“…The earliest maize macroremains, for example, date to the Middle Formative Machalilla phase (La Ponga site, 1200-800 BC, uncalibrated, [11]) and subsequent Late Formative Chorrera phase (sites in the Jama River valley, [24]); while microfossil evidence begins in the preceramic Vegas tradition (dated just prior to 5000-4700 BC, uncalibrated, [27,32,37,38]) and continues during the subsequent Valdivia tradition (Real Alto, 4400 to 1800 BC, calibrated, [17]; see also [19][20][21][22]; La Emerenciana, 2200-1900 BC, calibrated, [36]) and into the late Formative and after (see [23] for an overview of paleoethnobotanical data for the region). It is only in late Formative, Chorrera contexts and after, that charred maize remains become somewhat more common at sites, and this is not true of all sites.…”