Corrigendum to “Last glacial tephra layers in the Talos Dome ice core (peripheral East Antarctic Plateau), with implications for chronostratigraphic correlations and regional volcanic history” [Quaternary Sci. Rev. 165 (2017) 111–126] (S0277379116303833) (10.1016/j.quascirev.2017.04.025))

Biancamaria Narcisi, Jean Robert Petit, Antonio Langone

Research output: Contribution to journalComment/debate

Abstract

When this paper was originally published there was an error in Table 1. The age of the TD sample 914 should be 26.16 ± 0.71 (not 21.16 ± 0.71). The correct Table 1 is printed below: Table 1. Major element composition of glass shards from TALDICE tephra horizons determined by electron microprobe analysis. Data in weight percent (wt%) are recalculated to a sum of 100 wt% and are presented as mean and one standard deviation of n analyses of different glass shards. Original oxide totals before recalculation are also given. Total iron expressed as FeO. -a, -b, etc. denote separate populations of glass inside samples. Based on measurements of reference glasses, typical analytical errors (RSD) are as follows: <1% for SiO2; 1–2% for CaO, Al2O3, K2O; 2–3% for FeO; 3–6% for MnO, TiO2; 2–9% for NaO2and MgO. Rock type after TAS plot (Rickwood, 1989, and references therein). Age of tephras are based on AICC2012 timescale (Veres et al., 2013). [Table presented]
Original languageEnglish
Pages (from-to)142 - 143
Number of pages2
JournalQuaternary Science Reviews
Volume172
DOIs
Publication statusPublished - 15 Sep 2017
Externally publishedYes

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All Science Journal Classification (ASJC) codes

  • Global and Planetary Change
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Archaeology
  • Geology

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