Identificador persistente para citar o vincular este elemento:
http://hdl.handle.net/10662/20171
| Títulos: | When the worm turned: Concordance of Early Cambrian ichnofabric and trace-fossil record in siliciclastic rocks of South Australia |
| Autores/as: | Droser, Mary L. Gehling, James G, Jensen, Rolf Sören |
| Palabras clave: | Icnofósiles;Trace fossils;Bioturbación;Bioturbation;Australia;Cambrico;Cambrian |
| Fecha de publicación: | 1999 |
| Resumen: | Studies of sedimentary fabrics and trace fossils across the Precambrian-Cambrian interval in South Australia demonstrate that the appearance of Treptichnus pedum,which defines the base of the Cambrian, also marks the initial development of preservable infaunal activity. There is a significant shift in the amount and nature of bioturbation at this time. These results support the broad-scale utility of T. pedum as the indicator of the base of the Cambrian |
| URI: | http://hdl.handle.net/10662/20171 |
| ISSN: | 0091-7613 |
| DOI: | 10.1130/0091-7613(1999)027<0625:WTWTCO>2.3.CO;2 |
| Colección: | DBVET - Artículos |
Archivos
| Archivo | Descripción | Tamaño | Formato | |
|---|---|---|---|---|
| 0091-7613_1999_27_625.pdf ???org.dspace.app.webui.jsptag.ItemTag.accessRestricted??? | Droser_etal_1999_Geology | 464,55 kB | Adobe PDF | Descargar Pide una copia |
Este elemento está sujeto a una licencia Licencia Creative Commons
