Murat (1972) reported that the Eze-Aku Shale reflects deposits of marine condition in a tectonically controlled basin and the sandstone deposits marked a period of regression, while the shale deposits indicate a period of transgression.
The lower member of the Culebra Formation, dated between 23 and 21 Ma, indicates a local transgression during this interval, which is opposite from their global sea-level curve, which shows a lowering of sea level during this interval [67].
The results indicate an involvement of the Pc-G and trx-G genes: in Pc 3 /+ discs, the number and size of lineage transgressions is greatly increased with respect to controls, whereas in trx E2 /+ discs there are very few lineage transgressions.
In the experimental discs, the transgressions are greatly reduced, clearly indicating a requirement for JNK function.
Distances larger than this value indicate transgression (if both hybrid-parents are larger than expected).
Offshore facies are common in the northern end of the facies model, whereas it is also seen within the central eastern part of the model indicating possible transgression of the offshore facies toward the land.
H/L indicates whether transgression occurs with values higher and lower than the parents.
Overlap of wave agitated shoreface shelf sediments on the glaciogenic sediments indicates widespread marine transgression caused by glacier melting during ice house to green house climatic transition, and crustal downsagging related to glacioisostasy.
Since the A compartment was not in need of reconstruction, this observation indicates that the transgressions are caused by a transient collapse of the A/P boundary, which affects the two compartments.
Finally, according to the RDs the weak association with time of the day indicated that group transgressions were more likely to be observed in the morning, whereas pedestrians transgressing alone were associated with afternoon hours.
