This research not only provides the first clear evidence that microorganisms were directly involved in the deposition of Earth's oldest iron formations; it also indicates that large populations of oxygen - producing cyanobacteria were at
work in the shallow areas of the ancient oceans, while deeper water still reached by the light (the photic zone) tended to be populated by anoxyenic or micro-aerophilic iron - oxidizing bacteria which formed the iron deposits.
Not exact matches
Buildings used to be designed with the climate
in mind with big opening windows to the exterior; shading and bris de soliel to the south;
shallow working areas to maximize exposure to natural light.
Excited and bounding with energy, the child
worked on some new moves for a few minutes and then she proceeded to dive again
in the
shallow area.