NEIGE, P., MARCHAND, D., BONNOT, A. (1997) Ammonoid morphological signal versus sea-level changes. Geological Magazine, 134 (2) 261-264 doi:10.1017/s0016756897006687
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Ammonoid morphological signal versus sea-level changes | ||
| Journal | Geological Magazine | ||
| Authors | NEIGE, P. | Author | |
| MARCHAND, D. | Author | ||
| BONNOT, A. | Author | ||
| Year | 1997 (March) | Volume | 134 |
| Issue | 2 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756897006687Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 257288 | Long-form Identifier | mindat:1:5:257288:2 |
| GUID | 0 | ||
| Full Reference | NEIGE, P., MARCHAND, D., BONNOT, A. (1997) Ammonoid morphological signal versus sea-level changes. Geological Magazine, 134 (2) 261-264 doi:10.1017/s0016756897006687 | ||
| Plain Text | NEIGE, P., MARCHAND, D., BONNOT, A. (1997) Ammonoid morphological signal versus sea-level changes. Geological Magazine, 134 (2) 261-264 doi:10.1017/s0016756897006687 | ||
| In | (1997, March) Geological Magazine Vol. 134 (2) Cambridge University Press (CUP) | ||
| Abstract/Notes | The morphological diversity, considered as a biological signal, of a series of four Upper Callovian (Middle Jurassic) ammonite populations of Côte-d’Or (France) is quantified. These populations fall within two third-order sequences of a second-order transgression. A sampling method that adheres as closely as possible to the morphological characteristics of the populations is established. It is valuable in that it eliminates the subjectivity related to taxonomy to allow more objective comparisons between the biological signal (shell morphology) and the physical signal (eustasy). | ||
See Also
These are possibly similar items as determined by title/reference text matching only.
 | |
 | |
 | |
 | |
| |
 | |
 | |
 | |
| |
 | |
 |