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Late Pleistocene and Early Holocene aeolian deposits of Tasmania and their climatic implications – Corrigendum

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In the original publication of McIntosh et al. (2020), calibrated C ages in Table 1 were calculated from the OxCal IntCal13 curve. They should have been calculated from the Oxcal… Click to show full abstract

In the original publication of McIntosh et al. (2020), calibrated C ages in Table 1 were calculated from the OxCal IntCal13 curve. They should have been calculated from the Oxcal SHCal20 (southern hemisphere) curve (Hogg et al. 2020). Correct calibrated ages are shown in the fourth column of the table below. When quoting C ages from Table 1 or from the text of McIntosh et al. (2020) the values in column 4 of the table below should be used. The correction of calibrated C ages is minor and does not affect the interpretations and conclusions of McIntosh et al. (2020). REFERENCES

Keywords: calibrated ages; holocene aeolian; pleistocene early; mcintosh 2020; early holocene; late pleistocene

Journal Title: Quaternary Research
Year Published: 2021

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