Name: how early cells got their start
Uploaded: 2026-03-12T13:57:39.000Z
Duration: 1 min 24 s
Channel: JoVE

K12 Standards

Alabama Course of Study Science

9-12

Environmental Science

Earth's Systems

9-12.EVS.3.4

Origin of Cellular Life

Una delle diverse ipotesi suggerisce che le forme di vita più antiche probabilmente abbiano avuto origine nelle bocche idrotermali sul fondo oceanico.Le bocche idrotermali fornivano calore, gradienti chimici e composti inorganici, come idrogeno e solfuro di idrogeno. Questo ambiente potrebbe aver facilitato la sintesi abiotica di molecole organiche, inclusi amminoacidi, lipidi e nucleotidi.I pori minerali all'interno delle strutture delle bocche idrotermali avrebbero potuto servire come primi compartimenti biologici, concentrando queste molecole e unendole per reazioni chimiche.Alcuni modelli suggeriscono che le protocellule siano emerse quando si sono formate membrane lipidiche, sostituendo infine i compartimenti minerali.Queste cellule probabilmente contenevano RNA autoreplicante, capace di immagazzinare informazioni genetiche e catalizzare la sintesi proteica.Con l'emergere delle proteine, le loro interazioni con l'RNA probabilmente hanno guidato la transizione al DNA, un materiale genetico più stabile.Dal punto di vista metabolico, le prime cellule erano probabilmente chemolitotrofi, che utilizzavano idrogeno come donatore di elettroni e zolfo o anidride carbonica come accettori di elettroni per sintetizzare composti organici.

origine della vita cellulare

L'origine della vita sulla Terra è un evento complesso ed enigmatico radicato in antichi processi biochimici e condizioni geologiche. Le evidenze sperimentali supportano l'ipotesi che la vita sia iniziata con la formazione spontanea di molecole organiche come nucleotidi a RNA, amminoacidi e lipidi nelle condizioni terrestri primitive. Fattori come l'attività vulcanica, la radiazione UV intensa e un'atmosfera in riduzione senza ossigeno libero probabilmente hanno facilitato queste reazioni. Le bocche idrotermali sul fondale oceanico sono considerate un sito probabile per le prime forme di vita, poiché potrebbero fornire gas ridotti come idrogeno (H₂) e solfuro di idrogeno (H₂S), facilitando la chimica prebiotica. I pori minerali forniscono spazi confinati che concentrano i reagenti, a differenza dell'oceano aperto dove le molecole sarebbero fortemente diluite. Inoltre, le superfici minerali—spesso ricche di ferro e zolfo—possono agire come catalizzatori primitivi. Queste superfici potrebbero aver contribuito ad accelerare le reazioni chimiche portando le molecole in contatto stretto e abbassando l'energia necessaria affinché le reazioni avvengano.Si ritiene che l'RNA abbia avuto un ruolo centrale nella prima vita grazie alla sua capacità di immagazzinare informazioni genetiche e catalizzare reazioni biochimiche. I ribozimi dimostrano che l'RNA può svolgere funzioni simili a quelle degli enzimi, offrendo una plausibile fase intermedia prima dell'evoluzione degli enzimi a base proteica. L'emergere finale di DNA, RNA e proteine pose le basi per l'architettura molecolare tripartita condivisa da tutti gli organismi moderni. Si stima che l'ultimo antenato comune universale (LUCA) sia vissuto circa 3,8-3,7 miliardi di anni fa, segnando la divergenza tra batteri e archaea, anche se il momento esatto rimane incerto.La prima vita cellulare si diversificò metabolicamente nell'ambiente ossico terrestre. Gli autotrofi primitivi utilizzavano CO₂ come fonte di carbonio, spesso facendo affidamento su H₂ come donatore di energia. L'evoluzione della fissazione dell'azoto ampliò le possibilità metaboliche, mentre le vie energetiche a base di zolfo probabilmente fornivano ulteriori reazioni escargoniche. La chemolitotrofia alimentata dall'idrogeno ha permesso la sintesi di molecole organiche da CO₂, supportando ecosistemi sempre più complessi. Col tempo, le innovazioni microbiche—inclusa l'avvento della fotosintesi ossigenosa—hanno trasformato l'atmosfera terrestre, permettendo infine l'ascesa della vita aerobica.

Origine della vita cellulare

The origin of life on Earth is a complex and enigmatic event rooted in ancient biochemical processes and geological conditions. Experimental evidence ...

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Education

Didattica

JoVE Core

Microbiology

Microbiologia

Unit

Unità

Microbial Evolution

Evoluzione microbica

KEY TERMS AND CONCEPTS

TERMINI E CONCETTI CHIAVE

how early cells got their start

Early cellular life began under the harsh conditions of early Earth, where simple chemicals could form more complex organic molecules. Experimental evidence supports the idea that RNA nucleotides, amino acids, and lipids could arise spontaneously in this environment. Volcanic activity, strong UV radiation, and an atmosphere with little or no free oxygen likely helped drive these reactions.

Hydrothermal vents on the ocean floor are considered one likely setting for the first life forms. These vents could supply reduced gases such as hydrogen and hydrogen sulfide, which support prebiotic chemistry, or chemistry that happens before life exists. Mineral pores would have trapped molecules in small spaces, so reactants were less diluted than they would be in the open ocean.

Mineral surfaces may also have helped early reactions. Many of these surfaces are rich in iron and sulfur, and they can act as primitive catalysts. A catalyst speeds up a reaction by lowering the energy needed and by bringing molecules close together.

RNA likely played a major role in early life because it can store genetic information and also help carry out chemical reactions. RNA molecules that act like enzymes are called ribozymes, and they show how RNA could have worked before protein enzymes evolved. Over time, DNA, RNA, and proteins formed the basic molecular system shared by modern organisms.

Scientists estimate that the last universal common ancestor, or LUCA, lived about 3.8 to 3.7 billion years ago. This was the point at which Bacteria and Archaea began to diverge, although the exact timing is still uncertain. Early cells then diversified in Earth’s oxygen-free environment.

Primitive autotrophs used carbon dioxide as a carbon source and often depended on hydrogen as an energy donor. Later, nitrogen fixation expanded the kinds of metabolism that were possible. Sulfur-based energy pathways also likely provided useful energy, and hydrogen-driven chemolithotrophy helped cells make organic molecules from carbon dioxide. Over time, microbial innovations, including oxygenic photosynthesis, changed Earth’s atmosphere and made aerobic life possible.

How Early Cells Got Their Start

origin of cellular life

Early cellular life began under the harsh conditions of early Earth, where simple chemicals could form more complex organic molecules. Experimental evidence supports the idea that RNA nucleotides, amino acids, and lipids could arise spontaneously in this environment. Volcanic activity, strong UV radiation, and an atmosphere with little or no free oxygen likely helped drive these reactions. Hydrothermal vents on the ocean floor are considered one likely setting for the first life forms. These...

origin of photosynthesis

How Photosynthesis Changed Earth

Photosynthesis changed Earth’s atmosphere and made complex life possible. It began about 3.4 to 3.8 billion years ago, when the first photosynthetic organisms used light energy to build organic compounds. These early organisms were anoxygenic phototrophs, which means they made food from light but did not release oxygen. Early photosynthesis used hydrogen sulfide (H2S) or ferrous iron (Fe2+) as electron donors instead of water. Because of that, it did not produce molecular oxygen (O2) as a...

evolutionary processes in microbes

How Microbes Gain New Traits

Microbes gain new traits through fast genetic change. Their short generation times help evolution happen quickly. Mutation, horizontal gene transfer, recombination, and genetic drift all contribute to this process. Together, these mechanisms help microbial populations adjust to changing environments. Horizontal gene transfer, or HGT, moves genes between different species. It happens in three main ways: conjugation, transformation, and transduction. Conjugation requires direct cell-to-cell...

evolution of new traits in microbes

Microbial Adaptation in Changing Environments

Microbial adaptation in changing environments can happen very quickly. Microorganisms often evolve fast because they have large population sizes and short generation times. In the lab, these changes can sometimes be measured within days. Natural selection acts on standing genetic variation, which is the genetic diversity already present in a population. When conditions change, helpful traits can be kept and increased because they improve fitness. This lets microbes respond to new pressures...

evolution of microbial genome

Microbial Core and Pan-Genome Changes

Microbial genomes change through gene gain and gene loss. These changes help microbes adapt to new environments and to other organisms they live with. In many species, genome evolution is fast and ongoing. A key idea is the difference between the core genome and the pan-genome. The core genome is the set of genes shared by all sampled strains of a species. These genes support basic cell functions. For example, Salmonella enterica has about 2,800 core genes, although the exact number can change...

microbial phylogeny

Reading Microbial Family Trees

Reading microbial family trees helps scientists study how microorganisms are related. These trees are important in microbial ecology and taxonomy. They use molecular sequences such as DNA, RNA, or proteins to compare bacteria and archaea and trace genetic changes over time. A phylogenetic tree has tips, branches, and nodes. The tips are the species that are sampled or still alive. The branches show evolutionary paths, and branch length reflects the number of genetic changes between nodes.

phylogenetic species concept in microbiology

phylogenetic-species-concept-in-microbiology

How DNA Defines Microbial Species

The phylogenetic species concept helps define microbial species by looking at DNA and evolutionary relatedness. It focuses on shared ancestry and genetic traits that can be diagnosed in different organisms. This approach is especially useful in microbiology, where other species concepts often do not work well. Traditional morphological and biological species concepts rely on body form or reproduction. Those methods can fall short for microbes because many reproduce asexually, show little...

key terms and concepts

Explore how early cells may have formed on Earth, from RNA and hydrothermal vents to LUCA, early metabolism, and the rise of oxygenic photosynthesis.

How Early Cells Got Their Start | 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

Origin of Photosynthesis

Photosynthesis represents a fundamental biological process that transformed Earth's atmosphere and paved the way for complex life. Emerging roughly ...

Soil Microbial Ecology

Soil microbial ecology is defined by highly diverse, spatially structured communities that drive nutrient cycling, organic matter turnover, and overall ...

Acid Mine Drainage

Mining activities that disturb sulfide-rich rocks, particularly those containing pyrite (FeS&#8322;), initiate a cascade of geochemical and ...

Microbial Corrosion

Microbiologically Influenced Corrosion (MIC) is a significant form of material degradation caused by the metabolic activities of microorganisms. This ...

Microbial Bioremediation of Hydrocarbons

Bioremediation is an environmentally sustainable process that employs living organisms&#8212;primarily microorganisms&#8212;to degrade or neutralize ...

analysis-of-earthworm-populations-in-soil

Analysis of Earthworm Populations in Soil

Source: Laboratories of Margaret Workman and Kimberly Frye - Depaul University
Using mustard, Lumbricus terrestris earthworm populations can be sampled ...

What is an Ecosystem?

Overview

An ecosystem is the interaction between all abiotic and biotic factors in an environment and can be classified as terrestrial or aquatic. ...

4. Engage in an evidence-based argument to explain how Earth's systems affect the biosphere and the biosphere affects Earth's systems over various amounts of time. Examples: Use data to make a claim that microbial life increases the formation of soil or that corals create reefs and argue that these processes can alter patterns of erosion and deposition along coastlines. Clarification: This discussion should consider Earth's geological history.

Ecological Disturbance

An ecological disturbance is a temporary disruption in the environment resulting from abiotic, biotic, or anthropogenic factors, causing a pronounced ...

Investigation of Disease Outbreaks

Multistate foodborne outbreaks pose significant public health risks and require meticulous investigation to identify sources and implement control ...

Biodeterioration

Biodeterioration refers to the unwanted alteration of materials caused by microorganisms&#8212;especially fungi&#8212;which damage both organic substrates ...

Igneous Volcanic Rock

Source: Laboratory of Alan Lester - University of Colorado Boulder
Igneous rocks are the products of cooling and crystallization of magma. Volcanic rocks ...

applications-of-gis-disaster-management-and-emergency-response

Applications of GIS: Disaster Management and Emergency Response

Geographic Information System (GIS) technology is essential for risk identification, action prioritization, and resource optimization in critical ...

5. Obtain, evaluate, and communicate information regarding how short-term and long-term natural cyclic fluctuations cause ecosystem change. Examples: Explain how the eruption of volcanoes alters global temperatures or how the El Niño-Southern Oscillation shifts weather patterns. Share information regarding how forest fires can cause deforestation which increases water runoff and soil erosion. Describe how hurricanes destroy dunes and increase coastal flooding.

9-12.EVS.3.5

How Early Cells Got Their Start

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