Boron isotope composition of Cibicidoides wuellerstorfi in sediment core TR163-25 over the last deglaciation

Boron isotope composition of C. Wuellerstorfi at site TR163-25 used to reconstruct ocean pH over the last glacial cycle. Paired with Dd13C based oxygen reconstructions and used to reconstruct ocean alkalinity in the publication 'Alkalinity cycling rapidly buffers deep ocean pH during the last glacial cycle' (Trudgill, publication year) and asses the drivers of ocean alkalinity cycling.