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Early life on land and the first terrestrial ecosystems

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TLDR
The rapid adaptations seen in modern terrestrial microbes, their outstanding tolerance to extreme and fluctuating conditions, their early and rapid diversification, and their old fossil record collectively suggest that they constituted the earliest terrestrial ecosystems, at least since the Neoarchean, further succeeding on land and forming a biomass-rich cover with mature soils where plant-dominated ecosystems later evolved.
Abstract
Terrestrial ecosystems have been largely regarded as plant-dominated land surfaces, with the earliest records appearing in the early Phanerozoic ( 3,400 Ma-old paleosols endorses the idea that life on land perhaps occurred in parallel with aquatic life back in the Paleoarchean. The rapid adaptations seen in modern terrestrial microbes, their outstanding tolerance to extreme and fluctuating conditions, their early and rapid diversification, and their old fossil record collectively suggest that they constituted the earliest terrestrial ecosystems, at least since the Neoarchean, further succeeding on land and forming a biomass-rich cover with mature soils where plant-dominated ecosystems later evolved. Understanding how life diversified and adapted to non-aquatic conditions from the actualistic and paleontological perspective is critical to understanding the impact of life on the Earth’s systems over thousands of millions of years.

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Journal ArticleDOI

Earliest signs of life on land preserved in ca. 3.5 Ga hot spring deposits

TL;DR: New discoveries of hot spring deposits including geyserite, sinter terracettes and mineralized remnants of hot springs pools/vents are presented, all of which preserve a suite of microbial biosignatures indicative of the earliest life on land.

Global Patterns in Bacterial Diversity

TL;DR: This work reports the most comprehensive analysis of the environmental distribution of bacteria to date, based on 21,752 16S rRNA sequences compiled from 111 studies of diverse physical environments, and finds that sediments are more phylogenetically diverse than any other environment type.
Journal ArticleDOI

Phylogenomic Analyses Indicate that Early Fungi Evolved Digesting Cell Walls of Algal Ancestors of Land Plants

TL;DR: Shared pectinases of Dikarya and Gonapodya provide evidence that even ancient aquatic fungi had adapted to extract nutrients from the plants in the green lineage, and imply the geological timing of the plant–fungus association is 750 million years old.
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Interpreting carbonate and organic carbon isotope covariance in the sedimentary record

TL;DR: Paired carbonate and organic δ(13)C records are presented that exhibit a coupled negative excursion resulting from multiple periods of meteoric alteration of the carbonateδ( 13)C record, and consequent contributions of isotopically negative terrestrial organic matter to the sedimentary record.
References
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Book

The nature and properties of soils

Nyle C. Brady, +1 more
TL;DR: The nature and properties of soils are studied to establish an understanding of the phytochemical properties of soil and how these properties change over time.
Book

Brock Biology of Microorganisms

TL;DR: A six-part presentation covers principles of microbiology; evolutionary microbiology and microbial diversity; metabolic diversity and microbial ecology; immunology, pathogenicity, and host responses; microbial diseases; andmicroorganisms as tools for industry and research.
Journal ArticleDOI

A Molecular View of Microbial Diversity and the Biosphere

TL;DR: Over three decades of molecular-phylogenetic studies, researchers have compiled an increasingly robust map of evolutionary diversification showing that the main diversity of life is microbial, distributed among three primary relatedness groups or domains: Archaea, Bacteria, and Eucarya.
Journal ArticleDOI

Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate

TL;DR: The iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production, is reviewed.
Journal ArticleDOI

Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets

TL;DR: This model not only naturally explains the Late Heavy Bombardment, but also reproduces the observational constraints of the outer Solar System.
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