Chemical destaining and the delta correction for blue intensity measurements of stained lake subfossil trees
<p>The stain of wood samples from lake subfossil trees (LSTs) is challenging the wide application of the blue intensity (BI) technique for millennial dendroclimatic reconstructions. In this study, we used seven chemical destaining reagents to treat samples of subfossil black spruce (<i>P...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-09-01
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Series: | Biogeosciences |
Online Access: | https://bg.copernicus.org/articles/17/4559/2020/bg-17-4559-2020.pdf |
Summary: | <p>The stain of wood samples from lake subfossil trees
(LSTs) is challenging the wide application of the blue intensity (BI)
technique for millennial dendroclimatic reconstructions. In this study, we
used seven chemical destaining reagents to treat samples of subfossil black
spruce (<i>Picea mariana</i> (Mill.) B.S.P.) trees from two lakes in the eastern Canadian boreal
forest. We subsequently compared latewood BI (LBI) and delta BI (DBI) time
series along with conventional maximum latewood density (MXD) measured from
the stained and destained samples. Results showed that the stain of our
samples is most likely caused by postsampling oxidation of dissolved
ferrous iron in lake sediments that penetrated into wood. Three reagents
(ascorbic acid, sodium ascorbate, and sodium dithionite all mixed with
ethylenediaminetetraacetic acid) could remove <span class="inline-formula"><i>></i>90 <i>%</i></span> of Fe.
However, even for the best chemical protocol, a discrepancy of about
<span class="inline-formula">+2</span> <span class="inline-formula"><sup>∘</sup></span>C compared to MXD data remained in the LBI-based temperature
reconstruction due to incomplete destaining. On the contrary, the simple
mathematical delta correction, DBI, was unaffected by the Fe stain and showed
very similar results compared to MXD data (<span class="inline-formula"><i>r</i><i>></i>0.82</span>) from annual
to centennial timescales over the past <span class="inline-formula">∼360</span> years. This study
underlines the difficulty of completely destaining lake subfossil samples while confirming the robustness of the DBI approach. DBI data measured from
stained LSTs can be used to perform robust millennial temperature
reconstructions.</p> |
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ISSN: | 1726-4170 1726-4189 |