Biological diversification linked to environmental stabilization following the Sturtian Snowball glaciation. [PDF]
Bowyer FT +14 more
europepmc +1 more source
Modern investigations into spectral gamma-ray (SGR) records enhance understanding of sedimentary environments and paleoenvironmental conditions. This study examines a 111 m sand and shale interval in the Tak-1 well, Niger Delta Basin, to characterize ...
Oluwakemi Efemena, Franklin Lucas
doaj +1 more source
Nickel isotopes link Siberian Traps aerosol particles to the end-Permian mass extinction. [PDF]
Li M +9 more
europepmc +1 more source
Large igneous provinces played a major role in oceanic oxygenation events during the mid-Proterozoic
Low atmospheric oxygen levels during the mid-Proterozoic were occasionally interrupted by transient high oxygen levels. The cause of mid-Proterozoic ocean redox variability remains unclear.
Anbo Luo +3 more
doaj +1 more source
Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction. [PDF]
Kozik NP +8 more
europepmc +1 more source
Solar irradiance and ENSO affect food security in Lake Tanganyika, a major African inland fishery. [PDF]
McGlue MM +8 more
europepmc +1 more source
Mercury abundance and isotopic composition indicate subaerial volcanism prior to the end-Archean "whiff" of oxygen. [PDF]
Meixnerová J +6 more
europepmc +1 more source
A transient peak in marine sulfate after the 635-Ma snowball Earth. [PDF]
Peng Y +7 more
europepmc +1 more source
Chemostratigraphy Across the Triassic–Jurassic Boundary
The Triassic‐Jurassic transition (~201.5 Ma) is marked by one of the largest mass extinctions in Earth’s history. This was accompanied by significant perturbations in ocean and atmosphere geochemistry, including the global carbon cycle, as expressed by major fluctuations in carbon isotope ratios.
openaire +2 more sources
European mammal turnover driven by a global rapid warming event preceding the Paleocene-Eocene Thermal Maximum. [PDF]
Tabuce R +11 more
europepmc +1 more source

