Testing the D / H ratio of alkenones and palmitic acid as salinity proxies in the Amazon Plume
The stable hydrogen isotope composition of lipid biomarkers, such as alkenones, is a promising new tool for the improvement of palaeosalinity reconstructions. Laboratory studies confirmed the correlation between lipid biomarker δD composition (δD<sub>Lipid</sub>), water δD composition (δ...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-12-01
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Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/12/7239/2015/bg-12-7239-2015.pdf |
Summary: | The stable hydrogen isotope composition of lipid biomarkers, such as
alkenones, is a promising new tool for the improvement of palaeosalinity
reconstructions. Laboratory studies confirmed the correlation between lipid
biomarker δD composition (δD<sub>Lipid</sub>), water δD
composition (δD<sub>H<sub>2</sub>O</sub>) and salinity; yet there is limited insight
into the applicability of this proxy in oceanic environments. To fill this
gap, we test the use of the δD composition of alkenones (δD<sub>C<sub>37</sub></sub>) and palmitic acid (δD<sub>PA</sub>) as salinity proxies using
samples of surface suspended material along the distinct salinity gradient
induced by the Amazon Plume. Our results indicate a positive correlation
between salinity and δD<sub>H<sub>2</sub>O</sub>, while the relationship between
δD<sub>H<sub>2</sub>O</sub> and δD<sub>Lipid</sub> is more complex: δD<sub>PAM</sub> correlates strongly with δD<sub>H<sub>2</sub>O</sub> (<i>r</i><sup>2</sup> = 0.81) and
shows a salinity-dependent isotopic fractionation factor. δD<sub>C</sub>37</sub></sub> only correlates with δD<sub>H<sub>2</sub>O</sub> in a small number (<i>n</i> = 8) of
samples with alkenone concentrations > 10 ng L<sup>−1</sup>, while
there is no correlation if all samples are taken into account. These
findings are mirrored by alkenone-based temperature reconstructions, which
are inaccurate for samples with low alkenone concentrations. Deviations in
δD<sub>C</sub>37</sub></sub> and temperature are likely to be caused by limited
haptophyte algae growth due to low salinity and light limitation imposed by
the Amazon Plume. Our study confirms the applicability of δD<sub>Lipid</sub> as a salinity proxy in oceanic environments. But it raises a
note of caution concerning regions where low alkenone production can be
expected due to low salinity and light limitation, for instance, under
strong riverine discharge. |
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ISSN: | 1726-4170 1726-4189 |