Earth Research CardsFrom the Solar System to Complex Life

Every research card for Eras 5 to 8 in the game, from the Solar System to the origin of life and complex life, with year, authors, journal and paper title.

Every research card in the game matches a real published paper. This page covers the Earth section: Era 5 through Era 8, from the formation of the Solar System through the origin of life to complex life, more than thirty cards in all. We sort them into seven groups. Each entry says in one sentence what was found, with the source in parentheses (authors, Journal year).

How Earth and the Moon formed

  • Lead isotopes in meteorites put Earth's age at about 4.55 billion years. To remove lead contamination, the measurer later helped drive the ban on leaded gasoline (Patterson, Geochimica et Cosmochimica Acta 1956).
  • Decay products of aluminum-26 in meteorites show that a star had just died nearby when the Solar System was born (Lee, Papanastassiou & Wasserburg, The Astrophysical Journal Letters 1977).
  • Computer simulations showed that a Mars-sized body struck Earth at an angle, and the debris came together to form the Moon (Canup & Asphaug, Nature 2001).
  • Jupiter once migrated inward and was then "pulled back" by Saturn, eating up the raw material for Mars on the way. That is why Mars is so small (Walsh et al., Nature 2011).
  • A violent shake-up of the giant planets' orbits flung many small bodies into the inner Solar System and caused the Late Heavy Bombardment (Gomes, Levison, Tsiganis & Morbidelli, Nature 2005).
  • A zircon grain the size of a grain of sand shows that Earth may have had liquid water only about 150 million years after it formed (Wilde, Valley, Peck & Graham, Nature 2001).

Planets beyond the Solar System

  • A giant planet was found around 51 Pegasi, circling its star in 4 days. The Solar System was no longer unique, and the discoverers won the 2019 Nobel Prize (Mayor & Queloz, Nature 1995).
  • The Kepler telescope looks for new worlds by the faint dimming when a planet crosses its star, and went on to find thousands (Borucki et al., Science 2010).
  • Seven Earth-sized planets crowd around a small red dwarf star, and a few of them may have liquid water (Gillon et al., Nature 2017).

Where the raw materials of life came from

  • A graduate student sealed water, methane, ammonia and hydrogen in a flask and sent sparks through it, and got the amino acids that make up proteins (Miller, Science 1953).
  • Amino acids of non-terrestrial origin were found in the Murchison meteorite, so the raw materials of life may be common in the universe (Kvenvolden et al., Nature 1970).
  • Found a more "natural" chemical route that builds RNA components directly under primitive conditions (Powner, Gerland & Sutherland, Nature 2009).
  • Ecosystems around deep-sea vents live without sunlight, which gave the origin of life a new candidate site (Corliss et al., Science 1979).

The RNA world

  • RNA can catalyze reactions like an enzyme, so RNA is both information and tool. The work won the 1989 Nobel Prize (Kruger, Cech et al., Cell 1982).
  • The part of an enzyme that actually does the catalysis is RNA, not protein (Guerrier-Takada, Altman et al., Cell 1983).
  • The earliest life may have been made entirely of RNA, with DNA and proteins added later (Gilbert, Nature 1986).
  • Two RNA enzymes copied each other and kept growing exponentially in number, a step toward "molecular life" (Lincoln & Joyce, Science 2009).
  • The core of the ribosome, where proteins are made, is RNA. This is direct evidence left over from the RNA world, and the work won the 2009 Nobel Prize (Nissen et al., Science 2000).

The Tree of Life and the common ancestor

  • Comparing ribosomal RNA showed that "bacteria" were really two very different kinds of life, and archaea became their own branch (Woese & Fox, PNAS 1977).
  • The Tree of Life was redrawn with three domains: Bacteria, Archaea and Eukaryota (Woese, Kandler & Wheelis, PNAS 1990).
  • Mitochondria and chloroplasts were once free-living bacteria. After being swallowed, they became part of the cell. When the idea was proposed, more than a dozen journals rejected it (Margulis, published as Sagan, Journal of Theoretical Biology 1967).
  • The common ancestor of all life may have lived near hot, oxygen-free, hydrogen-rich deep-sea vents (Weiss et al., Nature Microbiology 2016).
  • Lokiarchaeum, found in deep-sea sediment, carries many genes once thought to belong only to eukaryotes (Spang et al., Nature 2015).
  • DNA is a double helix, and its base pairing hints at how genetic information is copied (Watson & Crick, Nature 1953).

Oxygen, ice and the earliest fossils

  • Oxygen in the air did not arrive all at once. It rose over a long, back-and-forth process (Lyons, Reinhard & Planavsky, Nature 2014).
  • About 700 million years ago the Earth may have been almost entirely covered in ice (Hoffman et al., Science 1998).
  • Rocks in Greenland may preserve 3.7-billion-year-old microbial structures, though this reading is still disputed (Nutman et al., Nature 2016).
  • A fossil of an ancient red alga shows that sexual reproduction and multicellular life are at least 1 billion years old (Butterfield, Paleobiology 2000).
  • Cholesterol-like molecules preserved in Dickinsonia fossils prove that this mysterious organism was an animal (Bobrovskiy et al., Science 2018).
  • Finds of Myllokunmingia and Haikouichthys at Chengjiang in Yunnan pushed the history of vertebrates back to the early Cambrian (Shu et al., Nature 1999).

Evolution, extinction and dinosaurs

  • The theory of natural selection was published jointly by Darwin and Wallace, and On the Origin of Species came out the next year (Journal of the Proceedings of the Linnean Society 1858).
  • Species may stay stable for a long time and then change rapidly in a short time, rather than evolving at a steady rate (Eldredge & Gould, Models in Paleobiology 1972).
  • Scientists predicted which rock layers should hold a transitional fossil, then found Tiktaalik in the Canadian Arctic (Daeschler, Shubin & Jenkins, Nature 2006).
  • The ancestors of whales were hoofed land animals that ran on land and are related to hippos (Thewissen et al., Nature 2001).
  • Rock layers from the end of the Cretaceous hold unusually high levels of iridium, leading to the inference that an asteroid had hit the Earth (Alvarez et al., Science 1980).
  • Under Mexico's Yucatán Peninsula lies a crater about 180 km across, matching the asteroid that did it (Hildebrand et al., Geology 1991).
  • The end-Permian extinction may have lasted only about 60,000 years, which fits the Siberian volcanic activity (Burgess, Bowring & Shen, PNAS 2014).
  • Feathers grew on dinosaurs before birds appeared (Ji, Currie, Norell & Ji, Nature 1998).
  • Archaefructus from Liaoning was taken to be one of the earliest flowering plants, though its age was later revised to the early Cretaceous (Sun et al., Science 1998).

Real basis

  • The first exoplanet: A giant planet was found around 51 Pegasi, circling its star in 4 days. The solar system was no longer unique. Nobel Prize 2019.

    Source: Mayor & Queloz, Nature 1995, "A Jupiter-mass companion to a solar-type star"

  • Birth of the Moon: Computer simulations show a Mars-sized body hit Earth at a slant, and the debris came together to form the Moon.

    Source: Canup & Asphaug, Nature 2001, "Origin of the Moon in a giant impact near the end of the Earth's formation"

  • The Nice model: A violent reshuffling of the giant planets' orbits flung many small bodies into the inner solar system, causing the Late Heavy Bombardment.

    Source: Gomes, Levison, Tsiganis & Morbidelli, Nature 2005, "Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets"

  • Jupiter's Grand Tack: Jupiter once migrated inward and was “pulled back” by Saturn, eating Mars's raw material on the way, which is why Mars is so small.

    Source: Walsh et al., Nature 2011, "A low mass for Mars from Jupiter's early gas-driven migration"

  • The ocean 4.4 billion years ago: A zircon the size of a grain of sand suggests Earth may have had liquid water only about 150 million years after it formed.

    Source: Wilde, Valley, Peck & Graham, Nature 2001, "Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago"

  • The age of the Earth: Patterson used lead isotopes in meteorites to date Earth at about 4.55 billion years. To eliminate lead pollution, he later pushed for a ban on leaded gasoline.

    Source: Patterson, Geochimica et Cosmochimica Acta 1956, "Age of meteorites and the earth"

  • The aluminum-26 puzzle: Decay products of aluminum-26 in meteorites show that a star had just died nearby when the solar system was born.

    Source: Lee, Papanastassiou & Wasserburg, The Astrophysical Journal Letters 1977, "Aluminum-26 in the early solar system: Fossil or fuel?"

  • Seven temperate planets: Seven Earth-sized planets crowd around a small red dwarf, and several may have liquid water.

    Source: Gillon et al., Nature 2017, "Seven temperate terrestrial planets around the nearby ultracool dwarf star TRAPPIST-1"

  • Kepler: The Kepler telescope stared at one patch of sky and looked for new worlds by the faint dimming when planets transit, eventually finding thousands.

    Source: Borucki et al., Science 2010, "Kepler planet-detection mission: introduction and first results"

  • The Miller–Urey experiment: A graduate student sealed water, methane, ammonia and hydrogen in a flask and kept sparking it, and got the amino acids that make up proteins.

    Source: Miller, Science 1953, "A production of amino acids under possible primitive earth conditions"

  • Nucleotides without enzymes: Found a more “natural” chemical route to directly make RNA components under primitive conditions.

    Source: Powner, Gerland & Sutherland, Nature 2009, "Synthesis of activated pyrimidine ribonucleotides in prebiotically plausible conditions"

  • RNA that cuts itself: Cech found that RNA can catalyze reactions like an enzyme. RNA is both information and tool. Nobel Prize 1989.

    Source: Kruger, Cech et al., Cell 1982, "Self-splicing RNA: autoexcision and autocyclization of the ribosomal RNA intervening sequence of Tetrahymena"

  • Ribonuclease P: Altman independently found that the part of one enzyme that really does the catalysis is RNA, not protein.

    Source: Guerrier-Takada, Altman et al., Cell 1983, "The RNA moiety of ribonuclease P is the catalytic subunit of the enzyme"

  • RNA world: Gilbert proposed that the earliest life may have been made entirely of RNA, with DNA and proteins added later.

    Source: Gilbert, Nature 1986, "Origin of life: The RNA world"

  • Self-replicating RNA: Two RNA enzymes copy each other, and their numbers can keep growing exponentially, a step closer to “molecular life.”

    Source: Lincoln & Joyce, Science 2009, "Self-sustained replication of an RNA enzyme"

  • Amino acids in space: Amino acids of non-terrestrial origin were found in the Murchison meteorite. The raw materials of life may be common in the universe.

    Source: Kvenvolden et al., Nature 1970, "Evidence for extraterrestrial amino-acids and hydrocarbons in the Murchison meteorite"

  • The ribosome is a ribozyme: The core of the ribosome's protein synthesis is RNA, direct evidence left by the RNA world. Nobel Prize 2009.

    Source: Nissen, Hansen, Ban, Moore & Steitz, Science 2000, "The structural basis of ribosome activity in peptide bond synthesis"

  • Deep-sea hot springs: Ecosystems that do not depend on sunlight exist around deep-sea hot springs, giving the origin of life a new candidate site.

    Source: Corliss et al., Science 1979, "Submarine thermal springs on the Galápagos Rift"

  • 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"

  • Natural selection: Darwin and Wallace jointly published the theory of natural selection. The next year, On the Origin of Species came out.

    Source: Darwin & Wallace, Journal of the Proceedings of the Linnean Society 1858, "On the tendency of species to form varieties; and on the perpetuation of varieties and species by natural means of selection"

  • The dinosaur extinction puzzle: Iridium is anomalously enriched in the end-Cretaceous layer, and the Alvarezes, father and son, concluded that an asteroid had hit Earth.

    Source: Alvarez et al., Science 1980, "Extraterrestrial cause for the Cretaceous-Tertiary extinction"

  • Finding the crater: Buried under Mexico's Yucatán Peninsula is a crater about 180 km across, exactly what that asteroid left behind.

    Source: Hildebrand et al., Geology 1991, "Chicxulub Crater: A possible Cretaceous/Tertiary boundary impact crater on the Yucatán Peninsula, Mexico"

  • Tiktaalik: Scientists predicted which age of rock the transitional fossil should be in, and then really found it in the Canadian Arctic.

    Source: Daeschler, Shubin & Jenkins, Nature 2006, "A Devonian tetrapod-like fish and the evolution of the tetrapod body plan"

  • The earliest animals: Dickinsonia fossils preserve cholesterol-type molecules, proving this mysterious creature was an animal.

    Source: Bobrovskiy et al., Science 2018, "Ancient steroids establish the Ediacaran fossil Dickinsonia as one of the earliest animals"

  • The earliest vertebrates: Myllokunmingia and Haikouichthys found in Chengjiang, Yunnan, pushed the history of vertebrates back to the early Cambrian.

    Source: Shu et al., Nature 1999, "Lower Cambrian vertebrates from south China"

  • Feathered dinosaurs: Fossils from Liaoning show that feathers grew on dinosaurs before birds appeared.

    Source: Ji, Currie, Norell & Ji, Nature 1998, "Two feathered dinosaurs from northeastern China"

  • The first flower: Archaefructus from Liaoning was considered one of the earliest flowering plants, and its age was later revised to the Early Cretaceous.

    Source: Sun et al., Science 1998, "In search of the first flower: a Jurassic angiosperm, Archaefructus, from northeast China"

  • Punctuated equilibrium: Species may stay stable for a long time and then change rapidly in a short time, rather than evolving at a steady rate.

    Source: Eldredge & Gould, Models in Paleobiology 1972, "Punctuated equilibria: an alternative to phyletic gradualism"

  • The worst mass extinction: Precise dating shows the end-Permian extinction may have lasted only about 60,000 years, matching Siberian volcanic activity.

    Source: Burgess, Bowring & Shen, PNAS 2014, "High-precision timeline for Earth's most severe extinction"

  • Whales that walked on land: Fossils from Pakistan show that the ancestors of whales were hoofed animals that ran on land, related to hippos.

    Source: Thewissen et al., Nature 2001, "Skeletons of terrestrial cetaceans and the relationship of whales to artiodactyls"