Lindars, E. S., Grimes, S. T., Mattey, D. P., Collinson, M. E., Hooker, J. J. and Jones, Timothy Peter ![]() |
Abstract
A direct laser-fluorination (DLF) method is presented for phosphate d18O analysis (mass 1 — 2mg). The automated system heats samples in the presence of excess BrF5 using a 25 W CO2 laser, at 10.66mm. d18O ratios of the liberated O2 were measured using a dual inlet Optima mass spectrometer. As DLF measures whole apatite oxygen, non-phosphate bound oxygen must be removed by pre-treatment. Two methods were investigated: 1) heating to 1000°C; and 2) heating to 400°C followed by laser fusing. Method 2 is recommended as samples heated to 1000°C showed evidence of oxygen exchange with atmospheric water. To validate the DLF method, and show the potential of rodent teeth in palaeoclimate reconstruction, modern rodent teeth d18O results from 2 species are presented (d18Op). Large inter- and intra-jaw heterogeneity indicates that single teeth cannot be used for palaeothermometry. However, the overall standard deviations were low (Glis glis d18Op 5 110.4 6 0.7‰ n 5 38 and Apodemus sylvaticus d18Op 5 114.4 6 1.3‰ n 5 24). Using equations, derived from lab rodents, an ingested water value of 25.6 6 2.2‰ was calculated for Apodemus sylvaticus, only 21.3‰ lower than measured local water (24.3‰). This suggests that the phosphate d18O of rodent teeth can be used as a proxy for palaeoclimate reconstruction.
Item Type: | Article |
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Date Type: | Publication |
Status: | Published |
Schools: | Earth and Environmental Sciences |
Subjects: | G Geography. Anthropology. Recreation > GE Environmental Sciences Q Science > Q Science (General) |
Publisher: | Elsevier |
ISSN: | 0016-7037 |
Last Modified: | 19 Oct 2022 09:41 |
URI: | https://orca.cardiff.ac.uk/id/eprint/21841 |
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