Echinoderm palaeoecology from fragments: a tool for facies recognition in mesozoic carbonate sequences
Echinoderms such as crinoids (sea lilies), are a major component of the marine benthos from the late Palaeozoic onwards, where they occurred in such high number so as to be rock forming. On death echinoderms will typically disarticulate into many thousands of ossicles which are considered by many pa...
| Main Author: | |
|---|---|
| Format: | Conference Paper |
| Published: |
2011
|
| Online Access: | http://hdl.handle.net/20.500.11937/16291 |