Supplemental Material: Gamma-ray attenuation bulk density as an indicator of diatom valve abundance and fragmentation in Pleistocene biosiliceous sediments of the Bering Sea

Table S1: Site U1340 (53.4°N, 179.52°W) newly generated laser particle size data and smear slide count data, and Table S2: Site U1339 (53.67°N, 169.97°W) newly generated laser particle size data and smear slide count data.