2018
DOI: 10.1016/j.catena.2018.02.009
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Age-erosion constraints on an Early Pleistocene paleosol in Yukon, Canada, with profiles of 10Be and 26Al: Evidence for a significant loess cover effect on cosmogenic nuclide production rates

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Cited by 24 publications
(16 citation statements)
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“…For more than a century of glaciological research, the investigated region has been assumed to be never glaciated (Table 1), in periglacial proximity to but nevertheless beyond the limits of late Miocene (Spurr 1897;Péwé 1975;Eyles and Eyles 1989;Lagoe et al 1993;Harris 1994;Rea and Snoeckx 1995;White et al 1997;Trop and Ridgway 2007;Bill et al 2018) and subsequent Cordilleran ice sheet (CIS) glaciations of late Pliocene and thereafter (Froese et al 2000;Duk-Rodkin et al 2004, 2010Hidy et al 2013Hidy et al , 2018.…”
Section: Fig 1 (A)mentioning
confidence: 99%
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“…For more than a century of glaciological research, the investigated region has been assumed to be never glaciated (Table 1), in periglacial proximity to but nevertheless beyond the limits of late Miocene (Spurr 1897;Péwé 1975;Eyles and Eyles 1989;Lagoe et al 1993;Harris 1994;Rea and Snoeckx 1995;White et al 1997;Trop and Ridgway 2007;Bill et al 2018) and subsequent Cordilleran ice sheet (CIS) glaciations of late Pliocene and thereafter (Froese et al 2000;Duk-Rodkin et al 2004, 2010Hidy et al 2013Hidy et al , 2018.…”
Section: Fig 1 (A)mentioning
confidence: 99%
“…No evidence exists to indicate that the investigated region was ever affected by a Laurentide or other continental ice sheet (Duk-Rodkin 1999). The supposedly earliest periglacial CIS was dated to 2.64 Ma and subsequently pushed back to 2.84 Ma (Hidy et al 2013(Hidy et al , 2018, and estimates for subsequent CIS glaciations advancing toward the investigated region exist (Table 1). Duk-Rodkin and Barendregt (2011) correlated glaciological findings in northwestern Canada, and Lagoe et al (1993) followed by Gulick et al (2003) did the same for Alaska.…”
Section: Glaciological Historymentioning
confidence: 99%
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“…The wide scatter in the concentrations reflects variability in nuclide inheritance, possibly due to a shift in the sediment supply source. Since depth-profile dating requires uniform inheritance, this variability disables computing a deposition age using the singlenuclide or dual-nuclide depth-profile models (Braucher et al, 2009;Hidy et al, 2010Hidy et al, , 2018. Similarly, combining 10 Be and 26 Al for burial isochron dating (Balco and Rovey, 2008) provides no age solution due to the high and variable inheritance concentrations and insufficient time to cause a measurable deviation in the 26 Al inventory.…”
Section: Fluvial Terrace Agesmentioning
confidence: 99%