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Bermuda Station S hydrography shows the oxygen isotope ratio that a foram would have if it deposited its shell in equilibrium with the annual average sea surface temperature and salinity observed since 1954 at Station S near Bermuda. The large decrease in sea surface temperature and increase in salinity in the late 1960s was caused by unusually unpleasant weather those years. (Temperature and salinity data provided by Terry Joyce)[back]
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