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Stromatolites
Geological Time: Paleocene
Size: 165mm X 110mm X 95mm thick Fossil Site: Flagstaff Formation, Utah County, Utah
Item: OFS026
Price: $125.00
Remarks: The second picture shows the uncut naturally weathered back of this
specimen.
Stromatolites were formed by prokaryotic, photosynthetic bacterial, most likely
cyanobacteria, the primitive organisms that largely produced Earth's atmospheric
oxygen). This individual colony has been polished exhibiting the growth rings.
This stromatolite dates to the Paleocene ~ 60 million years ago when stromatolite
was no longer prevalent and abundant. By the Cambrian, photosynthetic bacteria
responsible for the biogenic formation of stromatolite structures no longer had
the earth to themselves. The oxygenated atmosphere had become toxic to some bacteria,
and they had to compete with other organisms, some of which would have been predaceous
to this most ancient of life forms. |
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Stromatolites
Geological Time: Paleocene
Size: 135mm X 60mm X115mm thick
Fossil Site: Flagstaff Formation, Utah County, Utah
Item: OFS025
Price: $125.00
Remarks: The second picture shows the uncut naturally weathered back of this
specimen.
Stromatolites were formed by prokaryotic, photosynthetic bacterial, most likely
cyanobacteria, the primitive organisms that largely produced Earth's atmospheric
oxygen). This individual colony has been polished exhibiting the growth rings.
This stromatolite dates to the Paleocene ~ 60 million years ago when stromatolite
was no longer prevalent and abundant. By the Cambrian, photosynthetic bacteria
responsible for the biogenic formation of stromatolite structures no longer had
the earth to themselves. The oxygenated atmosphere had become toxic to some bacteria,
and they had to compete with other organisms, some of which would have been predaceous
to this most ancient of life forms. |
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Stromatolites
Geological Time: Paleocene
Size: 205mm X 100mm X 130mm thick
Fossil Site: Flagstaff Formation, Utah County, Utah
Item: OFS024
Price: $150.00
Remarks: The second picture shows the uncut naturally weathered back of this
specimen.
Stromatolites were formed by prokaryotic, photosynthetic bacterial, most likely
cyanobacteria, the primitive organisms that largely produced Earth's atmospheric
oxygen). This individual colony has been polished exhibiting the growth rings.
This stromatolite dates to the Paleocene ~ 60 million years ago when stromatolite
was no longer prevalent and abundant. By the Cambrian, photosynthetic bacteria
responsible for the biogenic formation of stromatolite structures no longer had
the earth to themselves. The oxygenated atmosphere had become toxic to some bacteria,
and they had to compete with other organisms, some of which would have been predaceous
to this most ancient of life forms. |
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Stromatolites
Geological Time: Paleocene
Size: 100mm X 110mm X 120mm thick
Fossil Site: Flagstaff Formation, Utah County, Utah
Item: OFS023
Price: $50.00
Remarks: The second picture shows the uncut naturally weathered back of this
specimen.
Stromatolites were formed by prokaryotic, photosynthetic bacterial, most likely
cyanobacteria, the primitive organisms that largely produced Earth's atmospheric
oxygen). This individual colony has been polished exhibiting the growth rings.
This stromatolite dates to the Paleocene ~ 60 million years ago when stromatolite
was no longer prevalent and abundant. By the Cambrian, photosynthetic bacteria
responsible for the biogenic formation of stromatolite structures no longer had
the earth to themselves. The oxygenated atmosphere had become toxic to some bacteria,
and they had to compete with other organisms, some of which would have been predaceous
to this most ancient of life forms. |
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