An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary
A detailed analysis of sedimentation rates in the Upper Cretaceous-Paleocene section of pelagic limestones at Gubbio, Italy, based on the previously reported correlation of Gubbio magnetozones with the calibrated sequence of marine magnetic anomalies, suggests that the faunal overturn in planktonic...
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Columbia University
1977
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| Online Access: | https://dx.doi.org/10.7916/d8j39331 https://academiccommons.columbia.edu/doi/10.7916/D8J39331 |
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ftdatacite:10.7916/d8j39331 2023-05-15T18:00:30+02:00 An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary Kent, Dennis V. 1977 https://dx.doi.org/10.7916/d8j39331 https://academiccommons.columbia.edu/doi/10.7916/D8J39331 unknown Columbia University Geology Text Articles article-journal ScholarlyArticle 1977 ftdatacite https://doi.org/10.7916/d8j39331 2021-11-05T12:55:41Z A detailed analysis of sedimentation rates in the Upper Cretaceous-Paleocene section of pelagic limestones at Gubbio, Italy, based on the previously reported correlation of Gubbio magnetozones with the calibrated sequence of marine magnetic anomalies, suggests that the faunal overturn in planktonic foraminifera at the Cretaceous-Tertiary boundary may have happened rapidly, on the order of 10,000 yr or less. Text Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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unknown |
| topic |
Geology |
| spellingShingle |
Geology Kent, Dennis V. An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| topic_facet |
Geology |
| description |
A detailed analysis of sedimentation rates in the Upper Cretaceous-Paleocene section of pelagic limestones at Gubbio, Italy, based on the previously reported correlation of Gubbio magnetozones with the calibrated sequence of marine magnetic anomalies, suggests that the faunal overturn in planktonic foraminifera at the Cretaceous-Tertiary boundary may have happened rapidly, on the order of 10,000 yr or less. |
| format |
Text |
| author |
Kent, Dennis V. |
| author_facet |
Kent, Dennis V. |
| author_sort |
Kent, Dennis V. |
| title |
An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| title_short |
An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| title_full |
An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| title_fullStr |
An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| title_full_unstemmed |
An estimate of the duration of the faunal change at the Cretaceous-Tertiary boundary |
| title_sort |
estimate of the duration of the faunal change at the cretaceous-tertiary boundary |
| publisher |
Columbia University |
| publishDate |
1977 |
| url |
https://dx.doi.org/10.7916/d8j39331 https://academiccommons.columbia.edu/doi/10.7916/D8J39331 |
| genre |
Planktonic foraminifera |
| genre_facet |
Planktonic foraminifera |
| op_doi |
https://doi.org/10.7916/d8j39331 |
| _version_ |
1766169626467631104 |