Early lifewhat the first living things looked like
From the common ancestor to the three-domain tree: the first life, the rise of oxygen, endosymbiosis and the discovery of DNA's double helix.
On the Cosmic Calendar: Starts Sep 223.8 billion – 700 million years agoSee the full calendar
All life on Earth comes from one last universal common ancestor, LUCA, which lived 3.7 billion years ago. The tree of life then split for the first time into bacteria and archaea. 3 billion years ago cyanobacteria began releasing oxygen. 2.4 billion years ago the atmosphere contained oxygen and many anaerobic organisms died out. 2 billion years ago one cell swallowed another without digesting it, and mitochondria came from this.
The time range of this era is "3.8 billion – 700 million years ago", and its events run from the earliest common ancestor to a global ice age.
Nine events
- 3.7 billion years ago · LUCA: The last common ancestor of all life.
- 3.5 billion years ago · Bacteria and archaea: The tree of life splits for the first time.
- 3.5 billion years ago · Stromatolites: Microbial mats leave fossils.
- 3 billion years ago · Oxygenic photosynthesis: Cyanobacteria begin to release oxygen.
- 2.4 billion years ago · Great Oxidation Event: The atmosphere contains oxygen and many anaerobic organisms die out.
- 2 billion years ago · Mitochondrial endosymbiosis: One cell swallows another without digesting it.
- 1.8 billion years ago · Eukaryotic cells: Cells get a nucleus.
- 1.2 billion years ago · Sexual reproduction: Gene recombination speeds up evolution.
- 700 million years ago · Snowball Earth: Ice sheets cover almost the whole globe.
The common ancestor and the tree of life
Working backward from modern genes, the common ancestor of all life may have lived near deep-sea hydrothermal vents that were hot, oxygen-poor and rich in hydrogen (Weiss et al., Nature Microbiology, 2016). This study is about the physiology and habitat of the last universal common ancestor. Rocks in Greenland may preserve microbial structures 3.7 billion years old, but this reading is still disputed, so the uncertainty should be kept when citing it (Nutman et al., Nature, 2016). The paper's title stresses how rapidly life appeared.
A change in classification came from molecular comparison: comparing ribosomal RNA showed that what we called "bacteria" are really two quite different kinds of life, and archaea became a separate branch (Woese and Fox, PNAS, 1977). The tree of life was then redivided into three domains: Bacteria, Archaea and Eukarya (Woese, Kandler and Wheelis, PNAS, 1990). Lokiarchaeota, found in deep-sea sediments, carry many genes once thought to exist only in eukaryotes (Spang et al., Nature, 2015).
Oxygen and eukaryotic cells
Oxygen in the atmosphere did not arrive all at once. It rose over a long period, with setbacks, so the "Great Oxidation Event" should not be read as a change overnight (Lyons, Reinhard and Planavsky, Nature, 2014). Mitochondria and chloroplasts were once independent bacteria that became part of the cell after being swallowed. This theory was rejected by more than a dozen journals at the time (Lynn Margulis, published as Sagan, Journal of Theoretical Biology, 1967).
Sexual reproduction and Snowball Earth
Fossils of an ancient red alga show that sexual reproduction and multicellular life have a history of at least 1 billion years (Butterfield, Paleobiology, 2000). Rock layers in Namibia show that about 700 million years ago, Earth may have been almost completely covered in ice (Hoffman et al., Science, 1998).
The genetic material: DNA's double helix
A one-page paper proposed that the genetic material DNA is a double helix, and that base pairing hints at how genetic information is copied (Watson and Crick, Nature, 1953).
Want to read the originals? Search these titles
- Weiss et al. (2016): The physiology and habitat of the last universal common ancestor
- Nutman et al. (2016): Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures
- Woese and Fox (1977): Phylogenetic structure of the prokaryotic domain: The primary kingdoms
- Woese et al. (1990): Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya
- Spang et al. (2015): Complex archaea that bridge the gap between prokaryotes and eukaryotes
- Lyons et al. (2014): The rise of oxygen in Earth's early ocean and atmosphere
- Sagan (1967): On the origin of mitosing cells
- Butterfield (2000): Bangiomorpha pubescens n. gen., n. sp., a paper on sexual reproduction, multicellularity and the eukaryote radiation
- Hoffman et al. (1998): A Neoproterozoic snowball Earth
- Watson and Crick (1953): Molecular structure of nucleic acids: A structure for deoxyribose nucleic acid
How the game shows it
In the game, the Early life era has the resource cells, and its generators are Prokaryote fission, Chemosynthesis, Cyanobacterial photosynthesis and Horizontal gene transfer. They run from the simplest cell division, to living on chemical energy, to using light to make oxygen, and finally to genes moving between different organisms.
Real basis
LUCA (3.7 billion years ago): the last common ancestor of all life
Bacteria and archaea (3.5 billion years ago): the tree of life branches for the first time
Stromatolites (3.5 billion years ago): microbial mats leave fossils
Oxygenic photosynthesis (3 billion years ago): cyanobacteria begin releasing oxygen
Great Oxidation Event (2.4 billion years ago): the atmosphere gains oxygen, and many anaerobes die out
Mitochondrial endosymbiosis (2 billion years ago): one cell swallows another without digesting it
Eukaryotic cells (1.8 billion years ago): cells get a nucleus
Sexual reproduction (1.2 billion years ago): genetic recombination speeds up evolution
Snowball Earth (700 million years ago): ice sheets cover almost the whole globe
Related research
These studies relate to this topic but are not direct proof of this page.
A third kind of life: Comparing ribosomal RNA showed that “bacteria” are actually two very different kinds of life, and archaea became their own branch.
Source: Woese & Fox, PNAS 1977, "Phylogenetic structure of the prokaryotic domain: The primary kingdoms"
The three-domain system: The tree of life was redivided into three domains: Bacteria, Archaea and Eukaryotes.
Source: Woese, Kandler & Wheelis, PNAS 1990, "Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya"
Endosymbiotic theory: Margulis proposed that mitochondria and chloroplasts were once independent bacteria that were swallowed and became part of the cell. It was rejected by over a dozen journals.
Source: Sagan (Margulis), Journal of Theoretical Biology 1967, "On the origin of mitosing cells"
The home of LUCA: Working back from modern genes, the common ancestor of all life may have lived near hot, oxygen-free, hydrogen-rich deep-sea vents.
Source: Weiss et al., Nature Microbiology 2016, "The physiology and habitat of the last universal common ancestor"
Snowball Earth: Rock layers in Namibia show that about 700 million years ago Earth may have been almost completely covered in ice.
Source: Hoffman et al., Science 1998, "A Neoproterozoic snowball Earth"
The rise of oxygen: Oxygen in the atmosphere did not arrive all at once, but rose through a long, repeated process.
Source: Lyons, Reinhard & Planavsky, Nature 2014, "The rise of oxygen in Earth's early ocean and atmosphere"
The double helix: A one-page paper proposed that DNA is a double helix, and base pairing hinted at how genetic information is copied.
Source: Watson & Crick, Nature 1953, "Molecular structure of nucleic acids: A structure for deoxyribose nucleic acid"
Asgard archaea: Lokiarchaeota found in deep-sea sediments carry many genes once thought to exist only in eukaryotes.
Source: Spang et al., Nature 2015, "Complex archaea that bridge the gap between prokaryotes and eukaryotes"
The earliest sexual reproduction: Fossils of an ancient red alga show sexual reproduction and multicellular life have at least a billion years of history.
Source: Butterfield, Paleobiology 2000, "Bangiomorpha pubescens n. gen., n. sp.: implications for the evolution of sex, multicellularity, and the Mesoproterozoic/Neoproterozoic radiation of eukaryotes"
3.7-billion-year-old stromatolites: Rocks in Greenland may preserve microbial structures 3.7 billion years old, although this interpretation is still disputed.
Source: Nutman et al., Nature 2016, "Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures"
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