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Extracting the most from terrestrial plant-derived n-alkyl lipids and their carbon isotopes from the sedimentary record: A review
Terrestrial plant biomarkers and their carbon isotopes provide insights into carbon cycling,
paleovegetation and paleoclimate, ranging in scale from local to global. Over the past …
paleovegetation and paleoclimate, ranging in scale from local to global. Over the past …
Molecular paleohydrology: interpreting the hydrogen-isotopic composition of lipid biomarkers from photosynthesizing organisms
Hydrogen-isotopic abundances of lipid biomarkers are emerging as important proxies in the
study of ancient environments and ecosystems. A decade ago, pioneering studies made use …
study of ancient environments and ecosystems. A decade ago, pioneering studies made use …
Spatial patterns of climate change across the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM; 56 Ma) is one of our best geological
analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …
petagrams of carbon were released into the ocean-atmosphere system with attendant …
Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum
Abstract The Palaeocene/Eocene thermal maximum,∼ 55 million years ago, was a brief
period of widespread, extreme climatic warming,,, that was associated with massive …
period of widespread, extreme climatic warming,,, that was associated with massive …
Hydrological control of river and seawater lithium isotopes
Seawater lithium isotopes (δ7Li) record changes over Earth history, including a∼ 9‰
increase during the Cenozoic interpreted as reflecting either a change in continental silicate …
increase during the Cenozoic interpreted as reflecting either a change in continental silicate …
Production of n-alkyl lipids in living plants and implications for the geologic past
Leaf waxes (ie, n-alkyl lipids or n-alkanes) are land-plant biomarkers widely used to
reconstruct changes in climate and the carbon isotopic composition of the atmosphere …
reconstruct changes in climate and the carbon isotopic composition of the atmosphere …
Carbon-isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian Basin, Portugal)
The Toarcian Oceanic Anoxic Event (OAE) in the Early Jurassic (∼ 183 Ma ago) was
characterized by widespread near-synchronous deposition of organic-rich shales in marine …
characterized by widespread near-synchronous deposition of organic-rich shales in marine …
[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …