A New Reference Model for the Evolution of Oceanic Lithosphere in a Cooling Earth

We present a new reference model for the evolution of oceanic lithosphere, which incorporates the effects of incomplete viscous relaxation, radiogenic heating, and secular cooling. The new reference model is based solely on thermal conduction, that is, without involving the occurrence of small-scale convection, and unlike the plate model, it does not contain unphysical boundary conditions. Yet, our model can explain both bathymetry and the heat flow data on the normal seafloor. The success of the new model owes to the use of realistic material properties in conduction modeling as well as the consideration of all of major processes that take place ubiquitously beneath seafloor. The effect of secular cooling on the bathymetry of old seafloor is particularly notable. Whereas secular cooling brings only weak temperature variations with an amplitude of similar to 20 K, it can nonetheless affect global bathymetry substantially owing to the deep sensitivity of long-wavelength topography kernels. We suggest that the well-known fact that Earth has been cooling, which was not considered in any of previous reference models, may be the key to the long-standing puzzle of seafloor flattening. The new reference model is expected to be useful to better quantify the impact of the emplacement of hotspot islands and oceanic plateaus, the effect of small-scale convection, and the regional history of secular cooling in the convecting mantle.

Automated summary

The new reference model for the evolution of oceanic lithosphere is based on thermal conduction and realistic material properties, explaining bathymetry and heat flow data on normal seafloor successfully, with particular emphasis on the notable impact of secular cooling on old seafloor bathymetry.