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Boundless Biology: 46.3: Biogeochemical Cycles

Boundless Biology
46.3: Biogeochemical Cycles
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table of contents
  1. 1: The Study of Life
    1. 1.1: The Science of Biology
      1. 1.1.0: Introduction to the Study of Biology
      2. 1.1.1: Scientific Reasoning
      3. 1.1.2: The Scientific Method
      4. 1.1.3: Basic and Applied Science
      5. 1.1.4: Publishing Scientific Work
      6. 1.1.5: Branches and Subdisciplines of Biology
    2. 1.2: Themes and Concepts of Biology
      1. 1.2.0: Properties of Life
      2. 1.2.1: Levels of Organization of Living Things
      3. 1.2.2: The Diversity of Life
  2. 2: The Chemical Foundation of Life
    1. 2.1: Atoms, Isotopes, Ions, and Molecules
      1. 2.1.0: Overview of Atomic Structure
      2. 2.1.1: Atomic Number and Mass Number
      3. 2.1.2: Isotopes
      4. 2.1.3: The Periodic Table
      5. 2.1.4: Electron Shells and the Bohr Model
      6. 2.1.5: Electron Orbitals
      7. 2.1.6: Chemical Reactions and Molecules
      8. 2.1.7: Ions and Ionic Bonds
      9. 2.1.8: Covalent Bonds and Other Bonds and Interactions
      10. 2.1.9: Hydrogen Bonding and Van der Waals Forces
    2. 2.2: Water
      1. 2.2.0: Water’s Polarity
      2. 2.2.1: Water’s States: Gas, Liquid, and Solid
      3. 2.2.2: Water’s High Heat Capacity
      4. 2.2.3: Water’s Heat of Vaporization
      5. 2.2.4: Water’s Solvent Properties
      6. 2.2.5: Water’s Cohesive and Adhesive Properties
      7. 2.2.6: pH, Buffers, Acids, and Bases
    3. 2.3: Carbon
      1. 2.3.0: The Chemical Basis for Life
      2. 2.3.1: Hydrocarbons
      3. 2.3.2: Organic Isomers
      4. 2.3.3: Organic Enantiomers
      5. 2.3.4: Organic Molecules and Functional Groups
  3. 3: Biological Macromolecules
    1. 3.1: Synthesis of Biological Macromolecules
      1. 3.1.0: Types of Biological Macromolecules
      2. 3.1.1: Dehydration Synthesis
      3. 3.1.2: Hydrolysis
    2. 3.2: Carbohydrates
      1. 3.2.0: Carbohydrate Molecules
      2. 3.2.1: Importance of Carbohydrates
    3. 3.3: Lipids
      1. 3.3.0: Lipid Molecules
      2. 3.3.1: Waxes
      3. 3.3.2: Phospholipids
      4. 3.3.3: Steroids
    4. 3.4: Proteins
      1. 3.4.0: Types and Functions of Proteins
      2. 3.4.1: Amino Acids
      3. 3.4.2: Protein Structure
      4. 3.4.3: Denaturation and Protein Folding
    5. 3.5: Nucleic Acids
      1. 3.5.0: DNA and RNA
      2. 3.5.1: The DNA Double Helix
      3. 3.5.2: DNA Packaging
      4. 3.5.3: Types of RNA
  4. 4: Cell Structure
    1. 4.1: Studying Cells
      1. 4.1.0: Cells as the Basic Unit of Life
      2. 4.1.1: Microscopy
      3. 4.1.2: Cell Theory
      4. 4.1.3: Cell Size
    2. 4.2: Prokaryotic Cells
      1. 4.2.0: Characteristics of Prokaryotic Cells
    3. 4.3: Eukaryotic Cells
      1. 4.3.0: Characteristics of Eukaryotic Cells
      2. 4.3.1: The Plasma Membrane and the Cytoplasm
      3. 4.3.2: The Nucleus and Ribosomes
      4. 4.3.3: Mitochondria
      5. 4.3.4: Comparing Plant and Animal Cells
    4. 4.4: The Endomembrane System and Proteins
      1. 4.4.0: Vesicles and Vacuoles
      2. 4.4.1: The Endoplasmic Reticulum
      3. 4.4.2: The Golgi Apparatus
      4. 4.4.3: Lysosomes
      5. 4.4.4: Peroxisomes
    5. 4.5: The Cytoskeleton
      1. 4.5.0: Microfilaments
      2. 4.5.1: Intermediate Filaments and Microtubules
    6. 4.6: Connections between Cells and Cellular Activities
      1. 4.6.0: Extracellular Matrix of Animal Cells
      2. 4.6.1: Intercellular Junctions
  5. 5: Structure and Function of Plasma Membranes
    1. 5.1: Components and Structure
      1. 5.1.0: Components of Plasma Membranes
      2. 5.1.1: Fluid Mosaic Model
      3. 5.1.2: Membrane Fluidity
    2. 5.2: Passive Transport
      1. 5.2.0: The Role of Passive Transport
      2. 5.2.1: Selective Permeability
      3. 5.2.2: Diffusion
      4. 5.2.3: Facilitated transport
      5. 5.2.4: Osmosis
      6. 5.2.5: Tonicity
      7. 5.2.6: Osmoregulation
    3. 5.3: Active Transport
      1. 5.3.0: Electrochemical Gradient
      2. 5.3.1: Primary Active Transport
      3. 5.3.2: Secondary Active Transport
    4. 5.4: Bulk Transport
      1. 5.4.0: Endocytosis
      2. 5.4.1: Exocytosis
  6. 6: Metabolism
    1. 6.1: Energy and Metabolism
      1. 6.1.0: The Role of Energy and Metabolism
      2. 6.1.1: Types of Energy
      3. 6.1.2: Metabolic Pathways
      4. 6.1.3: Metabolism of Carbohydrates
    2. 6.2: Potential, Kinetic, Free, and Activation Energy
      1. 6.2.0: Free Energy
      2. 6.2.1: The First Law of Thermodynamics
      3. 6.2.2: The Second Law of Thermodynamics
      4. 6.2.3: Activation Energy
    3. 6.3: ATP: Adenosine Triphosphate
      1. 6.3.0: ATP: Adenosine Triphosphate
    4. 6.4: Enzymes
      1. 6.4.0: Enzyme Active Site and Substrate Specificity
      2. 6.4.1: Control of Metabolism Through Enzyme Regulation
  7. 7: Cellular Respiration
    1. 7.1: Energy in Living Systems
      1. 7.1.0: Transforming Chemical Energy
      2. 7.1.1: Electrons and Energy
      3. 7.1.2: ATP in Metabolism
    2. 7.2: Glycolysis
      1. 7.2.0: Importance of Glycolysis
      2. 7.2.1: The Energy-Requiring Steps of Glycolysis
      3. 7.2.2: The Energy-Releasing Steps of Glycolysis
      4. 7.2.3: Outcomes of Glycolysis
    3. 7.3: Oxidation of Pyruvate and the Citric Acid Cycle
      1. 7.3.0: Breakdown of Pyruvate
      2. 7.3.1: Acetyl CoA to CO2
      3. 7.3.2: Citric Acid Cycle
    4. 7.4: Oxidative Phosphorylation
      1. 7.4.0: Electron Transport Chain
      2. 7.4.1: Chemiosmosis and Oxidative Phosphorylation
      3. 7.4.2: ATP Yield
    5. 7.5: Metabolism without Oxygen
      1. 7.5.0: Anaerobic Cellular Respiration
    6. 7.6: Connections of Carbohydrate, Protein, and Lipid Metabolic Pathways
      1. 7.6.0: Connecting Other Sugars to Glucose Metabolism
      2. 7.6.1: Connecting Proteins to Glucose Metabolism
      3. 7.6.2: Connecting Lipids to Glucose Metabolism
    7. 7.7: Regulation of Cellular Respiration
      1. 7.7.0: Regulatory Mechanisms for Cellular Respiration
      2. 7.7.1: Control of Catabolic Pathways
  8. 8: Photosynthesis
    1. 8.1: Overview of Photosynthesis
      1. 8.1.0: The Purpose and Process of Photosynthesis
      2. 8.1.1: Main Structures and Summary of Photosynthesis
      3. 8.1.2: The Two Parts of Photosynthesis
    2. 8.2: The Light-Dependent Reactions of Photosynthesis
      1. 8.2.0: Introduction to Light Energy
      2. 8.2.1: Absorption of Light
      3. 8.2.2: Processes of the Light-Dependent Reactions
    3. 8.3: The Light-Independent Reactions of Photosynthesis
      1. 8.3.0: CAM and C4 Photosynthesis
      2. 8.3.1: The Calvin Cycle
      3. 8.3.2: The Carbon Cycle
  9. 9: Cell Communication
    1. 9.1: Signaling Molecules and Cellular Receptors
      1. 9.1.0: Signaling Molecules and Cellular Receptors
      2. 9.1.1: Forms of Signaling
      3. 9.1.2: Types of Receptors
      4. 9.1.3: Signaling Molecules
    2. 9.2: Propagation of the Cellular Signal
      1. 9.2.0: Binding Initiates a Signaling Pathway
      2. 9.2.1: Methods of Intracellular Signaling
    3. 9.3: Response to the Cellular Signal
      1. 9.3.0: Termination of the Signal Cascade
      2. 9.3.1: Cell Signaling and Gene Expression
      3. 9.3.2: Cell Signaling and Cellular Metabolism
      4. 9.3.3: Cell Signaling and Cell Growth
      5. 9.3.4: Cell Signaling and Cell Death
    4. 9.4: Signaling in Single-Celled Organisms
      1. 9.4.0: Signaling in Yeast
      2. 9.4.1: Signaling in Bacteria
  10. 10: Cell Reproduction
    1. 10.1: Cell Division
      1. 10.1.0: The Role of the Cell Cycle
      2. 10.1.1: Genomic DNA and Chromosomes
      3. 10.1.2: Eukaryotic Chromosomal Structure and Compaction
    2. 10.2: The Cell Cycle
      1. 10.2.0: Interphase
      2. 10.2.1: The Mitotic Phase and the G0 Phase
    3. 10.3: Control of the Cell Cycle
      1. 10.3.0: Regulation of the Cell Cycle by External Events
      2. 10.3.1: Regulation of the Cell Cycle at Internal Checkpoints
      3. 10.3.2: Regulator Molecules of the Cell Cycle
    4. 10.4: Cancer and the Cell Cycle
      1. 10.4.0: Proto-oncogenes
      2. 10.4.1: Tumor Suppressor Genes
    5. 10.5: Prokaryotic Cell Division
      1. 10.5.0: Binary Fission
  11. 11: Meiosis and Sexual Reproduction
    1. 11.1: The Process of Meiosis
      1. 11.1.0: Introduction to Meiosis
      2. 11.1.1: Meiosis I
      3. 11.1.2: Meiosis II
      4. 11.1.3: Comparing Meiosis and Mitosis
    2. 11.2: Sexual Reproduction
      1. 11.2.0: Advantages and Disadvantages of Sexual Reproduction
      2. 11.2.1: Life Cycles of Sexually Reproducing Organisms
  12. 12: Mendel's Experiments and Heredity
    1. 12.1: Mendel’s Experiments and the Laws of Probability
      1. 12.1.0: Introduction to Mendelian Inheritance
      2. 12.1.1: Mendel’s Model System
      3. 12.1.2: Mendelian Crosses
      4. 12.1.3: Garden Pea Characteristics Revealed the Basics of Heredity
      5. 12.1.4: Rules of Probability for Mendelian Inheritance
    2. 12.2: Patterns of Inheritance
      1. 12.2.0: Genes as the Unit of Heredity
      2. 12.2.1: Phenotypes and Genotypes
      3. 12.2.2: The Punnett Square Approach for a Monohybrid Cross
      4. 12.2.3: Alternatives to Dominance and Recessiveness
      5. 12.2.4: Sex-Linked Traits
      6. 12.2.5: Lethal Inheritance Patterns
    3. 12.3: Laws of Inheritance
      1. 12.3.0: Mendel's Laws of Heredity
      2. 12.3.1: Mendel's Law of Dominance
      3. 12.3.2: Mendel's Law of Segregation
      4. 12.3.3: Mendel's Law of Independent Assortment
      5. 12.3.4: Genetic Linkage and Violation of the Law of Independent Assortment
      6. 12.3.5: Epistasis
  13. 13: Modern Understandings of Inheritance
    1. 13.1: Chromosomal Theory and Genetic Linkage
      1. 13.1.0: Chromosomal Theory of Inheritance
      2. 13.1.1: Genetic Linkage and Distances
      3. 13.1.2: Identification of Chromosomes and Karyotypes
    2. 13.2: Chromosomal Basis of Inherited Disorders
      1. 13.2.0: Disorders in Chromosome Number
      2. 13.2.1: Chromosomal Structural Rearrangements
      3. 13.2.2: X-Inactivation
  14. 14: DNA Structure and Function
    1. 14.1: Historical Basis of Modern Understanding
      1. 14.1.0: Discovery of DNA
      2. 14.1.1: Modern Applications of DNA
    2. 14.2: DNA Structure and Sequencing
      1. 14.2.0: The Structure and Sequence of DNA
      2. 14.2.1: DNA Sequencing Techniques
    3. 14.3: DNA Replication
      1. 14.3.0: Basics of DNA Replication
      2. 14.3.1: DNA Replication in Prokaryotes
      3. 14.3.2: DNA Replication in Eukaryotes
      4. 14.3.3: Telomere Replication
    4. 14.4: DNA Repair
      1. 14.4.0: DNA Repair
  15. 15: Genes and Proteins
    1. 15.1: The Genetic Code
      1. 15.1.0: The Relationship Between Genes and Proteins
      2. 15.1.1: The Central Dogma: DNA Encodes RNA and RNA Encodes Protein
    2. 15.2: Prokaryotic Transcription
      1. 15.2.0: Transcription in Prokaryotes
      2. 15.2.1: Initiation of Transcription in Prokaryotes
      3. 15.2.2: Elongation and Termination in Prokaryotes
    3. 15.3: Eukaryotic Transcription
      1. 15.3.0: Initiation of Transcription in Eukaryotes
      2. 15.3.1: Elongation and Termination in Eukaryotes
    4. 15.4: RNA Processing in Eukaryotes
      1. 15.4.0: mRNA Processing
      2. 15.4.1: Processing of tRNAs and rRNAs
    5. 15.5: Ribosomes and Protein Synthesis
      1. 15.5.0: The Protein Synthesis Machinery
      2. 15.5.1: The Mechanism of Protein Synthesis
      3. 15.5.2: Protein Folding, Modification, and Targeting
  16. 16: Gene Expression
    1. 16.1: Regulation of Gene Expression
      1. 16.1.0: The Process and Purpose of Gene Expression Regulation
      2. 16.1.1: Prokaryotic versus Eukaryotic Gene Expression
    2. 16.2: Prokaryotic Gene Regulation
      1. 16.2.0: The trp Operon: A Repressor Operon
      2. 16.2.1: Catabolite Activator Protein (CAP): An Activator Regulator
      3. 16.2.2: The lac Operon: An Inducer Operon
    3. 16.3: Eukaryotic Gene Regulation
      1. 16.3.0: The Promoter and the Transcription Machinery
      2. 16.3.1: Transcriptional Enhancers and Repressors
      3. 16.3.2: Epigenetic Control: Regulating Access to Genes within the Chromosome
      4. 16.3.3: RNA Splicing
      5. 16.3.4: The Initiation Complex and Translation Rate
      6. 16.3.5: Regulating Protein Activity and Longevity
    4. 16.4: Regulating Gene Expression in Cell Development
      1. 16.4.0: Gene Expression in Stem Cells
      2. 16.4.1: Cellular Differentiation
      3. 16.4.2: Mechanics of Cellular Differentation
      4. 16.4.3: Establishing Body Axes during Development
      5. 16.4.4: Gene Expression for Spatial Positioning
      6. 16.4.5: Cell Migration in Multicellular Organisms
      7. 16.4.6: Programmed Cell Death
    5. 16.5: Cancer and Gene Regulation
      1. 16.5.0: Altered Gene Expression in Cancer
      2. 16.5.1: Epigenetic Alterations in Cancer
      3. 16.5.2: Cancer and Transcriptional Control
      4. 16.5.3: Cancer and Post-Transcriptional Control
      5. 16.5.4: Cancer and Translational Control
  17. 17: Biotechnology and Genomics
    1. 17.1: Biotechnology
      1. 17.1.0: Biotechnology
      2. 17.1.1: Basic Techniques to Manipulate Genetic Material (DNA and RNA)
      3. 17.1.2: Molecular and Cellular Cloning
      4. 17.1.3: Reproductive Cloning
      5. 17.1.4: Genetic Engineering
      6. 17.1.5: Genetically Modified Organisms (GMOs)
      7. 17.1.6: Biotechnology in Medicine
      8. 17.1.7: Production of Vaccines, Antibiotics, and Hormones
    2. 17.2: Mapping Genomes
      1. 17.2.0: Genetic Maps
      2. 17.2.1: Physical Maps and Integration with Genetic Maps
    3. 17.3: Whole-Genome Sequencing
      1. 17.3.0: Strategies Used in Sequencing Projects
      2. 17.3.1: Use of Whole-Genome Sequences of Model Organisms
      3. 17.3.2: Uses of Genome Sequences
    4. 17.4: Applying Genomics
      1. 17.4.0: Predicting Disease Risk at the Individual Level
      2. 17.4.1: Pharmacogenomics, Toxicogenomics, and Metagenomics
      3. 17.4.2: Genomics and Biofuels
    5. 17.5: Genomics and Proteomics
      1. 17.5.0: Genomics and Proteomics
      2. 17.5.1: Basic Techniques in Protein Analysis
      3. 17.5.2: Cancer Proteomics
  18. 18: Evolution and the Origin of Species
    1. 18.1: Understanding Evolution
      1. 18.1.0: What is Evolution?
      2. 18.1.1: Charles Darwin and Natural Selection
      3. 18.1.2: The Galapagos Finches and Natural Selection
      4. 18.1.3: Processes and Patterns of Evolution
      5. 18.1.4: Evidence of Evolution
      6. 18.1.5: Misconceptions of Evolution
    2. 18.2: Formation of New Species
      1. 18.2.0: The Biological Species Concept
      2. 18.2.1: Reproductive Isolation
      3. 18.2.2: Speciation
      4. 18.2.3: Allopatric Speciation
      5. 18.2.4: Sympatric Speciation
    3. 18.3: Hybrid Zones and Rates of Speciation
      1. 18.3.0: Hybrid Zones
      2. 18.3.1: Varying Rates of Speciation
    4. 18.4: Evolution of Genomes
      1. 18.4.0: Genomic Similiarities between Distant Species
      2. 18.4.1: Genome Evolution
      3. 18.4.2: Whole-Genome Duplication
      4. 18.4.3: Gene Duplications and Divergence
      5. 18.4.4: Noncoding DNA
      6. 18.4.5: Variations in Size and Number of Genes
    5. 18.5: Evidence of Evolution
      1. 18.5.0: The Fossil Record as Evidence for Evolution
      2. 18.5.1: Fossil Formation
      3. 18.5.2: Gaps in the Fossil Record
      4. 18.5.3: Carbon Dating and Estimating Fossil Age
      5. 18.5.4: The Fossil Record and the Evolution of the Modern Horse
      6. 18.5.5: Homologous Structures
      7. 18.5.6: Convergent Evolution
      8. 18.5.7: Vestigial Structures
      9. 18.5.8: Biogeography and the Distribution of Species
  19. 19: The Evolution of Populations
    1. 19.1: Population Evolution
      1. 19.1.0: Defining Population Evolution
      2. 19.1.1: Population Genetics
      3. 19.1.2: Hardy-Weinberg Principle of Equilibrium
    2. 19.2: Population Genetics
      1. 19.2.0: Genetic Variation
      2. 19.2.1: Genetic Drift
      3. 19.2.2: Gene Flow and Mutation
      4. 19.2.3: Nonrandom Mating and Environmental Variance
    3. 19.3: Adaptive Evolution
      1. 19.3.0: Natural Selection and Adaptive Evolution
      2. 19.3.1: Stabilizing, Directional, and Diversifying Selection
      3. 19.3.2: Frequency-Dependent Selection
      4. 19.3.3: Sexual Selection
      5. 19.3.4: No Perfect Organism
  20. 20: Phylogenies and the History of Life
    1. 20.1: Organizing Life on Earth
      1. 20.1.0: Phylogenetic Trees
      2. 20.1.1: Limitations of Phylogenetic Trees
      3. 20.1.2: The Levels of Classification
    2. 20.2: Determining Evolutionary Relationships
      1. 20.2.0: Distinguishing between Similar Traits
      2. 20.2.1: Building Phylogenetic Trees
    3. 20.3: Perspectives on the Phylogenetic Tree
      1. 20.3.0: Limitations to the Classic Model of Phylogenetic Trees
      2. 20.3.1: Horizontal Gene Transfer
      3. 20.3.2: Endosymbiotic Theory and the Evolution of Eukaryotes
      4. 20.3.3: Web, Network, and Ring of Life Models
  21. 21: Viruses
    1. 21.1: Viral Evolution, Morphology, and Classification
      1. 21.1.0: Discovery and Detection of Viruses
      2. 21.1.1: Evolution of Viruses
      3. 21.1.2: Viral Morphology
      4. 21.1.3: Virus Classification
    2. 21.2: Virus Infections and Hosts
      1. 21.2.0: Steps of Virus Infections
      2. 21.2.1: The Lytic and Lysogenic Cycles of Bacteriophages
      3. 21.2.2: Animal Viruses
      4. 21.2.3: Plant Viruses
    3. 21.3: Prevention and Treatment of Viral Infections
      1. 21.3.0: Vaccines and Immunity
      2. 21.3.1: Vaccines and Anti-Viral Drugs for Treatment
    4. 21.4: Prions and Viroids
      1. 21.4.0: Prions and Viroids
  22. 22: Prokaryotes: Bacteria and Archaea
    1. 22.1: Prokaryotic Diversity
      1. 22.1.0: Classification of Prokaryotes
      2. 22.1.1: The Origins of Archaea and Bacteria
      3. 22.1.2: Extremophiles and Biofilms
    2. 22.2: Structure of Prokaryotes
      1. 22.2.0: Basic Structures of Prokaryotic Cells
      2. 22.2.1: Prokaryotic Reproduction
    3. 22.3: Prokaryotic Metabolism
      1. 22.3.0: Energy and Nutrient Requirements for Prokaryotes
      2. 22.3.1: The Role of Prokaryotes in Ecosystems
    4. 22.4: Bacterial Diseases in Humans
      1. 22.4.0: History of Bacterial Diseases
      2. 22.4.1: Biofilms and Disease
      3. 22.4.2: Antibiotics: Are We Facing a Crisis?
      4. 22.4.3: Bacterial Foodborne Diseases
    5. 22.5: Beneficial Prokaryotes
      1. 22.5.0: Symbiosis between Bacteria and Eukaryotes
      2. 22.5.1: Early Biotechnology: Cheese, Bread, Wine, Beer, and Yogurt
      3. 22.5.2: Prokaryotes and Environmental Bioremediation
  23. 23: Protists
    1. 23.1: Eukaryotic Origins
      1. 23.1.0: Early Eukaryotes
      2. 23.1.1: Characteristics of Eukaryotic DNA
      3. 23.1.2: Endosymbiosis and the Evolution of Eukaryotes
      4. 23.1.3: The Evolution of Mitochondria
      5. 23.1.4: The Evolution of Plastids
    2. 23.2: Characteristics of Protists
      1. 23.2.0: Cell Structure, Metabolism, and Motility
      2. 23.2.1: Protist Life Cycles and Habitats
    3. 23.3: Groups of Protists
      1. 23.3.0: Excavata
      2. 23.3.1: Chromalveolata: Alveolates
      3. 23.3.2: Chromalveolata: Stramenopiles
      4. 23.3.3: Rhizaria
      5. 23.3.4: Archaeplastida
      6. 23.3.5: Amoebozoa and Opisthokonta
    4. 23.4: Ecology of Protists
      1. 23.4.0: Protists as Primary Producers, Food Sources, and Symbionts
      2. 23.4.1: Protists as Human Pathogens
      3. 23.4.2: Protists as Plant Pathogens
  24. 24: Fungi
    1. 24.1: Characteristics of Fungi
      1. 24.1.0: Characteristics of Fungi
      2. 24.1.1: Fungi Cell Structure and Function
      3. 24.1.2: Fungi Reproduction
    2. 24.2: Ecology of Fungi
      1. 24.2.0: Fungi Habitat, Decomposition, and Recycling
      2. 24.2.1: Mutualistic Relationships with Fungi and Fungivores
    3. 24.3: Classifications of Fungi
      1. 24.3.0: Chytridiomycota: The Chytrids
      2. 24.3.1: Zygomycota: The Conjugated Fungi
      3. 24.3.2: Ascomycota: The Sac Fungi
      4. 24.3.3: Basidiomycota: The Club Fungi
      5. 24.3.4: Deuteromycota: The Imperfect Fungi
      6. 24.3.5: Glomeromycota
    4. 24.4: Fungal Parasites and Pathogens
      1. 24.4.0: Fungi as Plant, Animal, and Human Pathogens
    5. 24.5: Importance of Fungi in Human Life
      1. 24.5.0: Importance of Fungi in Human Life
  25. 25: Seedless Plants
    1. 25.1: Early Plant Life
      1. 25.1.0: Early Plant Life
      2. 25.1.1: Evolution of Land Plants
      3. 25.1.2: Plant Adaptations to Life on Land
      4. 25.1.3: Sporophytes and Gametophytes in Seedless Plants
      5. 25.1.4: Structural Adaptations for Land in Seedless Plants
      6. 25.1.5: The Major Divisions of Land Plants
    2. 25.2: Green Algae: Precursors of Land Plants
      1. 25.2.0: Streptophytes and Reproduction of Green Algae
      2. 25.2.1: Charales
    3. 25.3: Bryophytes
      1. 25.3.0: Bryophytes
      2. 25.3.1: Liverworts and Hornworts
      3. 25.3.2: Mosses
    4. 25.4: Seedless Vascular Plants
      1. 25.4.0: Seedless Vascular Plants
      2. 25.4.1: Vascular Tissue: Xylem and Phloem
      3. 25.4.2: The Evolution of Roots in Seedless Plants
      4. 25.4.3: Ferns and Other Seedless Vascular Plants
      5. 25.4.4: The Importance of Seedless Vascular Plants
  26. 26: Seed Plants
    1. 26.1: Evolution of Seed Plants
      1. 26.1.0: The Evolution of Seed Plants and Adaptations for Land
      2. 26.1.1: Evolution of Gymnosperms
      3. 26.1.2: Evolution of Angiosperms
    2. 26.2: Gymnosperms
      1. 26.2.0: Characteristics of Gymnosperms
      2. 26.2.1: Life Cycle of a Conifer
      3. 26.2.2: Diversity of Gymnosperms
    3. 26.3: Angiosperms
      1. 26.3.0: Angiosperm Flowers
      2. 26.3.1: Angsiosperm Fruit
      3. 26.3.2: The Life Cycle of an Angiosperm
      4. 26.3.3: Diversity of Angiosperms
    4. 26.4: The Role of Seed Plants
      1. 26.4.0: Herbivory and Pollination
      2. 26.4.1: The Importance of Seed Plants in Human Life
      3. 26.4.2: Biodiversity of Plants
  27. 27: Introduction to Animal Diversity
    1. 27.1: Features of the Animal Kingdom
      1. 27.1.0: Characteristics of the Animal Kingdom
      2. 27.1.1: Complex Tissue Structure
      3. 27.1.2: Animal Reproduction and Development
    2. 27.2: Features Used to Classify Animals
      1. 27.2.0: Animal Characterization Based on Body Symmetry
      2. 27.2.1: Animal Characterization Based on Features of Embryological Development
    3. 27.3: Animal Phylogeny
      1. 27.3.0: Constructing an Animal Phylogenetic Tree
      2. 27.3.1: Molecular Analyses and Modern Phylogenetic Trees
    4. 27.4: The Evolutionary History of the Animal Kingdom
      1. 27.4.0: Pre-Cambrian Animal Life
      2. 27.4.1: The Cambrian Explosion of Animal Life
      3. 27.4.2: Post-Cambrian Evolution and Mass Extinctions
  28. 28: Invertebrates
    1. 28.1: Phylum Porifera
      1. 28.1.0: Phylum Porifera
      2. 28.1.1: Morphology of Sponges
      3. 28.1.2: Physiological Processes in Sponges
    2. 28.2: Phylum Cnidaria
      1. 28.2.0: Phylum Cnidaria
      2. 28.2.1: Class Anthozoa
      3. 28.2.2: Class Scyphozoa
      4. 28.2.3: Class Cubozoa and Class Hydrozoa
    3. 28.3: Superphylum Lophotrochozoa
      1. 28.3.0: Superphylum Lophotrochozoa
      2. 28.3.1: Phylum Platyhelminthes
      3. 28.3.2: Phylum Rotifera
      4. 28.3.3: Phylum Nemertea
      5. 28.3.4: Phylum Mollusca
      6. 28.3.5: Classification of Phylum Mollusca
      7. 28.3.6: Phylum Annelida
    4. 28.4: Superphylum Ecdysozoa
      1. 28.4.0: Superphylum Ecdysozoa
      2. 28.4.1: Phylum Nematoda
      3. 28.4.2: Phylum Arthropoda
      4. 28.4.3: Subphyla of Arthropoda
    5. 28.5: Superphylum Deuterostomia
      1. 28.5.0: Phylum Echinodermata
      2. 28.5.1: Classes of Echinoderms
      3. 28.5.2: Phylum Chordata
  29. 29: Vertebrates
    1. 29.1: Chordates
      1. 29.1.0: Characteristics of Chordata
      2. 29.1.1: Chordates and the Evolution of Vertebrates
      3. 29.1.2: The Evolution of Craniata and Vertebrata
      4. 29.1.3: Characteristics of Vertebrates
    2. 29.2: Fishes
      1. 29.2.0: Agnathans: Jawless Fishes
      2. 29.2.1: Gnathostomes: Jawed Fishes
    3. 29.3: Amphibians
      1. 29.3.0: Characteristics and Evolution of Amphibians
      2. 29.3.1: Modern Amphibians
    4. 29.4: Reptiles
      1. 29.4.0: Characteristics of Amniotes
      2. 29.4.1: Evolution of Amniotes
      3. 29.4.2: Characteristics of Reptiles
      4. 29.4.3: Evolution of Reptiles
      5. 29.4.4: Modern Reptiles
    5. 29.5: Birds
      1. 29.5.0: Characteristics of Birds
      2. 29.5.1: Evolution of Birds
    6. 29.6: Mammals
      1. 29.6.0: Characteristics of Mammals
      2. 29.6.1: Evolution of Mammals
      3. 29.6.2: Living Mammals
    7. 29.7: The Evolution of Primates
      1. 29.7.0: Characteristics and Evolution of Primates
      2. 29.7.1: Early Human Evolution
      3. 29.7.2: Early Hominins
      4. 29.7.3: Genus Homo
  30. 30: Plant Form and Physiology
    1. 30.1: The Plant Body
      1. 30.1.0: Plant Tissues and Organ Systems
    2. 30.2: Stems
      1. 30.2.0: Functions of Stems
      2. 30.2.1: Stem Anatomy
      3. 30.2.2: Primary and Secondary Growth in Stems
      4. 30.2.3: Stem Modifications
    3. 30.3: Roots
      1. 30.3.0: Types of Root Systems and Zones of Growth
      2. 30.3.1: Root Modifications
    4. 30.4: Leaves
      1. 30.4.0: Leaf Structure and Arrangment
      2. 30.4.1: Types of Leaf Forms
      3. 30.4.2: Leaf Structure, Function, and Adaptation
    5. 30.5: Plant Development
      1. 30.5.0: Meristems
      2. 30.5.1: Genetic Control of Flowers
    6. 30.6: Transport of Water and Solutes in Plants
      1. 30.6.0: Water and Solute Potential
      2. 30.6.1: Pressure, Gravity, and Matric Potential
      3. 30.6.2: Movement of Water and Minerals in the Xylem
      4. 30.6.3: Transportation of Photosynthates in the Phloem
    7. 30.7: Plant Sensory Systems and Responses
      1. 30.7.0: Plant Responses to Light
      2. 30.7.1: The Phytochrome System and Red Light Response
      3. 30.7.2: Blue Light Response
      4. 30.7.3: Plant Responses to Gravity
      5. 30.7.4: Auxins, Cytokinins, and Gibberellins
      6. 30.7.5: Abscisic Acid, Ethylene, and Nontraditional Hormones
      7. 30.7.6: Plant Responses to Wind and Touch
    8. 30.8: Plant Defense Mechanisms
      1. 30.8.0: Plant Defenses Against Herbivores
      2. 30.8.1: Plant Defenses Against Pathogens
  31. 31: Soil and Plant Nutrition
    1. 31.1: Nutritional Requirements of Plants
      1. 31.1.0: Plant Nutrition
      2. 31.1.1: The Chemical Composition of Plants
      3. 31.1.2: Essential Nutrients for Plants
    2. 31.2: The Soil
      1. 31.2.0: Soil Composition
      2. 31.2.1: Soil Formation
      3. 31.2.2: Physical Properties of Soil
    3. 31.3: Nutritional Adaptations of Plants
      1. 31.3.0: Nitrogen Fixation: Root and Bacteria Interactions
      2. 31.3.1: Mycorrhizae: The Symbiotic Relationship between Fungi and Roots
      3. 31.3.2: Nutrients from Other Sources
  32. 32: Plant Reproduction
    1. 32.1: Plant Reproductive Development and Structure
      1. 32.1.0: Plant Reproductive Development and Structure
      2. 32.1.1: Sexual Reproduction in Gymnosperms
      3. 32.1.2: Sexual Reproduction in Angiosperms
    2. 32.2: Pollination and Fertilization
      1. 32.2.0: Pollination and Fertilization
      2. 32.2.1: Pollination by Insects
      3. 32.2.2: Pollination by Bats, Birds, Wind, and Water
      4. 32.2.3: Double Fertilization in Plants
      5. 32.2.4: Development of the Seed
      6. 32.2.5: Development of Fruit and Fruit Types
      7. 32.2.6: Fruit and Seed Dispersal
    3. 32.3: Asexual Reproduction
      1. 32.3.0: Asexual Reproduction in Plants
      2. 32.3.1: Natural and Artificial Methods of Asexual Reproduction in Plants
      3. 32.3.2: Plant Life Spans
  33. 33: The Animal Body: Basic Form and Function
    1. 33.1: Animal Form and Function
      1. 33.1.0: Characteristics of the Animal Body
      2. 33.1.1: Body Plans
      3. 33.1.2: Limits on Animal Size and Shape
      4. 33.1.3: Limiting Effects of Diffusion on Size and Development
      5. 33.1.4: Animal Bioenergetics
      6. 33.1.5: Animal Body Planes and Cavities
    2. 33.2: Animal Primary Tissues
      1. 33.2.0: Epithelial Tissues
      2. 33.2.1: Connective Tissues: Loose, Fibrous, and Cartilage
      3. 33.2.2: Connective Tissues: Bone, Adipose, and Blood
      4. 33.2.3: Muscle Tissues and Nervous Tissues
    3. 33.3: Homeostasis
      1. 33.3.0: Homeostatic Process
      2. 33.3.1: Control of Homeostasis
      3. 33.3.2: Homeostasis: Thermoregulation
      4. 33.3.3: Heat Conservation and Dissipation
  34. 34: Animal Nutrition and the Digestive System
    1. 34.1: Digestive Systems
      1. 34.1.0: Digestive Systems
      2. 34.1.1: Herbivores, Omnivores, and Carnivores
      3. 34.1.2: Invertebrate Digestive Systems
      4. 34.1.3: Vertebrate Digestive Systems
      5. 34.1.4: Digestive System: Mouth and Stomach
      6. 34.1.5: Digestive System: Small and Large Intestines
    2. 34.2: Nutrition and Energy Production
      1. 34.2.0: Food Requirements and Essential Nutrients
      2. 34.2.1: Food Energy and ATP
    3. 34.3: Digestive System Processes
      1. 34.3.0: Ingestion
      2. 34.3.1: Digestion and Absorption
      3. 34.3.2: Elimination
    4. 34.4: Digestive System Regulation
      1. 34.4.0: Neural Responses to Food
      2. 34.4.1: Hormonal Responses to Food
  35. 35: The Nervous System
    1. 35.1: Neurons and Glial Cells
      1. 35.1.0: Neurons and Glial Cells
      2. 35.1.1: Neurons
      3. 35.1.2: Glia
    2. 35.2: How Neurons Communicate
      1. 35.2.0: Nerve Impulse Transmission within a Neuron: Resting Potential
      2. 35.2.1: Nerve Impulse Transmission within a Neuron: Action Potential
      3. 35.2.2: Synaptic Transmission
      4. 35.2.3: Signal Summation
      5. 35.2.4: Synaptic Plasticity
    3. 35.3: The Nervous System
      1. 35.3.0: The Nervous System
    4. 35.4: The Central Nervous System
      1. 35.4.0: Brain: Cerebral Cortex and Brain Lobes
      2. 35.4.1: Brain: Midbrain and Brain Stem
      3. 35.4.2: Spinal Cord
    5. 35.5: The Peripheral Nervous System
      1. 35.5.0: Autonomic Nervous System
      2. 35.5.1: Sensory-Somatic Nervous System
    6. 35.6: Nervous System Disorders
      1. 35.6.0: Neurodegenerative Disorders
      2. 35.6.1: Neurodevelopmental Disorders: Autism and ADHD
      3. 35.6.2: Neurodevelopmental Disorders: Mental Illnesses
      4. 35.6.3: Other Neurological Disorders
  36. 36: Sensory Systems
    1. 36.1: Sensory Processes
      1. 36.1.0: Reception
      2. 36.1.1: Transduction and Perception
    2. 36.2: Somatosensation
      1. 36.2.0: Somatosensory Receptors
      2. 36.2.1: Integration of Signals from Mechanoreceptors
      3. 36.2.2: Thermoreception
    3. 36.3: Taste and Smell
      1. 36.3.0: Tastes and Odors
      2. 36.3.1: Reception and Transduction
    4. 36.4: Hearing and Vestibular Sensation
      1. 36.4.0: Sound
      2. 36.4.1: Reception of Sound
      3. 36.4.2: Transduction of Sound
      4. 36.4.3: The Vestibular System
      5. 36.4.4: Balance and Determining Equilibrium
    5. 36.5: Vision
      1. 36.5.0: Light
      2. 36.5.1: Anatomy of the Eye
      3. 36.5.2: Transduction of Light
      4. 36.5.3: Visual Processing
  37. 37: The Endocrine System
    1. 37.1: Types of Hormones
      1. 37.1.0: Hormone Functions
      2. 37.1.1: Lipid-Derived, Amino Acid-Derived, and Peptide Hormones
    2. 37.2: How Hormones Work
      1. 37.2.0: How Hormones Work
      2. 37.2.1: Intracellular Hormone Receptors
      3. 37.2.2: Plasma Membrane Hormone Receptors
    3. 37.3: Regulation of Body Processes
      1. 37.3.0: Hormonal Regulation of the Excretory System
      2. 37.3.1: Hormonal Regulation of the Reproductive System
      3. 37.3.2: Hormonal Regulation of Metabolism
      4. 37.3.3: Hormonal Control of Blood Calcium Levels
      5. 37.3.4: Hormonal Regulation of Growth
      6. 37.3.5: Hormonal Regulation of Stress
    4. 37.4: Regulation of Hormone Production
      1. 37.4.0: Humoral, Hormonal, and Neural Stimuli
    5. 37.5: Endocrine Glands
      1. 37.5.0: Hypothalamic-Pituitary Axis
      2. 37.5.1: Thyroid Gland
      3. 37.5.2: Parathyroid Glands
      4. 37.5.3: Adrenal Glands
      5. 37.5.4: Pancreas
      6. 37.5.5: Pineal Gland and Gonads
      7. 37.5.6: Organs with Secondary Endocrine Functions
  38. 38: The Musculoskeletal System
    1. 38.1: Types of Skeletal Systems
      1. 38.1.0: Functions of the Musculoskeletal System
      2. 38.1.1: Types of Skeletal Systems
      3. 38.1.2: Human Axial Skeleton
      4. 38.1.3: Human Appendicular Skeleton
    2. 38.2: Bone
      1. 38.2.0: Bone
      2. 38.2.1: Cell Types in Bones
      3. 38.2.2: Bone Development
      4. 38.2.3: Growth of Bone
      5. 38.2.4: Bone Remodeling and Repair
    3. 38.3: Joints and Skeletal Movement
      1. 38.3.0: Classification of Joints on the Basis of Structure and Function
      2. 38.3.1: Movement at Synovial Joints
      3. 38.3.2: Types of Synovial Joints
      4. 38.3.3: Bone and Joint Disorders
    4. 38.4: Muscle Contraction and Locomotion
      1. 38.4.0: Structure and Function of the Muscular System
      2. 38.4.1: Skeletal Muscle Fibers
      3. 38.4.2: Sliding Filament Model of Contraction
      4. 38.4.3: ATP and Muscle Contraction
      5. 38.4.4: Regulatory Proteins
      6. 38.4.5: Excitation–Contraction Coupling
      7. 38.4.6: Control of Muscle Tension
  39. 39: The Respiratory System
    1. 39.1: Systems of Gas Exchange
      1. 39.1.0: The Respiratory System and Direct Diffusion
      2. 39.1.1: Skin, Gills, and Tracheal Systems
      3. 39.1.2: Amphibian and Bird Respiratory Systems
      4. 39.1.3: Mammalian Systems and Protective Mechanisms
    2. 39.2: Gas Exchange across Respiratory Surfaces
      1. 39.2.0: Gas Pressure and Respiration
      2. 39.2.1: Basic Principles of Gas Exchange
      3. 39.2.2: Lung Volumes and Capacities
      4. 39.2.3: Gas Exchange across the Alveoli
    3. 39.3: Breathing
      1. 39.3.0: The Mechanics of Human Breathing
      2. 39.3.1: Types of Breathing
      3. 39.3.2: The Work of Breathing
      4. 39.3.3: Dead Space: V/Q Mismatch
    4. 39.4: Transport of Gases in Human Bodily Fluids
      1. 39.4.0: Transport of Oxygen in the Blood
      2. 39.4.1: Transport of Carbon Dioxide in the Blood
  40. 40: The Circulatory System
    1. 40.1: Overview of the Circulatory System
      1. 40.1.0: The Role of the Circulatory System
      2. 40.1.1: Open and Closed Circulatory Systems
      3. 40.1.2: Types of Circulatory Systems in Animals
    2. 40.2: Components of the Blood
      1. 40.2.0: The Role of Blood in the Body
      2. 40.2.1: Red Blood Cells
      3. 40.2.2: White Blood Cells
      4. 40.2.3: Platelets and Coagulation Factors
      5. 40.2.4: Plasma and Serum
    3. 40.3: Mammalian Heart and Blood Vessels
      1. 40.3.0: Structures of the Heart
      2. 40.3.1: Arteries, Veins, and Capillaries
      3. 40.3.2: The Cardiac Cycle
    4. 40.4: Blood Flow and Blood Pressure Regulation
      1. 40.4.0: Blood Flow Through the Body
      2. 40.4.1: Blood Pressure
  41. 41: Osmotic Regulation and the Excretory System
    1. 41.1: Osmoregulation and Osmotic Balance
      1. 41.1.0: Introduction to Osmoregulation
      2. 41.1.1: Transport of Electrolytes across Cell Membranes
      3. 41.1.2: Concept of Osmolality and Milliequivalent
      4. 41.1.3: Osmoregulators and Osmoconformers
    2. 41.2: Nitrogenous Wastes
      1. 41.2.0: Nitrogenous Waste in Terrestrial Animals: The Urea Cycle
      2. 41.2.1: Nitrogenous Waste in Birds and Reptiles: Uric Acid
    3. 41.3: Excretion Systems
      1. 41.3.0: Contractile Vacuoles in Microorganisms
      2. 41.3.1: Flame Cells of Planaria and Nephridia of Worms
      3. 41.3.2: Malpighian Tubules of Insects
    4. 41.4: Human Osmoregulatory and Excretory Systems
      1. 41.4.0: Kidney Structure
      2. 41.4.1: Nephron: The Functional Unit of the Kidney
      3. 41.4.2: Kidney Function and Physiology
    5. 41.5: Hormonal Control of Osmoregulatory Functions
      1. 41.5.0: Epinephrine and Norepinephrine
      2. 41.5.1: Other Hormonal Controls for Osmoregulation
  42. 42: The Immune System
    1. 42.1: Innate Immune Response
      1. 42.1.0: Innate Immune Response
      2. 42.1.1: Physical and Chemical Barriers
      3. 42.1.2: Pathogen Recognition
      4. 42.1.3: Natural Killer Cells
      5. 42.1.4: The Complement System
    2. 42.2: Adaptive Immune Response
      1. 42.2.0: Antigen-presenting Cells: B and T cells
      2. 42.2.1: Humoral Immune Response
      3. 42.2.2: Cell-Mediated Immunity
      4. 42.2.3: Cytotoxic T Lymphocytes and Mucosal Surfaces
      5. 42.2.4: Immunological Memory
      6. 42.2.5: Regulating Immune Tolerance
    3. 42.3: Antibodies
      1. 42.3.0: Antibody Structure
      2. 42.3.1: Antibody Functions
    4. 42.4: Disruptions in the Immune System
      1. 42.4.0: Immunodeficiency
      2. 42.4.1: Hypersensitivities
  43. 43: Animal Reproduction and Development
    1. 43.1: Reproduction Methods
      1. 43.1.0: Methods of Reproducing
      2. 43.1.1: Types of Sexual and Asexual Reproduction
      3. 43.1.2: Sex Determination
    2. 43.2: Fertilization
      1. 43.2.0: External and Internal Fertilization
      2. 43.2.1: The Evolution of Reproduction
    3. 43.3: Human Reproductive Anatomy and Gametogenesis
      1. 43.3.0: Male Reproductive Anatomy
      2. 43.3.1: Female Reproductive Anatomy
      3. 43.3.2: Gametogenesis (Spermatogenesis and Oogenesis)
    4. 43.4: Hormonal Control of Human Reproduction
      1. 43.4.0: Male Hormones
      2. 43.4.1: Female Hormones
    5. 43.5: Fertilization and Early Embryonic Development
      1. 43.5.0: Fertilization
      2. 43.5.1: Cleavage, the Blastula Stage, and Gastrulation
    6. 43.6: Organogenesis and Vertebrate Formation
      1. 43.6.0: Organogenesis
      2. 43.6.1: Vertebrate Axis Formation
    7. 43.7: Human Pregnancy and Birth
      1. 43.7.0: Human Gestation
      2. 43.7.1: Labor and Birth
      3. 43.7.2: Contraception and Birth Control
      4. 43.7.3: Infertility
  44. 44: Ecology and the Biosphere
    1. 44.1: The Scope of Ecology
      1. 44.1.0: Introduction to Ecology
      2. 44.1.1: Organismal Ecology and Population Ecology
      3. 44.1.2: Community Ecology and Ecosystem Ecology
    2. 44.2: Biogeography
      1. 44.2.0: Biogeography
      2. 44.2.1: Energy Sources
      3. 44.2.2: Temperature and Water
      4. 44.2.3: Inorganic Nutrients and Other Factors
      5. 44.2.4: Abiotic Factors Influencing Plant Growth
    3. 44.3: Terrestrial Biomes
      1. 44.3.0: What constitutes a biome?
      2. 44.3.1: Tropical Wet Forest and Savannas
      3. 44.3.2: Subtropical Deserts and Chaparral
      4. 44.3.3: Temperate Grasslands
      5. 44.3.4: Temperate Forests
      6. 44.3.5: Boreal Forests and Arctic Tundra
    4. 44.4: Aquatic Biomes
      1. 44.4.0: Abiotic Factors Influencing Aquatic Biomes
      2. 44.4.1: Marine Biomes
      3. 44.4.2: Estuaries: Where the Ocean Meets Fresh Water
      4. 44.4.3: Freshwater Biomes
    5. 44.5: Climate and the Effects of Global Climate Change
      1. 44.5.0: Climate and Weather
      2. 44.5.1: Causes of Global Climate Change
      3. 44.5.2: Evidence of Global Climate Change
      4. 44.5.3: Past and Present Effects of Climate Change
  45. 45: Population and Community Ecology
    1. 45.1: Population Demography
      1. 45.1.0: Population Demography
      2. 45.1.1: Population Size and Density
      3. 45.1.2: Species Distribution
      4. 45.1.3: The Study of Population Dynamics
    2. 45.2: Environmental Limits to Population Growth
      1. 45.2.0: Exponential Population Growth
      2. 45.2.1: Logistic Population Growth
      3. 45.2.2: Density-Dependent and Density-Independent Population Regulation
    3. 45.3: Life History Patterns
      1. 45.3.0: Life History Patterns and Energy Budgets
      2. 45.3.1: Theories of Life History
    4. 45.4: Human Population Growth
      1. 45.4.0: Human Population Growth
      2. 45.4.1: Overcoming Density-Dependent Regulation
      3. 45.4.2: Age Structure, Population Growth, and Economic Development
    5. 45.5: Community Ecology
      1. 45.5.0: The Role of Species within Communities
      2. 45.5.1: Predation, Herbivory, and the Competitive Exclusion Principle
      3. 45.5.2: Symbiosis
      4. 45.5.3: Ecological Succession
    6. 45.6: Innate Animal Behavior
      1. 45.6.0: Introduction to Animal Behavior
      2. 45.6.1: Movement and Migration
      3. 45.6.2: Animal Communication and Living in Groups
      4. 45.6.3: Altruism and Populations
      5. 45.6.4: Mating Systems and Sexual Selection
    7. 45.7: Learned Animal Behavior
      1. 45.7.0: Simple Learned Behaviors
      2. 45.7.1: Conditioned Behavior
      3. 45.7.2: Cognitive Learning and Sociobiology
  46. 46: Ecosystems
    1. 46.1: Ecology of Ecosystems
      1. 46.1.0: Ecosystem Dynamics
      2. 46.1.1: Food Chains and Food Webs
      3. 46.1.2: Studying Ecosystem Dynamics
      4. 46.1.3: Modeling Ecosystem Dynamics
    2. 46.2: Energy Flow through Ecosystems
      1. 46.2.0: Strategies for Acquiring Energy
      2. 46.2.1: Productivity within Trophic Levels
      3. 46.2.2: Transfer of Energy between Trophic Levels
      4. 46.2.3: Ecological Pyramids
      5. 46.2.4: Biological Magnification
    3. 46.3: Biogeochemical Cycles
      1. 46.3.0: Biogeochemical Cycles
      2. 46.3.1: The Water (Hydrologic) Cycle
      3. 46.3.2: The Carbon Cycle
      4. 46.3.3: The Nitrogen Cycle
      5. 46.3.4: The Phosphorus Cycle
      6. 46.3.5: The Sulfur Cycle
  47. 47: Conservation Biology and Biodiversity
    1. 47.1: The Biodiversity Crisis
      1. 47.1.0: Loss of Biodiversity
      2. 47.1.1: Types of Biodiversity
      3. 47.1.2: Biodiversity Change through Geological Time
      4. 47.1.3: The Pleistocene Extinction
      5. 47.1.4: Present-Time Extinctions
    2. 47.2: The Importance of Biodiversity to Human Life
      1. 47.2.0: Human Health and Biodiversity
      2. 47.2.1: Agricultural Diversity
      3. 47.2.2: Managing Fisheries
    3. 47.3: Threats to Biodiversity
      1. 47.3.0: Habitat Loss and Sustainability
      2. 47.3.1: Overharvesting
      3. 47.3.2: Exotic Species
      4. 47.3.3: Climate Change and Biodiversity
    4. 47.4: Preserving Biodiversity
      1. 47.4.0: Measuring Biodiversity
      2. 47.4.1: Changing Human Behavior in Response to Biodiversity Loss
      3. 47.4.2: Ecological Restoration

46.3: Biogeochemical Cycles

46.3.1: Biogeochemical Cycles

The elemental components of organic matter are cycled through the biosphere in an interconnected process called the biogeochemical cycle.

Learning Objective

Summarize the concept of biogeochemical cycles

Key Points

  • Carbon, nitrogen, hydrogen, oxygen, phosphorus, and sulfur are conserved and recycled in the atmosphere, on land, in water, or beneath the earth's surface.
  • Materials are recycled via erosion, weathering, water drainage, and the movement of tectonic plates.
  • Water is essential to all living processes, while carbon is found in all organic macromolecules.
  • Nitrogen and phosphorus are major components of nucleic acids and play major roles in agriculture.
  • Sulfur plays a role in the three-dimensional folding of proteins and is released into the atmosphere by the burning of fossil fuels.

Key Terms

hydrosphere

combined mass of water found on, under, and over the surface of a planet

biogeochemical cycle

cycling of mineral nutrients through ecosystems and through the non-living world

Biogeochemocal Cycles: Introduction

Energy flows directionally through ecosystems, entering as sunlight (or inorganic molecules for chemoautotrophs) and leaving as heat during the many transfers between trophic levels. However, the matter that makes up living organisms is conserved and recycled. The six most common elements associated with organic molecules (carbon, nitrogen, hydrogen, oxygen, phosphorus, and sulfur) take a variety of chemical forms and may exist for long periods in the atmosphere, on land, in water, or beneath the earth's surface. Geologic processes, such as weathering, erosion, water drainage, and the movement of the continental plates, all play a role in this recycling of materials. Because geology and chemistry have major roles in the study of this process, the recycling of inorganic matter between living organisms and their environment is called a biogeochemical cycle.

The components of organic molecules are constantly being stored and recycled as part of their biogeochemical cycle. Water, which contains hydrogen and oxygen, is essential to all living processes. The hydrosphere is the area of the earth where water movement and storage occurs. Water can be liquid on the surface and beneath the surface or frozen (rivers, lakes, oceans, groundwater, polar ice caps, and glaciers) or exist as water vapor in the atmosphere . Carbon, found in all organic macromolecules, is an important constituent of fossil fuels. Nitrogen, a major component of our nucleic acids and proteins, is critical to human agriculture. Phosphorus, a major component of nucleic acid (along with nitrogen), is one of the main ingredients in artificial fertilizers used in agriculture and their associated environmental impacts on our surface water. Sulfur, critical to the 3–D folding of proteins (as in disulfide binding), is released into the atmosphere by the burning of fossil fuels, such as coal.

Importance of the hydrosphere

Importance of the hydrosphere

Earth has a hydrosphere, where water movement and storage occurs. It is important for leaching certain components of organic matter into rivers, lakes, and oceans, and is a reservoir for carbon.

The cycling of all of these elements is interconnected. For example, the movement of water is critical for the leaching of nitrogen and phosphate into rivers, lakes, and oceans. Furthermore, the ocean itself is a major reservoir for carbon. Thus, mineral nutrients are cycled, either rapidly or slowly, through the entire biosphere, from one living organism to another, and between the biotic and abiotic world.

46.3.2: The Water (Hydrologic) Cycle

Water has a large effect on climate, ecosystems, and living organisms and is continuously cycled through the environment.

Learning Objective

Explain the path of the hydrologic cycle and its importance

Key Points

  • Water cycling affects the climate, transports minerals, purifies water, and replenishes the land with fresh water.
  • Water with a longer residence time, such as water in oceans and glaciers, is not available for short-term cycling, which occurs via evaporation.
  • Surface water evaporates (water to water vapor) or sublimates (ice to water vapor), which deposits large amounts of water vapor into the atmosphere.
  • Water vapor in the atmosphere condenses into clouds and is eventually followed by precipitation, which returns water to the earth's surface.
  • Rain percolates into the ground, where it may evaporate or enter bodies of water.
  • Surface runoff enters oceans directly or via streams and lakes.

Key Terms

condensation

the conversion of a gas to a liquid; the condensate so formed

residence time

the average time a particular molecule of water will remain in a body of water

sublimation

the transition of a substance from the solid phase directly to the vapor state such that it does not pass through the intermediate liquid phase

surface runoff

overland flow of excess water (with or without accumulated contaminants) that cannot be absorbed by the ground as infiltration

Evaporation

the process of a liquid converting to the gaseous state

The Water (Hydrologic) Cycle

Water is the basis of all living processes. More than half of the human body is made up of water, while human cells are more than 70 percent water. Thus, most land animals need a supply of fresh water to survive. However, when examining the stores of water on earth, 97.5 percent of it is non-potable salt water. Of the remaining water, 99 percent is locked underground as water or as ice. Thus, less than 1 percent of fresh water is easily accessible from lakes and rivers . Many living things, such as plants, animals, and fungi, are dependent on the small amount of fresh surface water supply, a lack of which can have massive effects on ecosystem dynamics. Humans, of course, have developed technologies to increase water availability, such as digging wells to harvest groundwater, storing rainwater, and using desalination to obtain drinkable water from the ocean. Although this pursuit of drinkable water has been ongoing throughout human history, the supply of fresh water is still a major issue in modern times.

Water availability

Water availability

Only 2.5 percent of water on earth is fresh water. Less than 1 percent of fresh water is easily accessible to living things.

Water cycling is extremely important to ecosystem dynamics as it has a major influence on climate and, thus, on the environments of ecosystems. For example, when water evaporates, it takes up energy from its surroundings, cooling the environment. When it condenses, it releases energy, warming the environment. The evaporation phase of the cycle purifies water, which then replenishes the land with fresh water. The flow of liquid water and ice transports minerals across the globe. It is also involved in reshaping the geological features of the earth through processes including erosion and sedimentation. The water cycle is also essential for the maintenance of most life and ecosystems on the planet. Most of the water on earth is stored for long periods in the oceans, underground, and as ice . Residence time is a measure of the average time an individual water molecule stays in a particular reservoir. A large amount of the earth's water is locked in place in these reservoirs as ice, beneath the ground, and in the ocean, and, thus, is unavailable for short-term cycling (only surface water can evaporate).

Residence time of water

Residence time of water

This graph shows the average residence time for water molecules in the earth's water reservoirs. Most of the earth's water is unavailable for use because it is locked in ice, beneath the ground, or in the oceans.

There are various processes that occur during the cycling of water, which include the following :

Cycling of water

Cycling of water

Water from the land and oceans enters the atmosphere by evaporation or sublimation, where it condenses into clouds and falls as rain or snow. Precipitated water may enter freshwater bodies or infiltrate the soil. The cycle is complete when surface or groundwater reenters the ocean.

  • evaporation/sublimation
  • condensation/precipitation
  • subsurface water flow
  • surface runoff/snowmelt
  • streamflow

The water cycle is driven by the sun's energy as it warms the oceans and other surface waters. This leads to the evaporation (water to water vapor) of liquid surface water and the sublimation (ice to water vapor) of frozen water, which deposits large amounts of water vapor into the atmosphere. Over time, this water vapor condenses into clouds as liquid or frozen droplets, which is eventually followed by precipitation (rain or snow), returning water to the earth's surface. Rain eventually percolates into the ground, where it may evaporate again (if it is near the surface), flow beneath the surface, or be stored for long periods. More easily observed is surface runoff: the flow of fresh water either from rain or melting ice. Runoff can then make its way through streams and lakes to the oceans or flow directly to the oceans themselves. Rain and surface runoff are major ways in which minerals, including carbon, nitrogen, phosphorus, and sulfur, are cycled from land to water.

46.3.3: The Carbon Cycle

Carbon enters the atmosphere in the form of carbon dioxide via the carbon cycle and returns to organic carbon via photosynthesis.

Learning Objective

Distinguish between the biological and biogeochemical cycles of carbon

Key Points

  • Carbon is present in all organic molecules; carbon compounds contain large amounts of energy, which humans use as fuel.
  • The biological carbon cycle is the rapid exchange of carbon among living things; autotrophs use carbon dioxide produced by heterotrophs to produce glucose and oxygen, which are then utilized by heterotrophs.
  • The biogeochemical cycle occurs at a much slower rate than the biological cycle since carbon is stored in carbon reservoirs for long periods of time.
  • Carbon dioxide from the atmosphere dissolves in water, combining with water molecules to form carbonic acid, which then ionizes to carbonate and bicarbonate ions.
  • Most of the carbon in the ocean is in the form of bicarbonate ions, which can combine with seawater calcium to form calcium carbonate (CaCO3), a major component of marine organism shells.
  • Carbon can enter the soil as a result of the decomposition of living organisms, the weathering of rocks, the eruption of volcanoes, and other geothermal systems.

Key Terms

heterotroph

an organism that requires an external supply of energy in the form of food, as it cannot synthesize its own

autotroph

Any organism that can synthesize its food from inorganic substances, using heat or light as a source of energy

non-renewable resource

resource, such as fossil fuel, that is either regenerated very slowly or not at all

subduction

movement of one tectonic plate beneath another

The Carbon Cycle

Carbon, the second most abundant element in living organisms, is present in all organic molecules. Its role in the structure of macromolecules is of primary importance to living organisms. Carbon compounds contain especially- high forms of energy, which humans use as fuel. Since the 1800s (the beginning of the Industrial Revolution), the number of countries using massive amounts of fossil fuels increased, which raised the levels of carbon dioxide in the atmosphere. This increase in carbon dioxide has been associated with climate change and other disturbances of the earth's ecosystems. It is a major environmental concern worldwide.

The carbon cycle is most easily studied as two interconnected sub-cycles: one dealing with rapid carbon exchange among living organisms and the other dealing with the long-term cycling of carbon through geologic processes .

Carbon cycle

Carbon cycle

Carbon dioxide gas exists in the atmosphere and is dissolved in water. Photosynthesis converts carbon dioxide gas to organic carbon, while respiration cycles the organic carbon back into carbon dioxide gas. Long-term storage of organic carbon occurs when matter from living organisms is buried deep underground and becomes fossilized. Volcanic activity and human emissions bring this stored carbon back into the carbon cycle.

The Biological Carbon Cycle

Living organisms are connected in many ways, even between ecosystems. A good example of this connection is the exchange of carbon between autotrophs and heterotrophs. Carbon dioxide is the basic building block that most autotrophs use to build multi-carbon, high-energy compounds, such as glucose. The energy harnessed from the sun is used by these organisms to form the covalent bonds that link carbon atoms together. These chemical bonds store this energy for later use in the process of respiration. Most terrestrial autotrophs obtain their carbon dioxide directly from the atmosphere, while marine autotrophs acquire it in the dissolved form (carbonic acid, H2CO3−). However carbon dioxide is acquired, a by-product of the process is oxygen. The photosynthetic organisms are responsible for depositing approximately 21 percent of the oxygen content in the atmosphere that we observe today.

Heterotrophs acquire the high-energy carbon compounds from the autotrophs by consuming them and breaking them down by respiration to obtain cellular energy, such as ATP. The most efficient type of respiration, aerobic respiration, requires oxygen obtained from the atmosphere or dissolved in water. Thus, there is a constant exchange of oxygen and carbon dioxide between the autotrophs (which need the carbon) and the heterotrophs (which need the oxygen). Gas exchange through the atmosphere and water is one way that the carbon cycle connects all living organisms on Earth.

The Biogeochemical Carbon Cycle

The movement of carbon through the land, water, and air is complex and, in many cases, it occurs much more slowly than the biological carbon cycle. Carbon is stored for long periods in what are known as carbon reservoirs, which include the atmosphere, bodies of liquid water (mostly oceans), ocean sediment, soil, land sediments (including fossil fuels), and the earth's interior.

As stated, the atmosphere, a major reservoir of carbon in the form of carbon dioxide, is essential to the process of photosynthesis. The level of carbon dioxide in the atmosphere is greatly influenced by the reservoir of carbon in the oceans. The exchange of carbon between the atmosphere and water reservoirs influences how much carbon is found in each location; each affects the other reciprocally. Carbon dioxide (CO2) from the atmosphere dissolves in water, combining with water molecules to form carbonic acid. It then ionizes to carbonate and bicarbonate ions .

Formation of bicarbonate

Formation of bicarbonate

Carbon dioxide reacts with water to form bicarbonate and carbonate ions.

More than 90 percent of the carbon in the ocean is found as bicarbonate ions. Some of these ions combine with seawater calcium to form calcium carbonate (CaCO3), a major component of marine organism shells. These organisms eventually form sediments on the ocean floor. Over geologic time, the calcium carbonate forms limestone, which comprises the largest carbon reservoir on earth.

On land, carbon is stored in soil as a result of the decomposition of living organisms or the weathering of terrestrial rock and minerals. This carbon can be leached into the water reservoirs by surface runoff. Deeper underground, on land and at sea, are fossil fuels: the anaerobically-decomposed remains of plants that take millions of years to form. Fossil fuels are considered a non-renewable resource because their use far exceeds their rate of formation. A non-renewable resource is either regenerated very slowly or not at all. Another way for carbon to enter the atmosphere is from land by the eruption of volcanoes and other geothermal systems. Carbon sediments from the ocean floor are taken deep within the earth by the process of subduction: the movement of one tectonic plate beneath another. Carbon is released as carbon dioxide when a volcano erupts or from volcanic hydrothermal vents.

Carbon dioxide is also added to the atmosphere by the breeding and raising of livestock. The large numbers of land animals raised to feed the earth's growing population results in increased carbon dioxide levels in the atmosphere due to farming practices, respiration, and methane production. This is another example of how human activity indirectly affects biogeochemical cycles in a significant way. Although much of the debate about the future effects of increasing atmospheric carbon on climate change focuses on fossils fuels, scientists take natural processes, such as volcanoes and respiration, into account as they model and predict the future impact of this increase.

46.3.4: The Nitrogen Cycle

Nitrogen, the most abundant gas in the atmosphore, is cycled through the biosphere via the multi-step process of nitrogen fixation, which is carried out by bacteria.

Learning Objective

Describe the nitrogen cycle

Key Points

  • Bacteria, such as cyanobacteria, convert nitrogen into nitrogen gas via nitrogen fixation.
  • Nitrogen fixation occurs in three steps: ammonification, nitrification, and denitrification.
  • Human activity can release nitrogen into the environment by the combustion of fossil fuels and by the use of artificial fertilizers in agriculture.
  • Atmospheric nitrogen is responsible for acid rain, the release of greenhouse gasses, and eutrophication.
  • Nitrogen fixation can be performed by marine bacteria; nitrogen falls to the ocean floor as sediment and is then moved to land, becoming incorporated into terrestrial rock.

Key Terms

denitrification

process of converting nitrates into nitrogen gas, especially by the action of bacteria

nitrification

the conversion of ammonium into nitrites (NO2−) by nitrifying bacteria

ammonification

the formation of ammonia or its compounds from nitrogenous compounds, especially as a result of bacterial decomposition

The Nitrogen Cycle

Getting nitrogen into the living world is difficult. Plants and phytoplankton are not equipped to incorporate nitrogen from the atmosphere (which exists as tightly-bonded, triple-covalent N2), even though this molecule comprises approximately 78 percent of the atmosphere. Nitrogen enters the living world via free-living and symbiotic bacteria, which incorporate nitrogen into their macromolecules through nitrogen fixation (conversion of N2). Cyanobacteria live in most aquatic ecosystems where sunlight is present; they play a key role in nitrogen fixation. Cyanobacteria are able to use inorganic sources of nitrogen to "fix" nitrogen. Rhizobium bacteria live symbiotically in the root nodules of legumes (such as peas, beans, and peanuts), providing them with the organic nitrogen they need. Free-living bacteria, such as Azotobacter, are also important nitrogen fixers.

Organic nitrogen is especially important to the study of ecosystem dynamics as many ecosystem processes, such as primary production and decomposition, are limited by the available supply of nitrogen. The nitrogen that enters living systems by nitrogen fixation is successively converted from organic nitrogen back into nitrogen gas by bacteria . This process occurs in three steps in terrestrial systems: ammonification, nitrification, and denitrification. First, the ammonification process converts nitrogenous waste from living animals or from the remains of dead animals into ammonium (NH4+) by certain bacteria and fungi. Second, the ammonium is converted to nitrites (NO2−) by nitrifying bacteria, such as Nitrosomonas, through nitrification. Subsequently, nitrites are converted to nitrates (NO3−) by similar organisms. Third, the process of denitrification occurs, whereby bacteria, such as Pseudomonas and Clostridium, convert the nitrates into nitrogen gas, allowing it to re-enter the atmosphere.

Nitrogen fixation

Nitrogen fixation

Nitrogen enters the living world from the atmosphere via nitrogen-fixing bacteria. This nitrogen and nitrogenous waste from animals is then processed back into gaseous nitrogen by soil bacteria, which also supply terrestrial food webs with the organic nitrogen they need.

Human activity can release nitrogen into the environment by two primary means: the combustion of fossil fuels, which releases different nitrogen oxides, and the use of artificial fertilizers in agriculture, which are then washed into lakes, streams, and rivers by surface runoff. Atmospheric nitrogen is associated with several effects on earth's ecosystems, including the production of acid rain (as nitric acid, HNO3) and greenhouse gas (as nitrous oxide, N2O), potentially causing climate change. A major effect from fertilizer runoff is saltwater and freshwater eutrophication: a process whereby nutrient runoff causes the excess growth of microorganisms, depleting dissolved oxygen levels and killing ecosystem fauna.

A similar process occurs in the marine nitrogen cycle, where the ammonification, nitrification, and denitrification processes are performed by marine bacteria. Some of this nitrogen falls to the ocean floor as sediment, which can then be moved to land in geologic time by uplift of the earth's surface, becoming incorporated into terrestrial rock. Although the movement of nitrogen from rock directly into living systems has been traditionally seen as insignificant compared with nitrogen fixed from the atmosphere, a recent study showed that this process may indeed be significant and should be included in any study of the global nitrogen cycle.

46.3.5: The Phosphorus Cycle

Phosphorus is an essential element of living things, but, in excess, it can cause damage to ecosystems.

Learning Objective

Describe the phosphorus cycle and the effects of phosphorus on the environment

Key Points

  • Phosphorus, a major component of nucleic acid and phospholipids, also makes up the supportive components of our bones; it is often necessary for growth in aquatic ecosystems.
  • Phosphates (PO43−) are sent into rivers, lakes, and the ocean by leaching and natural surface runoff.
  • Phosphate-containing ocean sediments slowly move to land by the uplifting of areas of the earth's surface.
  • Excess phosphorus and nitrogen in the ecosystem leads to the death of many organisms, causing dead zones.
  • Dead zones are caused by by eutrophication, oil spills, dumping of toxic chemicals, and other human activities.

Key Terms

eutrophication

process whereby excess levels of nitrogen or phosphorus cause excessive growth of microorganisms, depleting dissolved oxygen levels and kill ecosystem fauna

dead zone

an area within a freshwater or marine ecosystem where large areas are depleted of their normal flora and fauna; caused by excessive nutrient pollution

The Phosphorus Cycle

Phosphorus is an essential nutrient for living processes. It is a major component of nucleic acid, both DNA and RNA; of phospholipids, the major component of cell membranes; and, as calcium phosphate, makes up the supportive components of our bones. Phosphorus is often the limiting nutrient (necessary for growth) in aquatic ecosystems.

Phosphorus occurs in nature as the phosphate ion (PO43−). In addition to phosphate runoff as a result of human activity, natural surface runoff occurs when it is leached from phosphate-containing rock by weathering, thus sending phosphates into rivers, lakes, and the ocean. This rock has its origins in the ocean. Phosphate-containing ocean sediments form primarily from the bodies of ocean organisms and from their excretions. However, in remote regions, volcanic ash, aerosols, and mineral dust may also be significant phosphate sources. This sediment then is moved to land over geologic time by the uplifting of areas of the earth's surface .

Phosphorus cycle

Phosphorus cycle

In nature, phosphorus exists as the phosphate ion (PO43−). Weathering of rocks and volcanic activity releases phosphate into the soil, water, and air, where it becomes available to terrestrial food webs. Phosphate enters the oceans via surface runoff, groundwater flow, and river flow. Phosphate dissolved in ocean water cycles into marine food webs. Some phosphate from the marine food webs falls to the ocean floor, where it forms sediment.

Phosphorus is also reciprocally exchanged between phosphate dissolved in the ocean and marine ecosystems. The movement of phosphate from the ocean to the land and through the soil is extremely slow, with the average phosphate ion having an oceanic residence time between 20,000 and 100,000 years.

Excess phosphorus and nitrogen that enters these ecosystems from fertilizer runoff and from sewage causes excessive growth of microorganisms and depletes the dissolved oxygen, which leads to the death of many ecosystem fauna, such as shellfish and finfish. This process is responsible for dead zones in lakes and at the mouths of many major rivers .

Dead zones

Dead zones

Dead zones occur when phosphorus and nitrogen from fertilizers cause excessive growth of microorganisms, which depletes oxygen, killing flora and fauna. Worldwide, large dead zones are found in coastal areas of high population density.

A dead zone is an area within a freshwater or marine ecosystem where large areas are depleted of their normal flora and fauna. These zones can be caused by eutrophication, oil spills, dumping of toxic chemicals, and other human activities. The number of dead zones has been increasing for several years; more than 400 of these zones were present as of 2008. One of the worst dead zones is off the coast of the United States in the Gulf of Mexico, where fertilizer runoff from the Mississippi River basin has created a dead zone of over 8,463 square miles. Phosphate and nitrate runoff from fertilizers also negatively affect several lake and bay ecosystems, including the Chesapeake Bay in the eastern United States, which was one of the first ecosystems to have identified dead zones.

46.3.6: The Sulfur Cycle

Sulfur is deposited on land as precipitation, fallout, and rock weathering, and reintroduced when organisms decompose.

Learning Objective

Describe the sulfur cycle

Key Points

  • Sulfur is an essential element for the macromolecules of living things since it determines the 3-D folding patterns of proteins.
  • On land, sulfur enters the atmosphere via acid rain, fallout, the weathering of rocks, decompostion of organic materials, and geothermal vents.
  • Sulfur enters the ocean via runoff, fallout, and underwater geothermal vents; some marine ecosystems also rely on chemoautotrophs as a sulfur source.
  • The burning of fossil fuels increases the amount of sulfide in the atmosphere and causes acid rain.
  • Acid rain is corrosive rain that causes damage to aquatic ecosystems by lowering the pH of lakes, killing many of the resident fauna; it also degrades buildings and human-made structures.

Key Terms

chemoautotroph

a simple organism, such as a protozoan, that derives its energy from chemical processes rather than photosynthesis

fallout

direct deposit of solid minerals on land or in the ocean from the atmosphere

acid rain

corrosive rain caused by rainwater falling to the ground through sulfur dioxide gas, turning it into weak sulfuric acid; can damage structures and ecosystems

The Sulfur Cycle

Sulfur is an essential element for the macromolecules of living things. As a part of the amino acid cysteine, it is involved in the formation of disulfide bonds within proteins, which help to determine their 3-D folding patterns and, hence, their functions. Sulfur cycles exist between the oceans, land, and atmosphere .

Sulfur cycle

Sulfur cycle

Sulfur dioxide from the atmosphere becomes available to terrestrial and marine ecosystems when it is dissolved in precipitation as weak sulfuric acid or when it falls directly to the earth as fallout. Weathering of rocks also makes sulfates available to terrestrial ecosystems. Decomposition of living organisms returns sulfates to the ocean, soil, and atmosphere.

On land, sulfur is deposited in four major ways: precipitation, direct fallout from the atmosphere, rock weathering, and decomposition of organic materials. Atmospheric sulfur is found in the form of sulfur dioxide (SO2). As rain falls through the atmosphere, sulfur is dissolved in the form of weak sulfuric acid (H2SO4), creating acid rain. Sulfur can also fall directly from the atmosphere in a process called fallout. The weathering of sulfur-containing rocks also releases sulfur into the soil. These rocks originate from ocean sediments that are moved to land by the geologic uplift. Terrestrial ecosystems can then make use of these soil sulfates (SO42−). Upon the death and decomposition of these organisms, sulfur is released back into the atmosphere as hydrogen sulfide (H2S) gas. Sulfur may also enter the atmosphere through geothermal vents .

Sulfur vents

Sulfur vents

At this sulfur vent in Lassen Volcanic National Park in northeastern California, the yellowish sulfur deposits are visible near the mouth of the vent.

Sulfur enters the ocean via runoff from land, fallout, and underwater geothermal vents. Some marine ecosystems rely on chemoautotrophs, using sulfur as a biological energy source. This sulfur then supports marine ecosystems in the form of sulfates.

Human activities have played a major role in altering the balance of the global sulfur cycle. The burning of large quantities of fossil fuels, especially from coal, releases large amounts of hydrogen sulfide gas into the atmosphere, creating acid rain. Acid rain is corrosive rain that causes damage to aquatic ecosystems and the natural environment by lowering the pH of lakes, which kills many of the resident fauna; it also affects the human-made environment through the chemical degradation of buildings. For example, many marble monuments, such as the Lincoln Memorial in Washington, DC, have suffered significant damage from acid rain over the years. These examples show the wide-ranging effects of human activities on our environment and the challenges that remain for our future.

Attributions

  • Biogeochemical Cycles
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "hydrosphere." http://en.wikipedia.org/wiki/hydrosphere. Wikipedia CC BY-SA 3.0.
    • "OpenStax College, Biology. December 9, 2013." http://cnx.org/content/m44889/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biology. October 23, 2013." http://cnx.org/content/m44889/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
    • "Atmosphere-Biosphere-Hydrosphere-Lithosphere." http://commons.wikimedia.org/wiki/File:Atmosphere-Biosphere-Hydrosphere-Lithosphere.png. Wikimedia CC BY.
  • The Water (Hydrologic) Cycle
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "Evaporation." http://en.wikipedia.org/wiki/Evaporation. Wikipedia CC BY-SA 3.0.
    • "Water cycle." http://en.wikipedia.org/wiki/Water_cycle. Wikipedia CC BY-SA 3.0.
    • "sublimation." http://en.wiktionary.org/wiki/sublimation. Wiktionary CC BY-SA 3.0.
    • "condensation." http://en.wiktionary.org/wiki/condensation. Wiktionary CC BY-SA 3.0.
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    • "residence time." http://en.wiktionary.org/wiki/residence_time. Wiktionary CC BY-SA 3.0.
    • "surface runoff." http://en.wiktionary.org/wiki/surface_runoff. Wiktionary CC BY-SA 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_02.jpg. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_03.jpg. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_01.jpg. OpenStax CNX CC BY 3.0.
  • The Carbon Cycle
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "autotroph." http://en.wiktionary.org/wiki/autotroph. Wiktionary CC BY-SA 3.0.
    • "heterotroph." http://en.wiktionary.org/wiki/heterotroph. Wiktionary CC BY-SA 3.0.
    • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44889/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_04.jpg. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_05.jpg. OpenStax CNX CC BY 3.0.
  • The Nitrogen Cycle
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "ammonification." http://en.wiktionary.org/wiki/ammonification. Wiktionary CC BY-SA 3.0.
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    • "denitrification." http://en.wiktionary.org/wiki/denitrification. Wiktionary CC BY-SA 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_06.png. OpenStax CNX CC BY 3.0.
  • The Phosphorus Cycle
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44889/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_07.jpg. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_08.jpg. OpenStax CNX CC BY 3.0.
  • The Sulfur Cycle
    • "Boundless." http://www.boundless.com/. Boundless Learning CC BY-SA 3.0.
    • "OpenStax College, Biology. October 17, 2013." http://cnx.org/content/m44889/latest/?collection=col11448/latest. OpenStax CNX CC BY 3.0.
    • "acid rain." http://en.wiktionary.org/wiki/acid_rain. Wiktionary CC BY-SA 3.0.
    • "chemoautotroph." http://en.wiktionary.org/wiki/chemoautotroph. Wiktionary CC BY-SA 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_10.jpg. OpenStax CNX CC BY 3.0.
    • "OpenStax College, Biogeochemical Cycles. October 17, 2013." http://cnx.org/content/m44889/latest/Figure_46_03_11.jpg. OpenStax CNX CC BY 3.0.

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