Improving temperature estimates derived from Mg/Ca of planktonic foraminifera using X-ray computed tomography-based dissolution index, XDX
Temperatures derived from Mg/Ca ratios of the calcite tests of planktonic foraminifera are distorted when samples are partially dissolved, and methods are required to quantify this source of inaccuracy. Here we compare a dissolution index (XDX), based on
Published in: | Paleoceanography |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/65073 https://doi.org/10.1029/2009PA001902 https://openresearch-repository.anu.edu.au/bitstream/1885/65073/5/01_Johnstone_Improving_temperature_2011.pdf.jpg |
Summary: | Temperatures derived from Mg/Ca ratios of the calcite tests of planktonic foraminifera are distorted when samples are partially dissolved, and methods are required to quantify this source of inaccuracy. Here we compare a dissolution index (XDX), based on |
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