Geochemical observations may help to deduce the global level of biological activity at a certain period, or the affinity of certain fossils. For example, geochemical features of rocks may reveal when life first arose on Earth, and may provide evidence of the presence of eukaryotic cells, the type from which all multicellular organisms are built. Analyses of carbon isotope ratios may help to explain major transitions such as the Permian–Triassic extinction event.
Geochemical observations may help to deduce the global level of biological activity at a certain period or the affinity of certain fossils For example geochemical features of rocks may reveal when life first arose on Earth and may provide evidence of the presence of eukaryotic cells the type from which all multicellular organisms are built Analyses of carbon isotope ratios may help to explain major transitions such as the Permian–Triassic extinction event