Abstract

Charles Darwin’s original intuition that life began in a “warm little pond” has for the last three decades been eclipsed by a focus on marine hydrothermal vents as a venue for abiogenesis. However, thermodynamic barriers to polymerization of key molecular building blocks and the difficulty of forming stable membranous compartments in seawater suggest that Darwin’s original insight should be reconsidered. I will introduce the terrestrial origin of life hypothesis, which combines field observations and laboratory results to provide a novel and testable model in which life begins as protocells assembling in inland fresh water hydrothermal fields. Hydrothermal fields are associated with volcanic landmasses resembling Hawaii and Iceland today and could plausibly have existed on similar land masses rising out of Earth’s first oceans. I will report on a field trip to the living and ancient stromatolite fossil localities of Western Australia, which provided key insights into how life may have emerged in Archaean, fluctuating fresh water hydrothermal pools, geological evidence for which has recently been discovered. Laboratory experimentation and fieldwork are providing mounting evidence that such sites have properties that are conducive to polymerization reactions and generation of membrane-bounded protocells. I will build on the previously developed coupled phases scenario, unifying the chemical and geological frameworks and proposing that a hydrogel of stable, communally supported protocells will emerge as a candidate Woese progenote, the distant common ancestor of microbial communities so abundant in the earliest fossil record.

Highlights

  • Most workers investigating the origin of life confine their horizons to theoretical papers, computational models or laboratory simulations that use a narrow spectrum of commercial reagents reacting in buffered aqueous solutions

  • A field trip in Western Australia to venues ranging from living marine stromatolites to inland

  • A novel terrestrial origin of life hypothesis was developed through the unification of chemical and geological settings

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Summary

Introduction

Most workers investigating the origin of life confine their horizons to theoretical papers, computational models or laboratory simulations that use a narrow spectrum of commercial reagents reacting in buffered aqueous solutions. The results are related to prebiotic conditions with the assumption that laboratory or in silico results can plausibly occur in the early Earth environment. A complementary approach is to visit sites that are analogs to candidate venues for biogenesis. Such fieldwork broadens our perspective by providing a more realistic assessment of the actual conditions in which physical and chemical reactions progressed toward life’s beginning approximately four billion years ago. Geologists familiar with the most ancient, Archaean fossil sites can interpret the rock record and provide knowledgeable advice about geochemical conditions to guide model building and laboratory experiments

A Field Trip in Deep Time to the Archaean
Routetaken taken from
LivingThe
Fossil
AAnovel novelModel
Linking Chemical Reactions to the Physical Properties of Hydrothermal Pools
A Gel Phase as Candidate Progenote
A Gel Phase as Candidate
The Adaptive Radiation of the Progenote
Summary of Novel Features and Testable Predictions of the Model
10. Conclusions

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