Home Publications List
Publication display API.
This one is used to display publications on the home page.
GET /api/organization/section/home/publications?format=api&offset=8180&ordering=link_original
{ "count": 10649, "next": "http://onegeo.com/api/organization/section/home/publications?format=api&limit=20&offset=8200&ordering=link_original", "previous": "http://onegeo.com/api/organization/section/home/publications?format=api&limit=20&offset=8160&ordering=link_original", "results": [ { "id": "a74ac125-0af8-4ea7-a7ea-c3a5f9e39c7e", "slug": "the-health-burden-and-racial-ethnic-disparities-of-air-pollution-from-the-major-oil-and-gas-lifecycle-stages-in-the-united-states-by-karn-vohra-and-others-for-science-post", "created_at": "2025-09-05T05:34:36.209976Z", "views": 14, "name": "The health burden and racial-ethnic disparities of air pollution from the major oil and gas lifecycle stages in the United States, by Karn Vohra and others for Science", "about": "The U.S. oil and gas industry drives major health harms each year, with Black and Asian communities facing the greatest and most unequal burdens.", "text": "The United States has one of the world’s largest oil and gas (O&G) industries, yet the health impacts and inequities from pollutants produced along the O&G lifecycle remain poorly characterized. Here, we model the contribution of major lifecycle stages (upstream, midstream, downstream, and end-use) to air pollution and estimate the associated chronic health outcomes and racial-ethnic disparities across the contiguous US in 2017. We estimate lifecycle annual burdens of 91,000 premature deaths attributable to fine particles (PM2.5), nitrogen dioxide (NO2), and ozone, 10,350 PM2.5-attributable preterm births, 216,000 incidences of NO2-attributable childhood-onset asthma, and 1610 lifetime cancers attributable to hazardous air pollutants (HAPs). Racial-ethnic minorities experience the greatest disparities in exposure and health burdens across almost all lifecycle stages.", "link_original": "https://www.science.org/doi/10.1126/sciadv.adu2241", "status": 2, "country": [ { "id": 240, "name": "United States of America", "icon": "" } ], "sections": [ { "id": 83, "name": "Oil & Gas" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [ { "id": 240, "name": "United States of America" } ], "regions": [ { "id": 4, "name": "North America" } ] }, "filters": [ { "id": 8, "name": "Enlightenment", "badge_name": "Enlightenment", "show_badge": false, "children": [ { "id": 27, "name": "Publications", "badge_name": "Publication", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "9,10,27,11,12" } ] }, { "id": "be98778c-aac5-410e-9add-0024c7f6e3e9", "slug": "instability-in-the-geological-regulation-of-earths-climat-i-by-dominik-hulse-and-andy-ridgwell-for-science-post", "created_at": "2025-11-07T11:33:26.029022Z", "views": 55, "name": "Instability in the geological regulation of Earth’s climat I by Dominik Hülse and Andy Ridgwell for Science", "about": "Interactions between carbon burial and phosphorus cycling can destabilize climate and cause overcooling after major CO₂ release.", "text": "This process reveals that Earth's long-term climate balance is not solely governed by silicate weathering but also by complex biogeochemical feedbacks involving organic matter and nutrient cycles. When large amounts of CO₂ enter the atmosphere, enhanced organic carbon burial and phosphorus regeneration can initially accelerate cooling instead of stabilizing temperatures. Such feedbacks demonstrate how the carbon-phosphorus-oxygen interactions within oceans and sediments can amplify or reverse expected climate responses. These mechanisms, sensitive to the redox state of the oceans, help explain why some past climate events, including ice ages, occurred after periods of intense greenhouse gas emissions. Understanding these processes is crucial for predicting how modern Earth systems might react to rapid anthropogenic CO₂ release and whether similar feedbacks could influence future global cooling or instability in climate regulation.", "link_original": "https://www.science.org/doi/10.1126/science.adh7730", "status": 2, "country": [], "sections": [ { "id": 224, "name": "Atmosphere & climate solutions" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": true, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [ { "id": 13, "name": "Media content", "badge_name": "Media content", "show_badge": false, "children": [ { "id": 14, "name": "Photo", "badge_name": "Photo", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "14,15,16" } ] }, { "id": "51852618-288a-45f7-bc9d-a66ec88c593b", "slug": "science-quantifying-the-global-biodiversity-of-proterozoic-eukaryotes-post", "created_at": "2025-06-13T08:26:23.923114Z", "views": 23, "name": "Science: Quantifying the global biodiversity of Proterozoic eukaryotes", "about": "The Proterozoic Eon in Earth history is marked by numerous transformative evolutionary, environmental, and tectonic events. However, a comprehensive quantification of Proterozoic eukaryote fossil diversity is lacking.", "text": "Fossil data from the Phanerozoic eon provide insight into long-term changes in global biodiversity and how it has been shaped by evolution, environmental change, and species interactions. Insights from the earlier Proterozoic eon are relatively lacking because of historic gaps and inconsistencies in data. Using recent advances in data and analytical methods, Tang et al. produced updated estimates of eukaryote diversity across the Proterozoic. They found a gradual increase in species richness during the “Boring Billion” pre-Cryogenian period, which is distinct from the higher diversity and dynamics of the later Ediacaran. Cryogenian glaciations appear to define this shift toward greater extinction and diversification rates. —Bianca Lopez\n\nScience\n20 Dec 2024\nVol 386, Issue 6728\nDOI: 10.1126/science.adm9137", "link_original": "https://www.science.org/doi/10.1126/science.adm9137", "status": 2, "country": [], "sections": [ { "id": 145, "name": "History of Earth: insights for the future" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [] }, { "id": "030a0534-4677-4b0d-b5af-9e84deddf517", "slug": "global-cases-of-groundwater-recovery-after-interventions-by-scott-jasechko-for-science-post", "created_at": "2026-03-26T13:04:34.812749Z", "views": 13, "name": "Global cases of groundwater recovery after interventions | by Scott Jasechko for Science", "about": "Groundwater depletion poses a challenge to irrigated agriculture and water access. Depleted aquifers can be refilled, but the interventions that have successfully refilled depleted aquifers are rarely reviewed.", "text": "This work reviews 67 cases of groundwater recovery, where groundwater levels rose after a prolonged period of decline. The interventions that spurred groundwater recovery included policy changes, artificial groundwater recharge, and increased reliance on another water source instead of groundwater. Groundwater recovery can improve water access, restore ecosystems, slow seawater intrusion, and halt land subsidence. However, excessive groundwater recovery can waterlog soils, destabilize buildings, increase liquefaction risks, and intensify flood hazards. \n\nThis Analytical Review describes how groundwater depletion trends have been reversed through interventions. Stakeholders and managers may consider adapting aspects of these interventions to address groundwater depletion elsewhere.", "link_original": "https://www.science.org/doi/10.1126/science.adu1370", "status": 2, "country": [], "sections": [ { "id": 142, "name": "Groundwater" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [] }, { "id": "3f719819-e872-4f0c-9897-38e4126a2829", "slug": "chernobyl-fungus-appears-to-have-evolved-an-incredible-ability-by-michelle-starr-for-sciencealert-post", "created_at": "2025-12-10T10:28:03.268068Z", "views": 32, "name": "Chernobyl Fungus Appears to Have Evolved an Incredible Ability | by Michelle Starr for ScienceAlert", "about": "Chernobyl’s black fungus, Cladosporium sphaerospermum, thrives amid ionizing radiation, hinting at an unknown process that may convert deadly radiation into energy and reveal extreme life adaptation.", "text": "Nearly forty years after the Chernobyl disaster, C. sphaerospermum survives and even flourishes in highly radioactive areas that are lethal to humans. Its dark pigment, melanin, may allow it to absorb ionizing radiation in a process dubbed radiosynthesis, similar to how plants capture light for energy, though no definitive metabolic pathway has been confirmed. Experiments on Earth and the International Space Station suggest the fungus can act as a natural radiation shield and may grow more vigorously under exposure, a trait not shared by all melanized fungi. \n\nThis remarkable adaptation remains unexplained, raising questions about whether it is a form of energy harvesting or a survival response. The fungus exemplifies how life can evolve extreme resilience, offering insights into biodiversity, radiation tolerance, and potential applications for biotechnology and space exploration.", "link_original": "https://www.sciencealert.com/chernobyl-fungus-appears-to-have-evolved-an-incredible-ability", "status": 2, "country": [ { "id": 237, "name": "Ukraine", "icon": "" } ], "sections": [ { "id": 85, "name": "Atomic" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": true, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [ { "id": 237, "name": "Ukraine" } ], "regions": [ { "id": 3, "name": "Europe" } ] }, "filters": [ { "id": 13, "name": "Media content", "badge_name": "Media content", "show_badge": false, "children": [ { "id": 15, "name": "Video", "badge_name": "Video", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "14,15,16" } ] }, { "id": "e2d30231-fac8-4939-b8a9-5a3362399933", "slug": "sciencealert-scientists-design-a-colorful-new-paint-that-could-cut-your-electricity-bill-26-august-2023-post", "created_at": "2023-08-26T08:18:24Z", "views": 109, "name": "ScienceAlert: Scientists Design a Colorful New Paint That Could Cut Your Electricity Bill", "about": "Scientists at Stanford University have developed a heat-reflective paint that, when applied to buildings, could reduce electricity consumption by cooling surfaces and lowering the demand for air conditioning.", "text": "Stanford University researchers have created a revolutionary paint that reflects 80% of mid-infrared light, offering substantial energy savings for heating and cooling buildings. It's capable of reducing energy consumption by almost 21% in warm conditions and 36% in cold conditions, with an estimated 7.4% overall energy savings for mid-rise apartment buildings. The paint, featuring a double-layer design with silver aluminum flakes and colorful inorganic nanoparticles, is both versatile and applicable to diverse surfaces, and its development aligns with the global push for zero-emissions solutions in construction and insulation.", "link_original": "https://www.sciencealert.com/scientists-design-a-colorful-new-paint-that-could-cut-your-electricity-bill", "status": 2, "country": [], "sections": [ { "id": 70, "name": "Housing" } ], "root_section": { "id": 68, "name": "Sustainable Human Habitats" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 4, "name": "North America" } ] }, "filters": [] }, { "id": "8ca6c926-7415-4c21-923c-1e553d8c9376", "slug": "early-earths-hot-mantle-may-have-led-to-archean-water-world-by-american-geophysical-union-for-sciencedaily-post", "created_at": "2025-08-18T08:03:38.393458Z", "views": 26, "name": "Early Earth's hot mantle may have led to Archean 'water world' | by American Geophysical Union for ScienceDaily", "about": "The research suggests early Earth’s hotter mantle held less water, possibly creating a larger ocean during the Archean, influencing climate, atmosphere, and early life development.", "text": "This study reveals that early Earth, during the Archean eon 4 to 3.2 billion years ago, may have had a larger global ocean than previously thought. Scientists from Harvard University developed a model linking mantle temperature and mineral water storage capacity to estimate how much water could have been held deep within Earth. The findings suggest that a hotter mantle stored less water, leaving more at the surface, which could have influenced early climate, atmospheric composition, and habitats for the first life. This challenges earlier assumptions that ocean size remained constant over geologic time. The study also offers insights into planetary water cycles, helping understand water distribution on Earth and other planets, such as Mars. By connecting mantle mineral physics to surface oceans, the research provides a new perspective on Earth’s water history and the conditions that may support life elsewhere.", "link_original": "https://www.sciencedaily.com/releases/2021/03/210330171018.htm", "status": 2, "country": [], "sections": [ { "id": 145, "name": "History of Earth: insights for the future" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [ { "id": 8, "name": "Enlightenment", "badge_name": "Enlightenment", "show_badge": false, "children": [ { "id": 27, "name": "Publications", "badge_name": "Publication", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "9,10,27,11,12" } ] }, { "id": "6d0e72c9-0023-4d3b-a276-67448dd2929d", "slug": "longest-known-continuous-record-of-the-paleozoic-discovered-in-yukon-wilderness-by-stanford-university-for-sciencedaily-post", "created_at": "2025-08-18T08:19:27.500740Z", "views": 29, "name": "Longest known continuous record of the Paleozoic discovered in Yukon wilderness | by Stanford University for ScienceDaily", "about": "New fossil discoveries in Yukon reveal 120M years of early Paleozoic ocean history, showing prolonged low oxygen levels that later surged, fueling the rise of complex life on Earth.", "text": "A major fossil discovery along the Peel River in Yukon, Canada, provides a continuous 120-million-year record of early Paleozoic oceans. Scientists uncovered rock layers and fossils, including trilobites, brachiopods, and graptolites, that reveal low oxygen levels persisted in the deep ocean far longer than previously thought. Oxygen levels surged during the Devonian, supporting the rapid diversification of plants and animals, including predatory fish and early forests. The findings suggest evolving plant life may have increased ocean nutrients, driving oxygenation and reshaping marine ecosystems. While higher oxygen benefited many species, some, like graptolites, lost their low-oxygen habitats. This record offers unprecedented insight into Earth's early oceans, the Cambrian explosion, and the environmental shifts that enabled complex life to thrive.", "link_original": "https://www.sciencedaily.com/releases/2021/07/210708185945.htm", "status": 2, "country": [ { "id": 43, "name": "Canada", "icon": "" } ], "sections": [ { "id": 145, "name": "History of Earth: insights for the future" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [ { "id": 43, "name": "Canada" } ], "regions": [ { "id": 4, "name": "North America" } ] }, "filters": [ { "id": 8, "name": "Enlightenment", "badge_name": "Enlightenment", "show_badge": false, "children": [ { "id": 27, "name": "Publications", "badge_name": "Publication", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "9,10,27,11,12" } ] }, { "id": "5332ef6f-5c35-47e7-b746-1f0bc5ffb5ac", "slug": "geologists-challenge-conventional-view-of-earths-continental-history-stability-with-new-study-by-university-of-illinois-for-sciencedaily-post", "created_at": "2025-12-29T10:48:00Z", "views": 31, "name": "Geologists challenge conventional view of Earth's continental history, stability with new study | by University of Illinois for ScienceDaily", "about": "New research shows that Earth’s ancient cratons, once thought stable, have experienced deep mantle deformation, challenging traditional plate tectonics and reshaping our understanding of continental evolution.", "text": "A study from the University of Illinois challenges long-held beliefs about Earth’s ancient cratons - stable continental cores thought to be unchanged for billions of years. Researchers found that while craton surfaces remain stable, their deep mantle roots, or keels, have undergone repeated deformation and delamination over time. Using density and gravity data, the team discovered that these mantle keels are denser than previously believed, causing vertical movement much like the flow in a lava lamp. These changes help explain crustal erosion, uplift, and features like the Great Unconformity. The findings suggest cratons are more dynamic than once thought, reshaping how scientists understand continental stability, evolution, and plate tectonics.", "link_original": "https://www.sciencedaily.com/releases/2023/06/230612114738.htm", "status": 2, "country": [], "sections": [ { "id": 167, "name": "Lithosphere" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [] }, { "id": "73059108-4219-4027-b637-8dee7640ff31", "slug": "earths-surface-water-dives-deep-transforming-cores-outer-layer-by-arizona-state-university-for-sciencedaily-post", "created_at": "2026-02-25T12:53:15Z", "views": 28, "name": "Earth's surface water dives deep, transforming core's outer layer | by Arizona State University for ScienceDaily", "about": "Arizona State University-led research shows that water from Earth’s surface can reach the core, triggering chemical reactions that form a distinct thin layer and reshape our understanding of deep Earth processes.", "text": "A team of international researchers, including scientists from Arizona State University, has discovered that water from Earth’s surface can reach the core-mantle boundary, triggering chemical reactions that alter the structure of the outermost core. This process forms a distinct, hydrogen-rich and silicon-depleted layer known as the E prime layer. Over billions of years, subducted tectonic plates have carried water deep into the Earth, where it reacts with core materials, forming silica crystals and creating a thin, film-like structure atop the outer core. These findings, published in Nature Geoscience, challenge previous beliefs that material exchange between the core and mantle is minimal. The study reveals a far more dynamic interaction, suggesting a deeper and more complex global water cycle. The discovery significantly advances our understanding of Earth's internal structure and geochemical processes.", "link_original": "https://www.sciencedaily.com/releases/2023/11/231113192124.htm", "status": 2, "country": [], "sections": [ { "id": 141, "name": "Surface water" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [] }, { "id": "f8dcac54-efa8-4cb4-877b-ed2193a0729c", "slug": "landscape-dynamics-determine-the-evolution-of-biodiversity-on-earth-post", "created_at": "2023-12-11T07:00:18.082567Z", "views": 46, "name": "Landscape dynamics determine the evolution of biodiversity on Earth", "about": "A landmark study into the geological timescale distribution of sediment and nutrients over 500 million years made by University of Sidney shows that species biodiversity on Earth is driven by landscape.", "text": "The interplay between Earth’s geological forces and the movement of rivers, mountains, oceans and sediments has emerged as a central driving force behind biodiversity evolution, shaping species diversity over 500 million years. A recent study unveils the influence of landscape dynamics on Earth’s living systems. Dr. Tristan Salles, the lead author of this research, emphasizes the profound impact of Earth’s surface on species diversity, emphasizing that the pace of biodiversity evolution closely aligns with the gradual shifts occurring in plate tectonics. While highlighting the incomparably slow rate of natural biodiversity evolution in contrast to the alarming speed of current extinctions, the study sheds light on the critical role of rivers in fragmenting landscapes and nurturing diverse habitats. By meticulously connecting physical, chemical, and biological systems across geological epochs, this study offers an understanding of the driving forces shaping species diversity.", "link_original": "https://www.sciencedaily.com/releases/2023/11/231129112401.htm", "status": 2, "country": [], "sections": [ { "id": 50, "name": "Safeguarding ecosystems and biodiversity" } ], "root_section": { "id": 108, "name": "Conserving Wild Nature" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [] }, "filters": [] }, { "id": "f3281d72-9f56-4739-ab38-2c851be275de", "slug": "early-stage-subduction-invasion-by-geological-society-of-america-for-sciencedaily-post", "created_at": "2025-08-20T06:48:07.498072Z", "views": 19, "name": "Early-stage subduction invasion | by Geological Society of America for ScienceDaily", "about": "The lithosphere shifts through the Wilson cycle, with oceans opening and closing. New research shows Gibraltar’s subduction may slowly invade the Atlantic, marking early steps in its eventual closure.", "text": "The lithosphere, Earth’s rigid outer shell, is divided into shifting tectonic plates that drive the Wilson cycle, where oceans open, expand, and eventually close. Today the Pacific Ocean is surrounded by subduction zones and active margins, while the Atlantic remains mostly passive. Yet even stable oceans are destined to change. Research shows that in regions like Gibraltar, subduction may already be starting to slowly invade the Atlantic. This process is thought to be one of the key ways new subduction zones form and drive the recycling of oceanic crust, eventually leading to ocean closure and the assembly of future supercontinents. Although the movement is currently extremely slow, models suggest it could accelerate over millions of years, marking the first steps in a new Wilson cycle. Locally, such processes also highlight the possibility of rare but powerful seismic events.", "link_original": "https://www.sciencedaily.com/releases/2024/02/240215113615.htm", "status": 2, "country": [], "sections": [ { "id": 167, "name": "Lithosphere" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [ { "id": 8, "name": "Enlightenment", "badge_name": "Enlightenment", "show_badge": false, "children": [ { "id": 27, "name": "Publications", "badge_name": "Publication", "show_badge": false, "children": [] } ], "all_children": false, "all_children_ids": "9,10,27,11,12" } ] }, { "id": "b5b5b048-ccd3-4999-9792-3f2469379f48", "slug": "new-research-suggests-that-our-universe-has-no-dark-matter-by-university-of-ottawa-for-sciencedaily-post", "created_at": "2025-08-21T09:14:10Z", "views": 29, "name": "New research suggests that our universe has no dark matter | by University of Ottawa for ScienceDaily", "about": "A new University of Ottawa study challenges the standard cosmological model, suggesting the universe may not require dark matter and instead can be explained by alternative theories of light and forces.", "text": "This article disputes the standard cosmological model by suggesting the universe may not require dark matter. Traditionally, dark matter has been invoked to explain how galaxies, planets, and stars behave, despite being invisible and undetectable except through gravitational effects. Physics professor Rajendra Gupta used a combined model of covarying coupling constants (CCC) and tired light (TL) theories, showing that cosmic phenomena such as galaxy distribution and redshifts can be explained without dark matter. According to his research, the accelerated expansion of the universe is not driven by dark energy but by weakening forces of nature as the universe expands. This work builds on Gupta’s earlier findings suggesting the universe is 26.7 billion years old. By eliminating the need for dark matter while remaining consistent with key observations, the study opens new directions for understanding the fundamental structure and evolution of the cosmos.", "link_original": "https://www.sciencedaily.com/releases/2024/03/240315160911.htm", "status": 2, "country": [], "sections": [ { "id": 190, "name": "Evolution of the Universe: the origin of Earth" } ], "root_section": { "id": 107, "name": "Life-friendly Earth" }, "is_photo": false, "is_video": false, "is_large_font": false, "show_in_news_list": false, "url_to_show_in_news_list": "", "location_filters": { "countries": [], "regions": [ { "id": 12, "name": "Global" } ] }, "filters": [] }, { "id": "82064d6a-b269-42b8-8807-ff3bb0f11b96", "slug": "first-warm-blooded-dinosaurs-may-have-emerged-180-million-years-ago-by-university-college-london-for-sciencedaily-post", "created_at": "2025-08-25T07:28:51.634613Z", "views": 23, "name": "First 'warm-blooded' dinosaurs may have emerged 180 million years ago | by University College London for ScienceDaily", "about": "A new study suggests some dinosaurs developed warm-bloodedness in the Early Jurassic, helping them adapt to colder climates, while others like sauropods stayed in warmer regions with different strategies.", "text": "A new study led by researchers from University College London and the University of Vigo suggests that the ability to regulate body temperature, a trait seen in modern mammals and birds, may have first evolved in some dinosaurs during the Early Jurassic, about 180 million years ago. By analyzing more than one thousand fossils, climate models, and evolutionary data, the team found that theropods, which include the ancestors of birds, and ornithischians, a group of plant-eaters such as Triceratops and Stegosaurus, expanded into colder climates, indicating they may have developed warm-bloodedness. In contrast, sauropods such as Brontosaurus and Diplodocus remained in warmer regions, possibly relying on their enormous body size to conserve heat. 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Using hydrothermal experiments with rare earth-rich fluids and common carbonate minerals like calcite and dolomite, the team found that different fluid compositions produce distinct rare earth minerals such as bastnasite, and cerianite. These minerals showed varied chemistries, structures, and transformations over time. The findings challenge existing models of rare earth mineral formation and highlight the need for advanced simulation tools to better predict mineral behavior. 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Led by Alex Shupinski and Kate Lyons, the research tracks functional diversity using fossil records in million-year increments. The study found that after the extinction of non-avian dinosaurs, mammalian functional diversity increased both locally and continentally for the first 10 million years. However, this pattern later diverged due to events like species immigration and environmental shifts. While climate and landscape changes influenced species over time, none had the same disruptive impact as the mass extinction. 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This revised timeline links the formation of these massive deposits to a period of intense geological activity, when ancient supercontinents were breaking apart and reforming. Lead author Dr Liam Courtney-Davies explained that this tectonic activity likely triggered the formation of billions of tonnes of iron-rich rock. 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Researchers from the University of Miami Rosenstiel School, working with the National Oceanic and Atmospheric Administration, analyzed three decades of ocean and atmosphere observations from satellites, moored buoys, and drifting instruments. They found that stronger atmospheric winds have intensified near-surface currents, making them both faster and shallower. In the central equatorial Pacific, westward currents accelerated by about twenty percent, while poleward currents north and south of the equator increased by sixty and twenty percent, respectively. 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The study shows that rain and snowmelt travel much farther and deeper underground than previously understood, taking from ten to one hundred thousand years before resurfacing in streams up to one hundred miles away. More than half of the water in rivers and streams originates from deep aquifers once thought to be disconnected from surface waters. The findings reveal extensive watershed connections, demonstrating that contaminants such as nitrate or per- and polyfluoroalkyl substances can persist and travel long distances. 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