Researchers analyzed 27,000 ancient seafloor samples and found a consistent pattern of manganese enrichment in sediments from high latitudes, indicating polar oceans remained oxygen-rich. This suggests that oxygen availability drove the observed differences in ocean conditions during ancient ice ages.
A new study suggests that slow uplift of the continent played a critical role in forming Antarctica's vast East Antarctic Ice Sheet. The research, published in Science, proposes that geological and climatic events that began over 120 million years ago led to rapid ice-sheet expansion.
A recent study reveals that Atlantic herring rewired its reproduction to survive in the Baltic Sea's low-salinity waters through four key genetic adaptations. These adaptations enabled the species to reproduce successfully despite the challenging environmental conditions, highlighting the importance of gene function and regulation in e...
The Science & Cinema format combines short movie clips with expert commentary to reflect on how science is portrayed on screen. The events engaged diverse audiences, including those not already interested in the topic, triggering reflection and emotional connections.
A new study reveals that four specific genes are crucial for the Atlantic herring's adaptation to low salinity in the Baltic Sea. The genes, expressed in sperm, eggs, and early embryos, enable the fish to reproduce successfully in brackish water.
A Harvard study resolves a longstanding climate puzzle by proposing that the Sturtian glaciation could have lasted 56 million years due to oscillating 'snowball' and 'hothouse' conditions. The researchers suggest intense weathering of volcanoes triggered global glaciations, which warmed and retreated over repeated cycles.
New research from the University of Virginia suggests that rear-edge populations of plants may be more resilient to climate change than expected. These populations, which have endured thousands of years of warming, have evolved specific traits allowing them to thrive in warmer climates.
Scientists have found that African frogs' diversity is linked to historical climate conditions, indicating they adapted to changing environments. The study suggests that even after 12,000 years, tropical frogs still remember the impact of past ice ages on their habitats.
A new study suggests that chemical weathering beneath thick continental ice sheets may have consumed atmospheric carbon dioxide and prolonged global glaciations during the snowball Earth event. This process could have slowed atmospheric warming and delayed deglaciation, helping to explain the long durations of some snowball Earth events.
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.
A large-scale population genomic study has shed new light on the evolutionary history of the button mushroom (Agaricus bisporus), one of the most widely cultivated edible fungi in the world. Climate dynamics and a key gene for adaptive evolution and domestication jointly shaped the mushroom's diversity.
A new study published in Science reveals that large fluctuations in global sea level occurred throughout the last ice age, rather than just at its end. This finding represents a significant shift in researchers' understanding of past climate history and challenges conventional wisdom on the middle Pleistocene transition.
New study reveals hippos inhabited Upper Rhine Graben in southwestern Germany between 47,000 and 31,000 years ago. The discovery challenges previous understanding of hippo extinction in central Europe during the last ice age.
A new study on Mars crater deposits reveals the planet went through repeated ice ages driven by shifts in its axial tilt, resulting in a gradual drying of the planet. The study provides insights that can be applied to Earth's changing environment and helps identify safe regions for future missions.
Research from Umeå University reveals that natural barriers shape the flow of water and hinder plant dispersal in rivers shaped by the last Ice Age. The study found no clear correlations between drainage area and channel width, or consistent increase in plant species diversity downstream.
A new study sequenced the genomes of glasswing butterflies, revealing six previously unrecognized species and shedding light on their rapid diversification. The research also showed that these butterflies use chemical communication to recognize each other, despite their similar appearances.
Researchers analyzed leaf waxes and found no significant drying trend in northern Africa between 3.5 and 2.5 million years ago. This challenges previous interpretations of the climate history of the region. The study suggests that dust deposits may be attributed to changes in wind patterns rather than rainfall.
The Late Ordovician Mass Extinction was caused by the rapid onset of global warming after the Hirnantian glaciation. The extinction lasted approximately 400 kyr with an average species extinction rate of 71.6% per 100 kyr during this period.
The study analyzed the impact of climate change during the late Palaeolithic and found that humans migrated eastwards to adapt to new climate conditions. The European population may have decreased by up to half during the Younger Dryas event, but populations in central and eastern Europe increased.
A new species of multisegmented fossil has been discovered in the Soom Shale with exceptionally preserved insides, including muscles, sinews, and tendons. The fossil, named Keurbos susanae, provides a unique glimpse into the evolutionary relationships of ancient arthropods.
A team of researchers has matched Earth's ice age cycles with orbital shifts, predicting the onset of the next ice age in approximately 10,000 years. The study analyzes a one-million-year record of climate change and finds a predictable pattern for glacial and interglacial periods.
Scientists at the University of Lausanne used AI to simulate the last Alpine glaciation, finding ice covers 35-50% thinner than previous models. The new approach enables unprecedented accuracy and resolution, making it possible to describe complex topography numerically.
A new study found that a unique population of large fish-eating herring has evolved in the Baltic Sea, exhibiting faster growth rates and lower levels of pollutants. These herring have adapted to the brackish water by switching from plankton-eating to a fish diet, with potential benefits for human consumption.
A new study has uncovered the diversity of Proterozoic eukaryotes, showing that severe Cryogenian glaciations drove a pivotal shift in their evolution. The research provides valuable insights into the relationship between environmental changes and the evolutionary history of life on Earth.
A new study reveals that industrial air pollution can trigger ice formation in supercooled clouds, reducing cloud cover and increasing regional snowfall. This phenomenon could help improve climate modeling and mitigation strategies.
Fossils from over 600,000 years ago show a shift in animal communities between warm and cold climate fluctuations. The Notarchirico site provides evidence of the emergence and disappearance of species such as cave lions, straight-tusked elephants, and red deer.
A new study published in Nature suggests that Earth's last ice age may provide crucial insights into future El Niño weather events. Researchers used ancient shells of marine organisms and advanced climate modeling to shed light on how El Niño patterns might change in a warming world.
Non-traditional field trip locations, such as urban settings and Disney Resorts, offer accessible outdoor educational opportunities. These locations showcase cross sections of corals and reef debris, ancient Ordovician fossils, and outcrop analogs that provide valuable insights into modern reef systems and broader earth history.
A rock formation spanning Ireland and Scotland has been confirmed as a rare record of the 'snowball Earth' period, when the globe was covered in ice. The Port Askaig Formation, composed of layers up to 1.1km thick, dates back to 662-720 million years ago during the Sturtian glaciation.
The Antarctic ice sheet formed around 34 million years ago in the eastern region of the continent, rather than the entire continent as previously thought. The study reveals that different regions of the ice sheet react differently to external influences and climatic changes.
A Yale-led research team suggests that large asteroids could have triggered 'Snowball Earth' events, where the planet's surface was covered in ice for thousands of years. The study found that asteroid strikes could have tipped Earth into a state with sea ice thickness of up to 10 meters, even if initial climate conditions were already ...
Researchers found that historically low volcanic carbon dioxide emissions, combined with weathering of a large pile of volcanic rocks in Canada, led to the prolonged Sturtian glaciation. The team used plate tectonic modeling and computer simulations to investigate the cause and duration of this ice age.
A new study from UB and CSIC challenges the classical view on the origins of the Antarctic Circumpolar Current, a key regulator of the planet's climate. The research reveals that the current dates later than the beginning of the Antarctic glaciation, making it sensitive to changes in climate conditions.
Scientists have discovered ancient ocean water trapped in mineral deposits in the Himalayas, providing insights into Earth's past climate and oxygen levels. The deposits suggest that slow-growing cyanobacteria may have triggered a major oxygenation event around 700-500 million years ago.
Researchers from Heidelberg University identified a pivotal step in the Earth's later climate development, finding that a warm ice age around 700,000 years ago led to changes in global climate rhythms. This 'warm ice age' caused accumulation of excess continental ice, resulting in prolonged and far-reaching glaciation.
The study reveals that Antarctic bottom water (AABW) has collapsed several times in the past, with these collapses linked to an enhancement of North Atlantic Deepwater and intensified Northern Hemisphere glaciation. AABW collapse may have pulled Earth into harsher glacial climates in the past.
Researchers from McGill University found that changes in sea levels during the Ice Age affected crocodile gene flow, isolating Caribbean and Pacific populations with distinct genetic mutations. The study reveals the resilience of American crocodiles to climate swings and highlights the need for targeted conservation efforts in Panama.
Researchers discovered hydrated glass in Antarctic rocks that indicates polar glaciation during the Late Cretaceous, around 66-100 million years ago. The findings suggest that climate conditions in Antarctica were more complex than previously thought, with evidence of ice sheets existing alongside a generally warm and humid environment.
Researchers have extracted a detailed record of 700,000 years of tropical climate change from an Andean lakebed, shedding light on the past 160,000 years. The discovery reveals that glaciers in the tropics followed a roughly 100,000-year cycle, with periods of wetness and dryness affecting global temperatures.
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 new study finds that cold-water corals thrive when food supply and oxygen content are available, but decline in response to changes. The research, led by MARUM, analyzed sediments from six locations and found that these factors have been critical to coral survival over the past 20,000 years.
Researchers have discovered a 30-mile-long, 9-mile-wide subglacial lake in East Antarctica that may hold the key to understanding the continent's glaciation history. The sediments at the bottom of Lake Snow Eagle could provide valuable insights into climate change and the ice sheet's possible demise.
Researchers identified glacial refugia for Campanula americana and found that populations nearest the refugia had highest potential for speciation. This discovery highlights the importance of conserving habitats in Southeastern regions.
Scientists have found that the West Antarctic Ice Sheet formed 35 million years ago, with warm deep water delaying its expansion to the sea. This discovery helps improve forecasts of its future stability and ice retreat.
Researchers from Texas A&M University have discovered past methane release in the Southern Ocean during a peak glaciation 23 million years ago. This finding suggests that ancient methane gas hydrates could contribute to ocean acidification and low oxygen levels, similar to recent environmental issues in the Gulf of Mexico.
A recent study published in PLOS Genetics found that genetic legacy from the last glaciation influences reindeer's migratory behavior. Caribou with more northern ancestry were more likely to migrate longer distances, highlighting an evolutionary adaptation to harsh tundra environments.
Researchers reconstructed bedrock geometry using gravity measurements, finding that glaciers of 'Würm' glaciation mainly widened valleys rather than deepening them. The study also revealed U-shaped cross-sections and asymmetric geometries in overdeepenings beneath Aare and Gürbe valleys.
A recent study analyzing air bubbles preserved in Antarctic ice for up to 1.5 million years suggests that glacial erosion is likely responsible for the decline of atmospheric oxygen levels over the past 800,000 years.
A research team has reconstructed the preglacial topography of North America's mid-continent, revealing how ice sheets reshaped the landscape and allowing researchers to understand rock erosion and deposition under ice. The findings also provide insights into water resources and availability in the region.
Researchers found that intense volcanic activity led to a surge in phosphorus levels, driving ocean oxygen levels down and triggering a severe mass extinction. The study suggests that natural weathering of volcanic material may have been responsible for the sudden cooling events.
A recent study revealed Asian climate variability across the early-to-middle Pliocene Warm Period, providing insights into future climate change. The research found that CO2-induced global warming led to increased summer monsoon moisture transport over East Asia and aridification in Central Asia.
Researchers discovered an ancient mangrove ecosystem in the Yucatan Peninsula, revealing how coastal mangroves adapted to a warmer world with higher sea levels. The study provides insights into past climate change impacts and its relevance to future scenarios of relative sea-level rise.
Researchers discovered glacial erosion features in Namibia's Kaokoland region, dated to 300 million years ago. These ancient fjords were formed when ice sheets retreated and sea levels rose, preserving a unique example of Late Paleozoic glaciation.
Researchers from Tohoku University uncovered possible photosynthetic activity during the Marinoan glaciation, a period of extreme cold in Earth's history. The study suggests that bacteria and early eukaryotes experienced low productivity before the Ediacaran period, when complex multicellular life emerged.
A new study by Professor Danika Bannasch and colleagues reveals that five distinct dog coat patterns have an ancient origin, dating back over 2 million years. The research suggests that lighter coat colors would have been advantageous to an extinct canid ancestor in arctic environments during glaciation periods.
Scientists discovered that changes in Earth's orbit allowed for ice-free regions to develop on 'Snowball Earth', enabling periodic survival of animal life. The research found evidence of iron-rich sedimentary rocks forming in the icy ocean near colossal ice sheets, providing a sanctuary for complex multicellular life.
Researchers propose novel sulfur cycle model incorporating volatile organosulfur compounds to explain global occurrence of superheavy pyrite. The Cryogenian interglacial interval saw sulfidic oceans with pervasive VOSC generation, leading to vertical isotopic gradients and superheavy pyrite precipitation.
New research reveals ancient Chinese arc magmatism preserved in the Chicxulub impact structure, shedding light on the Maya Block basement. Additionally, detrital zircon U-Pb ages from Antarctica's Victoria Land provide new constraints on the glaciation of southern Gondwana during the Late Paleozoic Ice Age.
Researchers found glacial deposits in the Bodui Zangbo River valley that date back to before MIS-6. The age of these deposits suggests a glacial advance occurred during MIS-12, likely due to surface uplift and decreased temperatures.
New research published in Nature Geoscience reveals that early Mars was covered in ice sheets, not flowing rivers. The study analyzed over 10,000 Martian valleys and found striking similarities with subglacial channels in the Canadian Arctic Archipelago.