Articles tagged with Geologic Periods
A new study provides a refined framework for understanding biotic evolution immediately preceding the Late Ordovician Mass Extinction in South China. The study reveals diverse shallow marine biotas in the region and reconstructs the regional ecosystem with high resolution.
Scientists have discovered evidence of repeating climate cycles operating every few years to decades during the Cryogenian glaciation, a period known as Snowball Earth. The findings suggest that these cycles were likely exceptions rather than the norm, and were triggered by small patches of open ocean in the tropics.
Scientists have developed a new way to track landscape development over millions of years using cosmogenic krypton in zircon minerals. This method reveals how climate, tectonics, and sediment transport are linked, providing insights into the Earth's surface history.
Mars plays a measurable role in shaping Earth's long-term climate patterns, including ice ages, through its gravitational influence and orbital cycles. The study suggests that Mars' presence is necessary for the existence of major climate cycles, which have driven evolutionary changes on Earth.
A new study from GreenDrill reveals that the Prudhoe Dome ice cap melted approximately 7,000 years ago due to mild Holocene-era temperatures. This finding highlights the region's vulnerability to human-induced climate change and has significant implications for sea level rise predictions.
A study by University of Washington researchers found that climate changes over 56 million years ago led to diversification of modern carnivores. The Eocene-Oligocene Transition and Mid-Miocene Climate Transition drove the emergence of new body shapes among species such as dogs, cats, bears, and seals.
Research led by the University of Washington found that climate transitions over 56 million years ago fueled the emergence of diverse carnivoran body shapes. The Eocene-Oligocene Transition led to changes between families, while the Mid-Miocene Climate Transition drove diversification within families.
Researchers from the University of Göttingen have identified oxygen isotopes in 'cherts' as indicators of heat flow on early Earth. The study reveals that cherts record paleo-heat flow on the Shatsky Rise oceanic plateau, providing insights into the conditions on the Earth's surface up to 3.5 billion years ago.
A study has found that high-latitude phytoplankton communities responded to a pre-PETM warming event, highlighting the importance of examining background intervals in determining ecosystem change. The results suggest even small environmental changes can have dramatic impacts on marine ecosystems.
A new study suggests that prolonged nitrate depletion delayed marine ecosystem recovery after the end-Permian mass extinction. Nitrate availability remained consistently low in South China during this period, with temperatures rising and falling to impact ocean stratification and upwelling.
Stanford researchers measured biomass of ocean life over the past half-billion years, finding a generally increasing trend. The study aligns with evidence for a rise in marine biodiversity and suggests an evolutionary connection between biomass and biodiversity.
A recent study has discovered that cold-adapted species began evolving 2.6 million years ago, with many modern species emerging around 700,000 years ago. The research provides insights into the evolution of Arctic ecosystems and highlights the importance of understanding past adaptations to inform conservation efforts.
Researchers from Utrecht University studied icebergs' routes during rapid ice cap deterioration and found evidence of ancient material from Antarctica near South Orkney Island. The study suggests that Antarctica had an ice cap in the late Eocene, and large icebergs could survive in warm ocean conditions.
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 groundbreaking study led by Virginia Tech provides the first direct geochemical evidence of a massive, rapid melting period on Earth after the last global ice age. The researchers analyzed lithium isotopes in carbonate rocks formed during this time and found strong evidence for freshwater meltwater interacting with the ocean.
A new AI tool called SandAI can analyze sand grains to determine their history, including whether they were shaped by wind, water, or glacial movements. This technology has the potential to help with modern-day forensic investigations into illegal sand mining and related issues.
Researchers discovered that blending crushed rock with arable soil could help reduce global temperatures. The process, known as enhanced chemical weathering, works by releasing calcium and magnesium from rocks, which bind atmospheric carbon dioxide and prevent its release back into the atmosphere.
New research from Rice University suggests that ancient microorganisms helped cause massive volcanic events by facilitating the precipitation of minerals in banded iron formations. The study provides insight into processes that could produce habitable exoplanets and reframes scientists' understanding of Earth's early history.
A team of paleontologists has discovered that countless sea anemone fossils were misinterpreted as jellyfish due to their soft bodies. However, when re-examined with a new perspective, the fossils were found to be anemones, showcasing the importance of fresh thinking in fossil interpretation.
A new study reveals that climate change is affecting Andean glaciers in sync with polar ice, suggesting the entire planet is connected. Researchers used sediment deposits from Lake Junín to create a record of glacial changes spanning 700,000 years.
A massive volcanic eruption at the end of the Triassic period caused a global cooling effect, leading to the mass extinction. The event paved the way for the rise of dinosaurs as their natural predators went extinct.
Researchers from Vrije Universiteit Brussel used new techniques to determine the age of limestone layers and fossils in Maastricht quarries, dating back to the last dinosaur age. The study found that the shallow sea was rich in oxygen, suitable for sustaining a diverse ecosystem.
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 have proposed new radioisotopic dates for Ediacaran fossil assemblages and carbon isotope perturbations, providing age constraints for both. The study reveals two negative carbon isotope excursions in the 575–550 Ma period, with the Shuram event occurring between 575 Ma and 565 Ma.
A new study reconstructed the Kuroshio Current Extension's past behavior, finding it was sensitive to global climate change during the Pliocene era. The current's sensitivity to CO2 levels is a concern for its potential impact on ecosystems, weather patterns, and regional climates.
Research from UBC and HKU Earth scientists reveals that massive volcanism played a key role in triggering oceanic anoxia, with CO2-induced environmental warming creating 'dead zones' over short timescales. The findings provide important insights into the sensitivity of the Earth system to global biogeochemical cycles and marine biology.
A team of researchers has identified over 1,100 unique large methane point sources across the Permian Basin using airborne imaging spectrometry. The study found that most sources were highly intermittent, but those that were persistent accounted for a significant portion of total emissions.
A new study using European satellite data found that Permian oil and gas operations are releasing methane at twice the average rate, with implications for reducing greenhouse gas emissions. The data highlights the importance of satellite technology in tracking methane emissions from large areas.
The discovery of exceptionally preserved late-Permian plant fossils in Jordan pushes back the ages of important seed plant lineages and suggests that drought-prone tropical habitats served as evolutionary cradles for early plant diversification. The findings indicate that these plant lineages survived the mass extinction event at the e...
Scientists have found fossilized starch granules on ancient plant megaspores, suggesting they were used as a spore-dispersal device. This discovery provides early evidence for mutualism between plants and animals in the Permian period.
A new study maps induced earthquake risk in the Permian Basin of West Texas, highlighting areas prone to seismic activity from fluid injection. The detailed stress map provides quantitative data for oil companies to inform more effective drilling operations and reduce the probability of larger earthquakes.
A study on late Permian ecosystems sheds light on biodiversity and species distribution near the equator. The research found an unusual variety of species in fiery, hot deserts, challenging the assumption that tropical regions are diversity hubs.
Climate model simulations suggest that a significant decrease in atmospheric CO2 concentrations could have led to global glaciation. The study indicates that Earth's coal deposits formed during this period may have been the trigger for such an event.
Researchers found that reusing produced water from hydraulic fracturing sites can reduce water management issues and potentially induced seismicity. The study analyzed 10 years of water data, revealing a significant difference in water use between conventional and unconventional wells.
New fossils support Andrey Martynov's theory that wasps emerged from snakefly-like ancestors around 260-270 million years ago. The study also identifies the origins of alderfly and nanosialid families.
A new study reveals that a Pangean desert supported a unique fauna, including the giant pareiasaur Bunostegos, which sported large, bulbous skulls resembling modern giraffe horns. The discovery supports the theory of central Pangea being climatically isolated, allowing this relict fauna to evolve distinct anatomical features.
The study provides a comprehensive review of the Yuzhou Flora, recognizing 111 genera and 307 species from 40 fossil plant layers. The authors propose hypotheses on evolutionary trends in leaf structure and venation patterns, as well as a new morphotype classification scheme for Gigantopteridales.
Scientists discovered Lepidopteris baodensis, a 251-million-year-old seed fern with subepidermal swellings that may have allowed it to survive in hot, arid environments. The finding expands knowledge of the genus' biology and taxonomy, as well as its relationship to other plant species.
Scientists have discovered primary exhalative hydrothermal dolostone in the Santanghu area of Xinjiang, China. The dolostone is believed to have formed via mantle-originated hydrothermal activities, providing valuable evidence for primary dolomite formation in geological history.
Researchers have discovered that massive volcanic eruptions in the late Permian period likely caused the extinction of nearly all marine species and a majority of land life. Mercury levels were found to be significantly higher than today's human-caused emissions, contributing to the loss of 95% of life in the sea.