The Ordovician Bioerosion Revolution was a dramatic diversification of macroboring ichnotaxa during the Middle and Late Ordovician. This was also a time during which the intensity of carbonate substrate bioerosion greatly increased, reaching a peak in the Late Ordovician and Early Silurian that was not achieved again until the Jurassic. This burst of ichnological diversity was a function of the Ordovician Radiation of marine invertebrates, and it reflects the range and rate of niche differentiation on hard substrates at that time.
RetroSearch is an open source project built by @garambo | Open a GitHub Issue
Search and Browse the WWW like it's 1997 | Search results from DuckDuckGo
HTML:
3.2
| Encoding:
UTF-8
| Version:
0.7.4