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, 516, 608, 672, and 730 were taken from the North Atlantic, South Atlantic, and Indian Ocean Basins. New age models were developed using biostratigraphy and chemostratigraphic datams. Compound-specific isotope analyses of terrestrial leaf wax-derived odd-carbon number n-alkanes (n-C25 to n-C33) extracted from deep-sea drill cores were employed to evaluate relative contributions of C3 and C4 plant material delivered to marine sediments from the last 45 million years, with particular focus between 25-33 Ma. The purpose of this study was to assess the effects of CO2 decr...
We present stable hydrogen isotope (dD) and carbon isotope (d13C) of sedimentary terrestrial leaf wa...
An isobathic transect of marine surface sediments from 1°N to 28°S off southwest Africa was used to ...
The Paleocene-Eocene Thermal Maximum (PETM; similar to 56 Ma) and Eocene Thermal Maximum 2 (ETM2; si...
Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured ...
The data are measurements of leaf wax n-alkane compound abundance and associated metrics of compound...
Carbon isotope ratios in higher-plant organic matter (i13Cplant) have been shown in several studies ...
The carbon isotope ratio (δ13C) of plant-derived organic carbon preserved in geological archives can...
The stratigraphic utility of carbon-isotope values from terrestrial organic matter is explored for M...
Site information and leaf wax n-alkane carbon isotope data from sediment samples collected from foss...
Aeolian deposition in the central North Pacific has been well recognized to originate from arid Asia...
The intensification of Northern Hemisphere Glaciation (iNHG) is one of the critical climate threshol...
Sedimentary high molecular weight (HMW) n-alkyl lipids derived from the waxes of terrestrial plants ...
Sedimentary high molecular weight (HMW) n-alkyl lipids derived from the waxes of terrestrial plants ...
Stable carbon isotope ratios of archaeal glycerol dibiphytanyl glycerol tetraether (GDGT) lipids hav...
Trees and shrubs in tropical Africa use the C3 cycle as a carbon fixation pathway during photosynthe...
We present stable hydrogen isotope (dD) and carbon isotope (d13C) of sedimentary terrestrial leaf wa...
An isobathic transect of marine surface sediments from 1°N to 28°S off southwest Africa was used to ...
The Paleocene-Eocene Thermal Maximum (PETM; similar to 56 Ma) and Eocene Thermal Maximum 2 (ETM2; si...
Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured ...
The data are measurements of leaf wax n-alkane compound abundance and associated metrics of compound...
Carbon isotope ratios in higher-plant organic matter (i13Cplant) have been shown in several studies ...
The carbon isotope ratio (δ13C) of plant-derived organic carbon preserved in geological archives can...
The stratigraphic utility of carbon-isotope values from terrestrial organic matter is explored for M...
Site information and leaf wax n-alkane carbon isotope data from sediment samples collected from foss...
Aeolian deposition in the central North Pacific has been well recognized to originate from arid Asia...
The intensification of Northern Hemisphere Glaciation (iNHG) is one of the critical climate threshol...
Sedimentary high molecular weight (HMW) n-alkyl lipids derived from the waxes of terrestrial plants ...
Sedimentary high molecular weight (HMW) n-alkyl lipids derived from the waxes of terrestrial plants ...
Stable carbon isotope ratios of archaeal glycerol dibiphytanyl glycerol tetraether (GDGT) lipids hav...
Trees and shrubs in tropical Africa use the C3 cycle as a carbon fixation pathway during photosynthe...
We present stable hydrogen isotope (dD) and carbon isotope (d13C) of sedimentary terrestrial leaf wa...
An isobathic transect of marine surface sediments from 1°N to 28°S off southwest Africa was used to ...
The Paleocene-Eocene Thermal Maximum (PETM; similar to 56 Ma) and Eocene Thermal Maximum 2 (ETM2; si...