Articles tagged with Permian Extinction
A new Stanford-led study confirms the primary cause of the Permian–Triassic extinction event, which wiped out 96% of marine species and 70% of land animals. The research reveals that organisms with slower metabolisms and more vulnerable conditions were disproportionately affected by warming oceans and decreased oxygen availability.
The discovery of an ancient egg containing the embryo of Lystrosaurus reveals that its ancestors laid eggs, and offers insights into their reproductive strategy. The large eggs suggest that Lystrosaurus did not produce milk for its young, and its precocial hatchlings were capable of feeding themselves.
The discovery sheds light on marine ecosystems' rapid recovery and complexification after the end-Permian mass extinction. The Spitsbergen fossil deposit reveals diverse marine reptiles, including archosauromorphs and ichthyosaurs, with some species reaching 5m in length.
Researchers developed a model that predicts how creatures like clams and snails flourished in warmer, less-oxygenated waters after the end-Permian extinction. The findings suggest that climate change provided an environmental explanation for the global presence of surviving species.
Researchers discovered that tropical riparian ecosystems recovered rapidly within two million years of the end-Permian mass extinction, indicating a faster-than-thought adaptation. This finding contradicts previous theories on ecosystem recovery and suggests that life on land may have been more resilient than previously believed.
A 265-million-year-old fossil discovery in Brazil yields the oldest and largest known predator in South America, predating the rise of dinosaurs. The exquisitely preserved Pampaphoneus biccai had a skull over 40cm long and sharp canine teeth adapted for capturing prey.
Scientists detected compounds in 250 million-year-old pollen grains that function like sunscreen, suggesting UV-B radiation played a key role in the end-Permian mass extinction event. The discovery supports the theory of palaeoclimate emergency triggered by volcanic eruptions and global warming.
Scientists discovered that the first complex, multicellular life forms on Earth were wiped out 550 million years ago due to oxygen loss in the oceans. The researchers used nearly every known Ediacaran animal's environment and habits to disprove previous explanations for their disappearance.
Researchers found that the return of radiolarians, a tiny marine organism, helped restore habitable conditions after the massive extinction event. The study suggests that every microorganism plays a vital role in regulating biogeochemical cycles and conservation of the planet.
Harvard researchers found that rapid evolution of reptiles began much earlier than previously thought, connected to increasing temperatures. The study used a dataset of over 1,000 fossil specimens and analyzed their adaptation to climatic shifts.
The end-Permian mass extinction was characterized by a 10-degree climate warming, with 75% of organisms going extinct on land and 90% in oceans. Machine learning analysis reveals that declining oxygen levels, rising water temperatures, and ocean acidification were the key factors in organism survival or extinction.
Researchers found a sudden increase in ocean oxygen levels at the start of the Permian period's largest extinction event, marking a geologically rapid shift. This rapid fluctuation had a more significant impact than gradual decreases, highlighting its importance for modern-day life adapted to high oxygen levels.
A new type of footprint made by 247-million-year-old reptiles has been discovered in the Pyrenees. The discovery suggests that archosauromorphs played a large role in vertebrate recovery following the Permian mass extinction.
A study published in PLOS ONE suggests that marine recovery after the late Permian mass extinction was likely delayed by subsequent biotic crises. The researchers found that extinction rates of marine invertebrates peaked twice during the early Triassic, and ecological diversity increased only after a relaxation of environmental stresses.
A new study reveals that the deadliest mass extinction, 'The Great Dying', was not a sudden event but occurred gradually. The researchers found evidence of gradual decline in marine life, with some species dying up to 100,000 years before the main extinction event.
Researchers found that terrestrial biodiversity recovered in about 5 million years, compared to the 15- to 30-million year recovery period estimated earlier. This suggests a more rapid recovery than initially thought and rules out theories stating a severe spill-over effect into the terrestrial realm.
Researchers found no evidence of an asteroid impact during the Great Dying, a mass extinction event that occurred 250 million years ago. Instead, they suggest that atmospheric warming due to greenhouse gases from volcanic eruptions led to the extinction of 90% of marine life and nearly three-quarters of land-based plant and animal life.
The study found that only the Permian and Cretaceous extinction events led to significant changes in ocean ecosystem structure. The analysis suggests that life's evolution played a crucial role in shaping these ecosystems after the massive extinctions.
Researchers Ebersole and Miller analyzed fossil data and found no regional differences in extinction rates during the Late Permian mass extinction event. They also discovered that environmental zones and latitude had little impact on the severity of the extinction, suggesting a global cause.