| 17.9 |
The pre-Cambrian/Vendian extinctions (500m BCE) |
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| o Pre Cambrian period (4.6 billion to 523 million years ago) |
| o Vendian period (523-543 million years ago) |
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The Pre Cambrian era was a period in
Earth history before the evolution of hard-bodied and complex organisms.
Throughout the extent of both periods, dominant Pre Cambrian and Vendian
organisms were soft-bodied, simple, and entirely marine. |
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They swum around the water close to the
surface of the immersed Earth, feeding of the very much stronger radiation from
the Sun and the internal warmth of the Earth, still cooling down. Even at these
Early stages there would have been land. Places where asteroids had smashed
into the 100 metre deep ocean and created huge gaping holes and pockets of
islands. But these few dotted islands of land were bare, warm, warped rock.
Nothing yet lived on land. The diversification of life to hard-bodied organisms
did not occur until the beginning of the Cambrian, when the first shelly fauna
appeared. |
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About 650 million years ago, seventy
percent of the dominant Pre cambrian life totally living in the oceans perished
in the first great extinction. This extinction strongly affected stromatolites,
acritarchs, and was also the predetermining factor that encouraged the
diversification of the Vendian fauna that followed. However, pre Cambrian life
totally in the oceans resembled modern-day soft-bodied organisms such as sea
pens, jellyfish, and segmented worms that also perished in a second extinction
event at the close of the Vendian. |
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| 17.9.1
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What happened then? |
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The impact of the asteroids had several
effects. Firstly it fractured the Earths surface, releasing massive amounts of
the inner core and creating volcanoes. Second, it twisted and re-shaped the
Earths crust into mountain ranges, rather like the folding of a giant rug, when
someone trips on the end. |
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The stretch of the Earth's crust could also accounts
for secondary fissures at the other end, where another object hit, causing the
crust to snap and thus create two or possibly three edges of a "mini" plate. |
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At this time, the temperature of the Earths oceans
would have been incredibly het (possibly for over a year). Huge volcanic
eruptions would have added to the massive amounts of dust particles creating
thick, dense clouds in the Earth's atmosphere. Finally, the blanket of dust
plummeted the Earth's surface into darkness. |
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Quickly the oceans cooled. Life that hadn't been
boiled now faced the prospect of being snapped frozen. For the oceans quickly
began freezing up, all across the globe. A massive ice age occurred where the
entire globe was covered in ice for years. |
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The life most likely to have survived the heat wave of
the oceans, closer to the poles now face being the first to freeze to death.
They may have got half way, say around where Europe now is located and the
early islands that may have eventually become Australia. And there- the miracle
of snap freezing took place. |
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Life, growing the conditions for growing ceased to be
possible. But life was not dead. It was frozen in the frozen oceans of the
globe. |
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As the dust gradually settled, the sunlight started to
break through again and the oceans thawed after several thousands of years.
During this period, the floor of the oceans were scowled by the giant glacier.
Ridges and mountains were warped even higher, crushed by the expanded massive
ice pack. |
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| 17.9.2 |
The signature pattern of life |
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But we also see from the extinction, that life through
DNA understood the conditions and the need to adapt to possible future changes.
From now on, life had to adapt with harder bodies. Harder bodies could
withstand the greater changes of heat and cold. It certainly the reason that we
see basic organisms develop into shelly types during the next period, apart
from the continuation of soft bodied creatures. |
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