Niedermeyer, Eva M; Forrest, M; Beckmann, Britta; Sessions, Alex L; Mulch, Andreas; Schefuß, Enno (2016): dD values of C31 n-alkane (dD wax) from sediment core GeoB9501-4 offshore the Northwest African Sahel. PANGAEA, https://doi.org/10.1594/PANGAEA.864242, Supplement to: Niedermeyer, EM et al. (2016): The stable hydrogen isotopic composition of sedimentary plant waxes as quantitative proxy for rainfall in the West African Sahel. Geochimica et Cosmochimica Acta, 184, 55-70, https://doi.org/10.1016/j.gca.2016.03.034
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Various studies have demonstrated that the stable hydrogen isotopic composition (dD) of terrestrial leaf waxes tracks that of precipitation (dDprecip) both spatially across climate gradients and over a range of different timescales. Yet, reconstructed estimates of dDprecip and corresponding rainfall typically remain largely qualitative, due mainly to uncertainties in plant ecosystem net fractionation, relative humidity, and the stability of the amount effect through time. Here we present dD values of the C31n-alkane (dDwax) from a marine sediment core offshore the Northwest (NW) African Sahel covering the past 100 years and overlapping with the instrumental record of rainfall. We use this record to investigate whether accurate, quantitative estimates of past rainfall can be derived from our dDwax time series. We infer the composition of vegetation (C3/C4) within the continental catchment area by analysis of the stable carbon isotopic composition of the same compounds (d13Cwax), calculated a net ecosystem fractionation factor, and corrected the dDwax time series accordingly to derive dDprecip. Using the present-day relationship between dDprecip and the amount of precipitation in the tropics, we derive quantitative estimates of past precipitation amounts. Our data show that (a) vegetation composition can be inferred from d13Cwax, (b) the calculated net ecosystem fractionation represents a reasonable estimate, and (c) estimated total amounts of rainfall based on dDwax correspond to instrumental records of rainfall. Our study has important implications for future studies aiming to reconstruct rainfall based on dDwax; the combined data presented here demonstrate that it is feasible to infer absolute rainfall amounts from sedimentary dDwax in tandem with d13Cwax in specific depositional settings.
Latitude: 16.839660 * Longitude: -16.732660
Date/Time Start: 2005-06-12T20:01:00 * Date/Time End: 2005-06-12T20:01:00
Datasets listed in this publication series
- Niedermeyer, EM; Forrest, M; Beckmann, B et al. (2016): (Figure 2b) Stable carbon isotopic composition of the n-C31 alkane (δ¹³Cwax) and d13Cwax corrected for the ''Suess Effect” of sediment core GeoB9501-4. https://doi.org/10.1594/PANGAEA.864230
- Niedermeyer, EM; Forrest, M; Beckmann, B et al. (2016): (Figure 2c) Stable hydrogen isotopic composition of the n-C31 alkane (dDwax) of sediment core GeoB9501-4. https://doi.org/10.1594/PANGAEA.864231
- Niedermeyer, EM; Forrest, M; Beckmann, B et al. (2016): (Figure 3) Reconstructed rainfall amounts and reconstructed stable hydrogen isotopic composition of precipitation of sediment core GeoB9501-4. https://doi.org/10.1594/PANGAEA.864238
- Niedermeyer, EM; Forrest, M; Beckmann, B et al. (2016): (Table 1) n-Alkane concentrations in dried sediment, carbon preference index (CPI), and normalized C31 index of sediment core GeoB9501-4. https://doi.org/10.1594/PANGAEA.864240
- Niedermeyer, EM; Forrest, M; Beckmann, B et al. (2016): (Table 2) Values of δ¹³Cwax and dDwax of the n-C31 alkane from sediment core GeoB9501-4. https://doi.org/10.1594/PANGAEA.864241