This study presents a global analysis of seafloor roughness derived from marine gravity data and finds that residual roughness anomalies remain over large swaths of ocean floor. The Atlantic ocean floor that formed over mantle previously overlain by the Pangaea supercontinent displays anomalously low roughness, and attribute this observation to a sub-Pangaean supercontinental mantle temperature anomaly leading to slightly thicker than normal Atlantic crust. In contrast, ocean crust formed above Pacific superswells is not associated with basement roughness anomalies.
- Joanne M. Whittaker
- R. Dietmar Müller
- Walter H. F. Smith