In this paper, we formally define a series of bioclastic eolianites and protosols exposed on
high-energy bank margins throughout the Bahamas archipelago as the Whale Point …

We describe in detail a unique succession of Lower Pleistocene shallow-water carbonates
exposed at the Misery Point sea cliff along the northern shoreline of Mayaguana Island (SE …

Abstract Throughout the Pliocene and Pleistocene, a hierarchy of sea-level fluctuations
alternately flooded and exposed the Great Bahama Bank, controlling its sedimentary …

Landward-pointing V-shaped sand ridges several kilometers long are common along the
windward margin of the Bahama Islands. Their axes share a northeast–southwest trend …

The geology of the Last Interglaciation (sensu stricto, marine isotope substage (MIS) 5e) in
the Bahamas records the nature of sea level and climate change. After a period of quasi …

During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas
margin from marginal to deep basin environments was an essential requirement for the …

Paleorecords and modeling studies suggest that instabilities in the Atlantic Meridional
Overturning Circulation (AMOC) strongly affect the low-latitude climate, namely via …

Surficial deposits of the Bahama islands consist of late Quaternary limestones that were
deposited during glacioeustatic highstands of sea level. Other than marine deposits formed …

The Bahama Islands offer a unique opportunity to examine Late Quaternary sea-level
position, as the island group places significant constraints on the time and space boundary …

Abstract 87Sr/86Sr-dated marine and beach sediments exposed along the north shore of
Mayaguana Island (Bahamas) provide new estimates of the elevation of high sea stands …