National Geographic Naked Science - Birth of the EarthXviD codec | AVI 688x432 - 16:9 - 25fps 1995Kbps | English AC3 192KB/s - 48000Hz | 00:47:29 | 745 Mb
Genre: DocumentaryHow
did the Earth evolve to support life? Our planet now supports a huge
diversity of living creatures requiring very special conditions, but
what was the series of events that brought this unique set of
conditions together? What did it take to make a world that would
support human life?
Tagish Lake meteorite
The Tagish Lake
meteorite impacted the Earth on January 18, 2000; the reported sighting
in the Tagish Lake area in the Yukon Territory and northern British
Columbia, Canada was followed-up by gathering more than 500 fragments
of the meteorite, collected upon the lake's frozen surface. Post-event
atmospheric photographs, also yielded the meteor trajectory. Most of
the stony, carbonaceous fragments landed on the Taku Arm of the lake,
becoming encased in ice as they entered the lake's frozen surface. As
the meteorite fell to Earth, it set off a wide array of satellite
sensors, as well as seismographs.
Analyses have shown that they
are of a primitive age, containing unchanged stellar dust granules that
may have been part of the cloud of material that created our solar
system and Sun. The meteorite has proven to have come from the outer
limits of the asteroid belt in our solar system. The Tagish Lake
meteorite, before it impacted, was estimated at 4 metres in diameter
and 56 tonnes in weight. However, when the fragments of the massive
lump of rock were found, only 1.3 tonnes remained, meaning that around
97% of the meteorite had vaporised on its descent, during which the
meteor finally exploded with around 1.7 kilotons of energy. Of these
1.3 tonnes of fragmented rock, only 0.1% was found and collected.
Stromatolites
Stromatolites
were much more abundant on the planet in Precambrian (Pre-Cambrian)
times.Prior to 2.4 billion years ago, the earth's atmosphere was rich
in carbon dioxide. However, the Precambrian air lacked the oxygen that
sustains the complex multicellular life that has evolved since the
"Cambrian explosion" 540 million years ago. Stromatolites in the fossil
record decline sharply in both diversity and number during the late
Proterozoic eon, although they are present, but not common, in
Paleozoic era strata. Today, stromatolites are quite uncommon in marine
environments. As a result, they have become valuable "living fossils."
Modern
stromatolites are mostly found in hypersaline lakes and marine lagoons
where extreme conditions exclude animal grazing. One such location is
Hamelin Pool Marine Nature Reserve, Shark Bay in Western Australia
where excellent specimens are today observed. Fresh-water stromatolites
can be found in Cuatro Cinegas, a unique ecosystem in the Mexican desert
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