-
Temperatures from TEX86 measurements performed on middle Miocene sediment mat...
This table includes temperatures calculated from organic biomarker (TEX86) measurements performed on middle Miocene sediment material from Ocean Drilling Program (ODP) Hole... -
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... -
(Table 1) Lipid biomarkers in surface sediments from the Gulf of Genoa
A series of molecular organic markers were determined in surface sediments from the Gulf of Genoa (Ligurian Sea) in order to evaluate their potential for palaeo-environmental... -
Chemical characterization of marine sub-micrometer aerosol particles during t...
Sub-micron marine aerosol particles (PM1) were collected during the MERIAN cruise MSM 18/3 between 22 June 2011 and 21 July 2011 from the Cape Verde island Sao Vicente to Gabun... -
Biomarker analysis from IODP Hole 337-C0020A
Geocode = [m CSF-A] Top Core depth (below sea floor) -
(Table 1) Carbon and lipids at DSDP Hole 61-462
The lipids of a Pliocene and a Cretaceous sample from Site 462 were analyzed to assess their source and diagenetic history. Judging from the distributions of the n-alkanes,... -
(Table 1) Sample descriptions and geochemistry for core material at DSDP Hole...
Laminated and nonlaminated sediments from Holes 480 and 479 have been analyzed for potential differences in the composition of organic matter. Their lipid composition is very... -
(Table 1) Sample descriptions and results: Carbon, lipid, and kerogen analyse...
Pleistocene sediments in the Guaymas Basin, Gulf of California, have been intruded by sills and their organic matter thus subjected to thermal stress. Sediment samples from... -
(Table 1) Lipid and kerogen content at DSDP Leg 64 Holes
Diatomaceous mud and an organically-rich claystone from holes at Sites 474 and 476 at the mouth of the Gulf of California were analyzed by organic geochemical methods to... -
(Table) Carbon, nitrogen and n-alkane content and isotopic composition of bot...
The chemical composition of organic matter (Corg, Norg, d13C, d1SN, and n-alkanes) was studied in the top layer of bottom sediments of the East Siberian Sea. Possible ways were... -
(Table 1) Sample descriptions, carbon contents, and lipid yields across the K...
This reconnaissance study was undertaken to determine whether the mass extinctions and faunal successions that mark the Cretaceous/Tertiary (K/T) boundary left a discernible... -
(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... -
(Table 1) Concentration and geological parameters of n-alkanes and n-alkenes ...
Abstract Hydrocarbons in surface sediments were studied quantitatively and qualitatively in 18 stations along the coastline of Gabes Gulf in Tunisia. The results show that the... -
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.