1 / 11

Banded Iron Formations: The Evolution of Earth’s Surface and Life

Banded Iron Formations: The Evolution of Earth’s Surface and Life. Mike Tice 6 August 2009. Earth History. The Most Important Organisms in Earth History:. The Cyanobacteria!. Bacteria The first organisms to produce oxygen during photosynthesis

tarmon
Télécharger la présentation

Banded Iron Formations: The Evolution of Earth’s Surface and Life

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Banded Iron Formations: The Evolution of Earth’s Surface and Life Mike Tice 6 August 2009

  2. Earth History

  3. The Most Important Organisms in Earth History: The Cyanobacteria! • Bacteria • The first organisms to produce oxygen during photosynthesis • The ultimate source of all oxygen in our atmosphere https://eapbiofield.wikispaces.com/file/detail/I11-30-cyanobacteria.jpg

  4. Banded Iron Formation

  5. This is a photograph of a slab of banded iron formation cut with a rock saw.

  6. This image uses color to represent the composition of a small part of the slab. Here, red represents the element Fe. This is a photograph of a slab of banded iron formation cut with a rock saw.

  7. Is this piece of banded iron formation more like a shale or a conglomerate? • Why are they similar? shale conglomerate http://commons.wikimedia.org/wiki/File:Limestone_on_shale.jpg http://en.wikipedia.org/wiki/File:Lehigh_conglom.jpg

  8. Model of BIF Deposition • Dissolved iron (and no oxygen) in the deep ocean • Cyanobacteria producing oxygen in the shallow ocean

  9. Another Model of BIF Deposition UV light • Dissolved iron (and no oxygen) in the deep ocean • UV light passing through the upper atmosphere with no ozone layer

  10. Another Model of BIF Deposition anoxygenic bacteria • Dissolved iron (and no oxygen) in the deep ocean • Non-oxygen producing (anoxygenic) photosynthetic bacteria in shallow water

  11. Questions • What do banded iron formations tell us about changing environments in the Earth’s oceans? • What do banded iron formations tell us about the evolution of photosynthesis? • How were changing conditions in the atmosphere and oceans related in time? How would organisms living in the shallow and deep oceans have reacted to changing environmental conditions?

More Related