How deep do bacteria travel within the Earth's crust?

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Bacteria may be subducted deep within the Earth's crust, potentially reaching depths of around 10 km, aided by water that could transport single-celled organisms. Sulfur-based bacteria are proposed to survive at high temperatures, up to 250°F, for extended periods. However, the availability of hydrogen sulfide, essential for their energy, in subduction zones raises questions about their metabolic activity. While conditions may allow for bacterial survival, it remains uncertain whether these organisms are thriving or merely in a state of suspended animation due to limited resources, particularly water.
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How far might bacteria have been subducted within the Earth's crust? I suppose water could have carried single celled organisms to the current record, ~10 km down. Here I'm offering that sulfur-based bacteria could live at temperatures near 250o F, for possibly thousands of years, traveling many more miles beneath Earth's surface than now known.
 
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Interesting idea, to which I would ask - if they require hydrogen sulfide as their energy source, such as that found at deep-ocean rift ecosystems, would that still be available (under the conditions required to support life) in these subduction zones? I would think at least water, a critical component, would be in short supply. This doesn't mean that the bacteria couldn't survive under the conditions present in subduction zones, but are they actually metabolically active and thriving or are they simply in a type of suspended animation?
 
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