Abstract
The end of the Proterozoic Eon was a time of pronounced biological, biogeochemical, climatic and tectonic change. New bio- and chemostratigraphic data provide an improved framework for stratigraphic correlation, making possible a deeper understanding of latest Proterozoic Earth history and providing tools for a chronostratigraphic division of late Proterozoic time.
| Original language | English |
|---|---|
| Pages (from-to) | 673-678 |
| Number of pages | 6 |
| Journal | Nature |
| Volume | 356 |
| Issue number | 6371 |
| Publication status | Published - 1992 |