“…Here we present a late Holocene storminess and climate record from Bermuda based on costratigraphic signals of terrestrial erosion and oxygen isotopic ratios of benthic foraminifera (δ 18 O c ) archived in Walsingham Cavern, a Bermudian submarine cave. Submarine cave environments exhibit a global distribution across Atlantic [ Rasmussen and Brett , ; Ohtsuka et al ., ; Ortiz et al ., ], Pacific [ Ohtsuka et al ., ; Luter et al ., ; Kano and Kase , ], and Mediterranean [ Zabala et al ., ; Airoldi and Cinelli , ; Corriero et al ., ; Surić et al ., ] coastal carbonate landscapes, and their submerged speleothems have been used in sea level research for decades [ Spalding and Matthews , ; Richards et al ., ; Dutton et al ., ; Surić et al ., ].…”