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In response to the comment of Madsen and Liu (2018), we explain why our quartz optically stimulated luminescence (OSL) ages showing the early MIS 3 lake highstand are robust. We also demonstrate that the difference in the age estimates between ours (Long et al., 2018) and other studies should be attributed to contrasting equivalent dose (De) values, rather than water contents (hence the dose rate) which was claimed by Madsen and Liu (2018).
Original languageEnglish
JournalQuaternary Geochronology
Pages (from-to)14-15
Publication statusPublished - 2019
CitationsWeb of Science® Times Cited: No match on DOI

ID: 164668616