‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life

While most advances in the study of the origin of life on Earth (OoLoE) are piecemeal, tested against the laws of chemistry and physics, ultimately the goal is to develop an overall scenario for life’s origin(s). However, the dimensionality of non-equilibrium chemical systems, from the range of poss...

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Main Authors: Clifford F. Brunk, Charles R. Marshall
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Life
Subjects:
Online Access:https://www.mdpi.com/2075-1729/11/7/690
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author Clifford F. Brunk
Charles R. Marshall
author_facet Clifford F. Brunk
Charles R. Marshall
author_sort Clifford F. Brunk
collection DOAJ
description While most advances in the study of the origin of life on Earth (OoLoE) are piecemeal, tested against the laws of chemistry and physics, ultimately the goal is to develop an overall scenario for life’s origin(s). However, the dimensionality of non-equilibrium chemical systems, from the range of possible boundary conditions and chemical interactions, renders the application of chemical and physical laws difficult. Here we outline a set of simple criteria for evaluating OoLoE scenarios. These include the need for containment, steady energy and material flows, and structured spatial heterogeneity from the outset. The Principle of Continuity, the fact that all life today was derived from first life, suggests favoring scenarios with fewer non-analog (not seen in life today) to analog (seen in life today) transitions in the inferred first biochemical pathways. Top-down data also indicate that a complex metabolism predated ribozymes and enzymes, and that full cellular autonomy and motility occurred post-LUCA. Using these criteria, we find the alkaline hydrothermal vent microchamber complex scenario with a late evolving exploitation of the natural occurring pH (or Na<sup>+</sup> gradient) by ATP synthase the most compelling. However, there are as yet so many unknowns, we also advocate for the continued development of as many plausible scenarios as possible.
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spelling doaj.art-d71e125161924345ab6d2b040bdaf6642023-11-22T04:13:13ZengMDPI AGLife2075-17292021-07-0111769010.3390/life11070690‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of LifeClifford F. Brunk0Charles R. Marshall1Department of Ecology and Evolutionary Biology, University of California Los Angeles, Los Angeles, CA 90095-1606, USADepartment of Integrative Biology, Museum of Paleontology, University of California, Berkeley, CA 94720-4780, USAWhile most advances in the study of the origin of life on Earth (OoLoE) are piecemeal, tested against the laws of chemistry and physics, ultimately the goal is to develop an overall scenario for life’s origin(s). However, the dimensionality of non-equilibrium chemical systems, from the range of possible boundary conditions and chemical interactions, renders the application of chemical and physical laws difficult. Here we outline a set of simple criteria for evaluating OoLoE scenarios. These include the need for containment, steady energy and material flows, and structured spatial heterogeneity from the outset. The Principle of Continuity, the fact that all life today was derived from first life, suggests favoring scenarios with fewer non-analog (not seen in life today) to analog (seen in life today) transitions in the inferred first biochemical pathways. Top-down data also indicate that a complex metabolism predated ribozymes and enzymes, and that full cellular autonomy and motility occurred post-LUCA. Using these criteria, we find the alkaline hydrothermal vent microchamber complex scenario with a late evolving exploitation of the natural occurring pH (or Na<sup>+</sup> gradient) by ATP synthase the most compelling. However, there are as yet so many unknowns, we also advocate for the continued development of as many plausible scenarios as possible.https://www.mdpi.com/2075-1729/11/7/690origin of life scenariosalkaline hydrothermal vent microchambersprebiotic chemistryRNA worldInitial Darwinian Ancestor (IDA)LUCA
spellingShingle Clifford F. Brunk
Charles R. Marshall
‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
Life
origin of life scenarios
alkaline hydrothermal vent microchambers
prebiotic chemistry
RNA world
Initial Darwinian Ancestor (IDA)
LUCA
title ‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
title_full ‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
title_fullStr ‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
title_full_unstemmed ‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
title_short ‘Whole Organism’, Systems Biology, and Top-Down Criteria for Evaluating Scenarios for the Origin of Life
title_sort whole organism systems biology and top down criteria for evaluating scenarios for the origin of life
topic origin of life scenarios
alkaline hydrothermal vent microchambers
prebiotic chemistry
RNA world
Initial Darwinian Ancestor (IDA)
LUCA
url https://www.mdpi.com/2075-1729/11/7/690
work_keys_str_mv AT cliffordfbrunk wholeorganismsystemsbiologyandtopdowncriteriaforevaluatingscenariosfortheoriginoflife
AT charlesrmarshall wholeorganismsystemsbiologyandtopdowncriteriaforevaluatingscenariosfortheoriginoflife