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Compiled compound-specific δ¹³C isotope values for the individual n-alkanes (...
n-alkanol (corrected for TMS = Trimethylsilyether) / Depth = composite depth -
Carbon isotope records from seven globally distributed marine sediment cores
Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured from seven sediments cores. Sediment cores from DSDP/ODP Sites 94, 354, 511,... -
n-alkane hydrogen and carbon isotopes from sediment core ODP-161-976A
Hydrogen (δD) and carbon isotopic data (δ13C) from sediment core ODP-161-976A are presented for three n-alkane homologues (n-C29, n-C31, and n-C33). -
Pliocene stable carbon and hydrogen isotopes of plant wax of ODP Site 108-659
The Pliocene is regarded as a potential analogue for future climate with conditions generally warmer-than-today and higher-than-preindustrial atmospheric CO2 levels. Here we... -
Long chain n-alkanes deposited from borehole PRGL1P (ROMESS1) in the upper sl...
During the PROMESS campaign (summer 2004) a borehole (PRGL1) was drilled in the upper slope of the Gulf of Lions. Previous studies showed that the deposition of the sedimentary... -
(Table T1) Stable carbon isotopic composition of n-alkanes and carbon prefere...
Carbon isotope ratios of terrestrial biomarkers extracted from Ocean Drilling Program Hole 1263A show a prominent negative excursion across the Paleocene/Eocene boundary. The... -
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... -
Stable carbon isotope ratios of alkane of IODP Hole 302-M0004A
The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming approx ~55 million years ago, superimposed on an already warm world (Zachos et al.,... -
Stable carbon isotope ratios of n-alkane in ODP Hole 175-1083A in the South A...
The intensification of Northern Hemisphere Glaciation (iNHG) is one of the critical climate thresholds in the Cenozoic. This study focuses on marine sediments recovered from... -
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... -
Carbon isotope (δ13C) measured from leaf-wax n-alkanes in sediment core Sarda...
The proxy data reported here are measured from a sediment core collected from Lake Sardarya (28° 38' 03" N, 61° 00' 44" E, 2675 m a.s.l.) situated on the western slope of Taftan... -
Biomarkers in a sediment core from Lake Otjikoto, Namibia
This dataset has no description
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Temperature difference vs. dD of sediment core GeoB16202-2
This dataset has no description
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Sedimentary n-alkane concentration of lake Nam Co sediment core NC 08/01
Missing values = below detection limit. This study is part of DFG Priority Programme (Schwerpunktprogramm) 1372 "Tibetan Plateau: Formation - Climate - Ecosystems (TiP)" -
dD values of hydrocarbon biomarkers in Lake Qalluuraq sediments
This dataset has no description
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δ¹³C values of hydrocarbon biomarkers in Lake Qalluuraq sediments
This dataset has no description
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Downcore abundance of hydrocarbon biomarkers and n-alkane derived average cha...
This dataset has no description
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Hydrogen isotopes of n-alkanes of lake Nam Co sediment core NC 08/01
This study is part of DFG Priority Programme (Schwerpunktprogramm) 1372 "Tibetan Plateau: Formation - Climate - Ecosystems (TiP)" -
dD of C29 and C31 plant wax n-alkanes from sediment core GeoB16202-2
This dataset has no description
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δ¹³C of C29 and C31 plant wax n-alkanes from sediment core GeoB16202-2
This dataset has no description
