Changes

* Numerical ages for rate-dependent analyses

* Numerical ages for rate-dependent analyses

==Chronostrati-graphic correlation==

==Chronostratigraphic correlation==

The sequence stratigraphy model postulates a worldwide succession of depositional events such as coastal onlap and oceanic anoxic events<ref name=ch17r5>Arthur, M., A., Dean, W., E., 1986, Cretaceous paleoceanography, in Tucholke, B., E., Vogt, P., R., eds., Decade of North American Geology, Western North Atlantic Basin Synthesis Volume: Geological Society of America, p. 617–630.</ref> primarily reflecting global cyclic changes in eustatic sea level. This succession ideally is represented by a sea level onlap-offlap curve such as the Haq et al.<ref name=ch17r43>Haq, B., U., Hardenbol, J., Vail, P., R., 1988, Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change, in Wilgus, C., K., Hastings, B., S., Kendall, C., G. St. C., Posamentier, H., W., Ross, C., A., Van Wagoner, John C., eds., Sea-level Change: An Integrated Approach: SEPM Special Publication 42, p. 71–108.</ref> cycle chart.

The sequence stratigraphy model postulates a worldwide succession of depositional events such as coastal onlap and oceanic anoxic events<ref name=ch17r5>Arthur, M., A., Dean, W., E., 1986, Cretaceous paleoceanography, in Tucholke, B., E., Vogt, P., R., eds., Decade of North American Geology, Western North Atlantic Basin Synthesis Volume: Geological Society of America, p. 617–630.</ref> primarily reflecting global cyclic changes in eustatic sea level. This succession ideally is represented by a sea level onlap-offlap curve such as the Haq et al.<ref name=ch17r43>Haq, B., U., Hardenbol, J., Vail, P., R., 1988, Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change, in Wilgus, C., K., Hastings, B., S., Kendall, C., G. St. C., Posamentier, H., W., Ross, C., A., Van Wagoner, John C., eds., Sea-level Change: An Integrated Approach: SEPM Special Publication 42, p. 71–108.</ref> cycle chart.