In connection to an iron ore introduced in the previous essay, I have focused on oxygen this time, which played a vital role in the formation of an iron ore. The origin of oxygen is also intriguing. The evidence that oxygen had been generated huge in mass in a short term could be found in far north of Canada.
We inhale air unconsciously every day. By taking in air, we absorb oxygen
and discharge carbon dioxide in the process of generating energy. It is
a physiological phenomenon, called respiration. Most organisms on earth
breathe. Then, how is oxygen generated and where does carbon dioxide go?
May 1st 2003 |
This is the false color image of one entire ASTER scene (60x60km), of eastern part of Great Slave Lake. The colors red, green and blue are allocated to ASTER band 3, 2 and 1 respectively. The difference of stratums is well reflected by the difference in colors.
This is an enlargement of 7x7km in Image - 1 centering on the stromatolite stratum. The stratum can be separated in 5 parts based on the color appear in the image, mixture of red and green (A in the image), thin stripe pattern with much green and little white (B in the image), thick stripe pattern with much white and little green (C in the image), stripe pattern with green and while and sporadical red (D in the image) and red (E in the image). It corresponds to the difference in types of rocks. Area A shows igneous rock in later age (1.6~1 billion years ago), B shows dolomite stratum containing stromatolites, C shows limestone, D shows dolomite with stromatolites older than B, and E shows shale, the oldest stratum in the area. I talked about stromatolites in D in the essay.
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Picture - 1 Stratum at the east of Great Slave Lake in Northern Territories of Canada A cliff of stratum is found along the lakeside. Stromatolites are contained
in it. This stratum continues as long as 200km in the eastern lakeside
of the huge Great Slave Lake. You can imagine the magnitude of the stromatolites
formed approx. 2 billion years ago. |
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Picture - 2 Stromatolite One round rock in the picture is one stromatolite. You can find numerous
round rocks along the lakeside in the area. |
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Picture - 3 Cross section of stromatolites You can see concentric patterns in the cross section well. The word "stromatolite" means concentric rock. |
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Picture - 4 Vertical section of stromatolites Pattern in vertical section is a little different from cross section.
Hundreds of layers are piled up to form a mushroom like pattern. |
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Picture - 5 Sample of stromatolite (vertical section) Numerous minute stripe patterns can be found in the sample of a stromatolite (92x40mm). These stripes are comparable to the rings of a tree since it was formed by the accumulation of cyanobacteria over time. |
Copyright of image - 1 and - 2 belongs to JSS, while Picture - 1~ 5 and the text belong to Prof. Yoshiyuki Koide of Sapporo Gakuin University. Permission of JSS is need of their use for other purposes.