A long-term decrease in the persistence of soil carbon caused by ancient Maya land use
The long-term effects of deforestation on tropical forest soil carbon reservoirs are important
for estimating the consequences of land use on the global carbon cycle, but are poorly …
for estimating the consequences of land use on the global carbon cycle, but are poorly …
[HTML][HTML] GC-MS Metabolomics to Evaluate the Composition of Plant Cuticular Waxes for Four Triticum aestivum Cultivars
FD Lavergne, CD Broeckling, DM Cockrell… - International journal of …, 2018 - mdpi.com
Wheat (Triticum aestivum L.) is an important food crop, and biotic and abiotic stresses
significantly impact grain yield. Wheat leaf and stem surface waxes are associated with traits …
significantly impact grain yield. Wheat leaf and stem surface waxes are associated with traits …
Leaf wax n-alkanes in modern plants and topsoils from eastern Georgia (Caucasus) – implications for reconstructing regional paleovegetation
M Bliedtner, IK Schäfer, R Zech… - …, 2018 - bg.copernicus.org
Long-chain n-alkanes originate from leaf waxes of higher terrestrial plants, they are
relatively resistant against physical and chemical degradation and are preserved in …
relatively resistant against physical and chemical degradation and are preserved in …
[HTML][HTML] A multiproxy record of palaeoenvironmental conditions at the Middle Palaeolithic site of Abric del Pastor (Eastern Iberia)
R Connolly, M Jambrina-Enríquez… - Quaternary Science …, 2019 - Elsevier
This paper presents a multiproxy palaeoenvironmental study from Abric del Pastor (Alcoy,
Spain), a rock shelter which has yielded evidence for Middle Palaeolithic human occupation …
Spain), a rock shelter which has yielded evidence for Middle Palaeolithic human occupation …
Biomarker proxies for reconstructing Quaternary climate and environmental change
EL McClymont, H Mackay… - Journal of …, 2023 - Wiley Online Library
To reconstruct past environmental changes, a range of indirect or proxy approaches can be
applied to Quaternary archives. Here, we review the complementary and novel insights that …
applied to Quaternary archives. Here, we review the complementary and novel insights that …
[HTML][HTML] Evaluating different methods for calculating the Carbon Preference Index (CPI): Implications for palaeoecological and archaeological research
AV Herrera-Herrera, L Leierer… - Organic …, 2020 - Elsevier
Abstract The Carbon Preference Index (CPI) is a molecular ratio often used to assign the
biological source and maturity of organic matter. This parameter is frequently employed in …
biological source and maturity of organic matter. This parameter is frequently employed in …
Eastern Mediterranean hydroclimate reconstruction over the last 3600 years based on sedimentary n-alkanes, their carbon and hydrogen isotope composition and …
Understanding past hydroclimate variability and related drivers is essential to improve
climate forecasting capabilities especially in areas with high climatic sensitivity, such as the …
climate forecasting capabilities especially in areas with high climatic sensitivity, such as the …
Paleogene plants fractionated carbon isotopes similar to modern plants
The carbon isotope composition (δ 13 C) of terrestrial plant biomarkers, such as leaf waxes
and terpenoids, provides insights into past carbon cycling. The δ 13 C values of modern …
and terpenoids, provides insights into past carbon cycling. The δ 13 C values of modern …
[HTML][HTML] Different hydrogen isotope fractionations during lipid formation in higher plants: Implications for paleohydrology reconstruction at a global scale
J Liu, W Liu, Z An, H Yang - Scientific reports, 2016 - nature.com
Leaf wax δD n-alkane values have shown to differ significantly among plant life forms (eg,
among grasses, shrubs and trees) in higher plants. However, the underlying causes for the …
among grasses, shrubs and trees) in higher plants. However, the underlying causes for the …
Sedimentary n-alkanes and n-alkanoic acids in a temperate bog are biased toward woody plants
Sedimentary plant waxes and their hydrogen and carbon (δ 2 H and δ 13 C) isotopes are
important proxies for past hydrologic and vegetation change. However sedimentary waxes …
important proxies for past hydrologic and vegetation change. However sedimentary waxes …