0 thoughts on “Friday fold: Banded iron formation from the University of Wisconsin geology museum”

  1. I asked for a piece of BIF for Christmas last year from my 83 y/o mother, who never knows what to get me. She thinks I’m a little crazy sometimes, but I have everything I need, so I ask for small things I would like.

    To me, banded iron is a fossil from the oxygenation of Earth’s atmosphere, a 2 Ga remnant of some Archean stromatolite in some long gone tropical sea, converting water and CO2 to hydrocarbon chains and releasing oxygen as a waste product. It’s a remnant from a time when the oceans were saturated with iron. It’s a relic from a different Earth. It’s an astounding thing, to me, to hold a piece of that in your hand. And equally astounding that we can understand it: how it formed, when it happened, why it exists, what created it.

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    • There can be stromatolites in BIF, and the source of free oxygen for BIFs is thought to be nearby shallow water stromatolite photosynthesis, but not all BIFs are stromatolites.

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