Researchers at Indiana University and Virginia Tech develop a method to assess the validity of the principle of detailed balance, widely used in models for environmental projects. The study confirms that the principle applies in systems where rates of forward and reverse processes are balanced.
A UCLA-led research team discovered life likely existed on Earth at least 4.1 billion years ago, 300 million years earlier than previously thought. The study suggests that life may have begun shortly after the planet formed and could be abundant in the universe.
Researchers discovered that bacteria can use magnetite to create a 'natural battery' by loading and discharging electrons. This mechanism has implications for cleaning up toxic metals and could be adapted for other types of bacteria, expanding its potential uses.
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Researchers find that the Earth's crust formed relatively slowly from 1.7 to 0.75 billion years ago, with little activity and stable environments, before speeding up, potentially inducing evolutionary changes. This discovery has implications for the interpretation of climate models.
A team of scientists has discovered that the Yellowstone hotspot is less likely to erupt again soon, as evidenced by crystals found in Idaho rocks. The analysis suggests that the magma chambers are 'recycled', meaning they have been re-used before, and that this process could lead to a longer eruption cycle for the region.
New research presents evidence suggesting that life may have originated on Mars and was brought to Earth via a Martian meteorite. The study tackles two paradoxes related to the origin of life on Earth, including the 'tar paradox' and the difficulty in starting life due to water coverage.
New research by Dr Bernard Grobety reveals that crystalline particles in Icelandic volcanic ash are more harmful to jet engines and fall out of the cloud faster than glassy particles. The study aims to improve authorities' response to future eruptions by understanding the behavior of these particles.
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Researchers predict increased likelihood of large-volume lava flows and phreatomagmatic eruptions at Yellowstone National Park along three NNW-trending fault lines. Geochemistry suggests rapid magma ascent without storage, supporting a higher probability of future volcanism along these regions.
Scientists have developed a method to distinguish between primary and secondary organic carbon in ancient sediments, providing insights into the earliest life forms on Earth. By analyzing chemical fossils from Neoproterozoic glacial sediments, researchers have revealed new information about the environment and ecosystems of this period.
A geochemist raised concerns about the efficiency of carbon storage projects by highlighting the impact of underground chemical reactions on mineral dissolution. Research is needed to analyze reaction rates and affected minerals for better carbon storage project evaluation.
New intense sources of radiation at national facilities are allowing geochemists to gather images and data on minerals in one second, revolutionizing the field. The enhanced power of x-rays and pulsed neutrons enable researchers to detect, characterize and understand mineral components and contaminants.
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A 150-million-year-old 'Dinobird' fossil has been found to contain remnants of the animal's original chemistry, including phosphorous and sulfur in its feathers. The discovery could revolutionize the field of palaeontology by providing a new avenue for learning about long-extinct creatures.
New research by UCLA geochemists suggests that plate tectonics began more than 4 billion years ago, with ancient mineral grains indicating low heat flow and water presence on Earth during its first 500 million years.
The new five-year grant from NASA's Astrobiology Institute will focus on developing indicators of life, including analyzing cells, metals, and DNA. The team will search for microbial life in extreme locations on Earth and study ancient rocks for signs of past life.
Researchers reconciled inconsistencies between two pre-existing data sets for kaolinite, a major earth and industrial material. The findings provide a unifying approach for explaining crystal and mineral dissolution and growth, with implications for understanding geological time, nuclear waste storage, and biomedical issues.
Researchers discovered minimum melting conditions on early Earth, 200 million years after solar system formation, using a new zircon thermometer technique. This finding provides important information about the first eon of Earth's history and opens up possibilities for life's early foothold.
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Dr. Paul Ribbe will be honored with a symposium for his significant advances in the crystallography of feldspars, which led to the creation of definitive work on mineralogy. The symposium features keynote addresses from internationally recognized scientists and explores the 'micro to macro' approach pioneered by Ribbe.
The Penn State Center for Environmental Kinetics Analysis will bring together experts to measure and synthesize kinetic data for environmental systems, with a focus on scaling and modeling. The center aims to increase understanding of environmental systems among researchers and the general public through education and outreach initiati...
A recent study published in Nature announces a major advance in the study of Amazon Basin's hydrology and geochemistry dynamics. The research partnership has yielded precise measurements of water, sediment, and geochemical inputs contributed by the Amazon's main tributaries.
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Researchers at UC Davis and UC Santa Barbara have discovered a link between rapid changes in ocean carbon chemistry during the last ice age and shifts in ocean circulation. The study sheds light on how human-induced global warming may affect ocean currents, weather patterns, and climate worldwide.