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P1 1799, AH found granite boulders near OR
• Smooth, black, and as if coated with plumbago.
• Indian legend: rocks have been burnt by the tropical sun.
P2 boulders have generated scientific mystery for two centuries.
• CD found rocks in BB. Others found in rainforests, underneath glaciers.
• Hypothesis:
Deposits left by the ancient ocean, residues from decomposing organic matter
Most popular hypothesis: Rock sweating
But: was the sun hot enough?
P3 physical and chemical structure of rock varnish
• Recent scientific name: rock varnish
• While the origin of rock varnish is enigmatic, structure become understood
A thin layer on the rock’s surface
60% clay minerals, 20-30% oxide, more than 30 minor compounds
Amount of manganese determines the color of varnish.
Black: manganese levels up to 100 times
Brown orange: lacks manganese, abundant iron oxides. Appear in the bottom of rock and inside the rock
In Peru desert, manganese is intermediate, brownish orange
P4 1981, TMO and I suggested that bacteria concentrate manganese in rock varnish
• First: manganese-rich varnish often forms where water flows rocks. Moisture=>microrganism
• Second: varnish develop well on the porous surface where easily flushed and poor in nutrients. Oxidizng mixotrophs able to live, heterophic organisms unable to live
P5 third observation: dark varnish grows on rocks with a nearly neutral PH
• Mg-O operates in alkaline environment, where ph>9 => plausible candidates
• Local ph too high => organe
P6 there are many documented interactions between clay and bacteria
• Clay particles absorb onto the surface of bacteria
• Clay concentrate neutrients,
P7 Examination: the presence of bacteria
• Found Mg-concentrating bacteria
• Produce similar bacteria
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