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- W2000964854 abstract "Solution conduits or caves can provide a measure of glacio-eustatic sea level position for the Quaternary. In high latitudes, cave deposits contain artifacts, fossils and sediments that reflect surface conditions with respect to climate. Secondary calcite deposits, most notably stalagmites, record growth episodes during ice minima and non-growth during ice maxima. They provide an indirect estimate of areal ice cover at high latitudes, and are an indirect measure of sea level. In low latitudes, stable carbonate platforms contain caves that provide a direct measure of past sea level position. Solution conduits developing in a fresh water lens will record the position of the lens and therefore sea level. As sea level fluctuates, fresh water lens horizons and conduit development horizons will shift, preserving a record of past sea level position. Cave wall rock and cave deposits can produce a chronology for given conduit positions. Secondary calcite deposits, notably stalagmites, record growth periods during sea level low stands (or ice maxima) and record growth hiatuses during flooding by sea level high stands (or ice minima); the inverse of high latitude stalagmites. Lighthouse Cave, San Salvador Island, Bahamas, records a sea level high stand at +1 to +6 m for some time period between 85,000 and 70,000 years ago, based on position and timing of conduit development; and records sea level at present elevation for some time period between 49,000 and 37,000 years ago, based on a stalagmite with a marine overgrowth." @default.
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- W2000964854 date "1988-01-01" @default.
- W2000964854 modified "2023-09-25" @default.
- W2000964854 title "Solution conduits as indicators of late Quaternary sea level position" @default.
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- W2000964854 doi "https://doi.org/10.1016/0277-3791(88)90093-5" @default.
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