M. crassatus HOZ zone
40 - 38.1 Ma
The definition of this interval in the timescale Planktic Foraminiferal Zones is taken from the following source:
- B. S. Wade, P. N. Pearson, W. A. Berggren and H. Pälike. 2011. Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale. Earth-Science Reviews 104(1-3):111-142 view
There are intervals in 10 timescales which overlap this one. show
This interval is used in the definition of 20 collections
A total of 1904 collections with 23781 occurrences lie within this time span
| International Chronostratigraphic Timescale | Planktic Foraminiferal Zones | |||
|---|---|---|---|---|
| 22.96 | ||||
| Paleogene | Oligocene | Chattian | P. pseudokugleri LOZ | 23.04 |
| G. ciperoensis PRZ | 25.2 | |||
| P. opima HOZ | 26.9 | |||
| Rupelian | 27.3 | |||
| G. angulisuturalis/C.cubensis CRZ | 28 | |||
| D. sellii PRZ | 29.2 | |||
| T. ampliapertura HOZ | 30.3 | |||
| P. naguewichiensis HOZ | 32 | |||
| H. alabamensis HOZ | 33.8 | |||
| Eocene | Priabonian | 33.9 | ||
| G. index HOZ | 34.3 | |||
| G. semiinvoluta HOZ | 35.8 | |||
| Bartonian | 37.71 | |||
| M. crassatus HOZ | 38.1 | |||
| O. beckmanni TRZ | 40 | |||
| M. lehneri PRZ | 40.5 | |||
| Lutetian | 41.03 | |||
| A. topilensis PRZ | 42.3 | |||
| G. kugleri/M. aragonensis CRZ | 43.6 | |||
| G. nuttalli LOZ | 44.4 | |||
| A. cuneicamerata LOZ | 46.4 | |||
| Ypresian | 48.07 | |||
| A. pentacamerata PRZ | 50.4 | |||
| M. aragonensis/M. subbotinae CRZ | 50.8 | |||
| M. formosa LOZ | 52.3 | |||
| M. marginodentata PRZ | 54 | |||
| P. wilcoxensis/M. velascoensis CRZ | 54.5 | |||
| A. sibaiyaensis LOZ | 55.4 | |||
| M. velascoensis PRZ | 55.5 | |||
| G. pseudomenardii TRZ | 55.9 | |||
| Paleocene | Thanetian | 56 | ||
| Selandian | 59.24 | |||
| M. angulata LOZ | 59.4 | |||
| P. uncinata LOZ | 61 | |||
| E. edita PRZ | 61.4 | |||
| Danian | 61.66 | |||
| P. eugubina TRZ | 64.8 | |||
| G. cretacea PRZ | 64.97 | |||
| Abathomphalus mayaroensis | 65 | |||
| 66 | ||||
| 68.6 | ||||