Abstract
We assess d18O‐ and Mg/Ca–based paleothermometry in relation to seasonal variations in the shell fluxes of
the surface‐dwelling planktonic foraminifera G. ruber and G. trilobus. Using deep‐moored sediment traps in the
Mozambique Channel, upstream of the Agulhas Current, we find a distinct antiphase response to the annual
cycle in sea surface temperature (SST)
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