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...

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Bibliographic Details
Main Authors: C. Häggi, C. M. Chiessi, E. Schefuß
Format: Article
Language:English
Published: Copernicus Publications 2015-12-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/12/7239/2015/bg-12-7239-2015.pdf
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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 (&delta;D<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: &delta;D<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 &delta;D<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.
ISSN:1726-4170
1726-4189