The
Triassic period stands out in Earth’s history as the time when
dinosaurs first evolved. It was followed by the Jurassic and Cretaceous
periods – at the end of the latter, the dinosaurs were wiped out in a mass extinction event along with the majority of all other life.
As a period of geologic time, the boundaries of the Triassic are defined on the basis of rocks and the fossil
record. It was the German geologist Friedrich August von Alberti who
first marked the Triassic out. He discovered in 1834 that rocks
throughout Europe of a certain age contained a unique fossil fauna,
bookended with layers of rock that contained far fewer fossils, which
clearly signified extinctions.
When did the Triassic period start?
The
Triassic began 252 million years ago and ended 201 million years ago.
The period of time before the Triassic was called the Permian. This was a
time when a wide variety of animals lived, including a group of animals
called the synapsids, which would later evolve into mammals. One member
of this group was a large, sail-backed animal called dimetrodon, which looks like it could be a dinosaur but isn’t.
Then
252 million years ago came the Permian-Triassic extinction event. This
is the biggest extinction event our planet has ever seen, in which 70
per cent of species on land disappeared along with 95 per cent of those in the oceans.
This not only marked the end of the Permian period and the start of the
Triassic, it was such a serious catastrophe that it is used as the
marker of the end of a geologic era, the palaeozoic era.
Which dinosaurs lived during the Triassic period?
Out
of the ashes of this extinction, several new groups of reptiles began
to evolve in the Triassic. One particularly successful group was called
the pseudosuchians. This is the lineage to which present-day crocodiles
and alligators belong. They are a paltry bunch today, about 25 species
all told. But back in the Triassic, there were scores of them, including
armoured ones that ate plants, toothless omnivores that sprinted on
their hind legs and apex predators called rauisuchians that were 9
metres from nose to tail and had teeth like steak knives.
Alongside
these terrestrial vertebrates, the first dinosaurs began to appear.
They were mostly much smaller and meeker creatures, many not much bigger
than a cow. One example is Tanystropheus,
which had an extraordinary neck that was twice as long as its body.
Another is Coelophysis, a predator that looked a bit like a miniature
T-rex.
Pangaea
When these animals lived, Earth’s
land was all mushed together into one big C-shaped supercontinent called
Pangaea. Around the back of the “C” was a vast ocean called Panthalassa
and the expanse of water nestled in its curve is called the Tethys Sea.
The interior of Pangaea would have been an intensely hot and inhospitable desert.
It’s thought that the dinosaurs mostly stuck to its coastal edges while
the pseudosuchians were better able to endure the inner regions.
How did the Triassic differ from the Jurassic?
The
pseudosuchians remained the dominant group for the whole of the
Triassic, with the dinosaurs skulking in the shadows. It was only in the
next geologic period, the Jurassic, that the powerful pseudosuchians
died back and the dinosaurs really took over, evolving into huge animals
like the stegosaurus and the long-necked diplodocus. It’s always been a
major mystery how the dinosaurs went from pipsqueaks to rulers.
The end Triassic extinction event
About
200 million years ago, during a period known as the Triassic-Jurassic
boundary, Pangaea started to crack. North America separated from Europe;
South America from Africa. As they parted, Earth haemorrhaged lava from volcanoes
in what is now the bottom of the Atlantic Ocean. Released with the lava
were huge volumes of carbon dioxide and sulphur dioxide. These gases
continually warmed the atmosphere, while bursts of ash from the
eruptions shut out the sun’s light.
As you might expect, this
change in global climate killed off a huge number of species and
decimated the pseudosuchian populations. Dinosaurs, somehow, seem to
have emerged from this time relatively unscathed and gone on to prosper
in the gaps left by the ancient crocs. Exactly how they managed still
remains unclear, though recent evidence points to their unusual lungs as a clinching factor.
The compounds responsible for the earthy smell of recent rain are produced by a wide variety of bacteria and fungi. Recent research sheds light on why microbes bother.
Use
of an artificial blood substitute can reverse cell damage caused by
lack of oxygen and could make more organs available for transplants,
treat heart attacks and strokes and even reverse death
The transfusion led an increased number of senescent cells – which
accumulate as we get older - in the young mice, suggesting that
cellular ageing isn't just a case of wear and tear
Mixtures of viruses that attack inflammatory bowel disease–causing
bacteria in mice also survive the digestive tract and are well-tolerated
in humans, a study finds.