Articles tagged with Mass Extinction
The Deccan Traps volcanic province shows that magmas rich in carbon dioxide erupted prior to the end-Cretaceous mass extinction. The study suggests that both surface eruptions and underground gas release are necessary to account for global warming leading up to this event.
A new study builds a multilayered computer model of marine life's history over the last 500 million years, echoing J. John Sepkoski's work on sudden mass extinctions. The analysis reveals a fourth major evolutionary fauna driven by biological interactions between predators and prey.
Researchers found that mass extinctions of land-dwelling animals, including amphibians, reptiles, mammals, and birds, coincide with major asteroid impacts and devastating volcanic outpourings of lava. The study suggests that these periodic events may be triggered by comets and are linked to the Earth's orbit in the Galaxy.
A new study using AI to examine the fossil record found that mass extinctions rarely create productive periods of species evolution, or 'radiations,' contrary to traditional ideas. Instead, the study suggests that many remarkable times of evolutionary radiation occurred when life entered new environments.
A study reveals carbon dioxide from volcanic eruptions likely caused the end-Triassic mass extinction. The apparent increase in light carbon may have been caused by local sea level decline and microbial mats prior to the event.
Researchers found evidence of a large volcanic cause of the largest mass extinction, with sedimentary mercury enrichments detected in rocks from the end of the Permian period. The study suggests that high-temperature volcanic combustion contributed to global warming and the loss of land and marine creatures.
A three-year $591,000 NSF grant will help geoscientist Ben Gill solve the riddle of the Triassic mass-extinction event. The study aims to determine the longer-term timeline of changes in life and environment before and after the extinction, as well as assess the role of oxygen content changes in the oceans.
A new study reconstructs the Permian-Triassic boundary event, revealing that massive volcanic activities in Siberia triggered the extinction of 95% of ocean life. The team used fossil brachiopod shells to analyze isotopes and simulate Earth's processes, concluding that warming and acidification led to catastrophic consequences.
A team of researchers reconstructed the key events leading to the Permian-Triassic mass extinction, which wiped out three-quarters of land species and 95% of ocean species. Volcanic eruptions released massive amounts of CO2, causing extreme warming and acidification of the ocean.
The Permian-Triassic mass extinction marked the origin of endothermy in both synapsids and archosaurs, with evidence suggesting a 'switch' around 250 million years ago. This coincided with the emergence of erect posture and hair in mammal ancestors, as well as feathers in bird ancestors.
A study analyzed biogeographic distributions of 52,318 marine fossils and found the latitudinal diversity gradient flattened rapidly during the Permian-Triassic mass extinction due to intense global warming and reduced ocean oxygen levels. The curve gradually returned to resemble modern biodiversity patterns after around 5 million years.
A new article validates the paradigm of multigenerational attritional loss of reproductive fitness (MALF) as a complete explanation for extinction. This shift from 'extinction' to 'evanescence' provides a clearer understanding of cause and effect, allowing for intervention in ongoing extinction events.
A new study examines Permo-Triassic mass extinction event's impact on tetrapod diversity, finding temperate latitudes held higher biodiversity before and after the extinction. The research suggests that regions now known for rich ecosystems were once too hot to support large animal communities.
A new study by Stanford researchers links the Late Ordovician Mass Extinction to ocean deoxygenation, revealing severe and prolonged anoxic conditions. The findings suggest that low oxygen levels in modern oceans will put strain on many organism types, potentially leading to extinction.
Researchers found corals exhibiting dynamic survival responses akin to the last big extinction event, including increased deep-water residing and solitary colonies. This study highlights how human-driven climate change is rapidly increasing stressors on coral communities, threatening 75% of species with extinction.
New research at CCNY suggests that carbon gases released by ancient volcanoes do not match geochemical clues of past mass extinctions, implying an unknown factor drove these events. The study provides insights into Earth's climate and how volcanic CO2 release affects the planet.
Scientists found that periodic changes in Earth's orbit and volcanic activity controlled the global carbon cycle during ancient mass extinctions. The study suggests that solar system processes had a significant impact on climate and environmental change over 200 million years ago.
A single primitive turtle species, Laurasichersis relicta, survived the mass extinction event that wiped out dinosaurs 66 million years ago in the northern hemisphere. The turtle's unique shell features and armor-like spikes allowed it to thrive in humid environments with forest areas.
A Yale-led team of researchers argue that asteroid impacts, not volcanoes, were the primary cause of the mass extinction event that killed the dinosaurs. The study's findings contradict recent work on the Deccan Traps, massive eruptions in India that occurred around the time of the K-Pg extinction event.
Researchers found that asteroid impact was primary cause of K/Pg mass extinction, while volcanic outgassing played role in shaping species after event. Volcanic emissions altered carbon cycle, allowing oceans to absorb CO2, limiting global warming and potentially influencing Cenozoic life.
A new study found that fossilized shells from around the globe show evidence of both rapid ocean warming and elevated mercury levels during the Deccan Traps volcanic eruptions. The findings suggest that the mass extinction event that killed off dinosaurs may have been triggered by both asteroid impact and massive volcanic eruptions.
Researchers found that increased mercury levels in the environment contributed to the mass extinction of three out of four species on Earth 201 million years ago. The study suggests a cocktail effect of CO2, global warming, and toxic substances like mercury, challenging the traditional theory of greenhouse gas-induced climate change.
Researchers found evidence of rapid ocean surface acidification following the Chicxulub asteroid impact, which may have contributed to the K-Pg mass extinction. The study suggests that this acidification led to a significant reduction in global marine primary productivity, lasting up to 40,000 years.
A Yale University study reveals that the Cretaceous-Paleogene extinction event was triggered by a sharp drop in ocean acidity, leading to the demise of marine calcifiers and a 50% decline in species productivity. The research provides new insights into the recovery of marine life after the event.
Researchers analyze two recent global warming events, the Cretaceous-Paleogene boundary and Paleocene-Eocene Thermal Maximum, to understand how oceans, animals, and plants respond to rapid climate change. The studies reveal that both events were caused by massive greenhouse gas releases, including carbon emissions from volcanic eruptions.
Scientists have confirmed a new mass extinction event occurred 260 million years ago, affecting life on land and in the seas. The event is correlated with massive flood-basalt eruptions, similar to those causing other known severe mass extinctions.
A 420 million-year-old mass extinction event, one of the most dramatic ever recorded, was caused by rapid and widespread depletion of oxygen in global oceans. The study provides a mechanism for the step-wise extinction event, driven in part by sulfidic ocean conditions.
A mathematical model explains relationship between oceans' carbon storage and environmental disruptions during mass extinctions. The study suggests that Earth's carbon cycle determines the magnitude of disruption, with external inputs influencing surges resulting from mass extinctions.
A new study reveals that lichens, organisms made of fungi and algae, seized the opportunity to evolve and diversify rapidly after the mass extinction event that wiped out the dinosaurs. The research found that some lichens grew sophisticated structures similar to plant leaves, filling the niches left vacant by extinct plants.
A Florida State University team has uncovered conclusive evidence linking sea level rise and ocean oxygen depletion to the Ireviken extinction event. The study reveals that reduced oxygen conditions played a central role in the mass extinction, with only about 8% of global oceans experiencing significant reductions.
A team led by Dr. Adriana López-Arbarello identifies three new species of the genus Eosemionotus, a type of ancient ray-finned fish, found in the Swiss Alps. The discovery provides insights into the rapid diversification of life after a mass extinction event.
Researchers precisely dated Deccan Traps volcanic eruptions, finding four pulses that released toxic gases into the atmosphere. The findings suggest a possible link between volcanic activity and dinosaur extinction, but the exact cause remains uncertain.
Scientists have discovered an iguana-sized reptile, named Antarctanax shackletoni, with unique adaptations to the extreme Antarctic environment. The ancient creature, a carnivore that hunted early mammals and amphibians, provides insights into prehistoric Antarctica's rapid evolution and diversification after mass extinction events.
Researchers uncover fossilized remains of Antarctanax shackletoni, an iguana-sized reptile with unique adaptations for hunting and survival. The discovery provides insights into prehistoric Antarctica's rapid evolution and diversification following a mass extinction event.
A new study has found that increased marine temperatures and reduced oxygen availability led to the extinction of nearly 96% of ancient ocean life during the catastrophic end-Permian mass extinction event. Tropical marine animals were more resilient to these changes, highlighting a potential pattern for future extinction events.
Researchers found Haiti's primary forest declined from 4.4% to 0.32% between 1988 and 2016, with 42 of 50 highest peaks deforested in the same period. The study predicts near-total loss by 2035, with up to 83% of species becoming extinct due to deforestation.
Deforestation in Haiti has led to the loss of primary forest cover on 42 of its 50 largest mountains. This has resulted in mass extinctions among reptiles, amphibians, and other vertebrates. The study's findings suggest that over the next two decades, all of Haiti's remaining primary forest will be lost.
A study found that the end-Cretaceous mass extinction event led to the shift in dominance from lamniform to carcharhiniform sharks. Carcharhiniforms, including Tiger and Hammerhead sharks, proliferated in the post-extinction world.
Researchers from Arizona State University study the Ediacaran-Cambrian transition and find a severe marine anoxic event coincided with the decline of early animals. The team integrated geochemical data and fossil records to precisely match evolutionary and environmental events, shedding light on this pivotal moment in Earth's history.
A team from University of Bristol identified the Carnian event through breakpoint analysis, a statistical method that compared species counts across Triassic samples. The event marked a sudden shift in ecosystems from dinosaur domination to modern groups like turtles and mammals.
A study published in PNAS found that powerful volcanoes depleted oceans of oxygen millions of years ago, driving mass extinctions. The researchers reconstructed Early Jurassic ocean oxygen levels and linked the event to massive volcanic activity and carbon dioxide increases.
Researchers analyzed plant fossil record and evolutionary relationships to conclude that global forest collapse led to the survival of only a few ancestral bird lineages. These early survivors adapted to life on the ground, laying the foundation for the diverse range of modern bird species.
A study published in Geology suggests that major volcanism led to the late Devonian extinction event, marked by a sharp increase in mercury levels in rocks from Morocco, Germany, and northern Russia. The discovery provides new evidence for the role of volcanism in mass extinctions.
By combining fossil occurrence data with social network analysis, researchers identified distinct associations of ancient marine animal life and investigated the representation of these communities over geologic time. This approach enabled the quantification of ecological impacts of mass extinctions and major ecological shifts.
A team of researchers used network analysis techniques to study the fossil records of marine life, revealing patterns in Earth's natural history. The analysis showed that major events like mass extinctions had significant ecological impacts, with some effects previously underestimated or overestimated.
Researchers analyzed sedimentary rocks and found light lithium isotopes in South China's seawater, potentially linking terrestrial and marine ecological crises. The findings suggest a connection between the Siberian Traps' eruptions and the Permian-Triassic mass extinction event.
Scientists found little evidence of negative impact from two major mass extinctions on ray-finned fishes, with no significant changes in body shape or jaw shape. The group's remarkable modern diversity is attributed to 400 million years of evolution.
A study by University of Chicago scientists found that mass extinctions removed species but retained ecological variety, whereas environmental changes lead to significant losses in functional diversity. The researchers analyzed two major mass extinctions and discovered a pattern of survival among functional groups.
Research suggests that asteroid impacts on hydrocarbon-rich areas may have caused global climate changes, leading to mass extinctions. The Chicxulub impact, occurring 66 million years ago, is a rare case of this phenomenon.
A study published in Palaeontology found that the Late Triassic mass extinction did not fundamentally alter marine ecosystem function. Despite significant species loss, marine ecosystems continued to operate with reduced diversity among remaining species.
A new study reveals that mass extinctions have predictable consequences, leading to low diversity and the emergence of dominant species. The researchers analyzed nearly 900 animal species between 260-175 million years ago and found a global pattern of 'disaster faunas'.
Two mass extinction events led to the survival of a low number of 'weedy' species that spread globally, affecting ecosystems and biogeography. The findings shed light on modern high extinction rates and potential consequences for current biodiversity loss.
Asteroid impact led to rapid genetic evolution in surviving birds, potentially influencing modern bird diversity. Human activities may accelerate similar 'Lilliput Effect', impacting evolution across species.
A study by MIT professor Daniel Rothman suggests that a sixth mass extinction may occur if the world's oceans hold enough carbon to destabilize the system. By 2100, human activities are estimated to add about 310 gigatons of carbon to the oceans, potentially tipping the planet into unknown territory.
A new study compares the recovery of land-dwelling vertebrates from different localities in southern Pangaea, finding stark differences in ecological diversity levels. The research suggests that carnivores and archosaurs were diverse and abundant in Zambia and Tanzania but relatively uncommon or absent in South Africa.
Large soot injections at the Cretaceous-Paleogene boundary could have prevented photosynthesis and reduced global temperatures by up to 16C for several years. The effects likely contributed to mass extinction through ozone layer depletion and stratospheric warming.
A study by James Muirhead and colleagues suggests that the formation of intrusive igneous rock sills triggered the End-Permian Mass Extinction. The team found that extreme heat from sill emplacement exposed sediments to contact metamorphism, liberating massive greenhouse gas volumes that drove extinction.
Researchers discovered a massive predatory fish species called Birgeria americana in Nevada's Early Triassic fossils, rewriting the history of apex predators. The find shows that marine ecosystems recovered faster than previously thought, and temperature conditions were suitable for life near the equator.
A new study reveals that a mass extinction 66 million years ago sparked an explosion of new frog species on different continents. The research, compiled by scientists from the University of Texas at Austin and other institutions, provides the most accurate frog family tree to date.
Researchers dated flood basalts to confirm magmatic activity coincided with mass extinction, linking CO2 release and climate change to species disappearance.