Articles tagged with Cenozoic Era
A new study reveals five primary sources of iron have influenced the South Pacific Ocean over 93 million years, including dust and hydrothermal sources. This evolution has shaped marine ecosystems and atmospheric carbon dioxide levels.
A new study by Connecticut College reveals that palm trees once thrived in subarctic Canada during the late early Eocene, approximately 48 million years ago. This finding indicates a warmer climate with ice-free winters, unlike previous assumptions.
A new study from the University of Nebraska-Lincoln examines fossil records going back 66 million years, tracking changes in mammalian ecosystems and species diversity. The research reveals that following the mass extinction of non-avian dinosaurs, mammalian communities experienced a surge in functional diversity for 10 million years.
A geologist from the University of Texas at Arlington is investigating the origin and climate importance of loess, a sediment formed by wind-blown dust, in Montana, Wyoming, and northeast Colorado. Her research aims to identify the sediment's source, when it appeared, and the climate changes that caused it to form.
Researchers have discovered a new genus and species of tardigrade fossil, Paradoryphoribius chronocaribbeus, preserved in 16-million-year-old Dominican amber. The specimen is the first tardigrade fossil recovered from the Cenozoic era and offers insights into the evolution of this ancient lineage.
A recent study found that changes in marine fossilization conditions led to a significant increase in diatom abundance during the Cenozoic Era. The researchers built a model of sedimentation rate and ocean temperature on biogenic silica burial efficiency, revealing improved preservation conditions around 5-20 million years ago.
Researchers found significant changes in the Pacific Walker circulation between 54-48 million years ago, with a broadening of ~38°. The circulation's intensity increased as the climate cooled, but its location was controlled by plate movements and CO2 concentrations.
Researchers analyzed core samples from the Chicxulub impact crater, revealing that top layers contained soil biomarkers suggesting a tsunami brought terrestrial material back to the site. The study also found evidence of impact-induced wildfires and a lack of sulfur-rich evaporites, implying a massive release of sulfate aerosols.