Hi Chris,
A cutoff of -19‰ seems a bit high to me for English samples, and I would think about using a marine correction above -20‰ (which I did for Medieval samples from Hull[1]). Looking at the lowest δ¹³C in other humans from the area may help in deciding an appropriate value. But -19.5‰ giving an estimated 18% marine contribution seems too high to me. The 100% marine endpoint is about -12 to -14‰ (depending on which resources are taken as representative), and when combined with a -20‰ terrestrial endpoint this implies a marine contribution more like 8% than 18%.
Elevated δ¹⁵N is an indicator of aquatic food sources, but a small shift in δ¹³C caused by a small marine component will be accompanied by a small shift in δ¹⁵N. However, freshwater foods can cause elevated δ¹⁵N with little difference in δ¹³C from a terrestrial diet.
[1] Roberts CA, Millard AR, Nowell GM, Gröcke DR, Macpherson CG, Pearson DG, Evans DH. 2013. Isotopic tracing of the impact of mobility on infectious disease: The origin of people with treponematosis buried in Hull, England, in the late medieval period. American Journal of Physical Anthropology 150:273-285.
Best wishes
Andrew
--
Dr. Andrew Millard
Associate Professor of Archaeology,
Durham University, UK
Email: A.R.M...@durham.ac.uk
Personal page: https://www.durham.ac.uk/staff/a-r-millard/
Dunbar 1650 MOOC: https://www.futurelearn.com/courses/battle-of-dunbar-1650
From: ox...@googlegroups.com <ox...@googlegroups.com>
On Behalf Of ineslopezl...@gmail.com
Sent: 15 October 2024 10:16
To: OxCal <ox...@googlegroups.com>
Subject: Re: Marine offset thresholds
[EXTERNAL EMAIL]
--
You received this message because you are subscribed to the Google Groups "OxCal" group.
To unsubscribe from this group and stop receiving emails from it, send an email to
oxcal+un...@googlegroups.com.
To view this discussion on the web visit https://groups.google.com/d/msgid/oxcal/dd041579-230a-4bc9-915a-550029747e87n%40googlegroups.com.