Kusch, Stephanie; Rethemeyer, Janet; Hopmans, Ellen C; Wacker, Lukas; Mollenhauer, Gesine (2016): 14C concentrations of algal and archaeal lipids and their associated sea surface temperature proxies in the Black Sea. PANGAEA, https://doi.org/10.1594/PANGAEA.863329, Supplement to: Kusch, S et al. (2016): Factors influencing 14C concentrations of algal and archaeal lipids and their associated sea surface temperature proxies in the Black Sea. Geochimica et Cosmochimica Acta, 188, 35-57, https://doi.org/10.1016/j.gca.2016.05.025
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Understanding the preservation and deposition history of organic molecules is crucial for the understanding of paleoenvironmental information contained in their abundance ratios such as Uk'37 and TEX86 used as proxies for sea surface temperature (SST). Based on their relatively high refractivity, alkenones and glycerol dialkyl glycerol tetraethers (GDGTs) can survive postdepositional processes like lateral transport, potentially causing inferred SSTs to be misleading. Likewise, selective preservation of alkenones and GDGTs may cause biases of the SST proxies themselves and can lead to decoupling of both proxy records. Here we report compound-specific radiocarbon data of marine biomarkers including alkenones, GDGTs, and low molecular weight (LMW) n-fatty acids from Black Sea sediments deposited under different redox regimes to evaluate the potentially differential preservation of both biomarker classes and its effect on the SST indices Uk'37 and TEX86 . The decadal D14C values of alkenones, GDGTs, and LMW n-fatty acids indicate similar preservation under oxic, suboxic, and anoxic redox regimes and no contribution of pre-aged compounds, e.g., by lateral supply. Moreover, similar 14C concentrations of crenarchaeol, alkenones, and LMW n-fatty acids imply that the thaumarchaeotal GDGTs preserved in these sediments are produced in the euphotic zone rather than in subsurface/thermocline waters. However, we observe biomarker-based SSTs that strongly deviate (deltaSST up to 8.4 °C) from in situ measured mean annual SSTs in the Black Sea. This is not due to redox-dependent differential biomarker preservation as implied by their D14C values and spatial SST pattern. Since contributions from different sources can largely be excluded, the deviation of the Uk'37 and TEX86 proxy-derived SSTs from in situ SSTs requires further study of phylogenetic and other yet unknown environmental controls on alkenone and GDGT lipid distributions in the Black Sea.
Median Latitude: 43.423048 * Median Longitude: 33.297151 * South-bound Latitude: 41.615000 * West-bound Longitude: 29.190500 * North-bound Latitude: 45.661500 * East-bound Longitude: 41.466617
Date/Time Start: 2001-12-16T05:01:00 * Date/Time End: 2008-03-21T06:43:00
Datasets listed in this publication series
- Kusch, S; Rethemeyer, J; Hopmans, EC et al. (2016): (Table 1) Sampling locations and previously published geochemical data (TOC and BIT index) for the investigated sediments. https://doi.org/10.1594/PANGAEA.863324
- Kusch, S; Rethemeyer, J; Hopmans, EC et al. (2016): (Table 2) Results of radiocarbon and stable carbon isotope measurements of surface sediments from the Black Sea. https://doi.org/10.1594/PANGAEA.863325
- Kusch, S; Rethemeyer, J; Hopmans, EC et al. (2016): (Table 3) Sea surface temperature (SST) proxy data and in situ SSTs calculated from surface sediments from the Black Sea. https://doi.org/10.1594/PANGAEA.863326
- Kusch, S; Rethemeyer, J; Hopmans, EC et al. (2016): (Table 4) GDGT relative distributions and ratios from surface sediments from the Black Sea. https://doi.org/10.1594/PANGAEA.863327
- Kusch, S; Rethemeyer, J; Hopmans, EC et al. (2016): (Table S2) Additional samples from the Black Sea used for core-top SST assessment. https://doi.org/10.1594/PANGAEA.863328