“…Radionuclides and isotopically labelled particles are usually quantified using alpha or gamma spectrometry (Goldberg & Koide 1962, Thomson et al 2000, Schmidt et al 2007), while metal-doped sediment particles are analyzed using instrumentation neutron activation analysis , and chl a using HPLC (Sun et al 1991, Gérino et al 1998). All visually distinguishable tracers, such as microtektites, glass beads, microtaggants and luminophores, are either classically counted under a dissecting microscope (Glass et al 1973, Wheatcroft 1991, Blair et al 1996, Madsen et al 1997, Fernandes et al 2006), or quantified using automated image acquisition and analysis techniques (Gilbert et al 2003, Solan et al 2004, Maire et al 2006). The quantification of particle tracers within the sediment column can become difficult when their distribution is patchy or when the concentration approaches the detection limit.…”