Discovery of a submerged relic reef and shoreline off Grand Cayman: further support for an early Holocene jump in sea level

Drilling close to the base of a submerged sea-cliff on the terraced eastern shelf of Grand Cayman has revealed a relic Acropora palmata reef at a depth of 21 in below msl. Ten cores from its crest are principally composed of cobble-sized clasts of A. palmata set in a matrix of cemented skeletal grainstone. The clasts have a distinctive succession of encrusters that indicate rapid burial: a photophilic association of crustose coralline algae, foraminifera and vermetid gastropods superimposed by a cryptic association of sclerosponges, foraminifera and serpulids. In addition to rapid burial, U-Th thermal ionization mass spectrometer (TIMS) dating of coral clasts within I in of the relic-reef surface indicates minor temporal mixing with ages between 8.9 and 8.1 ka. Such mixing and rapid burial is consistent with a hurricane deposit and is identical to deposits found on the crests of modern reefs. In relation to its age, the preservation of a - 18.5-m intertidal notch cut into the submerged sea-cliff on the,western shelf of Grand Cayman implies that the crest of the relic reef has been lowered 1.5-2 in by marine abrasion,/ bioerosion at a rate of similar to 0.25 mm yr(-1). Reconstructing this eroded section using average Holocene accretion rates indicates that the reef likely ceased accreting at similar to 7.6 ka at a depth of similar to 19 in. Comparing these data with other relic reefs in the Caribbean indicates that the relic reef on Grand Cayman died within 160 years of relic reefs on Barbados, St. Croix, St. Thomas and north Florida. This narrow interval of reef demise also coincides with the time when modem reefs were establishing themselves some 4-9 m higher upslope-a fact that can only be resolved by invoking a rapid 6-m jump in sea level similar to 7.5 ka ago. Such a jump would also account for two unexplained events around this time: the restricted interval of global delta initiation and the catastrophic flooding of the glacially lowered Black Sea. (C) 2002 Elsevier Science B.V. All rights reserved.