Early Earth

Early Earth

On early earth, the prokaryotes faced overpopulation and food shortage. After a mass extinction, some learnt to capture light in a molecular net, and use it as food. Others learnt to eat the dead bodies of other cells. Again they flourished. The cells did not understand what they did or what it would lead to; they just did, and it happened to work for some of them.

The next problem was waste. Oxygen was a waste product from living cells, and it became so prevalent that it invaded and disrupted all spheres of the earth, including the life that created it. Some cells learnt to seize this oxygen, and turn it to its own purposes. The ones that did now had ten times the energy.

Place of emergence

It is often said that all the conditions for the first production of a living organism are now present, which could ever have been present. But if (and oh! what a big if!) we could conceive in some warm little pond, with all sorts of ammonia and phosphoric salts, light, heat, electricity, &c., present, that a proteine compound was chemically formed ready to undergo stillmore complex changes, at the present day such matter would be instantly devoured or absorbed, which would not have been the case before living creatures were formed.

Another way of asking about the origin of life is to ask when chemistry became biochemistry.

The most plausible site for the origin of life was not the open ocean or dry land. Instead, there is reason to think that the most conducive conditions for life to begin were places where liquid water and the early atmosphere encountered mineral surfaces such as volcanic rocks. We call the contact between liquid, solid, and gas an interface. As you will see, interfaces have special properties because they allow certain essential processes to occur that do not happen anywhere else: wet-dry cycles, concentration and dilution, formation of compartments, and combinatorial chemistry.
Cycles: The local environment probably resembled pools in volcanic sites where hot water constantly goes through cycles of wetting and drying. We call this a fluctuating environment. The pools contained complex mixtures of dilute organic compounds from a variety of sources, including extraterrestrial material delivered during the last stages Earth's formation, and other compounds produced by chemical reactions associated with volcanoes and atmospheric reactions. Because of their fluctuating environment, the compounds underwent continuous cycles in which they were dried and concentrated, then diluted upon rewetting.
Compartments: During the drying cycle, the dilute mixtures formed very thin films on mineral surfaces—a process that is necessary for chemical reactions to occur. Not only did the compounds react with one another under these conditions, but the products of the Reactions became encapsulated in microscopic compartments by membranes that self-assembled from soaplike organic compounds called amphiphiles. This process resulted in vast numbers of protocells that appeared all over early Earth, wherever water solutions were undergoing wet-dry cycles in volcanic environments similar to today's Hawaii or Iceland.
Combinatorial chemistry: The protocells represented compartmented systems of molecules. each different in composition from the next. and each representing a kind of microscopic natural experiment. Most of the protocells remained inert, but a few happened to contain a mixture that could be driven toward greater complexity by capturing energy and smaller molecules from outside the encapsulated volume. As the smaller molecules were transported into the internal compartment, energy was used to link them into long chains.

Deep sea vents

Meet Luca, the Ancestor of All Living Things** By NICHOLAS WADE JULY 25, 2016

William F. Martin says that the Last Universal Common Ancestor can be traced back to deep sea vents like this one off the Galápagos. Credit Universal History Archive/UIG, via Getty Images

A surprisingly specific genetic portrait of the ancestor of all living things has been generated by scientists who say that the likeness sheds considerable light on the mystery of how life first emerged on Earth.

This venerable ancestor was a single-cell, bacterium-like organism. But it has a grand name, or at least an acronym. It is known as Luca, the Last Universal Common Ancestor, and is estimated to have lived some four billion years ago, when Earth was a mere 560 million years old.

The new finding sharpens the debate between those who believe life began in some extreme environment, such as in deep sea vents or the flanks of volcanoes, and others who favor more normal settings, such as the “warm little pond” proposed by Darwin.

The nature of the earliest ancestor of all living things has long been uncertain because the three great domains of life seemed to have no common point of origin. The domains are those of the bacteria, the archaea and the eukaryotes. Archaea are bacteria-like organisms but with a different metabolism, and the eukaryotes include all plants and animals.

Specialists have recently come to believe that the bacteria and archaea were the two earliest domains, with the eukaryotes emerging later. That opened the way for a group of evolutionary biologists, led by William F. Martin of Heinrich Heine University in Düsseldorf, Germany, to try to discern the nature of the organism from which the bacterial and archaeal domains emerged.

Their starting point was the known protein-coding genes of bacteria and archaea. Some six million such genes have accumulated over the last 20 years in DNA databanks as scientists with the new decoding machines have deposited gene sequences from thousands of microbes.

Genes that do the same thing in a human and a mouse are generally related by common descent from an ancestral gene in the first mammal. So by comparing their sequence of DNA letters, genes can be arranged in evolutionary family trees, a property that enabled Dr. Martin and his colleagues to assign the six million genes to a much smaller number of gene families. Of these, only 355 met their criteria for having probably originated in Luca, the joint ancestor of bacteria and archaea.

Genes are adapted to an organism’s environment. So Dr. Martin hoped that by pinpointing the genes likely to have been present in Luca, he would also get a glimpse of where and how Luca lived. “I was flabbergasted at the result, I couldn’t believe it,” he said.

The 355 genes pointed quite precisely to an organism that lived in the conditions found in deep sea vents**, the gassy, metal-laden, intensely hot plumes caused by seawater interacting with magma erupting through the ocean floor.

Deep sea vents are surrounded by exotic life-forms and, with their extreme chemistry, have long seemed places where life might have originated. The 355 genes ascribable to Luca include some that metabolize hydrogen as a source of energy as well as a gene for an enzyme called reverse gyrase, found only in microbes that live at extremely high temperatures, Dr. Martin and colleagues reported Monday in Nature Microbiology.

The finding has “significantly advanced our understanding of what Luca did for a living,” James O. McInerney of the University of Manchester wrote in a commentary, and provides “a very intriguing insight into life four billion years ago.”

Dr. Martin’s portrait of Luca seems likely to be widely admired. But he has taken a further step that has provoked considerable controversy. He argues that Luca is very close to the origin of life itself. The organism is missing so many genes necessary for life that it must still have been relying on chemical components from its environment. Hence it was only “half alive,” he writes.

The fact that Luca depended on hydrogen and metals favors a deep sea vent environment for the origin of life, Dr. Martin concludes, rather than the land environment posited in a leading rival theory proposed by the chemist John Sutherland of the University of Cambridge in England.

Others believe that the Luca that Dr. Martin describes was already a highly sophisticated organism that had evolved far beyond the origin of life, meaning the formation of living systems from the chemicals present on the early Earth.

Luca and the origin of life are “events separated by a vast distance of evolutionary innovation,” said Jack Szostak of Massachusetts General Hospital, who has studied how the first cell membranes might have evolved.

From Dr. Martin’s data, it is clear that Luca could manage the complicated task of synthesizing proteins. So it seems unlikely that it could not also synthesize simpler components, even though the genes for doing so have not yet been detected, said Steven A. Benner of the Foundation for Applied Molecular Evolution. “It’s like saying you can build a 747 but can’t refine iron.”

Dr. Sutherland too gave little credence to the argument that Luca might lie in some gray transition zone between nonlife and life just because it depended on its environment for some essential components. “It’s like saying I’m half alive because I depend on my local supermarket.”

Dr. Sutherland and others have no quarrel with Luca’s being traced back to deep sea vents. But that does not mean life originated there, they say. Life could have originated anywhere and later been confined to a deep sea environment because of some catastrophic event like the Late Heavy Bombardment, which occurred 4 billion to 3.8 billion years ago. This was a rain of meteorites that crashed into Earth with such force that the oceans were boiled off into an incandescent mist.

Life is so complex it seems to need many millions of years to evolve. Yet evidence for the earliest life dates to 3.8 billion years ago, as if it emerged almost the minute the bombardment ceased. A refuge in the deep ocean during the bombardment would allow a longer period in which life could have evolved. But chemists like Dr. Sutherland say they are uneasy about getting prebiotic chemistry to work in an ocean, which powerfully dilutes chemical components before they can assemble into the complex molecules of life.

Dr. Sutherland, working from basic principles of chemistry, has found that ultraviolet light from the sun is an essential energy source to get the right reactions underway, and therefore that land-based pools, not the ocean, are the most likely environment in which life began.

“We didn’t set out with a preferred scenario; we deduced the scenario from the chemistry,” he said, chiding Dr. Martin for not having done any chemical simulations to support the deep sea vent scenario.

Dr. Martin’s portrait of Luca “is all very interesting, but it has nothing to do with the actual origin of life,” Dr. Sutherland said.

If the same reaction happened today, it would be destroyed

Processes analogous to these must have given rise to the 'primeval soup' which biologists and chemists believe constituted the seas some three to four thousand million years ago. The organic substances became locally concentrated, perhaps in dry-ing scum round the shores, or in tiny suspended droplets. Under the further influence of energy such as ultraviolet light from the sun, they combined into larger molecules. Nowadays large organic molecules would not last long enough to be noticed: they would be quickly absorbed and broken down by bacteria or other living creatures. But bacteria and the rest of us are late-comers, and in those days large organic molecules could drift unmolested through the thickening broth.

This was a huge period of time

And consequently, you could say that working out genes and the first cells was pretty difficult.


Paleozoic, Mesozoic, and Cenzoic are the three sections of the Phanerozoic. Before the Phanerozoic was the Archaean and the Proterozoic, which lasted for the bulk of Earth's history.

Life started very early

Oldest fossils ever found suggest life in the universe is common. By Jake Parks | Published: Thursday, December 21, 2017

Unexpectedly complex microbes found in a nearly 3.5-billion-year-old rock imply that life can begin and evolve more quickly than previously thought.*


These microorganisms were discovered in a sample of rock collected from the Apex Chert in western Australia. Researchers recently used sophisticated chemical analysis to confirm the 3.5-billion-year-old microbes were indeed biological. Their complex and varied structures at such an early point in Earth’s history suggest that life can begin and evolve much more quickly than previously thought.

J. William Schopf/UCLA

In a study published December 18 in the *Proceedings of the National Academy of Sciences*, scientists confirmed that the oldest fossils ever discovered — found in a nearly 3.5-billion-year-old rock from western Australia — contain 11 complex microbes that are members of five distinct species.

The findings not only suggest that life on our planet originated some 4 billion years ago, but also help support the increasingly widespread theory that life in the universe is much more common than we previously thought.

“By 3.465 billion years ago, life was already diverse on Earth; that’s clear,” said J. William Schopf, a professor of paleobiology at UCLA and the study’s lead author, in a press release. “This tells us life had to have begun substantially earlier, and it confirms that it was not difficult for primitive life to form and to evolve into more advanced microorganisms.”


J. William Schopf, UCLA professor of paleobiology and lead author of the study.

John Vande Wege/UCLA

To analyze the microorganisms, the researchers used an instrument called a secondary ion mass spectrometer (SIMS) — one of only a few in the world. By measuring the ratio of carbon-12 to carbon-13 isotopes, SIMS helped the scientists determine the microbes’ anatomies, and revealed how they lived.

“The difference in carbon isotope ratios correlate with their shapes,” said John Valley, professor of geoscience at the University of Wisconsin-Madison and co-author of the study. “Their C-13-to-C-12 ratios are characteristic of biology and metabolic function.”

Based on the chemical analysis, the researchers concluded that the 11 fossilized microbes spanned five different taxonomical groups. Some of the microbes were a type of now-extinct bacteria from the domain Archaea, while others were more similar to microbial species still around today. The analysis also suggests that the microbes existed when there was very little oxygen present in Earth’s atmosphere.


John Valley, professor of geoscience at the University of Wisconsin-Madison and co-author of the study.

Jeff Miller/University of Wisconsin-Madison

According to Schopf, the process of photosynthesis, as we know it today, had probably not even evolved yet. In fact, he thinks that oxygen did not appear on Earth until roughly half a billion years later. Because of this, oxygen would have most likely poisoned and killed the microorganisms.

Whether or not oxygen was deadly to the microbes, the results show that “these are a primitive but diverse group of organisms,” Schopf said. Their complex and varied structures at such an early point in Earth’s history demonstrate that life can take root and evolve much more rapidly than previously thought.

When combined with the fact that there are trillions of stars in the universe — and the growing consensus among astronomers that exoplanets are commonplace — the case for life existing elsewhere in the universe has never been stronger. “If the conditions are right, it looks like life in the universe should be widespread,” Schopf said.


In 1982, this sample of rock was taken from one of the oldest and best-preserved rock formations in the world: Apex Chert in western Australia. Soon after, scientists found it contained evidence of early life on Earth. Recently, UCLA and UW-Madison scientists chemically analyzed the ancient fossil to confirm the microscopic structures in the rock were indeed biological. They also determined the fossils were 3.5 billion years old, making them the most ancient fossils ever discovered.

John Valley/UW-Madison

Schopf previously described the fossils in the journal *Science* in 1993, and he confirmed their biological origin in the journal *Nature* in 2002. However, this is the first study to reveal both how complex the fossils are and to describe exactly what they are. (Schopf’s work also made news in 2015 when he helped discover a deep-sea microorganism that apparently hasn’t evolved in over 2 billion years.)

The most recent findings “will probably touch off a flurry of new research into these rocks as other researchers look for data that either support or disprove this new assertion,” said Alison Olcott Marshall, a geobiologist at the University of Kansas in Lawrence who was not involved in the study, in a press release.

“People are really interested in when life on Earth first emerged,” Valley said in a press release. “This study was 10 times more time-consuming and more difficult than I first imagined, but it came to fruition because of many dedicated people who have been excited about this since day one … I think a lot more microfossil analyses will be made on samples of Earth and possibly from other planetary bodies.”


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