Mineral Convolutions
The backdrop texts recast geologic history as mineral evolution, which studies the intertwined co-evolution of geosphere and biosphere.[i] At top, a possible discovery of primeval fossils shows how "life begets rock, rocks beget life."[ii] Skeptics classify them as "dubiofossils," structures in rock that resemble fossils but may not be biogenic in origin.[iii] At bottom, evidence of the Anthropocene is found in 'human-mediated minerals,' new kinds of crystals found in mines, shipwrecks, and museum storage.[iv]
The enigmatic amalgamated geophysical chunks are composed of three mineralogical materials cited in the news reports (Hematite tubes, Fiedlerite (formed by slag meeting seawater), Simonkolleite (formed by weathering of zinc-bearing slag)), attached to a piece of Fordite, or Motor Agate (built up layers of enamel auto paint slag, cut and polished).
[i] See Robert M. Hazen, The Story of Earth (Viking, 2012).
[ii] Hazen, quoted in Maya Wei-Haas, "Life and Rocks May Have Co-Evolved on Earth" (Smithsonian Magazine, 2016) www.smithsonianmag.com/science-nature/life-and-rocks-may-have-co-evolved-on-earth-180957807/.
[iii] Deborah Netburn, "In 3.7-billion-year-old rock, scientists find what could be the oldest fossils on Earth." Los Angeles Times, March 1, 2017.
[iv]Deborah Netburn, "You are living in a unique time on planet Earth — mineralogically speaking." Los Angeles Times, March 3, 2017.
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