Sea-Level Highstand Chronology from Stable Carbonate Platforms (Bermuda and the Bahamas)

A history of sea-level highstands representing the past 1.2 my is assembled from geological and geochronological data from Bermuda and the Bahamas. Outcrops of marine and eolian limestones exhibit sea-level indicators on tectonically stable islands. Because of the low-lying nature of the islands, they preserve a record of both highstand (limestone) and lowstand (paleosol) events. Geomorphology and sequence stratigraphy are critical for ranking deposit age, while U-series, amino acid racemization (AAR), electron spin resonance (ESR), and paleomagnetics have provided absolute and relative age estimates. In Bermuda, two early Pleistocene marine sequences are estimated to be > 700 ka and > 880 ka. The younger of the two is associated with a +22 m marine terrace cut into the older Walsingham Fm, which exposes marine limestones at < + 5 m a.s.l. During the latter half of the middle Pleistocene (Stages 11, 9, and 7; 500 to 180 ka), sea level rose above the present at least three times to approximately + 4 m, + 4 m, and + 2.5 m, respectively. Stage 5e includes at least two major positive oscillations of sea level (early at + 4 m and late at > + 6 m). The two 5e marine units are separated by an extensive, rubified protosol, interpreted as evidence of a minor regression (interstadial) of several thousand years. The late Sangamonian (Southampton Fm) is characterized by an extensive skeletal eolianite on high-energy shorelines, offlapped bya-lmto+lm marine deposit dated at ca. 85 ka. There is no evidence to support a Holocene sea level rising significantly above the present datum. Unlike tectonic coastline and isotopic studies that require major assumptions of constant uplift and temperature/ice-volume/salinity in order to calculate ancient sea levels, precise elevations of paleo-seduced can be obtained from deposits on stable carbonate platforms. Regardless, the inexact models provided by deep- sea oxygen isotope and U-series dating of uplifted reef terraces are valuable to establish a framework for the timing, duration and relative magnitude of Quaternary high sea levels.