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Geobiology Course
More than 2 million students worldwide

Geobiology Course

Geobiology sits at the intersection of life, Earth, and deep time — and this course gives you the scientific tools to explore all three. From microbial ecosystems to mass extinctions, you'll learn how life and the planet have shaped each other across billions of years. Whether your focus is palaeontology, planetary science, or environmental research, this course builds the rigorous foundation you need.

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What you'll learn:

This course covers the full scope of geobiology, from biogeochemical cycles and microbial metabolism to biosignature detection and astrobiology. You will learn how to read the rock record for evidence of ancient life, reconstruct palaeoenvironments using geochemical proxies, and analyse major biological transitions including the Great Oxidation Event and mass extinctions. The curriculum also addresses modern geobiological systems, analytical laboratory methods, and quantitative modelling techniques. By the end, you will be equipped to design original geobiological research and communicate findings to both scientific and public audiences.

How you study in practice Geobiology Course

How you practise Geobiology Course

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Course content

8 Chapters • 39 LessonsDuration between 4 and 360 hours (you decide)

Chapter 1See details

Foundations of Geobiology

  • Lesson 1 • Fundamental Biogeochemical Cycles

    Carbon, nitrogen, sulfur, and phosphorus cycles are examined as geobiological drivers. Understanding these cycles is prerequisite for interpreting biosignatures and Earth history.

  • Lesson 2 • Deep Time and Geological Timescales

    Introduces the geological time scale and methods for reading Earth's rock record. Students develop intuition for the vast temporal scales central to geobiology.

  • Lesson 3 • Defining Geobiology as a Discipline

    Geobiology's scope, history, and relationship to adjacent sciences are mapped. This context anchors all later technical content within a unified scientific framework.

  • Lesson 4 • Earth Systems and Life Interactions

    Covers feedbacks between the biosphere, lithosphere, hydrosphere, and atmosphere. Students understand how life both responds to and reshapes Earth's physical systems.

Chapter 2See details

Microbial Life and Earth Processes

  • Lesson 1 • Biomineralisation by Microorganisms

    Covers biologically induced and controlled mineral precipitation by microbes. These processes produce diagnostic textures preserved in the rock record.

  • Lesson 2 • Microbial Diversity and Metabolism

    Surveys the metabolic strategies microbes use to harvest energy from inorganic and organic substrates. This diversity underpins microbial roles in geochemical cycling.

  • Lesson 3 • Microbial Weathering of Minerals

    Microbial dissolution and transformation of silicate and sulfide minerals are examined. Students link microbial activity to soil formation and elemental release.

  • Lesson 4 • Microbial Mats and Biofilms

    Structured microbial communities are analysed as geochemically active units. Their spatial organisation creates steep chemical gradients that drive mineral transformations.

  • Lesson 5 • Subsurface Microbial Ecosystems

    Deep subsurface environments host chemolithotrophic communities independent of sunlight. These systems reveal the limits of life and inform models of early Earth and other planets.

Chapter 3See details

Origin and Early Evolution of Life

  • Lesson 1 • Earliest Evidence of Life on Earth

    The oldest putative biosignatures from Archaean rocks are critically evaluated. Students apply biosignature criteria from Chapter 3 to assess claims of early life.

  • Lesson 2 • Origin of Eukaryotes and Endosymbiosis

    Endosymbiotic theory and the geobiological context of eukaryote emergence are examined. Students link cellular complexity to environmental and ecological transitions.

  • Lesson 3 • Great Oxidation Event and Its Consequences

    The rise of atmospheric oxygen around 2.4 billion years ago transformed Earth's surface chemistry. Students analyse causes, timing, and biological and geological consequences.

  • Lesson 4 • Evolution of Photosynthesis

    The development of anoxygenic and oxygenic photosynthesis is traced through the rock record. Students connect photosynthetic evolution to planetary-scale geochemical change.

  • Lesson 5 • Prebiotic Chemistry and Abiogenesis

    Chemical pathways leading to organic molecules and proto-cellular structures are examined. Students assess how early Earth environments may have facilitated life's origin.

Chapter 4See details

Biosignatures and the Fossil Record

  • Lesson 1 • Molecular Fossils and Biomarkers

    Lipid biomarkers preserved in sedimentary rocks record the presence of specific biological groups. Students learn extraction, analysis, and interpretation of these molecular archives.

  • Lesson 2 • Types of Biosignatures

    Morphological, chemical, and isotopic biosignatures are classified and compared. Recognising each type is essential for interpreting ancient life in the rock record.

  • Lesson 3 • Microfossils and Their Interpretation

    Techniques for identifying and authenticating microfossils in cherts and carbonates are covered. Students apply criteria to distinguish genuine microfossils from pseudofossils.

  • Lesson 4 • Stable Isotope Geobiology

    Carbon, sulfur, and nitrogen isotope systems are applied to reconstruct biological activity. Isotopic fractionation patterns serve as quantitative biosignatures in ancient rocks.

  • Lesson 5 • Stromatolites as Biological Archives

    Stromatolite morphology, formation mechanisms, and geological distribution are analysed. Students use stromatolites as proxies for ancient microbial ecosystems and environmental conditions.

Chapter 5See details

Geochemical Proxies and Palaeoenvironments

  • Lesson 1 • Ocean Chemistry Through Time

    Redox state, salinity, and trace metal concentrations of ancient oceans are reconstructed. These records reveal how ocean chemistry co-evolved with life and atmosphere.

  • Lesson 2 • Integrating Proxies into Palaeoenvironmental Models

    Multiple proxy datasets are combined to construct coherent palaeoenvironmental reconstructions. Students practise synthesising conflicting proxy signals into robust interpretations.

  • Lesson 3 • Atmospheric Proxies and Palaeoatmosphere

    Methods for reconstructing ancient atmospheric oxygen and carbon dioxide levels are covered. Students connect atmospheric reconstructions to biological and climatic events.

  • Lesson 4 • Principles of Proxy Reconstruction

    The logic of using chemical and physical signals in rocks as environmental proxies is established. Students learn to assess proxy fidelity, diagenetic alteration, and uncertainty.

  • Lesson 5 • Sedimentary Facies and Depositional Environments

    Sedimentary rock types and facies associations are linked to specific depositional settings. Students use facies analysis to place biological events in their environmental context.

Chapter 6See details

Major Biological Transitions and Mass Extinctions

  • Lesson 1 • Patterns and Causes of Mass Extinctions

    The five major mass extinctions are analysed for their geobiological signatures and causes. Students identify common environmental stressors and biological vulnerabilities.

  • Lesson 2 • Recovery and Radiation After Extinction

    Post-extinction recovery dynamics and evolutionary radiations are examined across multiple events. Students analyse how survivors reshape ecosystems and drive new geobiological cycles.

  • Lesson 3 • Cambrian Explosion and Animal Origins

    The rapid diversification of animal body plans in the Cambrian is examined through fossil and geochemical evidence. Students evaluate environmental triggers and ecological drivers.

  • Lesson 4 • Neoproterozoic Snowball Earth Events

    Global glaciation events and their biological consequences are analysed using sedimentary and isotopic evidence. Students connect extreme climate perturbations to evolutionary transitions.

  • Lesson 5 • End-Permian Extinction: A Case Study

    The largest mass extinction is dissected using geochemical, palaeontological, and sedimentological data. Students apply multi-proxy analysis to reconstruct the extinction mechanism.

Chapter 7See details

Modern Geobiological Systems and Environments

  • Lesson 1 • Soil Geobiology and Critical Zone Science

    The critical zone from bedrock to canopy is analysed as an integrated geobiological system. Students examine how organisms drive weathering, nutrient cycling, and soil development.

  • Lesson 2 • Wetlands, Peatlands, and Carbon Storage

    Organic carbon accumulation in wetland and peatland systems is examined as a geobiological process. Students link microbial decomposition rates to long-term carbon burial.

  • Lesson 3 • Hydrothermal Vent Ecosystems

    Chemosynthetic communities at mid-ocean ridges are examined as models of early Earth ecosystems. Students analyse energy flow, mineral precipitation, and community structure.

  • Lesson 4 • Carbonate Systems and Reef Geobiology

    Biological carbonate production in reefs and shallow marine settings is analysed. Students connect organism-scale calcification to basin-scale carbonate accumulation.

  • Lesson 5 • Extreme Environments as Geobiological Analogues

    Hypersaline lakes, acid mine drainage, and polar environments are studied as analogues for ancient and extraterrestrial settings. Students evaluate habitability limits and biosignature preservation.

Chapter 8See details

Astrobiology and the Search for Life

  • Lesson 1 • Ocean Worlds and Icy Moon Habitability

    Subsurface oceans on Europa, Enceladus, and similar bodies are evaluated as potential habitats. Students connect deep-sea geobiology to extraterrestrial ocean environments.

  • Lesson 2 • Mars as a Geobiological Target

    Mars's geological and geochemical history is evaluated for past and present habitability. Students apply geobiological proxy methods to interpret Mars mission data.

  • Lesson 3 • Habitability: Concepts and Requirements

    The physical and chemical requirements for life as we know it are defined and evaluated. Students apply habitability criteria to assess environments on Earth and other worlds.

  • Lesson 4 • Panspermia and Life's Cosmic Context

    Hypotheses for interplanetary transfer of life are evaluated against geobiological and physical evidence. Students place Earth's biosphere within a broader cosmic perspective.

  • Lesson 5 • Biosignature Detection in Planetary Science

    Remote and in-situ biosignature detection methods are evaluated for planetary missions. Students design detection frameworks using geobiological principles established throughout the course.

Certification

Your valid completion certificate

This course is for you:

  • Geology student: wants to understand how life has driven Earth's chemical evolution.

  • Astrobiology enthusiast: seeks rigorous grounding before pursuing planetary habitability research.

  • Environmental scientist: needs deeper knowledge of microbial roles in geochemical systems.

  • Palaeontology researcher: aims to interpret fossil evidence within broader Earth system contexts.

  • Biology graduate student: ready to connect evolutionary history to large-scale geological processes.

  • Science educator: building expertise to teach Earth history with biological and chemical depth.

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