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The age of dinosaurs, from the Triassic to Chicxulub

A timeline, a family tree and moving plates, with a source behind every date

Topics
dinosaurs · palaeontology · K-Pg extinction · Chicxulub · plate tectonics · Pangaea

Two hundred and fifty-two million years, to scale

Each band is as wide as its period was long. Pick a period on the scale or with the buttons below: they do the same thing.

252 Ma 201 Ma 145 Ma 66 Ma today

Triassic (252-201 Ma)

Dinosaurs appear around 230 million years ago, during the middle and late Triassic. They are small, agile bipeds, one or two metres long, such as Eoraptor and Herrerasaurus, found in Argentina.

The land is still welded into a single continent, Pangaea. The climate is hot and arid. Dinosaurs share their ecosystems with rauisuchians, dicynodonts and cynodonts, but they remain a minor component.

The end-Triassic extinction (201 Ma), tied to the opening of the Atlantic and to massive volcanism, removes most of their competitors. The dinosaurs inherit the space left free.

A simplified phylogenetic tree

Open a name to read the entry for that group.

Saurischians (lizard hips)

The pubis points forwards, as in reptiles. They take in bipedal carnivores and gigantic long-necked herbivores.

Ornithischians (bird hips)

The pubis turns backwards. All of them herbivores, often armoured or carrying elaborate crests and horns.

Continental drift

A schematic reconstruction, drawn by hand: no coordinates, no map projection. Pick a step, or press Animate the drift to run through them all.

250 million years ago

equator ANTARCTICA EURASIA N. AMERICA GREENLAND S. AMERICA AFRICA INDIA AUSTRALIA

dry land oceans and epicontinental seas

Pangaea: one continent only

All the dry land is welded into a single block ringed by the Panthalassa ocean. The interior of the continent is desert, with extreme swings of temperature and violent monsoons along the coasts. The first dinosaurs will appear in this setting, and they can walk from one pole to the other without meeting the sea.

The K-Pg event, 66 million years ago

An asteroid about 10-15 km in diameter strikes the Yucatán, in what is now Mexico, leaving the 180 km Chicxulub crater. It is the trigger for a chain of events that wipes out around 75% of living species.

  • Immediate impact

    The asteroid arrives at about 20 km/s, the typical speed at which an asteroid meets the Earth. Energy of the order of 10²³ joules, which nobody measures: it follows from the mass and the speed attributed to the asteroid, and the published models do not agree. Ground shaking estimated between magnitude 9 and 11. In the Gulf of Mexico the simulations give waves of over a hundred metres, far lower on distant coasts. Fires set off by the rain of white-hot glass spherules falling back out of the atmosphere.

  • Impact winter

    Dust and sulphate aerosols darken the sun for months or years. Photosynthesis collapses, the food chain is cut at its base. All the non-avian dinosaurs disappear, along with the pterosaurs, the ammonites and the mosasaurs.

  • The Deccan Traps

    Massive volcanism in India, on a continental scale, active between 67 and 65 Ma: it puts ecosystems under stress with greenhouse gas emissions and acidification well before the impact, and carries on after it.

  • Long-term effects

    Acidification of the oceans, cooling followed by warming from CO₂, the carbon cycle altered for millennia.

Who survives?

Small nocturnal mammals, crocodiles, turtles, amphibians, some fish, insects, seed plants. And one particular group of small feathered theropods, the ancestors of modern birds. Technically the dinosaurs have never gone extinct: every sparrow, every chicken, every eagle is an avian dinosaur.

What these numbers do not say

The dates of geological boundaries are estimates carrying an error margin, not fixed numbers: the Cretaceous-Paleogene boundary is written as 66 million years ago, but the measured value is 66.043 with about eleven thousand years of uncertainty, and the chronostratigraphic scale is revised with every new calibration. The plate reconstruction shown here is a hand-drawn sketch rather than a georeferenced model, and ancient positions grow less certain the further back you go, because the ocean crust that recorded them has been subducted away. The family tree is simplified for legibility, and the split between saurischians and ornithischians, treated as settled in textbooks, was challenged in 2017 and remains open. On the extinction itself, the relative weight of the impact and of Deccan volcanism is still being measured, and research groups disagree about it.

Methods and applicable ranges

  • Radiometric dating: U-Pb on zircon and Ar-Ar on sanidine Range: From a few thousand years back to the age of the Earth, with a relative precision that now reaches a few parts in ten thousand. It needs a mineral that crystallised at the moment of the event, which in the Mesozoic almost always means a volcanic ash layer: the ash is what gets dated, not the fossil above or below it. Every date on this page rests on that, from the 201 million year boundary down to 66.043. Ages published before 2008 and after it do not compare word for word, because the calibration of the Ar-Ar standards changed and shifted some dates by a few hundred thousand years. The date of 66 million years ago is the rounded form of 66.043 plus or minus 0.011.
  • Magnetostratigraphy Range: Covers the whole Phanerozoic. Rocks record the Earth's magnetic field at the moment they form, and polarity reversals leave a sequence of chrons that can be recognised anywhere. The K-Pg boundary falls inside chron C29r, which is what lets a section in Montana be correlated with one in Tunisia when neither contains datable ash. On its own it says only normal or reversed, so it yields no ages: a radiometric or astronomical anchor is needed before a number can be attached to each chron. Slow or interrupted sedimentation can erase a short chron from the sequence, and the correlation then goes wrong.
  • Biostratigraphy Range: Works from the Cambrian onwards, wherever fossils are both widespread and short-lived. Planktic foraminifera and calcareous nannofossils define biozones that the Cretaceous-Paleogene transition cuts through sharply, and it was on that basis that period boundaries were recognised in the field long before anyone could date them in years. Where a species appears and disappears in a section depends partly on how much has been collected: the last specimen found is not the last one that lived, and the sampling gap tends to make extinctions look earlier than they were. Biozones are also not synchronous between different latitudes.

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Data provenance

  • SVG plate outlines, demetriotriglia.com ↗ Licence: Original drawing, no external dataset involved. Reusable with attribution. The eight plate outlines are hand-drawn and schematic rather than georeferenced: no coordinates, no map projection, no rotation model. The intermediate positions are graphical interpolations meant to make the motion readable, not the output of a tectonic reconstruction. For quantitative configurations see Seton et al. 2012 and Merdith et al. 2021.

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