Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Weiss, Gabriella M; Pfannerstill, Eva Y; Schouten, Stefan; Sinninghe Damsté, Jaap S; van der Meer, Marcel T J (2017): Hydrogen isotope fractions of long-chain alkenones produced by Emiliania huxleyi during experiments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.883192, Supplement to: Weiss, GM et al. (2017): Effects of alkalinity and salinity at low and high light intensity on hydrogen isotope fractionation of long-chain alkenones produced by Emiliania huxleyi. Biogeosciences, 14(24), 5693-5704, https://doi.org/10.5194/bg-14-5693-2017

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX Citation

Abstract:
Over the last decade, hydrogen isotopes of long-chain alkenones have been shown to be a promising proxy for reconstructing paleo sea surface salinity due to a strong hydrogen isotope fractionation response to salinity across different environmental conditions. However, to date, the decoupling of the effects of alkalinity and salinity, parameters that co-vary in the surface ocean, on hydrogen isotope fractionation of alkenones has not been assessed. Furthermore, as the alkenone-producing haptophyte, Emiliania huxleyi, is known to grow in large blooms under high light intensities, the effect of salinity on hydrogen isotope fractionation under these high irradiances is important to constrain before using dDC37 to reconstruct paleosalinity. Batch cultures of the marine haptophyte E. huxleyi strain CCMP 1516 were grown to investigate the hydrogen isotope fractionation response to salinity at high light intensity and independently assess the effects of salinity and alkalinity under low light conditions. Our results suggest that alkalinity does not significantly influence hydrogen isotope fractionation of alkenones, but salinity does have a strong effect. Additionally, no significant difference was observed between the fractionation responses to salinity recorded in alkenones grown under both high and low light conditions. Comparison with previous studies suggests that the fractionation response to salinity in culture is similar under different environmental conditions, strengthening the use of hydrogen isotope fractionation as a paleosalinity proxy.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1SpeciesSpeciesWeiss, Gabriella M
2StrainStrainWeiss, Gabriella M
3SalinitySalWeiss, Gabriella MPSU
4Temperature, waterTemp°CWeiss, Gabriella M
5Radiation, photosynthetically activePARµmol/m2/sWeiss, Gabriella M
6Growth rateµ#/dayWeiss, Gabriella M
7δ Deuterium, waterδD H2O‰ SMOWWeiss, Gabriella Mculture water, initial
8δ Deuterium, standard deviationδD std dev±Weiss, Gabriella Mculture water, initial
9δ Deuterium, waterδD H2O‰ SMOWWeiss, Gabriella Mculture water, end
10δ Deuterium, standard deviationδD std dev±Weiss, Gabriella Mculture water, end
11δ Deuterium, alkenone, C37δD C37‰ SMOWWeiss, Gabriella M
12δ Deuterium, alkenone, C37, standard deviationδD C37 std dev±Weiss, Gabriella M
13Fractionation factorFrac FactorWeiss, Gabriella Malpha C37, between water and C37 alkenones
14Fractionation factor, errorFrac Factor e±Weiss, Gabriella M
15Alkalinity, totalATmmol(eq)/lWeiss, Gabriella Mculture water, initial
16Alkalinity, totalATmmol(eq)/lWeiss, Gabriella Mculture water, end
17pHpHWeiss, Gabriella Mculture water, initial
18pHpHWeiss, Gabriella Mculture water, end
Size:
628 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML