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20.5: Return of the BIF

  • Page ID
    22762
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    Photo of an outcrop of rock showing a dropstone of quartzite in banded iron formation.
    Figure \(\PageIndex{1}\): A dropstone (of quartzite) in banded iron formation strata of the Rapitan Group, Northwestern Canada. (Photo by Galen Halverson; reproduced with permission.)

    There is an additional chemical sedimentary rock that also appears in some Snowball Earth sedimentary sequences: banded iron formation (BIF). This is cited as evidence of radically altered oceanic chemistry during the Snowball glaciation, and therefore an indirect evidence of extensive sea ice cover.

    As we saw in the Archean, the chemical precipitation of banded iron formation is a consequence of anoxic ocean waters. It is a broad generalization that BIFs are an “extinct rock” that “died out” at the Paleoproterozoic / Mesoproterozoic boundary with the build-up of copious free oxygen in the planet’s atmosphere and oceans. But that turns out to be not quite true.

    During the Neoproterozoic Snowball Earth glaciations, BIFs make a reappearance in the geologic record. They were “resurrected” because the conditions that allow their formation occurred again, this time due to the Snowball.

    A graph showing the relative abundance of banded iron formation through Earth history. There is a small bump in the early Archean (3.9 Ga), then a *big* bump that lasts through the Archean and Paleoproterozoic (3.5 Ga to 1.8 Ga), and then no more BIF until a third bump, also small, that coincides precisely with the timing of the Snowball Earth glaciations during the Neoproterozoic (0.7 to 0.55 Ga). Formation names and localities are labeled for reference.
    Figure \(\PageIndex{2}\): A plot showing the relative abundance of banded iron formation (BIF) through geologic time. Note the small “BIF blip” that coincides with the timing of the Neoproterozoic Snowball Earth glaciations. (Callan Bentley figure, redrawn from Klein (2005))

    Because BIFs are the geologic signature of an anoxic ocean, their reappearance after a long absence is cited as strong evidence that sea ice over of Earth’s oceans was indeed global. That is, they were entirely or almost-entirely sealed off from interacting with the oxygenated atmosphere. Any dissolved oxygen in the oceans was consumed through chemical reactions, but was not replaced by diffusion from the atmosphere. This allowed deep sea black smokers to again permeate ocean water with dissolved iron.

    Did I Get It? - Quiz

    Exercise \(\PageIndex{1}\)

    What rock type is evidence that significant portions of Earth's oceans were anoxic during the Snowball Earth glaciations?

    a. cap carbonates

    b. turbidites

    c. banded iron formations

    d. granites

    e. evaporites

    f. tidal rhythmites

    Answer

    c. banded iron formations

    Exercise \(\PageIndex{2}\)

    Why do anoxic ocean waters support the idea of a total planetary freezeover during the Snowball Earth?

    a. It suggests that temperatures were too cold for oxygen to be stable as a gas, and instead it formed a liquid.

    b. It suggests that the first animals (which were very cool) were sucking all the oxygen out of the oceans.

    c. It suggests a lack of gas exchange between the atmosphere and the oceans: blocked by extensive sea ice cover.

    Answer

    c. It suggests a lack of gas exchange between the atmosphere and the oceans: blocked by extensive sea ice cover.


    This page titled 20.5: Return of the BIF is shared under a CC BY-NC 4.0 license and was authored, remixed, and/or curated by Callan Bentley, Karen Layou, Russ Kohrs, Shelley Jaye, Matt Affolter, and Brian Ricketts (VIVA, the Virginia Library Consortium) via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.