Please use this identifier to cite or link to this item:
http://hdl.handle.net/10662/20171
Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Droser, Mary L. | - |
| dc.contributor.author | Gehling, James G, | - |
| dc.contributor.author | Jensen, Rolf Sören | - |
| dc.date.accessioned | 2024-02-07T09:33:51Z | - |
| dc.date.available | 2024-02-07T09:33:51Z | - |
| dc.date.issued | 1999 | - |
| dc.identifier.issn | 0091-7613 | es_ES |
| dc.identifier.uri | http://hdl.handle.net/10662/20171 | - |
| dc.description.abstract | 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 | es_ES |
| dc.description.sponsorship | We thank the National Geographic Society for financial support covering logistics and field work for this project. Gehling acknowledges support from a University of South Australia Australian Research Council grant. Jensen is supported by a grant from Natural Environment Research Council. Donn Gorsline,Mark Webster,and Bob Gaines facilitated X-raying the samples. | en_US |
| dc.format.extent | 4 p. | es_ES |
| dc.format.mimetype | application/pdf | en_US |
| dc.language.iso | eng | es_ES |
| dc.subject | Icnofósiles | es_ES |
| dc.subject | Trace fossils | es_ES |
| dc.subject | Bioturbación | es_ES |
| dc.subject | Bioturbation | es_ES |
| dc.subject | Australia | es_ES |
| dc.subject | Cambrico | es_ES |
| dc.subject | Cambrian | es_ES |
| dc.title | When the worm turned: Concordance of Early Cambrian ichnofabric and trace-fossil record in siliciclastic rocks of South Australia | es_ES |
| dc.type | article | es_ES |
| dc.description.version | peerReviewed | es_ES |
| europeana.type | TEXT | en_US |
| dc.rights.accessRights | closedAccess | es_ES |
| dc.subject.unesco | 2416 Paleontología | es_ES |
| europeana.dataProvider | Universidad de Extremadura. España | es_ES |
| dc.identifier.bibliographicCitation | Mary L. Droser, James G. Gehling, Sören Jensen; When the worm turned: Concordance of Early Cambrian ichnofabric and trace-fossil record in siliciclastic rocks of South Australia. Geology 1999;; 27 (7): 625–628. doi: https://doi.org/10.1130/0091-7613(1999)027<0625:WTWTCO>2.3.CO;2 | en_US |
| dc.type.version | publishedVersion | es_ES |
| dc.contributor.affiliation | University of California. USA | en_US |
| dc.contributor.affiliation | Queen’s University. Canada | en_US |
| dc.contributor.affiliation | University of Cambridge. UK | en_US |
| dc.relation.publisherversion | http://doi.org/10.1130/0091-7613(1999)027<0625:WTWTCO>2.3.CO;2 | es_ES |
| dc.identifier.doi | 10.1130/0091-7613(1999)027<0625:WTWTCO>2.3.CO;2 | es_ES |
| dc.identifier.publicationtitle | Geology | es_ES |
| dc.identifier.publicationfirstpage | 625 | es_ES |
| dc.identifier.publicationlastpage | 628 | es_ES |
| dc.identifier.publicationvolume | 27 | es_ES |
| dc.identifier.e-issn | 1943-2682 | es_ES |
| dc.identifier.orcid | 0000-0001-5136-9586 | es_ES |
| Appears in Collections: | DBVET - Artículos | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| 0091-7613_1999_27_625.pdf ???org.dspace.app.webui.jsptag.ItemTag.accessRestricted??? | Droser_etal_1999_Geology | 464,55 kB | Adobe PDF | View/Open Request a copy |
This item is licensed under a Creative Commons License
