Articles tagged with Geologic History
Researchers analyzed barium sulfate minerals to determine biosphere productivity post-Great Oxidation Event. The study found a significant decrease in biosphere size following the event, potentially driven by decreased nutrient availability.
A new study of ancient rocks provides fresh insight into Earth's plate tectonics, which has evolved over the last 2.5 billion years. The findings challenge previous models suggesting plate tectonics operated throughout Earth's history.
A team of scientists used a microscopic drop of ancient seawater to show that plate tectonics on Earth began 3.3 billion years ago, 600 million years before the previous estimate. This discovery provides insight into the first stages of plate tectonics and the start of stable continental crust.
Researchers found that a global cycle of matter underpins modern plate tectonics, with excess water in the transition zone of the mantle originating from an ancient ocean on Earth's surface. Komatiitic magma samples revealed significant quantities of water and chlorine in minerals, indicating a 'pumping' of water into the planet's inte...
A study published in Nature Communications suggests that historical earthquake stresses can predict future seismic activity. Researchers analyzed centuries-old written records of damage to reveal 97% of earthquakes occurred on positively stressed faults.
Researchers at Syracuse University and international team discover evidence of abundant ammonium in pre-GOE oceans, providing a nutrient-rich environment for early life. This finding sheds light on the critical importance of nitrogen and phosphorus in Earth's history.
Researchers developed a novel laser-based measurement device to quantify rare CO2 variants, enabling accurate tracking of Earth's temperature. This breakthrough technology surpasses mass spectrometry in precision and can significantly shorten measurement times.
Researchers developed a new time scale using microfossils, doubling the resolution of published GoM time scales. The BP GNATTS provides valuable aid in seismic correlations, detecting unconformities, sediment redeposition, and faults.
A new characteristic 'biosignature' has been identified to track the remains of ancient life on Earth. The discovery suggests that graphite-like crystals alongside minerals such as apatite and carbonate are indicative of biological origin.
A new study published in the Bulletin of the Seismological Society of America has revealed signs of the 1906 San Francisco earthquake in a high-resolution map of the offshore northern San Andreas Fault. The map shows two large zones of slope failure on the seafloor, indicating that the fault ruptured in multiple strands.
The EarthScope National Office has compiled a list of the program's top 10 discoveries, showcasing revolutionary findings in North America's structure and evolution. These breakthroughs include insights into earthquakes, volcanoes, and groundwater, highlighting the continent's dynamic geological history.
Researchers calculated lunar crater ages using thermal data and found a rate of large impacts two to three times higher on both bodies over the last 290 million years. This discovery challenges the theory that Earth's craters were worn away through erosion, instead suggesting a lower impact rate prior to 290 million years ago.
A new study found the number of asteroid collisions with the Earth and moon has increased by up to three times over the past 290 million years. Researchers studied lunar craters using thermal data and images to determine their ages, revealing a surprising similarity between the two bodies' impact records.
Researchers analyzed historical data to determine the sources of destructive Indonesian earthquakes, finding that intraslab earthquakes were responsible for many damaging quakes. The study suggests that Indonesia's 2010 and 2017 seismic hazard assessments perform well in predicting ground motion in key Javanese cities.
A study compared projected future climate temperatures and precipitation to those of past warm periods on Earth. Mid-Pliocene climates (3.3-3 million years ago) emerged as the best analog for future climates after 2030 CE, while unmitigated greenhouse gas emissions scenarios led to Early Eocene-like conditions by 2150 CE.
Researchers found widespread strike-slip faulting on Ganymede, indicating complex geologic activity in the past. This discovery improves our understanding of Ganymede's tectonic history and its neighbor Europa's potential for hosting life.
Researchers use Earth's geological record to identify vegetation signatures on exoplanets, which can indicate the presence of life. The study found that as plants evolved on Earth, their signature became stronger, making older exoplanets more promising targets for detecting vegetation.
Researchers from Columbia University and USGS develop a physics-based model that replicates California's statistical seismic hazard model. This breakthrough marks a turning point in earthquake forecasting, providing accurate hazard estimates for engineers and regulators to make informed decisions on building codes and construction costs.
A new model provides the clearest picture yet of the geology below the Tibetan Plateau, revealing tears in the Indian upper mantle layer. The research suggests that these tears are responsible for earthquakes in the region, shedding light on the complex geological processes at play.
Scientists have discovered regions with lower seismic wave velocities beneath both ends of the Cascadia fault zone, indicating rising pieces of the Earth's upper mantle. These anomalies could modulate plate coupling forces and influence the location, frequency, and strength of earthquake events.
Researchers found low oxygen levels in early Earth rocks, indicating significant atmospheric variations during early life development. Oxygen concentrations were around 0.1% of present levels, affecting the evolution of complex organisms.
A team of scientists has discovered that Yosemite granite minerals crystallized at lower temperatures than previously thought, challenging our understanding of how granites form and record the planet's history. This finding has significant implications for geoscientists studying the Earth's crust formation and volcanic processes.
A new data-mining technique developed by Carnegie's Shaunna Morrison improves the understanding of Mars' geologic history and habitability. By analyzing mineral compositions and unit cell dimensions, scientists gained a more detailed picture of Martian minerals, including their origins and alteration processes.
Scientists reconstruct Earth's history with a new method that links astronomical theory to geological observation, enabling the analysis of ancient climate change. The study reveals days on Earth were over 18 hours long 1.4 billion years ago, and the moon's movement away contributed to the lengthening day.
Researchers developed a statistical approach combining astronomical theory and rock formation data to estimate Earth's axial precession rate and distance from the Moon. The study also reconstructed periods of astronomically influenced climate cycles, providing insights into ancient Solar System behavior.
Researchers reexamined historical seismograms from the 1906 Meishan earthquake to uncover a new mechanism that better fits fault rupture and damage patterns. This discovery will help improve understanding of complex fault systems in the region.
An international team of geoscientists has discovered an extensive buried mass of material on the seafloor, thought to have been eroded by the Zanclean flood. The mass covers an area equivalent to the island of Crete and is up to 900m thick in places.
Analysis of Réunion volcanic rocks indicates that their source material originates from isolated regions of the mantle with distinct chemistry. The discovery provides a unique fingerprint for the age and history of these ancient mantle pockets.
A study by Brown University researchers maps the mineralogy of the South Pole-Aitken basin, a giant impact crater on the Moon's far side. The research identified four distinct mineralogical regions within and around the basin, providing insights for future lunar exploration and landing site selection.
Researchers found that high atmospheric oxygen levels were not critical to the origin of animals, but rather occurred between 540 and 420 million years ago. The transition to a world with an oxygenated deep ocean required significant changes in atmospheric O2 levels, which approached modern levels around 400 million years ago.
A new study suggests that heat from a deep-seated oceanic mantle source, rather than a traditional mantle plume, drives crustal melting and surface volcanism in the western US. The research uses seismic tomography to peer into the subsurface and develop a hybrid geodynamic model that better matches observed geologic histories.
Researchers found that water in minerals can split up under extreme pressure, liberating oxygen to combine with iron and create a novel mineral. This discovery could have implications for the Earth's geologic history and potentially explain the Great Oxygenation Event.
Reservoirs of oxygen-rich iron between the Earth's core and mantle may have played a major role in shaping our planet's history. The discovery suggests that massive iron dioxide rocks could be generated annually above the core, releasing oxygen into the atmosphere, potentially triggering the Great Oxygenation Event.
Scientists confirm the presence of vinyl cyanide on Saturn's moon Titan, suggesting chemical processes analogous to those important for life on Earth. The findings provide insights into Titan's unique environment and potential prebiotic chemistry.
Researchers at UBC have discovered a unique sequence of pressure and temperature events required to form high-quality Canadian sapphires. This discovery will facilitate gemstone exploration in southern Baffin Island and potentially unlock new sources worldwide.
A new study published in Nature Communications suggests that the Tibetan Plateau's unique shape may be explained by the strength of the tectonic plates involved in its formation. The research found that a strong Asian plate results in a narrow plateau, while a weak Asian plate produces a broad one.
Researchers have discovered that sedimentary cycles are linked to sea level changes, rather than mountain erosion. The study uses carbon isotopes to predict sedimentary rock distribution and better understand the Earth's sedimentary history.
Researchers discovered that Titan's river networks, like Mars', formed topography without plate tectonics. This finding suggests a distinct geological history for the moons of Saturn and challenges our understanding of Earth's unique surface.
Scientists at ANU analyzed ancient zircon mineral grains to reconstruct the early Earth's surface. The study reveals that the planet remained relatively quiet and calm for its first 700 million years, with no major mountain-building events or continental collisions.
Scientists at McGill University propose a new theory on how Earth's crust was created, suggesting that silica-rich minerals condensed and fell back to earth over about a million years. This process, called aerial metasomatism, could provide clues for the search for life on exoplanets.
A study by Australian National University reveals the world's biggest volcanoes in Hawaii formed along twin tracks due to a shift in the Pacific Plate's direction three million years ago. The discovery helps reconstruct Earth's history and understand volcanic activity away from tectonic plate boundaries.
The Kaikoura earthquake triggered widespread slow slip events, producing simultaneous patches of slip in other areas. Ground faulting was complex, rupturing at nine to 12 faults with multiple orientations, resulting in a combined rupture length of about 180 kilometers.
A team of scientists has discovered a rare sample of the mineral majorite, which originated at least 235 miles below Earth's surface. The discovery provides valuable insights into the dynamic processes occurring deep inside the Earth and its history, including the formation of mountain ranges that persist today.
Researchers found geochemical anomalies, known as 'fingerprints' of early Earth conditions, in young volcanic rocks from Hawaii and Samoa. These signatures suggest that the planet's interior may not be well mixed after all.
The next generation TimeTree web combines molecular sequencing data with geological timelines and environmental information. Users can now explore the history of life on Earth in detail, tracing species evolution through time and comparing divergence times between species.
Scientists have found evidence of Earth's first example of recycling, where its own crust was reworked and reused over 4 billion years ago. The discovery uses neodymium isotope analysis to study variations in the element's abundance, indicating that ancient rocks were compositionally similar to younger basaltic oceanic crust.
A team of European paleontologists challenged the fundamentals of echinoderm evolution by discovering that some ancient groups survived the end-Paleozoic extinction. The findings revealed that these surviving echinoderms coexisted with modern sea urchins and brittle stars, stretching across various paleo-environments by the late Triassic.
Researchers propose that massive volcanic eruptions 717 million years ago led to a perfect storm of fire and ice, causing the largest glaciation event in Earth's history. The eruptions released sulfur dioxide into the atmosphere, blocking solar radiation and driving the formation of ice.
Researchers discovered that a mineral found in Martian meteorites could indicate a more water-rich history for the Red Planet. Synthetic whitlockite samples were subjected to shock experiments and X-ray studies, revealing partial conversion to merrillite, which is commonly found in Martian meteorites.
Researchers uncovered evidence of life at least 3,770 million years old from iron-rich deep-sea hydrothermal vents on Earth. The discovery provides direct proof of one of the oldest life forms on the planet.
Scientists found evidence of an ancient solid shell on Earth's surface using thermodynamic calculations and rock samples from Western Australia. The 'stagnant lid' model supports this theory, which contradicts the long-held assumption that plate tectonics began immediately after Earth formed.
Utah State University geologist Alexis Ault is investigating the earthquake history of the Wasatch Fault using nanoscale clues. She is collaborating with middle school students to explore this research, which provides a new window into processes that cause earthquakes at the nano-scale.
Researchers discovered minerals from 43 ancient meteorites, including rare and unknown types. This finding suggests a dramatically different solar system history, requiring a revision of current understanding. The study's results confirm a hypothesis presented last summer and show that the solar system is not stable over time.
A new analysis published in the Bulletin of the Seismological Society of America suggests that a tiny North Korean seismic event in May 2010 was an earthquake, not a nuclear explosion. The study's findings contradict previous reports that claimed it was a small nuclear test.
A newly discovered valley on Mercury is about 250 miles wide and 600 miles long, with steep sides that dip as much as 2 miles below the surrounding terrain. The valley likely formed due to rapid cooling of Mercury's interior, which would challenge previous assumptions about the planet's geologic past.
A new study published in the Bulletin of the Seismological Society of America suggests that a handful of damaging earthquakes in the Los Angeles Basin may have been induced by oil production activities in the early 20th century. The researchers found links between earthquakes and significant oil production activities nearby, but note t...
A new study confirms that the entire 2,400-kilometer Himalayan mountain range is seismogenic and can produce large earthquakes. Researchers discovered a major earthquake in Bhutan in 1714 using historical records and geologic data, shedding light on the region's potential for natural hazards.
A new study by Yale University researcher Jun Korenaga suggests that planets like Earth form through multiple giant impacts, leading to diverse sizes and internal temperatures. This lack of self-regulating mantle convection has significant implications for planetary habitability.
Researchers studied 7th-century A.D. temples in northwest India to reconstruct historic earthquakes, finding evidence of damage from magnitude 7.8 and 7.6 quakes. The study extended rupture zones for two major earthquakes, suggesting the region is prone to powerful earthquakes.
Researchers discovered microscopic crystals telling of unimaginable pressures and temperatures when a 12-kilometer asteroid formed Meteor Crater. The zircons endured temperatures of 2,000 degrees Celsius, revealing an unusual realm for geology where extreme pressure and temperature occur briefly.