Compound-specific oxygen and hydrogen isotopes in soils from South Africa and results of the coupled δ2H–δ18O paleohygrometer approach

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Strobel, Paul;Haberzettl, Torsten;Bliedtner, Marcel;Struck, Julian;Glaser, Bruno;Zech, Michael;Zech, Roland

Description

Here we present the data of the study by Strobel et al. (2020; doi:10.1016/j.scitotenv.2020.137045), who analysed topsoil samples from South Africa for their compound-specific hydrogen isotopic composition of leaf wax-derived n-alkanes (δ2Hn-alkane) and oxygen isotopic composition of hemicellulose-derived sugars (δ18Osugar). Apparent fractionation, which is the difference between δ2Hn-alkane and the isotopic signature of growing season precipitation δ2Hp (εapp 2H) and δ18Osugar and δ18Op (εapp 18O), was calculated. Coupling both δ2Hn-alkane and δ18O sugar using a 'paleohygrometer' approach enables the calculation of the plants-source water and relative humidity. For more details see Strobel et al. (2020; doi:10.1016/j.scitotenv.2020.137045).

Citations (0)

Mentions (0)

Metrics

Dataset Index

0.5

FAIR Score

92%

Citations

0

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

License

Creative Commons Attribution 4.0 International

Assigned Domain

Subfield

Atmospheric Science

Field

Earth and Planetary Sciences

Domain

Physical Sciences

Confidence Score

99%

Source

Open Alex

Keywords

Apparent fractionationBiomarkerCompound-specific hydrogen isotopesCompound-specific oxygen isotopesHemicellulose sugarsleaf waxesSouth AfricaLatitude of eventLongitude of eventElevation of eventEvent labelArea/localityDEPTH, soilAverage chain length, oddCarbon Preference Indexδ Deuterium, n-alkanesδ Deuterium, n-alkanes, standard deviationApparent hydrogen isotope fractionationApparent hydrogen isotope fractionation, standard deviationArabinose, δ18OArabinose, δ18O, standard deviationSugar, δ18OSugar, δ18O, standard deviationδ Deuterium, source waterδ18O, source waterHumidity, relativeSoil sampleReconstructed

Normalization Factors

FT

65.38

CTw

1.00

MTw

1.00