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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... -
Leaf wax n-alkane carbon isotope data from sediment samples collected from fo...
Site information and leaf wax n-alkane carbon isotope data from sediment samples collected from fossil leaf sites extending from New Mexico to the High Arctic and span 40... -
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.... -
n-Alkane composition from the Loess Paleosol Sequence Möhlin, Switzerland
We have measured leaf wax n-Alkanes from a Loess Paleosol Sequence (location: 47.56819 / 7.88053) ranging back to MIS 4. The data set contains n-Alkane patterns, Deuterium and... -
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... -
Plant leaf wax (n-alkane) data from sediment core MD96-2048
In this study we investigate Pleistocene vegetation and climate change in southern East Africa by examining plant leaf waxes in a marine sediment core that receives terrestrial... -
Organic-geochemical proxies (UK'37 and TEXH86) records in surface sediments o...
In this study we reconstruct sea surface temperatures (SSTs) using two lipid-based biomarker proxies (alkenone unsaturation index UK'37 and TEX86 index based on glycerol... -
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... -
Long-chain n-alkane data from GeoB3918-2
This dataset has no description
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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... -
Contents of n-alkanes and isoprenoids in bottom sediments of the Barents Sea ...
This dataset has no description
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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. -
Organic marker compounds in sediment core GIK23386-1
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl. -
Organic marker compounds in sediment core POS181_267
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl. -
Organic marker compounds in sediment core POS181_245
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl. -
Organic marker compounds in sediment core POS181_225
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl. -
Flux of biomarker from mooring BI2
No value is given if concentration was below the detection limit of gaschromatography of 500 pg/myl.