Articles tagged with Sedimentary Rocks
Researchers analyzed millions of high-frequency turbidity measurements to reconstruct daily sediment movement, revealing a major shift: Rivers are becoming more 'bursty', with a 20-day decrease in the time it takes to transport 90% of their annual sediment. This change can overwhelm water treatment systems and damage aquatic habitats.
Researchers found evidence that the Aleutian Islands' subduction beneath the North American Plate occurred at least 56 million years ago, significantly earlier than previously thought. This discovery has implications for understanding tectonic and climatic processes that shaped the Earth's history.
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 new study found that land and ocean weathering processes are linked, influencing the amount of carbon stored or released into the atmosphere. The research proposes a continuum approach to studying weathering reactions on both land and in the ocean.
The expedition aims to assess the storage potential of rocks and lay the foundation for their geophysical monitoring. Globally, basalt deposits beneath the ocean theoretically have a storage capacity of 40,000 gigatons.
A new study by Texas A&M University researchers has revealed insights into Mars' geological history and potential for ancient life. The team analyzed diverse volcanic rocks in the Jezero Crater, providing a window into the planet's distant past and signs of altered olivine.
A research team from the University of Göttingen investigated the influence of the Zagros Mountains on Earth's surface bending. They found that the Neotethys oceanic plate is breaking off horizontally, creating a depression in the region.
Researchers used Re–Os dating to uncover the timing of Japan's geological history, revealing key insights into the region's evolution. The study focused on Besshi-type VMS deposits, which provided precise markers for the timing of subduction and ridge subduction beneath Japanese Islands.
Researchers have refined the timing and duration of Ocean Anoxic Event 1a, an extreme environmental disruption that caused significant extinction among plankton. The study determined OAE 1a lasted for just over 1.1 million years, providing valuable insights into Earth's climate and ocean system.
A new study reveals that a giant meteorite impact, equivalent to four Mount Everests, triggered a tsunami that mixed ocean debris and heated the atmosphere. This led to a rapid recovery of bacterial life, with iron-metabolizing bacteria flourishing in its wake.
A study reveals a global unconformity, or gap in the rock record, around the edges of every continent at the time of the greenhouse-to-icehouse climatic transition. The finding challenges traditional ideas about sediment movement and accumulation in deep oceans.
Seven rock samples collected along the fan front of Mars' Jezero Crater show evidence of minerals formed in water, suggesting a watery environment. While organic matter cannot be confirmed, these rocks may hold the key to finding remnants of ancient Martian life.
The samples, obtained from river deposits in a dried-up lake on Mars, are crucial for understanding the Red Planet's water history. The fine-grained sediments in the rocks are believed to retain signs of past biological activity, including organic molecules, making them significant for searching for life on Mars.
Scientists have reconstructed climate information from rocks dating back to the Devonian period, finding significant geological events such as oceanic openings and mountain uplift. The study's findings may help improve the usability of deep geothermal energy.
Researchers found seawater mixed with ore fluids to form gold, revealing a new mechanism for gold vein formation. This discovery could lead to the identification of high-grade gold deposits in sub-seafloor settings, reducing environmental impact.
Researchers found that the energy dissipated by past earthquakes was significantly higher than expected, suggesting repeated earthquakes with magnitudes of 5.8-8.3 Mw. The unique pattern of fragmentation in the breccia provided valuable evidence to estimate the energy of past earthquakes.
The Perseverance rover has collected and remotely determined the original orientations of most bedrock samples to date. This breakthrough will help scientists answer key questions about Mars' past, including its magnetic field, water flow, and tectonic processes.
A clay mineral called smectite, formed through plate tectonics, efficiently traps organic carbon and could help buffer global warming. Smectite's accordion-textured folds effectively trap dead organisms, preventing them from being consumed by microbes.
Researchers use rhenium as a proxy for carbon to quantify the rate of fossil carbon dioxide release into the atmosphere. The study found that high rates of carbon breakdown persist from mountaintop to floodplain, offering valuable insights into the planet's history and response to climate challenges.
A team of researchers at Texas A&M University has developed a new model to accurately measure ancient ocean temperatures using clumped isotopes. By understanding the reordering process, they were able to identify the role of water as an accelerator in resetting clumped isotope temperatures.
Analysis of the Thwaites Glacier in West Antarctica shows there is less sedimentary rock than expected, a finding that could affect how the ice slides into the ocean. The new map of the geology of the region provides an exciting basis for better predictions of future ice flow and sea level rise.
Researchers have created a detailed map of the geology beneath Thwaites Glacier in West Antarctica, showing that only about a fifth of the ground is sedimentary rock. This finding could affect how the glacier behaves as it retreats due to climate change, with potential implications for ice flow and loss from other glaciers.
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.
The Zhurong rover has provided direct in-situ evidence of ancient oceans in the northern plains of Mars, with sedimentary structures forming during the regression of a paleo-ocean. The discovery sheds new light on the early history of Mars and its habitability.
Research at KAUST demonstrates that most of the Red Sea is underlain by oceanic crust, overturning the assumption that it's an extended rift basin. The team mapped the transition from a rift to seafloor spreading and found approximately two-thirds of the Red Sea is currently covered by oceanic crust.
Researchers analyzed 550 million-year-old cherts to uncover the secrets of early Earth's cooling. The study found that oxygen isotope ratios in ancient cherts are driven by the Earth's thermal evolution, not seawater temperatures, sparking new insights into the planet's history.
The largest earthquake on Mars, a 4.7 magnitude marsquake, revealed layers in the crust suggesting a massive meteoroid impact, with possible alternating volcanic and sedimentary rocks. This finding provides evidence for past collision events that shaped the planet.
Research suggests that varying oxygen levels in the Earth's atmosphere may have spurred the emergence of early animal life forms. The study reveals oscillations between high and low oxygen levels over 1.5 billion years, providing a new perspective on the development of animals.
The Perseverance rover has collected the first Martian rock samples that could be returned to Earth, shedding light on whether Mars ever hosted life. The rock samples come from the Jezero crater floor, where scientists believe a watery past may have supported life.
A new study in Frontiers in Earth Science questions the link between climate change and ecosystem diversity during the origin of dinosaurs in Argentina. The researchers found that variations in species abundance cannot be explained by climatic changes, instead attributing it to preservation and sampling biases.
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 McGill University found that oxygen levels rose with complex eukaryotic ecosystems, indicating low oxygen was a significant limitation on evolution for billions of years. The discovery has implications for searching for biosignatures in other planets, focusing on ozone detection.
A new study verifies that ancient glaciers caused the erosion of rocks up to 3 miles thick during the Snowball Earth period, resolving a long-standing debate. The research uses thermochronology to estimate temperature and thermal structure, finding a widespread signal of rapid cooling consistent with massive glacier erosion.
Researchers used Rayleigh waves to produce high-resolution images of the rocks underneath the ice sheet, identifying key factors controlling ice flow. The study provides a better understanding of processes contributing to accelerated ice discharge into the ocean and sea level rise.
The Sierra Nevada mountain range in California has a complex history, with two distinct periods of formation. The ancient range was formed around 100 million years ago as a volcanic chain, but was later dwarfed by a vast plateau. Volcanic activity around 40 million to 20 million years ago lifted the Earth's surface, forming new mountai...
The world's largest ammonite species, Parapuzosia seppenradensis, reached diameters of 1.5-1.8 meters around 80 million years ago. This evolution likely helped the species evade predation and survive in its environment.
Researchers used a see-through porous medium to analyze polymer solutions' movement, overturning the assumption of uniform laminar flow. The polymers stretched out, creating turbulence and slowing the velocity of the flow.
Researchers found that continents have always been rich in silica, contradicting previous models. Continental growth occurred in six major periods every 500-700 million years over the past 3.7 billion years.
Researchers from the University of Hong Kong propose that sedimentary rocks measured by Curiosity rover represent sand and silt deposited by air-fall and reworked by wind. The discovery suggests a reducing atmosphere on ancient Mars with conditions similar to those found in modern-day deserts.
Researchers recovered 10,000 extraterrestrial chrome-spinel grains to establish a paleoflux record of meteorites falling to Earth. The results suggest that meteorite delivery has been largely stable over the past 500 million years.
Researchers used statistical analysis of zircon ages to determine continental formation timelines. The study suggests that modern-scale watersheds formed as early as 2.7 billion years ago.
Fossils from the Huajiying Formation in northern China reveal that the Jehol Biota appeared around 135 million years ago and lasted for approximately 15 million years. This early biota includes feathered dinosaurs, early birds, mammals, insects, and flowering plants.
A significant increase in phosphorite deposition during the Ediacaran Period may have contributed to the emergence of large animals. The study found that nutrient upwelling from the oceans, rather than terrestrial erosion, drove this change.
A recent study reveals that Cr(III) dominates in all sedimentary marine carbonates, contradicting previous theories on the oxidation of Earth's early atmosphere and ocean. The findings suggest that either microbial reduction or preferential uptake of Cr(III) by carbonate may be responsible for the absence of Cr(VI) in these rocks.
Scientists have developed a new method to detect signs of early life in ancient rock formations by analyzing high concentrations of potassium. This approach is promising as it could help identify the presence of microorganisms in sedimentary rocks dating back 2.1 billion years.
The study suggests that late Proterozoic 'snowball Earth' events triggered rapid glacial erosion, transferring sediment from continents to ocean basins. This process may be linked to the formation of the Great Unconformity.
Researchers found 121 new millipede trackways in Ordovician sedimentary rocks, contradicting the current understanding of animal life on land. The discovery sheds light on a key evolutionary event and highlights the importance of ancient rock records in understanding global change.
Researchers identified four units with different deposition types, including conglomerates and ridges formed by moving water. The Martian deposits are similar to those found in Earth's Channelized Scablands and suggest large-scale global ice and dramatic outburst floods.
Researchers analyzed silicon and oxygen isotopes in zircon crystals to infer the presence of sedimentary rocks, such as cherts or banded iron formations, on early Earth. The findings suggest that these rocks may have existed over 4 billion years ago, providing a window into the planet's primordial chemistry.
A study of injection wells reveals that they can cause earthquakes up to 6 miles away from the well site. Injecting fluids into sedimentary rock produces bigger, more distant earthquakes compared to injecting into the underlying basement rock. This challenges current recommendations for hydraulic fracturing and wastewater disposal.
A new experiment by Iowa State University's Elizabeth Swanner simulated prehistoric oceans and found that much of the iron was reduced again into its dissolved form despite oxygenation by cyanobacteria. This unexpected result challenges traditional assumptions about how iron-rich sedimentary rocks are formed from ancient oceans.
Researchers analyzed sediment data to find that mudrock is rare in the first 3 billion-year record of sediments but common after the middle Paleozoic era. The steady increase of mudrock suggests a relationship between its emergence and that of plants.
Scientists have documented a clear-cut instance of a massive earthquake triggering slow slip events in New Zealand, some occurring as far away as 300 miles from the epicenter. This study provides new insights into the relationships between slow slip events and earthquakes.
A team of researchers has obtained an improved age for the Matuyama-Brunhes boundary, a geological event that occurred approximately 780,000 years ago. The team used radiometric dating and sedimentary rock samples to determine the exact age of this event, which is now confirmed as 770.2 thousand years ago.
Scientists at the National Oceanography Centre have discovered a new fundamental rock property that allows electricity to flow more easily through sedimentary rocks in the vertical direction. This finding will improve the interpretation of geological fluid flow from geophysical surveys.
Researchers used microscopic fossils to date sedimentary layers and shed light on the origin of the Canary Islands. The study supports the mantle plume model, suggesting oceanic volcanoes formed from an anomalously hot plume of molten rock from the Earth's mantle.
Researchers analyzed 1,400 damage sites to determine relationships between ground deformation and faults. They found evidence of reverse movement along preexisting faults, which caused widespread ground deformation in the San Andreas fault region.
A new rock formation, Tava sandstone, has been discovered in the Colorado Rockies, featuring an unusual relationship with older rocks. The formation is believed to have resulted from large earthquakes or other catastrophic events, and its age dates back to ~750 million years ago during the Cryogenian Period.
Researchers have discovered an ancient Hawaiian volcano, named Ka'ena, which is believed to be the first building block for the island of O'ahu. The study provides compelling evidence that Ka'ena's lava chemistry and volcanic evolution played a crucial role in shaping the island's landscape.
The end-Triassic extinction was caused by widespread volcanic eruptions in the Central Atlantic Magmatic Province, which spewed forth huge amounts of lava and gas. The eruptions occurred precisely when the extinction began, providing strong evidence that they triggered the event.