Steroids with unconventional side chains in ancient sediments and petroleum have been increasingly used as age diagnostic markers. Triaromatic dinosteroids and dinosteranes occur widely throughout the Eocene–Oligocene Shahejie Formation in the southeastern Bohai Bay Basin, China, consistent with its abundant fossil dinoflagellate assemblages. In addition, 24-norcholestane biomarkers, which commonly appear in marine oils, have been found in this lacustrine formation. Although a firm link has not been established between 24-norcholestane and specific modern taxa, both diatoms and dinoflagellates are shown to be likely sources of 24-norcholestanes. Although the Shahejie strata lack intact diatom frustules, they do exhibit a good relationship b...
A total of 225 rock samples and 37 oil samples from the Beibuwan Basin, South China Sea, were analyz...
China has a number of petroliferous lacustrine sedimentary basins of varying salinity and age (mainl...
Several oil shale beds, over 10 m thick, occur at the base of the first member of the Upper Cretaceo...
Diatoms are one of the major groups of algae which originated relatively recently and evolved in the...
Diatoms are one of the major groups of algae which originated relatively recently and evolved in the...
The use of C30 4-methylsteranes as an indicator of source organic matter relies on accurate identifi...
Molecular fossils record aspects of Neoproterozoic-Early Cambrian palaeobiology in the Bikaner-Nagau...
In this investigation, we monitored the stratigraphic occurrence and abundance of the fossil C30 ste...
Dinoflagellates are an important component of the extant eukaryotic plankton. Their organic-walled, ...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
The abundance and composition of total organic carbon, aliphatic and aromatic hydrocarbons including...
Molecular fossils provide a means to evaluate paleoenvironmental redox conditions and broad-scale as...
Climate fluctuations affect environment and sea levels, understanding the drivers of past sea levels...
Abstract: the 13C/12C compositions of n-alkanes and n-alkanoic acids from Eocene sediments are corre...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
A total of 225 rock samples and 37 oil samples from the Beibuwan Basin, South China Sea, were analyz...
China has a number of petroliferous lacustrine sedimentary basins of varying salinity and age (mainl...
Several oil shale beds, over 10 m thick, occur at the base of the first member of the Upper Cretaceo...
Diatoms are one of the major groups of algae which originated relatively recently and evolved in the...
Diatoms are one of the major groups of algae which originated relatively recently and evolved in the...
The use of C30 4-methylsteranes as an indicator of source organic matter relies on accurate identifi...
Molecular fossils record aspects of Neoproterozoic-Early Cambrian palaeobiology in the Bikaner-Nagau...
In this investigation, we monitored the stratigraphic occurrence and abundance of the fossil C30 ste...
Dinoflagellates are an important component of the extant eukaryotic plankton. Their organic-walled, ...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
The abundance and composition of total organic carbon, aliphatic and aromatic hydrocarbons including...
Molecular fossils provide a means to evaluate paleoenvironmental redox conditions and broad-scale as...
Climate fluctuations affect environment and sea levels, understanding the drivers of past sea levels...
Abstract: the 13C/12C compositions of n-alkanes and n-alkanoic acids from Eocene sediments are corre...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
A total of 225 rock samples and 37 oil samples from the Beibuwan Basin, South China Sea, were analyz...
China has a number of petroliferous lacustrine sedimentary basins of varying salinity and age (mainl...
Several oil shale beds, over 10 m thick, occur at the base of the first member of the Upper Cretaceo...