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View article: Archaeal tetraether lipids as tracers for past marine environmental change
Archaeal tetraether lipids as tracers for past marine environmental change Open
Archaea are single-celled microorganisms that are abundant in marine environments and play a key role in the carbon and nitrogen cycles. Archaea can biosynthesize a wide variety of isoprenoid membrane lipids, including isoprenoid glycerol …
View article: Reviews and syntheses: Best practices for the application of marine GDGTs as proxy for paleotemperatures: sampling, processing, analyses, interpretation, and archiving protocols
Reviews and syntheses: Best practices for the application of marine GDGTs as proxy for paleotemperatures: sampling, processing, analyses, interpretation, and archiving protocols Open
Marine glycerol dialkyl glycerol tetraethers (GDGTs) are used in various proxies (such as TEX86) to reconstruct past ocean temperatures. Over 20 years of improvements in GDGT sample processing, analytical techniques, data interpretation an…
View article: A high-resolution late Paleocene–early Eocene organic-walled dinoflagellate cyst zonation of the United States Atlantic Coastal Plain
A high-resolution late Paleocene–early Eocene organic-walled dinoflagellate cyst zonation of the United States Atlantic Coastal Plain Open
Over the past decades, many expanded sedimentary records from the US Atlantic Coastal Plain (ACP) have been studied in detail to assess causes and consequences of the Paleocene–Eocene Thermal Maximum (PETM; ∼ 56 Ma). In ACP sections, the P…
View article: Evidence for limited atmospheric CO2 rise at the onset of the Miocene Climatic Optimum
Evidence for limited atmospheric CO2 rise at the onset of the Miocene Climatic Optimum Open
View article: Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs
Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs Open
The stable carbon isotope composition (δ13C) of plants and algae is influenced by environmental factors, such as pCO2, water availability, and altitude. To effectively use the δ13C of fossil material as a proxy for these parameters, it is …
View article: Ocean Drilling Program Site 959 Datasets
Ocean Drilling Program Site 959 Datasets Open
-Version V4 now includes the raw data associated with the paper "Evidence for limited atmospheric pCO2 rise at the onset of the Miocene Climatic Optimum", by Wubben et al.: item 'Miocene CO2; raw data' (md5:972e685a012a1f1915b4cfb6a3c5292b…
View article: Integrated bio-chemo-cyclostratigraphy of early Eocene carbon cycle aberrations from the Northern Negev
Integrated bio-chemo-cyclostratigraphy of early Eocene carbon cycle aberrations from the Northern Negev Open
View article: Transient oxygenation of the Mediterranean after the Zanclean megaflood
Transient oxygenation of the Mediterranean after the Zanclean megaflood Open
The Mediterranean basin reconnected to the Atlantic Ocean ~5.33 Myr ago, following its partial desiccation during the preceding Messinian salinity crisis (5.97 to 5.33 Myr). While the extent of terminal Messinian drawdown and abruptness of…
View article: Phanerozoic orbital-scale glacio-eustatic variability
Phanerozoic orbital-scale glacio-eustatic variability Open
View article: Silicate Weathering and Diagenetic Reaction Balances in Deltaic Muds
Silicate Weathering and Diagenetic Reaction Balances in Deltaic Muds Open
Reactions between terrigenous sediments, marine-biogenic substances and seawater modulate multiple biogeochemical cycles, but the dynamics and factors governing these reactions are poorly constrained. Deltaic mobile muds are a major sedime…
View article: Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs
Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs Open
The stable carbon isotope composition (δ13C) of plants and algae is influenced by environmental factors, such as pCO2, water availability, and altitude. To effectively use the δ13C of fossil material as proxies for these parameters, it is …
View article: Supplementary material to "Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs"
Supplementary material to "Impact of chemical treatments on the molecular and stable carbon isotopic composition of sporomorphs" Open
View article: Reviews and syntheses: Best practices for the application of marine GDGTs as proxy for paleotemperatures: sampling, processing, analyses, interpretation, and archiving protocols
Reviews and syntheses: Best practices for the application of marine GDGTs as proxy for paleotemperatures: sampling, processing, analyses, interpretation, and archiving protocols Open
Marine glycerol dialkyl glycerol tetraethers (GDGTs) are used in various proxies (such as TEX86) to reconstruct past ocean temperatures. Over 20 years of improvements in GDGT sample processing, analytical techniques, data interpretation an…
View article: Dating Oligocene-Recent siliciclastic sediment sequences from the Norwegian Sea
Dating Oligocene-Recent siliciclastic sediment sequences from the Norwegian Sea Open
The Norwegian Sea is crucial for ocean circulation and global climate and has therefore long been a focus in paleoceanography. However, precise dating of sediments has often proved difficult, due to poor preservation and endemism among mic…
View article: Testing Scenarios for the End-Triassic Mass-Extinction: Teratology in Ferns Near Historical and Industrial Mercury Emission Sites (Czechia)
Testing Scenarios for the End-Triassic Mass-Extinction: Teratology in Ferns Near Historical and Industrial Mercury Emission Sites (Czechia) Open
View article: Global Warming and Equatorial Atlantic Paleoceanographic Changes During Early Eocene Carbon Cycle Perturbation V
Global Warming and Equatorial Atlantic Paleoceanographic Changes During Early Eocene Carbon Cycle Perturbation V Open
A series of transient global warming events (“hyperthermals”) in the early Eocene is marked by massive environmental and carbon cycle change. Among these events, the impacts of the Paleocene Eocene Thermal Maximum (∼56 Ma), Eocene Thermal …
View article: Orbital (Hydro)Climate Variability in the Ice‐Free Early Eocene Arctic
Orbital (Hydro)Climate Variability in the Ice‐Free Early Eocene Arctic Open
Early Eocene (∼56–48 Ma) climates are useful to investigate polar climate dynamics in the absence of ice. We explore early Eocene orbital variability of Arctic climate using sediments recovered by the Arctic Coring Expedition (ACEX). High …
View article: Light Limitation of Poleward Coral Reef Expansion During Past Warm Climates
Light Limitation of Poleward Coral Reef Expansion During Past Warm Climates Open
The latitudinal range of modern shallow‐water tropical corals is controlled by temperature, and presently limited to waters warmer than 16–18°C year‐round. However, even during Cenozoic climates with such temperatures in polar regions, cor…
View article: High Arctic late Paleocene and early Eocene dinoflagellate cysts
High Arctic late Paleocene and early Eocene dinoflagellate cysts Open
Palynomorphs, notably sporomorphs and organic-walled dinoflagellate cysts, or “dinocysts”, are the only abundant microfossils consistently present in the sole available central Arctic upper Paleocene to lower Eocene sedimentary succession …
View article: Light limitation of poleward coral reef expansion during past warm climates
Light limitation of poleward coral reef expansion during past warm climates Open
The latitudinal range of modern shallow-water tropical corals is controlled by temperature, and presently limited to waters warmer than 16-18 °C year-round. However, even during Cenozoic climates with such temperatures in polar regions, co…
View article: Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene
Climate variability, heat distribution, and polar amplification in the warm unipolar “icehouse” of the Oligocene Open
The Oligocene (33.9–23.03 Ma) had warm climates with flattened meridional temperature gradients, while Antarctica retained a significant cryosphere. These may pose imperfect analogues to distant future climate states with unipolar icehouse…
View article: Interlaboratory Comparison of Branched GDGT Temperature and pH Proxies Using Soils and Lipid Extracts
Interlaboratory Comparison of Branched GDGT Temperature and pH Proxies Using Soils and Lipid Extracts Open
Ratios of glycerol dialkyl glycerol tetraethers (GDGT), which are membrane lipids of bacteria and archaea, are at the base of several paleoenvironmental proxies. They are frequently applied to soils as well as lake‐ and marine sediments to…
View article: Oceanography of the Eastern Equatorial Pacific Ocean Across the Oligocene‐Miocene Transition
Oceanography of the Eastern Equatorial Pacific Ocean Across the Oligocene‐Miocene Transition Open
The functioning of the Pacific Ocean—the world's largest ocean—during a warmer‐than‐present paleoclimate state remains underexplored. We present planktonic and benthic foraminiferal stable oxygen (δ 18 O) and carbon (δ 13 C) isotope record…
View article: Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world Open
Climate variability is typically amplified towards polar regions. The underlying causes, notably albedo and humidity changes, are challenging to accurately quantify with observations or models, thus hampering projections of future polar am…
View article: Tropical Warming and Intensification of the West African Monsoon During the Miocene Climatic Optimum
Tropical Warming and Intensification of the West African Monsoon During the Miocene Climatic Optimum Open
Studying monsoon dynamics during past warm time periods such as the Miocene Climatic Optimum (MCO; ∼16.9–14.5 Ma) could greatly aid in better projecting monsoon intensity, in the context of future greenhouse warming. However, studies on re…
View article: Early to Middle Miocene Astronomically Paced Climate Dynamics in the Eastern Equatorial Atlantic
Early to Middle Miocene Astronomically Paced Climate Dynamics in the Eastern Equatorial Atlantic Open
Detailed analysis of tropical climate dynamics is lacking for the Early to Middle Miocene, even though this time interval bears important analogies for future climates. Based on high‐resolution proxy reconstructions of sea surface temperat…
View article: Climate-forced Hg-remobilization associated with fern mutagenesis in the aftermath of the end-Triassic extinction
Climate-forced Hg-remobilization associated with fern mutagenesis in the aftermath of the end-Triassic extinction Open
View article: Global warming and equatorial Atlantic paleoceanographic changes during early Eocene carbon cycle perturbation V
Global warming and equatorial Atlantic paleoceanographic changes during early Eocene carbon cycle perturbation V Open
A series of transient global warming events (“hyperthermals”) in the early Eocene is marked by massive environmental and carbon cycle change. Among these events, the impacts of the Paleocene Eocene Thermal Maximum (~56 Ma), Eocene Thermal …
View article: A plant-wax δD record of palaeohydrology over the Cretaceous–Paleogene boundary
A plant-wax δD record of palaeohydrology over the Cretaceous–Paleogene boundary Open
Alongside the mass extinction, the Cretaceous–Paleogene (K–Pg) boundary interval experienced major climate perturbations due to the Chicxulub meteorite impact and Deccan Trap volcanism. The volcanism and release of climate modi…
View article: Orbital (Hydro)Climate Variability in the Ice-Free early Eocene Arctic
Orbital (Hydro)Climate Variability in the Ice-Free early Eocene Arctic Open
We explore the imprint of orbital variability on Arctic temperature and hydrology using sediments recovered during the Arctic Coring Expedition in 2004. High resolution records of lipid biomarkers (GDGTs; 2-kyr) and palynological assemblag…