Chengjiang Maotianshan Zoolites Site
On July 1st, 1984, Mr Hou Xianguang, a renowned
paleontologist, discovered the
paleontological
fossil site in Maotianshan Mt of Chengjiang
County. A massive, systematic collecting work
was then launched.
paleontologist, discovered the
fossil site in Maotianshan Mt of Chengjiang
County. A massive, systematic collecting work
was then launched.
According
to the geological survey in 1984
and 1985, Chengjiang zoolites had been
found to widely distribute, and they can
date back to the early Cambrian Period which
is about 520 million years ago.
and 1985, Chengjiang zoolites had been
found to widely distribute, and they can
date back to the early Cambrian Period which
is about 520 million years ago.
These
fossils cover a complete range of marine
life, and they are currently considered the
best-preserved paleontological fossils in the
world. Most importantly, these fossils shed
light on the wonder and pristine features of
marine life during the Cambrian Period; and
they are pretty valuable proofs for study into
the origin of life, organic evolution, and ecology
in the early stage of the Earth.
life, and they are currently considered the
best-preserved paleontological fossils in the
world. Most importantly, these fossils shed
light on the wonder and pristine features of
marine life during the Cambrian Period; and
they are pretty valuable proofs for study into
the origin of life, organic evolution, and ecology
in the early stage of the Earth.
The
discovery of Chengjiang zoolites has shocked
the science circle of the world, and it has been
claimed “one of the most amazing discoveries
in the 20th century”.
the science circle of the world, and it has been
claimed “one of the most amazing discoveries
in the 20th century”.
What are there at the fossil site?
The Chengjiang biota came into being during
the Cambrian Explosion. Most representatives
of the existent animals can be found here. (Picture on the left:
Maotianshania)
The Chengjiang biota came into being during
the Cambrian Explosion. Most representatives
of the existent animals can be found here. (Picture on the left:
Maotianshania)
Porifera (Spongia)
The Spongia animal fossils vary, including at least 20 genera and species
which belong to Class Hexactinellida and Desmospongia.
The Spongia animal fossils vary, including at least 20 genera and species
which belong to Class Hexactinellida and Desmospongia.
Brachiopoda
Four genera and four species have been discovered so far.
Four genera and four species have been discovered so far.
Cnidaria (Coelenterate)
Two genera and two species have been discovered, belonging to Actinia
and Ctenophora.
Two genera and two species have been discovered, belonging to Actinia
and Ctenophora.
Nematomorpha
Worm (animals) fossils under this phylum are one of the most common
at Chengjiang fossil site. Their bodies resemble to slim cylinders. So far,
three genera and three species have been discovered.
Worm (animals) fossils under this phylum are one of the most common
at Chengjiang fossil site. Their bodies resemble to slim cylinders. So far,
three genera and three species have been discovered.
Priapulida
Four genera and four species
Four genera and four species
Kinorhyncha
At least four genera and four species
At least four genera and four species
Lobopodia
At least six genera and six species
At least six genera and six species
Mollusca
Four genera and four species
Four genera and four species
Arthropoda
It is the most enormous fossil category among the zoolites. At present,
40 genera and 40 species have been described, and they belong to
three super-classes. No uniramia animal fossils have been discovered.
It is the most enormous fossil category among the zoolites. At present,
40 genera and 40 species have been described, and they belong to
three super-classes. No uniramia animal fossils have been discovered.
Echinodermata
One genera and one species have been reported currently.
One genera and one species have been reported currently.
Uncategorised
Due to the insufficient research, there have been 12 genera and 12
species uncategorised, such as jellyfish-like fossils, Yunnanozoon, and
Facivermis yunnanicus Hou et Chen.
Due to the insufficient research, there have been 12 genera and 12
species uncategorised, such as jellyfish-like fossils, Yunnanozoon, and
Facivermis yunnanicus Hou et Chen.
Algae
A huge number of algae fossils have been found existing on rock surfaces
at Chengjiang fossil site. With most having no branches, these fossils
turn out to be filaments of different diameters, and a few of them are in
the shape of spiral.
A huge number of algae fossils have been found existing on rock surfaces
at Chengjiang fossil site. With most having no branches, these fossils
turn out to be filaments of different diameters, and a few of them are in
the shape of spiral.
(Yunnanzoon)
What is the significance?
Before the discovery of Chengjiang zoolites, the oldest fossil site had been
the Burgess Shale Fossil Beds of Canada, which can date back to the middle
Cambrian Period and is in fact 10 million years younger than Chengjiang
zoolites.
Before the discovery of Chengjiang zoolites, the oldest fossil site had been
the Burgess Shale Fossil Beds of Canada, which can date back to the middle
Cambrian Period and is in fact 10 million years younger than Chengjiang
zoolites.
Chengjiang
fossil site practically unveils the original look of the oldest marine
animals, making people realise: various animals have been living in the sea
since the Cambrian Explosion.
animals, making people realise: various animals have been living in the sea
since the Cambrian Explosion.
Chengjiang
zoolites have depicted a diagram of the complete and oldest
marine biota-for which there had been little knowledge before. To date, the
zoolites have offered not only knowledge of what animals appeared as a
result of the Cambrian Explosion of life, but also the first understanding of
how different animals lived and their feeding habits.
marine biota-for which there had been little knowledge before. To date, the
zoolites have offered not only knowledge of what animals appeared as a
result of the Cambrian Explosion of life, but also the first understanding of
how different animals lived and their feeding habits.
Furthermore,
these fossils are most likely to reveal the cause of the
Cambrian Explosion and more information about the later organic evolution.
Cambrian Explosion and more information about the later organic evolution.
On
July 1st, 2012, at the 36th World Heritage Conference held in St
Petersburg,
Russia, Chengjiang fossil site was inscribed into the World Natural Heritage List.
Russia, Chengjiang fossil site was inscribed into the World Natural Heritage List.
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