Leaf-wax n-alkanes are produced by terrestrial plants, and through long-term preservation in sediments their stable hydrogen-isotopic signature (δ²Hwax) provides useful information on past hydrological variation for paleoclimate reconstructions. However, gaps remain in our understanding of the isotopic relationships between the leaf waxes and the plants' source water. In this study, we investigated the influence of plant growth form, habitat and season on the distribution patterns and δ²Hwax values of 14 plant species (among which are two grasses, five trees and seven shrubs) sampled during four successive dry and wet seasons in three distinct habitats around Lake Chala in equatorial East Africa. Variation in δ²Hwax was analyzed with linear...
Hydrogen isotopic ratios of terrestrial plant leaf waxes (dD) have been widely used for paleoclimate...
The molecular hydrogen isotope composition ((delta D) of leaf waxes from terrestrial plants is incre...
The debate of climate versus CO2 in controlling the long-term dynamics of tropical African vegetatio...
Leaf-wax n-alkanes are produced by terrestrial plants, and through long-term preservation in sedimen...
Lake Chala (3 degrees 19' S, 37 degrees 42' E) is a steep-sided crater lake situated in equatorial E...
The hydrogen isotopic composition of plant leaf-wax n-alkanes (dDwax) is a novel proxy for estimatin...
Hydrogen isotope values (dD) of sedimentary terrestrial leaf wax such as n-alkanes or n-acids have b...
The observation that the hydrogen isotope composition (δD) of leaf wax lipids is determined mainly b...
International audienceThe hydrogen isotope composition of plant leaf wax (dD wax) has been found to ...
The hydrogen isotope composition of plant leaf wax (δDwax) has been found to record the isotope comp...
Compound specific hydrogen isotope ratios (delta D) of long chain sedimentary n-alkanes, which mostl...
A transect of marine surface sediment samples from 1° N to 28° S off southwest Africa was analysed t...
Hydrogen isotopic ratios of terrestrial plant leaf waxes (δD) have been widely used for paleoclimate...
Leaf wax n-alkanes are long-chain hydrocarbons that can persist in sedimentary records over geologic...
Leaf wax n -alkanes are long-chain hydrocarbons that can persist in sedimentary records over geologi...
Hydrogen isotopic ratios of terrestrial plant leaf waxes (dD) have been widely used for paleoclimate...
The molecular hydrogen isotope composition ((delta D) of leaf waxes from terrestrial plants is incre...
The debate of climate versus CO2 in controlling the long-term dynamics of tropical African vegetatio...
Leaf-wax n-alkanes are produced by terrestrial plants, and through long-term preservation in sedimen...
Lake Chala (3 degrees 19' S, 37 degrees 42' E) is a steep-sided crater lake situated in equatorial E...
The hydrogen isotopic composition of plant leaf-wax n-alkanes (dDwax) is a novel proxy for estimatin...
Hydrogen isotope values (dD) of sedimentary terrestrial leaf wax such as n-alkanes or n-acids have b...
The observation that the hydrogen isotope composition (δD) of leaf wax lipids is determined mainly b...
International audienceThe hydrogen isotope composition of plant leaf wax (dD wax) has been found to ...
The hydrogen isotope composition of plant leaf wax (δDwax) has been found to record the isotope comp...
Compound specific hydrogen isotope ratios (delta D) of long chain sedimentary n-alkanes, which mostl...
A transect of marine surface sediment samples from 1° N to 28° S off southwest Africa was analysed t...
Hydrogen isotopic ratios of terrestrial plant leaf waxes (δD) have been widely used for paleoclimate...
Leaf wax n-alkanes are long-chain hydrocarbons that can persist in sedimentary records over geologic...
Leaf wax n -alkanes are long-chain hydrocarbons that can persist in sedimentary records over geologi...
Hydrogen isotopic ratios of terrestrial plant leaf waxes (dD) have been widely used for paleoclimate...
The molecular hydrogen isotope composition ((delta D) of leaf waxes from terrestrial plants is incre...
The debate of climate versus CO2 in controlling the long-term dynamics of tropical African vegetatio...