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Biomarker concentrations of modern vegetation samples from Beerberg peatland ...
This dataset has no description
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Concentrations of long-chain n-alkanes, CPI values and compound-specific stab...
CPI25-33 = 0.5 * (SCodd27-33/SCeven26-32 + SCodd27-33/SCeven28-34); *corrected for global ice volume changes using data from Bintanja et al. (2005); SD is standard deviation of... -
Geochemical Measurements of Kelp in the Santa Barbara Basin, CA
<0 = concentrations below detection limit. -
Concentrations of n-alkanes C29 and C31, δD nC29 and nC31 values, Artemisia a...
This dataset has no description
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(Table S4a) Molecular biomarkers of sediment core GeoB16602-4, GeoB16602-5, G...
This dataset has no description
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(Table A4) Stable hydrogen isotopic composition of n-C27, n-C29 and n-C31 alk...
Standard deviations and n-values are not reported for aerosol dD values because no field replicates were collected. The pooled analytical uncertainty for these samples was 1.8... -
Plant wax biomarkers record from sediment core PEX19-01, Lake Peixão, Serra d...
These data comprise a downcore record (PEX19-01) of plant wax n-alkanes (concentration and compound-specific δ2H and δ13C isotopes) from Lake Peixão (40°20'35" N, 7°36'19" W), a... -
Concentration of n-alkanes and hydrogen isotopic compositions from modern we...
This data supporting the study Leaf wax n-alkane distribution and hydrogen isotopic fractionation in fen plant communities of two Mediterranean wetlands (Tenaghi Philippon, Nisí... -
Bulk organic matter composition, n-alkane distribution patterns, and compound...
Surface sediments (n=41) reflecting modern times (uppermost 10 cm) were collected during a November/December 2018 field campaign along the course of the Mkhuze River and a... -
Bulk organic carbon and n-alkane composition data for river sediment depth pr...
We extracted and analyzed n-alkane compounds from river suspended sediment collected from the Rio Bermejo in Argentina. We collected 24 river depth profile samples collected... -
Bulk organic carbon and n-alkane composition data for leaf litter, soil, and ...
Endmember samples were collected and analyzed to determine the sources of organic material in the river suspended sediment. Endmembers include soil, leaf litter, and floodplain... -
Conifers are a major source of sedimentary leaf wax n-alkanes when dominant o...
Paleobotanical site information, terpenoid, n-alkane, and other and biomarker quantification and carbon isotope data from sediment samples collected from North America Paleogene... -
Compound-specific carbon isotopes of plant waxes from site GeoB16602
This dataset has no description
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Results of organic and inorganic geochemical analysis, as well as pollen Coun...
This dataset has no description
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Elemental, biomarker, and macrofossil data for composite core Co1211
In this study, we use a combined biomarker and macrofossil approach to reconstruct the Holocene climate history recorded in Trifna Sø, Skallingen area, eastern North Greenland.... -
Sterol, n-alcohol and n-alkane composition of living fen plants
In groundwater-fed fen peatlands, the surface biomass decays rapidly and, as a result, highly humified peat is formed. A high degree of humification constrains palaeoecological... -
Averages and ranges of paleoenvironmental proxy records of ODP Hole 108-658C ...
Several high-resolution proxy environmental records have been obtained for the last 35 kyr from ODP Hole 658C, a well-studied site ca. 200 km off Cap Blanc, NW Africa. The... -
Accumulation rates of plant-wax-derived long-chain C25 to C35 odd-numbered n-...
The dominant forcing factors for past large-scale changes in vegetation are widely debated. Changes in the distribution of C4 plants-adapted to warm, dry conditions and low... -
Marker in suspended particulate matter at station M26/2_481-2
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl. -
Marker in suspended particulate matter at station M26/2_480-2
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl.