofi vengono classificati in base ai donatori elettronici preferenziali. I batteri che ossidano l&#8217;idrogeno utilizzano H_2 come fonte energetica e trasferiscono elettroni al NAD^+ o alla ETC mediante enzimi idrogenasi. I batteri nitrificanti svolgono un ruolo cruciale nel ciclo dell&#8217;azoto ossidando l&#8217;ammoniaca (NH_3) in nitrito (NO_2^-) e successivamente in nitrato (NO_3^-), in un processo noto come nitrificazione. I batteri ossidanti lo zolfo metabolizzano composti solforati come H_2S and S^2-, generando solfato (SO_4^2-) e ATP sia tramite fosforilazione ossidativa che per fosforilazione a livello del substrato. Inoltre, i batteri anammox eseguono l&#8217;ossidazione anaerobica dell&#8217;ammoniaca, un processo unico che converte NH_4^+ e NO_2^- in azoto gassoso (N_2), contribuendo alla perdita di azoto negli ambienti acquatici.
I chemiolitotrofi svolgono un ruolo fondamentale nei cicli biogeochimici globali, in particolare nei cicli dell&#8217;azoto, dello zolfo e del ferro. Essi contribuiscono alla trasformazione e al riciclo dei nutrienti essenziali negli ecosistemi, influenzando la chimica del suolo e delle acque. Inoltre, questi microrganismi sono impiegati in numerose applicazioni industriali e ambientali, come il biorisanamento, la bioestrazione e il trattamento delle acque reflue. La loro capacit&#224; di prosperare in ambienti estremi, tra cui le sorgenti idrotermali abissali e i siti di drenaggio acido di miniera, evidenzia la loro versatilit&#224; metabolica e rilevanza ecologica.

Vie di Conservazione dell’Energia

I chemiolitotrofi sono microrganismi che ottengono energia ossidando molecole inorganiche come l&#8217;idrogeno molecolare (H_2), l&#8217;ammoniaca ...

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how chemolithotrophs make atp

Chemolithotrophs make ATP by using inorganic chemicals as an energy source. They oxidize molecules such as hydrogen gas, ammonia, reduced sulfur compounds, and ferrous iron. Instead of relying on organic carbon like heterotrophs, they move electrons from these inorganic donors into the electron transport chain, or ETC.

That electron flow builds a proton motive force, or PMF. The PMF drives ATP synthesis through oxidative phosphorylation. Because inorganic electron donors usually release less energy than organic molecules, chemolithotrophs often need to oxidize large amounts of inorganic material to support growth.

Their energy yield depends on the redox potential of the electron donor and acceptor. Oxygen is the most common terminal electron acceptor because it has a highly positive redox potential and gives the best energy yield. Some chemolithotrophs can also use nitrate, sulfate, or carbon dioxide as acceptors when oxygen is not available.

These microbes usually make less ATP than heterotrophs because their ETCs often pump fewer protons across the membrane. Most chemolithotrophs are autotrophs, so they use ATP and reducing power to fix carbon dioxide and build organic molecules. Some donors, such as Fe2+ and NO2-, have a higher redox potential than the NAD+/NADH pair, so direct NADH formation is not favorable.

To solve this problem, many chemolithotrophs use reverse electron flow. This process spends energy to push electrons against the normal gradient and make NADH for biosynthesis. Hydrogen-oxidizing bacteria use H2 and transfer electrons with hydrogenase enzymes. Nitrifying bacteria oxidize ammonia to nitrite and then nitrate, which is called nitrification and is important in the nitrogen cycle.

Sulfur-oxidizing bacteria use compounds such as H2S and S2- and produce sulfate. They can make ATP through both oxidative phosphorylation and substrate-level phosphorylation. Anammox bacteria carry out anaerobic ammonia oxidation and convert NH4+ and NO2- into nitrogen gas, which contributes to nitrogen loss in aquatic environments.

Chemolithotrophs are key parts of the nitrogen, sulfur, and iron cycles. They help recycle nutrients and shape soil and water chemistry. They are also used in bioremediation, bioleaching, and wastewater treatment, and many can live in extreme places such as deep-sea hydrothermal vents and acidic mine drainage sites.

How Chemolithotrophs Make ATP

microbial nutrition

Microbial Energy and Carbon Sources

Microbial energy and carbon sources determine how microorganisms live and grow. These metabolic strategies help microbes survive in many habitats and keep energy moving through ecosystems. They also support nutrient cycling in nature. Microbes are grouped by where they get energy, electrons, and carbon. Phototrophs use light, while chemotrophs use chemical compounds for energy. Lithotrophs take electrons from reduced inorganic substances, and organotrophs take them from organic compounds.

atp and energy production

How Cells Make and Use ATP

ATP is the main energy carrier in cells. It is made of adenosine, which includes adenine and ribose, plus three phosphate groups. The bonds between the phosphate groups hold a large amount of potential energy. When ATP is hydrolyzed, it becomes ADP or AMP and releases energy for cell work. Cells use that energy for many essential tasks. It supports macromolecule synthesis, intracellular transport, and mechanical movement. ATP also acts as an energy manager by linking catabolic and anabolic...

redox reactions

Electron Carriers in Redox Metabolism

Redox reactions move electrons through metabolic pathways in cells. Oxidation is the loss of electrons, and reduction is the gain of electrons. These two steps happen together, which keeps electron flow moving through metabolism. A clear example appears in bacterial metabolism. Glucose is oxidized to carbon dioxide, while oxygen is reduced to water. This shows how one molecule loses electrons as another gains them. Cells use special electron carriers to make these transfers happen.

introduction to metabolism

Metabolism: Energy Use and Biomolecule Synthesis

Metabolism is the set of chemical reactions that keep living cells working. It includes reactions that break down biomolecules and reactions that build them up. These two sides of metabolism work together to support energy balance and cell function. Catabolic pathways break large molecules into smaller parts. Carbohydrates, lipids, and proteins can be broken down into monosaccharides, fatty acids, and amino acids. These reactions release energy, and cells store much of that energy as ATP, or...

carbohydrate catabolism

Glucose Breakdown and ATP Production

Glucose breakdown is a key part of cell metabolism that lets cells make ATP, the usable form of energy. The process follows two main paths: cellular respiration and fermentation. Both start with glycolysis, which does not require oxygen. Glycolysis splits one glucose molecule into two molecules of pyruvic acid. It also produces a net gain of two ATP molecules and two NADH molecules. This step sets up the cell to continue with respiration or switch to fermentation, depending on whether oxygen...

glycolysis

Glycolysis and Pyruvate Fate

Glycolysis is a central pathway in glucose catabolism and a major way cells make energy. It is also called the Embden-Meyerhof pathway. This process takes place in the cytoplasm and can work with or without oxygen, which makes it useful in many organisms and conditions. Glycolysis has ten steps and turns one glucose molecule into two pyruvate molecules. It has two phases. In the preparatory phase, the cell uses two ATP to add phosphate groups to glucose and split it into two three-carbon...

other glycolytic pathways

Pentose Phosphate Pathway and Entner-Doudoroff

The pentose phosphate pathway works alongside glycolysis in cells that need both sugar breakdown and building blocks for growth. It handles pentoses, which are five-carbon sugars, and also uses glucose as a starting point. The pathway has two parts, an oxidative phase and a non-oxidative phase. It does not make ATP directly, but its products can feed back into glycolysis when the cell needs them. The oxidative phase mainly makes NADPH, a reduced electron carrier. In this phase,...

cellular respiration

Cellular Respiration: ATP Production Pathways

Cellular respiration is the process cells use to turn glucose into ATP, the main energy molecule in the cell. It depends on oxidation and the transfer of electrons to a separate electron acceptor. This sequence of reactions supports energy production in both aerobic and anaerobic settings. Glycolysis is the first step. It takes place in the cytoplasm of both prokaryotic and eukaryotic cells. One glucose molecule is broken into two pyruvate molecules, and the cell gains a net 2 ATP and 2 NADH.

electron transport chain components

Electron Transport Chain and ATP Production

The electron transport chain helps cells make ATP by moving electrons through membrane protein complexes. In eukaryotic cells, it sits in the inner mitochondrial membrane. In prokaryotic cells, it is found in the plasma membrane and can differ in the number and type of complexes, depending on the organism and its environment. The chain uses several electron carriers to pass electrons along in redox reactions, which are reactions that involve oxidation and reduction. These carriers include...

chemiosmosis and atp synthesis

Electron Transport Chain Powers ATP Output

The electron transport chain powers ATP production during cellular respiration. It sits in the inner mitochondrial membrane and moves high-energy electrons from NADH and FADH2 to molecular oxygen, the final electron acceptor. As electrons move through the chain, protons are pushed across the membrane to build the gradient needed for ATP synthesis. Electrons from NADH enter the chain at Complex I, also called NADH: ubiquinone oxidoreductase. In prokaryotes, this step helps pump protons from the...

respiration pathways

TCA Cycle and Energy Pathways

Cellular respiration uses the TCA cycle, also called the Krebs cycle, to help cells make usable energy from organic molecules. This pathway is a central part of aerobic respiration and also supports biosynthesis. It links the breakdown of food molecules to the cell's energy needs. Pyruvate from glycolysis enters this process first. The pyruvate dehydrogenase complex converts pyruvate into acetyl-CoA through oxidative decarboxylation. This step produces one NADH and one carbon dioxide molecule.

microbial fermentation

Fermentation Products in Microbes

Fermentation is an anaerobic process that lets microbes make energy from sugar without oxygen or an electron transport chain. It is important in both biology and industry. The process is grouped by the products it makes. Pyruvate and its derivatives act as key electron acceptors in fermentative pathways. This step helps oxidize NADH back to NAD+, which is needed for glycolysis to keep running. Without NAD+ regeneration, glycolysis would stop and the cell would lose its main source of ATP under...

metabolism of chemolithotrophs

Chemolithotrophs make ATP by using inorganic chemicals as an energy source. They oxidize molecules such as hydrogen gas, ammonia, reduced sulfur compounds, and ferrous iron. Instead of relying on organic carbon like heterotrophs, they move electrons from these inorganic donors into the electron transport chain, or ETC. That electron flow builds a proton motive force, or PMF. The PMF drives ATP synthesis through oxidative phosphorylation. Because inorganic electron donors usually release less...

amino acid catabolism

Microbes Use Proteins for Energy

Microbes can use proteins as a carbon and energy source, especially when polysaccharides or lipids are scarce. But proteins are too large to pass through the plasma membrane on their own. To solve this, microbes secrete extracellular proteases and peptidases that break proteins into peptides. The peptides are then transported into the cell, where intracellular proteases cut them into free amino acids. Once amino acids are available, microbes break them down in two main ways: deamination and...

lipid catabolism

How Microbes Break Down Fats for Energy

Microbes break down triglycerides and fatty acids to make energy. Triglycerides are important long-term energy storage molecules in microorganisms. Lipases hydrolyze, or split with water, triglycerides into glycerol and free fatty acids. Each product then enters a different metabolic route that helps the cell make ATP, the main energy currency. Glycerol metabolism begins after glycerol is released from triglyceride hydrolysis. Glycerol kinase adds a phosphate group to form glycerol-3-phosphate.

oxygenic photosynthesis

How Plants Make Oxygen and ATP

Oxygenic photosynthesis is the process plants, algae, and cyanobacteria use to capture light energy and turn it into chemical energy. It uses water as the source of electrons and releases molecular oxygen, or O2. The process also produces ATP and NADPH, which cells need for later energy use and carbon fixation. The main reactions happen in the thylakoid membranes, where chlorophyll pigments absorb light. In cyanobacteria, these membranes come from folds in the plasma membrane. Two photosystems...

anoxygenic photosynthesis

Bacterial Light Capture Without Oxygen

Anoxygenic photosynthesis is a bacterial way to capture light energy without making oxygen. It supports carbon fixation, but it does not use water as the electron donor. Instead, these phototrophs use other electron donors such as hydrogen sulfide, elemental sulfur, thiosulfate, or organic compounds. This process is carried out by several groups of bacteria, including purple bacteria, green sulfur bacteria, heliobacteria, and other anoxygenic phototrophs. These organisms have evolved a...

biosynthesis in bacteria

How Bacteria Build Key Macromolecules

Bacteria build essential macromolecules through tightly controlled biosynthetic pathways. These anabolic reactions make proteins, nucleic acids, lipids, and polysaccharides. The products support growth, cell division, and normal cell function. Bacterial biosynthesis starts with precursor metabolites from glycolysis, the pentose phosphate pathway, and the Krebs cycle. Important precursors include pyruvate, acetyl-CoA, and glucose-6-phosphate. Cells use these compounds to make the monomers that...

carbon-dioxide fixation

Microbial Carbon Fixation Pathways

Microbial carbon fixation pathways let prokaryotes turn carbon dioxide into organic molecules. This process supports biosynthesis, helps sustain ecosystems, and plays a role in the global carbon cycle. It also has industrial uses in carbon capture and bioproduct synthesis. Autotrophic organisms depend on this process to use CO2 as a carbon source in many environments. The Calvin cycle is the most common carbon fixation pathway. Cyanobacteria and other autotrophic prokaryotes use it, and it...

biosynthesis of polysaccharides

Activated Sugars for Polysaccharide Synthesis

Activated sugars drive polysaccharide synthesis in cells. Glycogen and starch are built from nucleoside diphosphate sugars, mainly uridine diphosphate glucose (UDPG) and adenosine diphosphate glucose (ADPG). These sugar donors act as high-energy intermediates in carbohydrate metabolism and biosynthesis. UDPG supports glycogen synthesis in animals and many bacteria. It forms when glucose-1-phosphate reacts with uridine triphosphate (UTP). UDP-glucose pyrophosphorylase catalyzes this reaction.

inorganic nitrogen assimilation

Nitrogen Uptake by Microbes

Nitrogen uptake by microbes is essential for making proteins, nucleic acids, and other cell parts. Many bacteria and archaea take in nitrogen as nitrate or ammonia. They then convert it into forms that can be built into biomolecules. When nitrate enters a cell, it goes through assimilatory nitrate reduction. This is a two-step process. First, nitrate reductase changes nitrate to nitrite using NADH or FAD as an electron donor, depending on environmental and cellular conditions. Then nitrite...

sulfur assimilation

Sulfur Uptake and Cysteine Synthesis

Sulfur uptake and cysteine synthesis are key parts of microbial metabolism. Sulfur is needed to build important biomolecules, including the amino acids cysteine and methionine, as well as cofactors such as coenzyme A and biotin. Microorganisms usually take in sulfur from the environment as sulfate, but sulfate must be changed before cells can use it. Because sulfate is highly oxidized, it must go through assimilatory sulfate reduction to become biologically useful. Some microorganisms can also...

amino acid biosynthetic pathways

Amino Acid Building from Cell Metabolites

Amino acid biosynthesis lets cells build amino acids from common metabolic intermediates. These amino acids support cell growth, protein synthesis, and metabolic regulation. The main source molecules come from glycolysis, the tricarboxylic acid (TCA) cycle, and the pentose phosphate pathway. Key precursors include alpha-ketoglutarate, pyruvate, oxaloacetate, phosphoenolpyruvate, and erythrose-4-phosphate. They supply the carbon skeletons needed to form amino acids. Nitrogen must also be added...

biosynthesis of nucleic acids

Nucleotide Building Blocks for DNA and RNA

Nucleotide biosynthesis makes the building blocks needed for DNA and RNA. Cells use this pathway to make purine and pyrimidine nucleotides and keep their supply balanced. That balance helps protect genetic integrity and supports normal cell function. Purine nucleotide synthesis starts with ribose-5-phosphate, a sugar made in the pentose phosphate pathway. PRPP synthetase adds phosphate groups to form phosphoribosyl pyrophosphate, or PRPP, which is the activated starting point for the pathway.

biosynthesis of lipids

How Membrane Lipids Vary Across Life

Membrane lipids vary across Bacteria, Archaea, and Eukarya, and these differences help cells survive in different environments. The three domains of life make lipids through distinct biosynthetic pathways. Those pathways create membranes with different stability, permeability, and flexibility. Bacteria and eukaryotes both build fatty acid-based lipids from acetyl-CoA and malonyl-CoA. The pathway includes condensation, reduction, and dehydration steps. Bacteria use a type II fatty acid...

formation of lipopolysaccharides

Lipopolysaccharides and Gram-Negative Defense

Lipopolysaccharides (LPS) are important parts of the outer membrane of Gram-negative bacteria. They help stabilize the membrane and help protect bacteria from host immune responses. LPS has three main parts: lipid A, a core oligosaccharide, and an O antigen. LPS biosynthesis and assembly depend on a coordinated set of enzymes and transport steps. The molecule is also known as an endotoxin. It can activate Toll-like receptor 4 (TLR4) in the host and trigger strong immune responses. In severe...

key terms and concepts

Learn how chemolithotrophs use inorganic molecules like hydrogen, ammonia, sulfur, and iron to make ATP, fix CO2, and drive nitrogen and sulfur cycles.

How Chemolithotrophs Make ATP | 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.

microbiology

How Chemolithotrophs Make ATP

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