“…Prior to 2000, the only CRMs available for PGEs were geological in origin, e.g. SARM-7, mineralized ore [15,16]; TDB-1, diabase [17,18]; WPR-1, altered peridotite diabase [17,18], etc. These CRMs were unsatisfactory for environmental measurements, as concentrations were much higher, commonly in the mg kg À1 range, than those found in sediment, dusts, soil, or airborne particulate matter and there was little similitude between the geologic and environmental matrices.…”