Abstract
Supplementary figures and tables.
Highlights
Uncertainty is ± 0.017‰ (95% confidence interval). # One standard deviation from the mean of replicate analyses of the same sample. a Temperatures calculated from D47 values using the mollusk-specific calibration of Henkes et al (2013): D47 = 32700/T2 +0.3286 for new data, and D47
Note: Given the XRD detection limit of 0.3-0.4%, samples with less than 0.4% calcite are considered pure aragonite
Note: The last two samples analyzed in the UCLA lab were not included in the calculation of the average D47 - temperature values for modern samples because replicate analyses of these two samples yielded a very large temperature range of 28°C for T16-05G-3 and of 17°C for T16-05G-4, both of which are much larger than the reported analytical uncertainty (+6°C), and unreasonably high temperatures that exceed the observed maximum lake water temperature
Summary
AT (°C) D47 (‰) (Henkes (ARF)** calibration) Holocene and modern shells analyzed by Huntington et al (2015): nrc10-1071
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
