Early Life on Earth: Evolution, Diversification, and Interactions

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This book comprehensively explores the early evolution of life and the Archean environment. Topics include the differences between prokaryotes and eukaryotes, variations in metabolisms, concepts of ecosystems and biogeochemical cycles (nitrogen, sulfur, phosphorous), Archean geology and environments, and the widely accepted early evolutionary history of life. The text addresses controversies regarding early life and its environment, particularly the unusual microfossil assemblages from the 3.4 Ga Strelley Pool Formation and the 3.0 Ga Farrel Quartzite of Western Australia. Readers will get a fuller picture of the Archean world, and an appreciation of many still unresolved questions.

Key Features

    • Illustrated with figures visualizing ecosystems, biogeochemical cycles etc which are indispensable for understanding the Archean Earth.

    • Includes tables arranging key words, definitions, and interpretations.

    • Documents the Archean environment with photographic evidence and detailed descriptions the rocks, minerals and microfossils.

    • Summarizes the latest field research.

    • Details exciting unresolved questions for future study.

    Author(s): Kenichiro Sugitani
    Publisher: CRC Press
    Year: 2022

    Language: English
    Pages: 353
    City: Boca Raton

    Cover
    Half Title
    Title Page
    Copyright Page
    Table of Contents
    Preface
    Author
    Chapter 1 Space, Solar System, and the Earth
    1.1 Introduction
    1.2 Elements in the Universe and Their Origins
    1.3 Evolution of Our Solar System
    1.4 Evolution of the Earth’s Inner Structure
    1.5 Origins of the Oceans and the Atmosphere
    Column: Meteorite
    References
    Chapter 2 Solid Earth
    2.1 Introduction
    2.2 Plate Tectonics, Driving Force of Dynamism of the Earth
    2.3 Igneous Rocks
    2.3.1 Classification Scheme
    2.3.2 Granitic Rocks (Granitoids)
    2.3.3 Basaltic Rocks
    2.4 Sedimentary Rocks
    2.4.1 Volcaniclastic (Pyroclastic) Rocks
    2.4.2 Terrigenous Clastic Rocks
    2.4.2.1 Factors Controlling Chemistry and Mineralogy of Terrigenous Clastic Rocks
    2.4.2.2 Sedimentary Structures of Terrigenous Clastic Rocks and Their Implications
    2.4.3 Biogenic, Chemical, and Biochemical Sedimentary Rocks
    2.4.3.1 Biogenic Sedimentary Rocks
    2.4.3.2 Chemical Sedimentary Rocks
    2.4.3.3 Biochemical Sedimentary Rocks
    2.5 Metamorphic Rocks
    Column: Geochemistry of Igneous Rocks and of Magmatic Processes
    References
    Chapter 3 Life on the Earth 1
    3.1 Introduction
    3.2 Chemical Evolution and Emergence of Life on the Earth
    3.2.1 Revisit to Miller’s Experiment
    3.2.2 Delivery of Building Blocks of Life from Space
    3.2.3 Deep-Sea Hydrothermal Vent Systems and Origin of Life
    3.2.4 Terrestrial Hydrothermal Systems (Hot Springs): Another Candidates for Birthplace of Life
    3.3 Classification of Life on the Earth
    3.4 Diversity in Metabolisms
    3.4.1 Autotrophy and Heterotrophy
    3.4.2 Chemistry of Autotrophy
    3.4.3 Chemistry of Heterotrophy
    3.5 Ecosystem: Complex System of Life and Environment
    Column: Discovery of Deep-Sea Hydrothermal Systems
    References
    Chapter 4 Life on the Earth 2
    4.1 Introduction
    4.2 Carbon
    4.2.1 Deep Carbon Cycle
    4.2.2 Modern Surface Carbon Cycle
    4.2.2.1 Terrestrial Carbon Cycle
    4.2.2.2 Oceanic Carbon Cycle
    4.2.2.3 Sediment Carbon Cycle
    4.2.3 Archean Carbon Cycle
    4.3 Sulfur
    4.3.1 Modern Sulfur Cycle
    4.3.2 Archean Sulfur Cycle
    4.4 Nitrogen
    4.4.1 Modern Nitrogen Cycle
    4.4.2 Archean Nitrogen Cycle
    4.5 Phosphorous
    4.5.1 Modern Phosphorous Cycle
    4.5.2 Archean Phosphorous Cycle
    Column: Isotope and Isotope Fractionation
    References
    Chapter 5 Topics of the Early Precambrian Earth 1
    5.1 Introduction
    5.2 Archean Cratons
    5.2.1 Distributions and Compositions of Archean Cratons
    5.2.2 Origins of Archean Cratons
    5.3 Early Continental Growth and Its Implications
    5.3.1 Models of Continental Growth
    5.3.2 Plate Tectonics and Continental Growth and Implications
    5.4 Komatiite Volcanism and Its Significance
    5.4.1 Komatiite and Its Origin
    5.4.2 Serpentinization of Komatiite and Its Implications
    5.5 Large Asteroid Impact and Its Implications
    5.5.1 Paleo-and Mesoarchean Records of Asteroid Impacts
    5.5.2 Identification of Large Asteroid Impacts
    5.5.3 Implications of Large Asteroid Impacts
    5.6 Archean Seawater Compositions and Products 1: Iron Formations
    5.6.1 Clues to Archean Seawater Compositions
    5.6.2 What Are Iron Formations?
    5.6.3 Iron- Rich and Anoxic Deep Seawaters
    5.6.4 Origins of Early to Mesoarchean Iron Formations
    5.7 Archean Seawater Compositions and Products 2: Cherts
    5.7.1 Silica and Chert
    5.7.2 Archean Primary Cherts, Indicative of Silica- Rich Ocean
    5.7.3 Formation Processes of Secondary Cherts
    5.7.3.1 Hydrothermal Alteration of Oceanic Crusts
    5.7.3.2 Syndepositional Silicification
    5.7.3.3 Pervasive Silicification
    5.7.3.4 Chert Formation and Element Remobilization
    5.8 How Was the Earth’s Atmosphere Oxidized
    5.8.1 Archean Atmosphere
    5.8.2 Microbial Consumption and Production of H[sub(2)] and CH[sub(4)]
    5.8.3 Hydrogen Escape
    5.8.4 Archean Ocean Temperature and pH
    5.8.4.1 Temperature: Hot or Temperate?
    5.8.4.2 Acidic, Neutral, or Alkaline?
    Column: Zircon, Windows to the Hadean (4.6–4.0 Ga)
    References
    Chapter 6 Topics of the Early Precambrian Earth 2
    6.1 Introduction
    6.2 Photosynthesis and Its Evolution
    6.2.1 Anoxygenic and Oxygenic Photosynthesis
    6.2.2 Oxygenic Photosynthesis: Energetic and Physiological Perspective
    6.2.3 Oxygenic Photosynthesis: Nutritional Perspective
    6.3 Geochemical and Mineralogical Records of the Great Oxidation Event (GOE) and Earlier Oxygenation
    6.3.1 Occurrrences of Redox- Sensitive Minerals and Related Sediments
    6.3.1.1 Uraninite, Pyrite, and Siderite
    6.3.1.2 Red Beds
    6.3.2 Black Shales and Molybdenum
    6.3.3 Paleosol, Clue to Oxygen in the Atmosphere and Implications?
    6.3.3.1 Concept of Paleosol Geochemistry
    6.3.3.2 Classical Controversy on Paleosol Records
    6.3.3.3 Recent Controversies on Archean Oxygenic Atmosphere and Isotopic Approach to Paleosol
    6.3.4 Identification of Sulfur Mass-Independent Isotopic Fractionation (S-MIF)
    6.4 Sedimentary Records of Oxygenic Photosynthesis: Stromatolite and MISS
    Column: Oxygen is a Double-Edged Sword
    References
    Chapter 7 Biosignatures in Ancient Rocks and Related Issues
    7.1 Introduction
    7.2 Organic Matter
    7.2.1 Kerogen and Its Isotopic Compositions
    7.2.2 Hydrocarbons and Others – Archean Oils
    7.3 Pyrite and Sulfur
    7.4 Sedimentary Structures and Deposits
    7.4.1 Microbially- Induced Sedimentary Structures
    7.4.2 Stromatolites
    7.4.2.1 What are Stromatolites?
    7.4.2.2 Skepticisms to Archean Stromatolites
    7.4.2.3 The Oldest Stromatolites? – The 3.4 Ga-old Strelley Pool Formation
    7.4.2.4 The Oldest Stromatolites? – The 3.5 Ga Dresser Formation
    7.5 Ichnofossils in Volcanic Rocks
    7.6 Systematic Approach to Biogenicity Assessment of Cell-Like Structures
    7.6.1 Geological Context
    7.6.2 Syngenicity
    7.6.3 Biological Context: Size and Its Range
    7.6.4 Biological Context: Shape
    7.6.5 Biological Context: Occurrence
    7.6.6 Biological Context: Taphonomy
    7.6.7 Biological Context: Chemical and Isotopic Compositions
    Column: Biofilm
    References
    Chapter 8 Early (Paleo- to Meso-) Archean Cellularly Preserved Biosignatures
    8.1 Introduction
    8.2 Isua Supracrustal Belt, Greenland (Denmark)
    8.2.1 Geological Background
    8.2.2 Cellularly Preserved Biosignatures
    8.3 The Nuvvuagittuq Greenstone Belt, Canada
    8.3.1 Geological Background
    8.3.2 Cellularly Preserved Biosignature
    8.4 Kaapvaal Craton, South Africa
    8.4.1 The Onverwacht Group
    8.4.1.1 The Hoogenoeg Formation
    8.4.1.2 The Kromberg Formation
    8.4.2 The Fig Tree Group
    8.4.3 The Moodies Group
    8.5 Pilbara Craton, Western Australia
    8.5.1 The Warrawoona Group
    8.5.1.1 The Dresser Formation
    8.5.1.2 The Mount Ada Basalt
    8.5.1.3 The Apex Basalt
    8.5.1.4 The Panorama Formation
    8.5.2 The Strelley Pool Formation
    8.5.3 The Sulfur Springs Group
    8.5.4 The Gorge Creek Group and Others
    8.5.4.1 The Farrel Quartzite
    8.5.4.2 The Dixon Island Formation (Not Official)
    Column: Rare-Earth Elements and Significance of Shale (PAAS)-Normalization
    References
    Chapter 9 Overview of the Pilbara Microstructures 1: The Farrel Quartzite Assemblage
    9.1 Introduction
    9.2 Local Geology and Lithostratigraphy of the Goldsworthy Greenstone Belt
    9.2.1 Local Geology
    9.2.2 Overview of Lithostratigraphy
    9.3 Siliciclastic Unit (The Farrel Quartzite)
    9.3.1 Assignment to the Farrel Quartzite – Its Story and Remained Problem
    9.3.2 Lithostratigraphy and Sedimentary Geology
    9.3.3 Sources of Detrital Materials
    9.3.4 Detailed Descriptions of CE2
    9.3.4.1 Lithostratigraphy
    9.3.4.2 Petrography of Black Chert
    9.3.4.3 Rare- Earth Elements and Y Geochemistry
    9.4 The Chert- BIF Unit (The Cleaverville Formation)
    9.4.1 Lithostratigraphy and Petrography
    9.4.2 Rare-Earth Elements and Y Geochemistry
    9.5 Evolution of the Depositional Basin of the Farrel Quartzite – The Cleaverville Formation
    9.5.1 Lithostratigraphic Constraints
    9.5.2 Trace Element Constraints
    9.5.3 Depositional Environment of the Black Chert in CE2
    9.6 Fossil- Like Microstructures
    9.6.1 Spheroids
    9.6.1.1 Small Spheroids
    9.6.1.2 Large Spheroids
    9.6.2 Lenses
    9.6.3 Films
    9.6.4 Filaments
    Column: Evaporite
    References
    Chapter 10 Overview of the Pilbara Microstructures 2: The Strelley Pool Formation Assemblage
    10.1 Introduction
    10.2 The Panorama Greenstone Belt
    10.2.1 Local Geology and Lithostratigraphy
    10.2.2 Panorama Locality 1
    10.2.2.1 Lithostratigraphy and Petrography
    10.2.2.2 Fossil-Like Microstructures
    10.2.3 Panorama Locality 2
    10.2.3.1 Lithostratigraphy and Petrography
    10.2.3.2 Fossil-Like Microstructures
    10.2.4 Depositional Environment
    10.3 The Warralong Greenstone Belt
    10.3.1 Local Geology and Lithostratigraphy
    10.3.2 Petrography of Gray-Black Chert
    10.3.3 Depositional Environment
    10.3.4 Fossil-Like Microstructures
    10.4 The Goldsworthy Greenstone Belt
    10.4.1 Local Geology and Lithostratigraphy
    10.4.2 Lithofacies and Petrography of the Uppermost Cherty Unit
    10.4.3 Depositional Environment of the Uppermost Cherty Unit
    10.4.4 Fossil-Like Microstructures in the Massive Black Cherts
    10.4.4.1 Spheroids
    10.4.4.2 Lenses
    10.4.4.3 Filaments and Films
    10.4.5 Minor Occurrences of Fossil-Like Microstructures
    Column: Siliceous Sinter
    References
    Chapter 11 Biogenicity of the Pilbara Microstructures
    11.1 Introduction
    11.2 Geologic Context 1: Ages of Rocks
    11.2.1 The Farrel Quartzite
    11.2.2 The Strelley Pool Formation
    11.3 Geologic Context 2: Sedimentary Origin of Host Cherts
    11.4 Geologic Context 3: Primary Origin of Host Cherts
    11.5 Syngenicity
    11.6 Biogenicity
    11.6.1 Films
    11.6.2 Filaments
    11.6.3 Small Spheroids
    11.6.4 Large Spheroids
    11.6.4.1 Flexible- Walled Large Spheroids
    11.6.4.2 Robust and Thick- Walled Large Spherical Spheroid
    11.6.4.3 Robust- Walled Large Oblate Spheroids
    11.6.4.4 Robust and Thin- Walled Large Spherical Spheroids: The FQ Assemblage
    11.6.4.5 Robust and Thin- Walled Large Spherical Spheroids: The SPF Assemblage
    11.6.5 Lenses
    11.7 Refuting Objections
    11.7.1 Are Lenticular Microstructures Volcanic Vesicles or Those Microbially Colonized?
    11.7.1.1 Descriptions of Wacey’s Volcanic Vesicles Mimicking Microfossils
    11.7.1.2 Lenticular Microfossils Are Not Originated from Volcanic Vesicles
    11.7.1.3 Dresser Vesicles May Be Lenticular Microfossils
    11.7.2 Does the Farrel Quartzite Microfossil Assemblage Represent Soil Communities?
    11.7.2.1 Ambiguity of the Examined Locality
    11.7.2.2 Ambiguity of the Examined Materials
    11.7.2.3 Misunderstanding of Previous Studies and Incorrect Citations
    Column: Acritarchs
    References
    Chapter 12 Lifecycle and Mode of Life of the Pilbara Microfossils
    12.1 Introduction
    12.2 Reproduction Styles, Life Cycle, and Colony of Modern Microbes
    12.2.1 Alternative Reproduction Styles to Binary Fissions
    12.2.2 Morphological Change of Cells
    12.2.3 Morphology of Colonies
    12.3 Films
    12.4 Filaments
    12.5 Small Spheroids
    12.6 Large Spheroids
    12.6.1 Flexible-Walled Large Spheroids
    12.6.2 Robust and Thin-Walled Large Spherical Spheroids and Robust-walled Large Oblate Spheroid
    12.7 Lenses
    12.7.1 Variations in Morphology, Texture, and Colony
    12.7.1.1 Area, Oblateness, and Flange Width
    12.7.1.2 Symmetricity vs. Asymmetricity and Distortion
    12.7.1.3 Flange Fabrics
    12.7.1.4 Architectures of Colony
    12.7.2 Lifecycle and Reproduction Styles of Lenticular Microbes
    12.7.2.1 Simple Life Cycle with Binary Fission
    12.7.2.2 Multiple Fission with Baeocyte Formation
    12.7.2.3 Possible Asymmetric Division
    12.7.3 Morphometrics of Lenticular Microfossils
    12.7.3.1 Methodology
    12.7.3.2 Results of Morphometric Analyses
    12.7.3.3 Morphological Variations – Cell Growth and Taphonomy?
    12.7.3.4 Environmental Adaptation and Speciation of Lenticular Microbes
    12.7.4 Planktonic Mode of Life of Lenticular Microbes
    12.7.4.1 Methodology
    12.7.4.2 Parameters of Virtual Cells
    12.7.4.3 Sedimentation Simulation
    12.7.4.4 Effect of Flange and Flange Thickness
    12.7.4.5 Effect of Oblateness
    12.7.4.6 Summary
    Column: Thiomargarita and Big Bacteria
    References
    Chapter 13 Facts and Problems of the Pilbara Microfossils and Related Issues
    13.1 Introduction
    13.2 Cyanobacterial Microfossils in the Early Precambrian
    13.2.1 Records of Described Possible Cyanobacterial Microfossils
    13.2.2 Criteria for Cyanobacterial Microfossils
    13.3 Eukaryotic Fossils in the Early Precambrian
    13.3.1 Records of Eukaryotic Microfossils
    13.3.2 Criteria for Eukaryotic Microfossils
    13.3.3 Records of Eukaryotic Macrofossils
    13.4 Interpretation of the Pilbara Microfossil Assemblages
    13.4.1 Biological Affinity of Spheroid Microfossils
    13.4.2 Biological Affinity and Survival Strategy of Lenticular Microbes
    13.4.2.1 Possibility of Eukaryotic Affinities
    13.4.2.2 Survival Strategy and Evolutionary Ecology of Lenticular Microbes
    13.5 Future Directions of the Pilbara Microfossils
    13.5.1 Reexamination of Vertically to Subvertically Oriented Columnar Giant Crystals
    13.5.2 Potential of Biomarker Analyses of Microfossils
    13.5.3 Taxonomy of the Lenticular Microfossils and Life History of Lenticular Microbes
    Column: Endosymbiotic Theory
    References
    Index