Dating Deglaciation


photograph: R. Farrell - Alaska 2015

Age vs Latitude Plots

Sea Level Rise due to the Last Glacial Maximum

figure: Sea level and global ice volumes from the Last Glacial Maximum to the Holocene - Kurt Lambeck, Hélène Rouby, Anthony Purcell, Yiying Sun, and Malcolm Sambridgehttps://site.uvm.edu/geomorphology/files/2020/11/Lambeck-et-al.-2014-PNAS.pdf

Since there is a lag time with radiocarbon dating due to the delay in deposition of organic material, cosmogenic dating may offer a more accurate result. The figure of sea level and global ice volumes shows a spike in sea level between 20,000 to 15,000 years before present. Compared to the bulk sediment and macrofossil data, the cosmogenic nuclide plot shows data point clustered around 20,000 years ago. The plots for bulk sediment and macrofossils display this lag time as the data points are more clustered around 10,000 to 15,000 years. This lag time for organic sedimentation is around 5,000 to 10,000 years.

Data, Calculations, and Comparisons

This data was sorted in order of the age and uncertainty was considered for some data values.
1º latitude = 111.2 km

The average retreat rate for the Cosmogenic Nuclide Exposure Age method is 0.0544 km/year. For Macrofossils, the retreat rate is 38.03 km/year and for Bulk Sediment, the retreat rate is 1.09 km/year.

  1. Analysis of multiple cosmogenic nuclides constrains Laurentide Ice Sheet history and process on Mt. Mansfield, Vermont's highest peak
Lee B. Corbett, Paul R. Bierman, Stephen F. Wright, Jeremy D. Shakun, P. Thompson Davis, Brent M. Goehring, Christopher T. Halsted, Alexandria J. Koester, Marc W. Caffee, Susan R. Zimmermanhttps://site.uvm.edu/geomorphology/files/2020/11/Corbett_mansfield.pdf
2.Cosmogenic nuclide age estimate for Laurentide Ice Sheet recession from the terminal moraine, New Jersey, USA, and constraints on latest Pleistocene ice sheet historyLee B. Corbett, Paul R. Bierman, Byron D. Stone, Marc W. Caffee, Patrick L. Larsenhttps://site.uvm.edu/geomorphology/files/2020/11/Corbett-et-al-2017.pdf

The assumptions with cosmogenic nuclide dating method is "(1) that nuclides from previous periods of exposure were removed by erosion of at least several meters during the most recent glaciation (Briner et al., 2016), (2) that surfaces were not shielded by snow or sediment following deglaciation (Heyman et al., 2016; Schildgen et al., 2005), and (3) that surfaces have not been eroded following deglaciation (Zimmerman et al., 1994)" (1.) For radiocarbon dating methods, the assumptions are "the unknown lag time between ice margin retreat and the onset of organic matter deposition may make minimum age limits too young (Davis and Davis, 1980). The scarcity of organic material in postglacial sediments because of cold conditions also limits the utility of basal radiocarbon ages for developing accurate deglaciation chronologies (Cotter et al., 1986; Stone and Borns, 1986; Balco and Schaefer, 2006). Additionally, carbon unrelated to the material being dated can contaminate the sample, especially in the case of bulk sediments or concretions (Grimm et al., 2009)." (2.) "Bulk lake sediment ages are often too old because they contain recycled carbon (Davis et al., 1995) or are subject to hard water effects (Shotton, 1972). Several studies in Vermont have shown organic macrofossil ages to be hundreds of years younger than bulk sediment ages (Brown, 1999; Noren, 2002; Parris, 2003), likely because of carbon recycling." (1.)