Figure 10.1 Time scale and tempo of early animal evolution: the key metazoan groups are shown with the putative age of their last common ancestor, together.
Earth’s climate history. Cenozoic cooling CaCO 3 is taken up by marine organisms Coccolithophorid Foraminifer.
Carbon Isotope Variations in Aquatic Plants: Applications Onshore-Offshore (Benthic vs. Pelagic?) Kelp forest ecology Decreased productivity in the Bering.
Lecture 12: Global Redox Balance/Causes of the rise of O 2 Abiol 574 Global redox balance Causes of the Great Oxidation Event.
Earth’s climate history
