Anomalous MIS 7 sea level recorded on Bermuda

• New U-series dates for coral fragments confirm a MIS7 age for emergent, Belmont Formation, marine deposits on Bermuda.
• New sedimentary evidence reliably establishes the elevation of relative palaeo-sea-levels.
• First description of widespread Quaternary faulting in Bermuda.
• The concept of Bermuda as a stable “tide-gauge” for Quaternary sea-level is challenged.

Three new U-series ages from coral fragments found in the Belmont Formation of Bermuda fall in a range of ∼198 ka to ∼196 ka. These late MIS 7 ages are consistent with those of ∼201 ka and ∼199 ka measured in a previous study. The disputed interpretation of the Belmont Formation as a unit that is allostratigraphically distinct from subsequent MIS 5e deposits, of the Rocky Bay Formation, is vindicated by a minimum age of 196 ± 3 ka for the total of 6 coral fragments it has yielded. Emergent marine deposits of the Belmont Formation include sedimentary lithofacies that are considered to be reliable relative sea level indicators. Prominent among these is a facies representing the “beach step”: a feature that develops sub-tidally, directly at the base of the swash zone. From this facies, and others preserved along 6 km of Belmont Formation coastal exposure, it is concluded that MIS 7 relative mean sea level reached +4.5 m, and likely peaked at or above +6.0 m, relative to present sea level at Bermuda. Lower MIS 7 sea level positions that are evidenced and that have been quoted, in the past, are considered transitory positions, not maxima. The MIS 7 sea-level elevations on Bermuda, reconstructed in this study, are above the majority of those reported from elsewhere in the world. This challenges the long-standing notion of Bermuda as a vertically stable “tide-gauge”, but is consistent with glacio-hydroisostatic models which predict land-mass subsidence at intermediate field sites, such as Bermuda, at the end of long interglacials. However, because of evidence of instability at Bermuda in the form of seismic activity and faulting, which require further investigation, judgement is reserved on the global implications of this palaeo-sea-level anomaly.