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The evaporation path of seawater and the coprecipitation of Br (super -) and K (super +) with halite
Precise chronology of the last interglacial period: 234 U- 230 Th data from fossil coral reefs in the Bahamas
Quaternary Eustatic Sedimentary Accretion of Southern Bahamas Archpelago: ABSTRACT
Figure 3. Plots of major ions measured from fluid inclusions in halite from...
Overlapping species boundaries and hybridization within the Montastraea “ annularis ” reef coral complex in the Pleistocene of the Bahama Islands
Dactyloidites ottoi (Geinitz, 1849) in Bahamian Pleistocene carbonates: a shallowest-marine indicator
Abstract The rosetted trace fossil Dactyloidites ottoi ( Geinitz, 1849 ) is reported and described for the first time from late Pleistocene (MIS 5e) carbonates of the Bahama Archipelago in shallowing-upward, shelly calcarenites from Great Inagua and Great and Little Exuma islands. The distinctive, fan-shaped D. ottoi specimens from the Bahamas, while not preserved in fine detail and not revealing a shaft, compare favourably in shape and size with specimens from other localities around the world, including the oldest well-documented specimens from the Jurassic of Argentina. D. ottoi is interpreted as a fodinichnion formed by the activity of a deposit-feeding worm, probably a polychaete, consuming marine-plant remains within host sediment. The late Pleistocene palaeodepositional environment of these carbonate sediments is interpreted as within the lower foreshore–upper shoreface zone in full marine, tropical waters. This discovery of D. ottoi marks an addition to the Bahamian shallow-marine ichnocoenose within the Skolithos ichnofacies.