Faculty Publications
Corrigendum To “Revised Quaternary Glacial Succession And Post-Lgm Recession, Southern Wind River Range, Wyoming, Usa” (Quaternary Science Reviews (2018) 192 (167–184), (S027737911830026X), (10.1016/J.Quascirev.2018.05.020))
Document Type
Article
Journal/Book/Conference Title
Quaternary Science Reviews
Volume
212
First Page
219
Last Page
220
Abstract
When this paper was originally published, there was an error in the second from last sentence of the Abstract. The correct sentence should read: “From this evidence, the Temple Lake Alloformation of the Wind River Mountains now should correspond to the INTIMATE GS-2.1a (Oldest Dryas) stadial event while the Alice Lake Alloformation should correspond roughly to the INTIMATE GS-1 stadial (IACP-Younger Dryas).” The authors also inadvertently omitted from the discussion and Figure 9 the estimates for the re-advances of glaciers in the Sierra Nevada (California, USA) during Tioga-4 (∼16.2 ka) and Recess Peak (∼13.3 ka) reported by Phillips (2016, 2017). Please find the corrected references and Figure 9 below: References: Phillips, Fred M., 2016. Cosmogenic nuclide data sets from the Sierra Nevada, California, for assessment of nuclide production models: I. Late Pleistocene glacial chronology. Quat. Geochron. 35, 119–129. DOI: http://doi.org/10.1016/j.quageo.2015.12.003. Phillips, F., 2017. Glacial chronology of the Sierra Nevada, California, from the last Glacial Maximum to the Holocene. Cuad. de Invest. Geogr. 43 (2), 527–552. DOI: http://doi.org/10.18172/cig.3233. [figure-presented] Fig. 9 Summary of chronologies for Lateglacial-Holocene glacial activity in the Wind River Range [Fremont Lake Type Area (FLTA), Sinks Canyon, North Fork Canyon, Helen Lake, Bigfoot Lake, Temple Lake Type Locality (Marcott, 2011) and Titcomb Basin] normalized to the GISP2 2-m 18O record (Stuiver et al., 1995). Error bars approximate 1-sigma un-certainties. Grey dots represent individual 10Be exposure ages from Alice Lake moraines; black dots represent individual exposure ages from Temple Lake moraines. Black triangles represent exposure ages from terminal moraines at the FLTA and Pine Bar Ranch; open triangles represent ages from moraines PD-2 and PD-3 in Sinks Canyon and moraines DP-1 and DP-2 in North Fork Canyon. Solid grey and black squares represent unweighted arithmetic averages of ages on moraine groups mapped as ‘Alice Lake’ and ‘Temple Lake’. YD = Younger Dryas (GS-1 event of Rasmussen et al., 2014); IACP = Intra-Allerød Cold Period; BA = Bølling/Allerød; OD = Oldest Dryas (GS-2.1a event of Rasmussen et al., 2014). Ages for the Fremont Lake Type Area (FLTA) and Titcomb Lake are from Shakun et al. (2015). Average ages for the SE Alps are generalized from Ivy-Ochs (2015; personal oral communication, 2016) and Böhlert et al. (2011); average age estimates shown for the Sierras (CA) are from Phillips (2016, 2017). The age of Heinrich Event-1 is from Hemming (2004) and Rood et al. (2011).
Department
Department of Geography
Original Publication Date
5-15-2019
DOI of published version
10.1016/j.quascirev.2019.03.029
Repository
UNI ScholarWorks, Rod Library, University of Northern Iowa
Language
en
Recommended Citation
Dahms, Dennis; Egli, Markus; Fabel, Derek; Harbor, Jon; Brandová, Dagmar; de Castro Portes, Raquel; and Christl, Marcus, "Corrigendum To “Revised Quaternary Glacial Succession And Post-Lgm Recession, Southern Wind River Range, Wyoming, Usa” (Quaternary Science Reviews (2018) 192 (167–184), (S027737911830026X), (10.1016/J.Quascirev.2018.05.020))" (2019). Faculty Publications. 507.
https://scholarworks.uni.edu/facpub/507
