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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Exobiology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (362 pages)
    Edition: 1st ed.
    ISBN: 9783319961750
    Series Statement: Advances in Astrobiology and Biogeophysics Series
    DDC: 576.839
    Language: English
    Note: Intro -- Foreword -- Preface -- Acknowledgements -- Contents -- Contributors -- Part I: Biosignatures on Earth -- Chapter 1: Chemical Biosignatures at the Origins -- 1.1 Introduction -- 1.2 Chemical Prerequisites -- 1.2.1 Liquid Water -- 1.2.2 Organic Molecules -- 1.2.2.1 Production of Organics in the Atmosphere -- 1.2.2.2 Submarine Hydrothermal Systems -- 1.2.2.3 Delivery of Extraterrestrial Organic Matter -- 1.3 Chemical Biosignatures -- 1.3.1 Over Representation of Organics -- 1.3.1.1 Titan -- 1.3.1.2 Alien Life on Earth -- 1.3.2 One-Handedness -- 1.3.2.1 Enantiomeric Excess Via a Chance Mechanism -- 1.3.2.2 Determinate Mechanisms -- 1.3.2.3 Extraterrestrial Homochirality -- 1.4 Conclusions -- References -- Chapter 2: Organic Matter in Interplanetary Dusts and Meteorites -- 2.1 Introduction -- 2.2 Cosmomaterials Inherited by Telluric Planets -- 2.2.1 Past and Present Flux of Extraterrestrial Matter -- 2.2.2 Cosmomaterials in Earth Collections -- 2.2.3 Post-Accretion Processes on the Parent Body -- 2.3 Diversity and Complexity of Organics in Meteorites -- 2.3.1 Soluble Organic Matter -- 2.3.2 Insoluble Organic Matter -- 2.4 Organic Matter in Stratospheric IDPs and AMMs -- 2.5 Origin and Formation of Organics in Chondrites and Dust -- 2.6 Dust and Meteorites at the Surface of Mars -- 2.6.1 Flux of Exogenous Matter on Mars -- 2.6.2 Exogenous Organics on Mars: Detection and Preservation -- References -- Chapter 3: Biosignatures of Cellular Components and Metabolic Activity -- 3.1 Introduction -- 3.1.1 Biosignatures -- 3.1.2 Concepts of Life -- 3.1.3 Attributes of Life -- 3.2 Organic Molecular Biosignatures -- 3.2.1 Membrane Polar Lipids -- 3.2.2 Cyclic Triterpenoids -- 3.2.3 Modern Microbial Mat Ecosystems as Analogs for Life on the Early Earth -- 3.2.4 Linking Geological and Biological Records. , 3.3 Stable Isotope Abundance Patterns as Biosignatures -- 3.3.1 Stable Isotope Basics -- 3.3.2 Carbon Compounds and Microbial Metabolism -- 3.3.2.1 Isotopic Discrimination by Autotrophic Carbon Fixation -- 3.3.2.2 Isotopic Fractionation Within Intermediary Metabolism -- 3.3.2.3 Isotopic Compositions of Individual Lipids -- 3.3.2.4 Carbon Isotopic Abundance Patterns Within Molecules -- 3.3.3 Reduced Carbon and Carbonates in Sedimentary Rocks -- 3.3.3.1 Carbon Biogeochemical Cycles and the Ancient Rock Record -- 3.3.3.2 Early Isotopic Record in Reduced Carbon and Carbonates -- 3.3.4 Isotopic Patterns Arising from Biological Redox Reactions -- 3.3.4.1 Sulfur -- 3.3.4.2 Metals -- 3.4 Final Comments -- References -- Chapter 4: The Deep Subseafloor and Biosignatures -- 4.1 The Deep Biosphere: An Unseen World of Contrasting Habitats -- 4.1.1 Definition -- 4.1.2 Environmental Conditions of Subsurface Environments -- 4.1.2.1 Temperature and Pressure -- 4.1.2.2 Activity of Water and Porosity -- 4.1.2.3 Energy Sources -- 4.2 Tools to Detect Subsurface Biosignatures -- 4.2.1 Contamination Issues -- 4.2.2 Sensitive Analytical Methods -- 4.3 Microbiology of Subsurface Sediments Using the Canterbury Basin (CB) as a Case Study -- 4.3.1 Drilling Expeditions and Environmental Context -- 4.3.2 Cell Abundance -- 4.3.2.1 The Canterbury Basin Subseafloor Case Study -- 4.3.3 Evolution of Diversity with Depth -- 4.4 Activity Versus Viability -- 4.4.1 The Canterbury Basin Subseafloor Case Study -- 4.5 Possible Metabolisms -- 4.5.1 The Canterbury Basin Subseafloor Case Study -- 4.6 Physiological Potential -- 4.6.1 The Canterbury Basin Subseafloor Case Study -- References -- Chapter 5: A Systematic Way to Life Detection: Combining Field, Lab and Space Research in Low Earth Orbit -- 5.1 Introduction. , 5.2 Promising Locations in the Solar System for Life Detection: Mars, Europa and Enceladus -- 5.2.1 The Search for Habitable Worlds -- 5.2.2 Promising Potentially Habitable Targets of Relevance to Life Detection Missions -- 5.3 Finding Stable and Space-Resistant Biomolecules as Potential Biosignatures -- 5.3.1 The Content of a Life Detection Database -- 5.3.2 Low Earth Orbit Missions Supporting Exploration Missions to Search for Life -- 5.4 Relevance to Biosignature, Bio-Trace and Bio-Fingerprint Research -- 5.5 Experimental Approach -- 5.6 Analysis Strategy and Biosignature Database Concept -- References -- Chapter 6: Mineralogical Identification of Traces of Life -- 6.1 Introduction -- 6.2 How Does Life Influence the Formation of Minerals? -- 6.2.1 Impact of Life on Solution Saturation -- 6.2.2 Impact of Organic Molecules on Crystal Nucleation and Growth -- 6.2.3 Extracellular Versus Intracellular Biomineralization -- 6.3 Examples of Biominerals with Particular Physico-Chemical and Structural Properties -- 6.3.1 Genetic Control Over Biomineral Properties: Example of Magnetite Formed by Magnetotactic Bacteria (MTB) -- 6.3.2 Properties of Extracellular and Cell Wall-Associated Iron Biominerals -- 6.4 The Loss of the Biological Information Contained by Biominerals Upon Ageing -- 6.4.1 Structural Alteration of Biominerals in Natural Settings -- 6.4.2 (Geo)chemical Alteration of Biominerals in Natural Settings -- 6.4.3 Constraining Biomineral Ageing Processes in the Laboratory -- 6.5 The Thin Frontier Between Biominerals and Abiotic Minerals -- 6.5.1 Biogenic and Abiotic Framboidal Pyrite -- 6.5.2 Twisted Stalks -- 6.6 Conclusions -- References -- Chapter 7: Biosignatures in Deep Time -- 7.1 Introduction -- 7.2 Ancient Biosignatures from the Early-Mid Archaean Eon. , 7.2.1 Graphitic Biosignatures from Highly Metamorphosed Sediments from the 3.95 Uivak-Iquluk Gneiss, Labrador and Greenland -- 7.2.1.1 The 3.95 Uivak-Iqaluk Gneiss, Labrador -- 7.2.1.2 Greenland -- 7.2.2 Biosignatures from the 3.5-3.0 Ga Pilbara Greenstone Belt -- 7.2.2.1 The 3.43 Ga Strelley Pool Formation -- 7.2.2.2 The 3.46 Ga Apex Chert: A Contentious Case -- 7.2.2.3 The Kitty´s Gap Microfossils: Chemotrophic Fossil Colonies -- 7.2.3 Biosignatures of the 3.5-3.2 Ga Barberton Greenstone Belt -- 7.2.3.1 The 3.42 Ga Buck Reef Chert: Photosynthetic Fossil Biofilms -- 7.2.3.2 The 3.33 Ga Josefsdal Chert: Chemotrophic Fossil Biofilms -- 7.2.3.3 The 3.2 Ga Moodies Group -- 7.3 Significance of Early Earth Microorganisms for the Search for Extraterrestrial Life -- 7.4 Conclusions -- References -- Part II: Biosignatures in Space -- Chapter 8: The Search for Biosignatures in Martian Meteorite Allan Hills 84001 -- 8.1 Introduction -- 8.2 Petrologic Context for Claims of Biologic Activity -- 8.3 Biogenic Carbonates? -- 8.4 Biogenic Magnetite and Sulphide? -- 8.5 Biological Organic Matter? -- 8.6 Microfossils and Related Biogenic Structures? -- 8.7 Summary and Lessons Learned -- References -- Chapter 9: Role of Mineral Surfaces in Prebiotic Processes and Space-Like Conditions -- 9.1 Introduction -- 9.2 Role of Minerals in the Prebiotic Context -- 9.2.1 Adsorption Processes -- 9.2.2 Catalysis -- 9.3 Role of Minerals in the Context of Space Missions -- 9.3.1 Mission Instruments to Detect Biomarkers in Space -- 9.3.2 Future Exploration of Mars -- 9.3.3 Laboratory Studies to Support Life Detection Investigations -- 9.4 Conclusions -- References -- Chapter 10: Photochemistry and Photoreactions of Organic Molecules in Space -- 10.1 Why Are We Interested in Radiation Chemistry for Biosignatures? -- 10.2 Modes of Production and Delivery of Organic Material. , 10.2.1 Endogenous Delivery -- 10.2.2 Exogenous Delivery -- 10.2.2.1 Extraterrestrial Delivery -- 10.3 Radiation Studies on Earth versus Space -- 10.4 Space Experiments Relevant to Exposure of Organics -- 10.5 Conclusions and Perspectives -- References -- Chapter 11: Exoplanetary Biosignatures for Astrobiology -- 11.1 Introduction -- 11.2 Challenges of Defining Life and Its Needs -- 11.3 Preparing a Planetary Target List for Biosignature Assessment -- 11.3.1 Steps to Forming an Earth-Like Planet -- 11.3.2 Habitability and the Habitable Zone (HZ) -- 11.3.2.1 Classical HZ -- 11.3.2.2 Non-Classical HZ -- 11.3.3 HZ Around M-Dwarf Stars -- 11.3.4 Exoplanet Missions Providing Planetary Targets -- 11.4 Remote Biosignature Techniques -- 11.5 Spectroscopic Exoplanetary Biosignatures -- 11.5.1 Reflectivity Increase with Wavelength -- 11.5.2 Isotopic Ratios -- 11.5.3 Gas-Phase Species as Biosignatures -- 11.5.3.1 Modern Earth -- 11.5.3.2 Early Earth -- 11.5.3.3 Solar System -- 11.5.3.4 Earth-Like Exoplanets -- 11.5.4 Atmospheric Redox Disequilibrium as a Biosignature -- 11.5.5 Additional Atmospheric Biosignatures -- 11.5.5.1 Species Containing Sulphur -- 11.5.5.2 Chloromethane -- 11.6 Earth-Like Planets Without Life (`Dead Earths´) -- 11.7 Discussion and Conclusions -- References -- Part III: Biosignatures, Instruments and Missions -- Chapter 12: The Enigma of Methane on Mars -- 12.1 Observations -- 12.2 Methane Production -- 12.3 Methane Loss -- 12.4 Open Questions and Future Measurements -- References -- Chapter 13: Detection of Biosignatures Using Raman Spectroscopy -- 13.1 Introduction -- 13.2 Raman Effect and Instrumentation -- 13.3 Biosignatures Raman Detection -- 13.3.1 Organic Molecules -- 13.3.2 Pigments -- 13.3.3 Carbonaceous Matter and Microfossils -- 13.3.4 Minerals and Microfossils -- 13.3.5 Living Organisms -- 13.4 Summary -- References. , Chapter 14: Searching for Signs of Life on Other Planets: Mars a Case Study.
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  • 2
    Online Resource
    Online Resource
    Cham : Springer International Publishing
    Keywords: Biochemistry ; Paleontology  ; Microbiology ; Mineralogy ; Biology-Philosophy ; Astrobiology ; Astrobiology ; Biochemistry ; Paleontology  ; Microbiology ; Mineralogy ; Biology-Philosophy
    Description / Table of Contents: This book aims at providing a brief but broad overview of biosignatures. The topics addressed range from prebiotic signatures in extraterrestrial materials to the signatures characterising extant life as well as fossilised life, biosignatures related to space, and space flight instrumentation to detect biosignatures either in situ or from orbit. The book ends with philosophical reflections on the implications of life elsewhere. In the 15 chapters written by an interdisciplinary team of experts, it provides both detailed explanations on the nature of biosignatures as well as useful case studies showing how they are used and identified in ancient rocks, for example. One case study addresses the controversial finding of traces of fossil life in a meteorite from Mars. The book will be of interest not only to astrobiologists but also to terrestrial paleontologists as well as any reader interested in the prospects of finding a second example of life on another planet
    Type of Medium: Online Resource
    Pages: Online-Ressource (XXIV, 347 p. 64 illus., 37 illus. in color, online resource)
    ISBN: 9783319961750
    Series Statement: Advances in Astrobiology and Biogeophysics
    Language: English
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Franchi, Fulvio; Hofmann, Axel; Cavalazzi, Barbara; Wilson, Allan; Barbieri, Roberto (2015): Differentiating marine vs hydrothermal processes in Devonian carbonatemounds using rare earth elements (Kess Kess mounds, Anti-Atlas, Morocco). Chemical Geology, 409, 69-86, https://doi.org/10.1016/j.chemgeo.2015.05.006
    Publication Date: 2023-01-13
    Description: Petrological and geochemical analyses were carried out on Early Devonian Kess Kess mound limestones of the Seheb el Rhassel Group exposed in the Hamar Laghdad Ridge (Tafilalt Platform, Eastern Anti-Atlas, Morocco) in order to evaluate marine vs hydrothermal processes for the origin of the mounds. Hydrothermal fluid circulation affected limestone deposition resulting in the formation of a plumbing system preserved in the mound facies and inter-mound facies as cavities, veins, and dykes. Shale-normalized rare earth element (REE) patterns for limestones display pronounced light REE depletion compared to middle REE (average PrSN / DySN = 0.46) and heavy REE (average PrSN / YbSN = 0.55), a super-chondritic Y/Ho ratio (up to 87) and positive La anomaly consistent with precipitation from normal marine seawater. Within our data set the Ce anomaly, as well as U and other trace element concentrations vary with facies providing evidence for variable redox conditions. The presence of positive Ce anomaly in carbonates of the plumbing system is consistent with precipitation under anoxic condition. Samples from mound facies and quartz veinlets in the upper part of the group show REE patterns consistent with precipitation from hydrothermal fluids. Early Devonian hypothetical seawater REE patterns were calculated from samples showing normal marine REE patterns (i.e. inter-mound facies) and from samples with weaker marine signature (i.e. fossiliferous mound limestones and plumbing system deposits). Hypothetical patterns are slightly enriched in SumREE compared to modern open ocean seawater. This study reveals that REE analysis is a powerful tool for understanding polygenetic carbonate systems. It sheds light into the genesis of the Kess Kess mounds by reconstructing fluid pathways and palaeo-redox conditions.
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2023-01-13
    Keywords: Anti-Atlas, Morocco; Description; Event label; Kess-Kess_Mounts-05; Kess-Kess_Mounts-06; Kess-Kess_Mounts-12; KK12; KK5; KK6; Lithology/composition/facies; Minerals; Optional event label; Provenance/source
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 5
    Publication Date: 2023-01-13
    Keywords: Analytical method; Anti-Atlas, Morocco; Cerium/Cerium ratio; Event label; Kess-Kess_Mounts-01; Kess-Kess_Mounts-02; Kess-Kess_Mounts-05; Kess-Kess_Mounts-06; Kess-Kess_Mounts-07; Kess-Kess_Mounts-08; Kess-Kess_Mounts-09; Kess-Kess_Mounts-10; Kess-Kess_Mounts-11; Kess-Kess_Mounts-12; Kess-Kess_Mounts-20; Kess-Kess_Mounts-21; Kess-Kess_Mounts-25; KK1; KK10; KK11; KK12; KK2; KK20; KK21; KK25; KK5; KK6; KK7; KK8; KK9; Light rare-earth elements; Optional event label; Rare-earth elements; Ratio; Yttrium/Holmium ratio; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
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  • 6
    Publication Date: 2023-01-13
    Keywords: Aluminium oxide; Anti-Atlas, Morocco; Calcium oxide; Calculated from weight loss after ignition at 450 °C; Event label; Iron oxide, Fe2O3; Kess-Kess_Mounts-01; Kess-Kess_Mounts-02; Kess-Kess_Mounts-05; Kess-Kess_Mounts-06; Kess-Kess_Mounts-07; Kess-Kess_Mounts-08; Kess-Kess_Mounts-09; Kess-Kess_Mounts-10; Kess-Kess_Mounts-11; Kess-Kess_Mounts-12; Kess-Kess_Mounts-20; Kess-Kess_Mounts-21; Kess-Kess_Mounts-25; KK1; KK10; KK11; KK12; KK2; KK20; KK21; KK25; KK5; KK6; KK7; KK8; KK9; Loss on ignition; Magnesium oxide; Manganese oxide; Optional event label; Potassium oxide; Silicon dioxide; Sodium oxide; Titanium dioxide; Total
    Type: Dataset
    Format: text/tab-separated-values, 111 data points
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  • 7
    Publication Date: 2023-01-13
    Keywords: Anti-Atlas, Morocco; Arsenic; Barium; Cerium; Chromium; Cobalt; Comment; Copper; Dysprosium; Erbium; Europium; Event label; Gadolinium; Gallium; Holmium; Kess-Kess_Mounts-01; Kess-Kess_Mounts-02; Kess-Kess_Mounts-05; Kess-Kess_Mounts-06; Kess-Kess_Mounts-07; Kess-Kess_Mounts-08; Kess-Kess_Mounts-09; Kess-Kess_Mounts-10; Kess-Kess_Mounts-11; Kess-Kess_Mounts-12; Kess-Kess_Mounts-20; Kess-Kess_Mounts-21; Kess-Kess_Mounts-25; KK1; KK10; KK11; KK12; KK2; KK20; KK21; KK25; KK5; KK6; KK7; KK8; KK9; Lanthanum; Lead; Lithium; Lutetium; Neodymium; Nickel; Optional event label; Phosphorus; Praseodymium; Rare-earth elements; Rubidium; Samarium; Scandium; Strontium; Terbium; Thorium; Thulium; Titanium; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 530 data points
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  • 8
    Publication Date: 2023-01-13
    Keywords: Anti-Atlas, Morocco; Area/locality; Description; Event label; Kess-Kess_Mounts-01; Kess-Kess_Mounts-02; Kess-Kess_Mounts-05; Kess-Kess_Mounts-06; Kess-Kess_Mounts-07; Kess-Kess_Mounts-08; Kess-Kess_Mounts-09; Kess-Kess_Mounts-10; Kess-Kess_Mounts-11; Kess-Kess_Mounts-12; Kess-Kess_Mounts-14; Kess-Kess_Mounts-15; Kess-Kess_Mounts-16; Kess-Kess_Mounts-19; Kess-Kess_Mounts-20; Kess-Kess_Mounts-21; Kess-Kess_Mounts-22; Kess-Kess_Mounts-23; Kess-Kess_Mounts-24; Kess-Kess_Mounts-25; KK1; KK10; KK11; KK12; KK14; KK15; KK16; KK19; KK2; KK20; KK21; KK22; KK23; KK24; KK25; KK5; KK6; KK7; KK8; KK9; Lithology/composition/facies; Main Lithology; Optional event label; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 9
    Publication Date: 2020-02-19
    Description: We constrained the origin and genetic environment of modern iron ooids (sand-sized grains with a core and external cortex of concentric laminae) providing new tools for the interpretation of their fossil counterparts as well as the analogous particles discovered on Mars. Here, we report an exceptional, unique finding of a still active deposit of submillimetric iron ooids, under formation at the seabed at a depth of 80 m over an area characterized by intense hydrothermal activity off Panarea, a volcanic island north of Sicily (Italy). An integrated analysis, carried out by X-ray Powder Diffraction, Environmental Scanning Electron Microscopy, X-ray Fluorescence and Raman spectroscopy reveals that Panarea ooids are deposited at the seafloor as concentric laminae of primary goethite around existing nuclei. The process is rapid, and driven by hydrothermal fluids as iron source. A sub-spherical, laminated structure resulted from constant agitation and by degassing of CO2-dominated fluids through seafloor sediments. Our investigations point the hydrothermal processes as responsible for the generation of the Panarea ooids, which are neither diagenetic nor reworked. The presence of ooids at the seawater-sediments interface, in fact, highlights how their development and growth is still ongoing. The proposed results show a new process responsible for ooids formation and gain a new insight into the genesis of iron ooids deposits that are distributed at global scale in both modern and past sediments.
    Description: Published
    Description: id 7107
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2020-02-19
    Description: A variety of calcareous and siliceous skeletal components are associated with exceptional, still active deposits of modern iron ooids off Panarea, one of the volcanic islands of the Aeolian Arc (Tyrrhenian Sea, Italy). Both ooids and skeletal components occur as loose sediments influenced by submarine hydrothermal fluid vents. Whereas iron ooids are exclusively made of goethite laminae primarily nucleated on volcaniclastic material, sponge spicules – that represent most of the siliceous skeletal component – develop laminated coatings (concretions) of varying sizes. This partial or total coating consists of regularly banded Fe‒rich layers exhibiting the same textural features and mineralogical composition (goethite) of the ooid cortex developed around inorganic cores. Spicules did not reveal any obvious attaching structure or interfingering with the surrounding coating and did not undergo bioerosion or any other evidence of biological intervention during their development. A hydrothermal origin, compatible with the general setting, is therefore proposed for these armoured sponge spicules. We believe that this unique modern case of iron concretions produced on siliceous spicules can contribute to explain other known fossil cases as well as to understand the taphonomy of this type of biogenic silica that seems rarely to have been preserved in such an extreme habitat.
    Description: Published
    Description: 109379
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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