Results 61 to 70 of about 899,223 (198)
Abstract The pattern and cause of upper‐water temperature (UWT) variations on millennial timescales in the Southern Ocean (SO) and the mechanism of their interaction with high‐latitude Northern Hemisphere climate remain unclear. Here, we reconstructed millennial‐scale subsurface temperature (subST) records from the Weddell Sea during the Last Glacial ...
Tong Wang +9 more
wiley +1 more source
(Table 1) Mg/Ca paleotemperature estimates for ODP Sites 172-1055 and 172-1059
(Table 1) Mg/Ca paleotemperature estimates for ODP Sites 172-1055 and 172 ...
Healey, Stephanie +1 more
core +1 more source
Data for: Constraining the applicability of organic paleotemperature proxies for the last 90 Myrs
Data associated with "Constraining the applicability of organic paleotemperature proxies for the last 90 Myr ...
de Bar, M (via Mendeley Data) +1 more
core +2 more sources
Food availability impacts oxygen isotope composition in freshwater snail shells
Abstract Freshwater mollusk shells serve as valuable archives for the reconstruction of past environmental conditions as they record water temperatures in their stable isotopic compositions during biomineralization. Yet, the impact of food availability on these isotopic records has never been fully explored.
Tom de Vries +8 more
wiley +1 more source
Reconstruction of the paleotemperature of the Central Yakutia Ice Complex during the Holocene period
The increase in worldwide temperatures is leading to changes in permafrost landscapes in disturbed areas, which are causing the onset of cryogenic processes. Central Yakutia has a high population density and human impact on the permafrost, which contribute to the widespread occurrence of these processes.
V. A. Novopriezzhaya, A. N. Fedorov
openaire +1 more source
Oxygen Isotopic Composition of Miocene Meteoric Water (δ18Ow) in Alpine Foreland Basins
Abstract The reconstructed stable oxygen isotopic composition of meteoric water (δ18Ow) is widely used for paleoclimate reconstructions. Understanding past environmental factors that drove changes in δ18Ow is essential for interpreting past climate conditions.
Armelle Ballian +6 more
wiley +1 more source
Non‐Uniqueness, Symmetries and Invariance of Thermal History Modelling in Sedimentary Basins
This paper approaches non‐unique inverse problems by generating a representative ensemble of all possible solutions using the concept of symmetry. In the context of basin modelling, a symmetry is any manipulation of a forward model's parameters (e.g., thermal history) that leaves the model output (e.g., downhole vitrinite reflectance) unchanged ...
J. Xiao, D. Waltham, Y. Wang
wiley +1 more source
Robust multi-proxy data integration, using late Cretaceous paleotemperature records as a case study
In paleoclimate studies, multiple temperature records are often compared and combined to evaluate temperature trends. Yet, no standardized approach for integrating proxy-derived paleotemperature records exists.
Peterse, Francien +20 more
core +1 more source
Thermal and Structural Reconstruction of an Eroded Foreland Basin: Central Appalachian Basin, USA
New low‐temperature thermochronology and modelling reveal a complex thermal history for the central Appalachian Basin. Results indicate Carboniferous exhumation of the fold‐thrust belt and Mesozoic heating in the foredeep linked to the Rome Trough. Deeply buried Devonian source rocks were consequently pushed past the peak oil and gas windows.
Kristopher L. Symanski +3 more
wiley +1 more source
The relevance. The Arctic regions of Western Siberia became a priority area of research and exploration. They have the unique paleoclimate features, the inversion sedimentation in Paleogene-Neogene and the considerable variations of petromaternal deposit
Albina Albertovna Iskorkina +3 more
doaj +2 more sources

