作者: Shawna N. Little , Peter J. van Hengstum
DOI: 10.1016/J.MARMICRO.2019.03.005
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摘要: Abstract Coastal karst aquifers have an upper meteoric water mass stratified from a saline groundwater below that increasingly mix and discharge towards the ocean. Preserved sediment in caves sinkholes provide opportunity to evaluate long-term hydrodynamics local coastal aquifer (e.g., salinity, oxygenation, vertical displacement response sea-level forcing). Here we of shallow ( 45 μm versus >63 μm mesh sieve fractions. These modern analog results can be used interpret subfossil benthic foraminiferal records aquifers, especially during early cave inundation by concomitant rise.