Arctic & Alpine Research
Department or Program
chronology, coastal isolation basin, emergence, glaciomarine sediment, raised marine sediment, relative sea level, relative sea-level, sea level curve, sea-level curve, shell date, uplift
A new relative sea level curve for the Robeson Channel area constrasts with previously published curves for the area by inferring that rapid emergence may have commenced at c7400 BP, as much as 1200yr earlier than previously predicted. Subsequently, uplift may have occurred at much lower rates from c6000 BP to present. A comparison of shell dates used for the relative sea level curve and dates on disseminated total organic carbon (TOC) fraction from lacustrine and marine sediments from sediment cores from emerged coastal lakes shows wide discrepancies.
Retelle, M., Bradley, R.S., Stuckenwrath, R. (1989) "Relative Sea Level Chronology Determined from Raised Marine Sediments and Coastal Isolation Basins, Northeastern Ellesmere Island, Arctic Canada" Arctic and Alpine Research 21(2). 113-125. https://www.tandfonline.com/doi/abs/10.1080/00040851.1989.12002720
This is the publisher's version of the work. This publication appears in Bates College's institutional repository by permission of the copyright owner for personal use, not for redistribution.
Required Publisher's Statement
This is a Version of Record of an article published by Taylor & Francis in Arctic and Alpine Research in 1989, available online: https://www.tandfonline.com/doi/abs/10.1080/00040851.1989.12002720