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The Link between Large Igneous Province Eruptions and Mass Extinctions
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1007/s10347-004-0020-yopenalex-snapshot
Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction
inferredcites →https://doi.org/10.1016/j.epsl.2004.06.017openalex-snapshot
Basaltic explosive volcanism, but no comet impact, at the Paleocene–Eocene boundary: high-resolution chemical and isotopic records from Egypt, Spain and Denmark
inferredcites →https://doi.org/10.1016/j.lithos.2004.09.016openalex-snapshot
Volcanism, impact and mass extinctions: incredible or credible coincidences?☆
inferredcites →https://doi.org/10.1016/j.marmicro.2004.04.007openalex-snapshot
Calcareous nannofossils and Mesozoic oceanic anoxic events
inferredcites →https://doi.org/10.1016/s0012-821x(01)00317-xopenalex-snapshot
Erosion of Deccan Traps determined by river geochemistry: impact on the global climate and the 87Sr/86Sr ratio of seawater
inferredcites →https://doi.org/10.1016/s0012-821x(03)00390-xopenalex-snapshot
Biotic effects of impacts and volcanism
inferredcites →https://doi.org/10.1016/s0012-8252(00)00037-4openalex-snapshot
Large igneous provinces and mass extinctions
inferredcites →https://doi.org/10.1016/s0012-8252(99)00055-0openalex-snapshot
Mass extinctions and sea-level changes
inferredcites →https://doi.org/10.1016/s0031-0182(03)00543-1openalex-snapshot
The Cenomanian–Turonian extinction and oceanic anoxic event: evidence from southern Tibet
inferredcites →https://doi.org/10.1016/s0377-8398(03)00021-5openalex-snapshot
Planktonic foraminiferal response to the latest Maastrichtian abrupt warm event: a case study from South Atlantic DSDP Site 525A
inferredcites →https://doi.org/10.1016/s1631-0713(03)00006-3openalex-snapshot
On the ages of flood basalt events
inferredcites →https://doi.org/10.1029/1999pa900040openalex-snapshot
Onset of the Mid‐Cretaceous greenhouse in the Barremian‐Aptian: Igneous events and the biological, sedimentary, and geochemical responses
inferredcites →https://doi.org/10.1038/353225a0openalex-snapshot
Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene
inferredcites →https://doi.org/10.1073/pnas.0404472101openalex-snapshot
Environmental mutagenesis during the end-Permian ecological crisis
inferredcites →https://doi.org/10.1111/j.1502-3931.2002.tb00075.xopenalex-snapshot
How catastrophic was the end-Triassic mass extinction?
inferredcites →https://doi.org/10.1126/science.1089209openalex-snapshot
Chemostratigraphic Evidence of Deccan Volcanism from the Marine Osmium Isotope Record
inferredcites →https://doi.org/10.1126/science.258.5084.975openalex-snapshot
The Age of Paraná Flood Volcanism, Rifting of Gondwanaland, and the Jurassic-Cretaceous Boundary
inferredcites →https://doi.org/10.1126/science.284.5414.616openalex-snapshot
Extensive 200-Million-Year-Old Continental Flood Basalts of the Central Atlantic Magmatic Province
inferredcites →https://doi.org/10.1130/0091-7613(2000)28<747:sbejeo>2.0.co;2openalex-snapshot
Synchrony between Early Jurassic extinction, oceanic anoxic event, and the Karoo-Ferrar flood basalt volcanism
inferredcites →https://doi.org/10.1130/g20008.1openalex-snapshot
Valanginian Weissert oceanic anoxic event
inferredcites →https://doi.org/10.1144/gsjgs.155.4.0619openalex-snapshot
Oceanic plateau formation: a cause of mass extinction and black shale deposition around the Cenomanian–Turonian boundary?
inferredcites →https://doi.org/10.2113/gsecongeo.92.7-8.836openalex-snapshot
Potential links between ocean plateau volcanism and global ocean anoxia at the Cenomanian-Turonian boundary
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.2139/ssrn.4665223openalex-extracted
Multistage Dolomitization Influenced by the Emeishan Large Igneous Province:Petrological and Geochemical Evidence
inferred← citeshttps://doi.org/10.1002/9780470015902.a0001655.pub3openalex-snapshot
Extinction: End‐Triassic Mass Extinction
inferred← citeshttps://doi.org/10.1002/9780470015902.a0029301openalex-snapshot
Extinction: Late Devonian Mass Extinction
inferred← citeshttps://doi.org/10.1002/9781119507444.ch11openalex-snapshot
Sedimentary Mercury Enrichments as a Tracer of Large Igneous Province Volcanism
inferred← citeshttps://doi.org/10.1002/9781119507444.ch8openalex-snapshot
Preliminary Appraisal of a Correlation Between Glaciations and Large Igneous Provinces Over the Past 720 Million Years
inferred← citeshttps://doi.org/10.1002/9781119507444.ch9openalex-snapshot
Phanerozoic Large Igneous Province, Petroleum System, and Source Rock Links
inferred← citeshttps://doi.org/10.1002/ggge.20270openalex-snapshot
Lithological structure of the Galápagos Plume
inferred← citeshttps://doi.org/10.1002/gj.3057openalex-snapshot
Genetic analysis of bentonite—Permian Wangpo shale in Liangshan, Hanzhong, South Shaanxi Province
inferred← citeshttps://doi.org/10.1002/jctb.7702openalex-snapshot
Fabrication of an innovative phosphonate Schiff base adsorbent for molybdenum adsorption and its applications for molybdenum adsorption from spent hydrodesulfurization catalyst
inferred← citeshttps://doi.org/10.1007/978-3-030-41629-4_2openalex-snapshot
An Overview of Paleo-Climate Evidence in Egypt
inferred← citeshttps://doi.org/10.1007/978-3-319-57207-9_3openalex-snapshot
Of Collapses Large and Small
inferred← citeshttps://doi.org/10.1007/978-3-642-38800-2_9openalex-snapshot
Large Igneous Provinces: Deccan Traps and Columbia River Basalts
inferred← citeshttps://doi.org/10.1007/s00531-014-1078-6openalex-snapshot
The age of Earth’s largest volcano: Tamu Massif on Shatsky Rise (northwest Pacific Ocean)
inferred← citeshttps://doi.org/10.1007/s11430-014-4843-2openalex-snapshot
Paleo-redox conditions across the Permian-Triassic boundary in shallow carbonate platform of the Nanpanjiang Basin, South China
inferred← citeshttps://doi.org/10.1007/s11430-025-1695-7openalex-snapshot
Carbon isotope excursions in the Ediacaran carbonate strata: Insights from deep-shallow carbon cycle coupling
inferred← citeshttps://doi.org/10.1007/s12040-006-0007-xopenalex-snapshot
The emplacement of pahoehoe lavas on Kilauea and in the Deccan Traps
inferred← citeshttps://doi.org/10.1007/s12210-014-0317-xopenalex-snapshot
Anthropocene: another academic invention?
inferred← citeshttps://doi.org/10.1007/s12517-021-09180-yopenalex-snapshot
Oceanic anoxic events in the Earth’s geological history and signature of such event in the Paleocene-Eocene Himalayan foreland basin sediment records of NW Himalaya, India
inferred← citeshttps://doi.org/10.1007/s41247-016-0002-zopenalex-snapshot
What Future for the Anthropocene? A Biophysical Interpretation
inferred← citeshttps://doi.org/10.1016/b978-0-12-374739-6.00084-1openalex-snapshot
5.9 Hot Spots and Large Igneous Provinces
inferred← citeshttps://doi.org/10.1016/b978-0-12-409548-9.09087-4openalex-snapshot
Large Igneous Provinces
inferred← citeshttps://doi.org/10.1016/b978-0-12-409548-9.12528-xopenalex-snapshot
Large Igneous Provinces
inferred← citeshttps://doi.org/10.1016/b978-0-12-818234-5.00168-1openalex-snapshot
Hot Spots and Large Igneous Provinces
inferred← citeshttps://doi.org/10.1016/b978-0-12-824360-2.00012-7openalex-snapshot
Influence of Large Igneous Provinces
inferred← citeshttps://doi.org/10.1016/b978-0-443-26562-4.00006-6openalex-snapshot
Abundant metal systems
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2026.123712openalex-snapshot
Release and recapture: Limited carbon mobilization in sediment adjacent to Central Atlantic Magmatic Province sills, Florida, USA
inferred← citeshttps://doi.org/10.1016/j.earscirev.2007.08.008openalex-snapshot
Revised definition of Large Igneous Provinces (LIPs)
inferred← citeshttps://doi.org/10.1016/j.earscirev.2010.07.001openalex-snapshot
The largest volcanic eruptions on Earth
inferred← citeshttps://doi.org/10.1016/j.earscirev.2012.03.009openalex-snapshot
Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary
inferred← citeshttps://doi.org/10.1016/j.earscirev.2017.11.009openalex-snapshot
Evaluating the relationship between climate change and volcanism
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103266openalex-snapshot
The role of temperature in the initiation of the end-Triassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103716openalex-snapshot
Geochronology of the Paraná-Etendeka large igneous province
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103736openalex-snapshot
The geotectonic setting, age and mineral deposit inventory of global layered intrusions
inferred← citeshttps://doi.org/10.1016/j.earscirev.2023.104314openalex-snapshot
An appraisal of the ages of Phanerozoic large igneous provinces
inferred← citeshttps://doi.org/10.1016/j.earscirev.2023.104667openalex-snapshot
The role of LIPs in Phanerozoic mass extinctions: An Hg perspective
inferred← citeshttps://doi.org/10.1016/j.earscirev.2025.105072openalex-snapshot
Impact of Permian Tarim and Emeishan Large Igneous Provinces on Petroleum Systems and Gas Emissions in Tarim and Sichuan Basins
inferred← citeshttps://doi.org/10.1016/j.earscirev.2026.105489openalex-snapshot
Mantle plume dynamics and Gondwana breakup: Insights from the Comei large igneous province, Tethyan Himalaya
inferred← citeshttps://doi.org/10.1016/j.epsl.2006.03.036openalex-snapshot
Carbon solubility in mantle minerals
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.04.013openalex-snapshot
The significance of an Early Jurassic (Toarcian) carbon-isotope excursion in Haida Gwaii (Queen Charlotte Islands), British Columbia, Canada
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.01.057openalex-snapshot
F, Cl, and S concentrations in olivine-hosted melt inclusions from mafic dikes in NW Namibia and implications for the environmental impact of the Paraná–Etendeka Large Igneous Province
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.06.040openalex-snapshot
Estimating the impact of the cryptic degassing of Large Igneous Provinces: A mid-Miocene case-study
inferred← citeshttps://doi.org/10.1016/j.epsl.2015.01.009openalex-snapshot
Long duration (>4 Ma) and steady-state volcanic activity in the early Cretaceous Paraná–Etendeka Large Igneous Province: New palaeomagnetic data from Namibia
inferred← citeshttps://doi.org/10.1016/j.epsl.2015.06.064openalex-snapshot
Globally enhanced mercury deposition during the end-Pliensbachian extinction and Toarcian OAE: A link to the Karoo–Ferrar Large Igneous Province
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.08.014openalex-snapshot
Atmospheric constituents and surface-level UVB: Implications for a paleoaltimetry proxy and attempts to reconstruct UV exposure during volcanic episodes
inferred← citeshttps://doi.org/10.1016/j.gca.2006.06.236openalex-snapshot
CO2-recycling to the deep convecting mantle
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2011.05.009openalex-snapshot
Ammonite paleobiogeography during the Pliensbachian–Toarcian crisis (Early Jurassic) reflecting paleoclimate, eustasy, and extinctions
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2012.06.008openalex-snapshot
Paleoecological and paleoenvironmental changes during the continental Middle–Late Permian transition at the SE Iberian Ranges, Spain
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103155openalex-snapshot
Large environmental disturbances caused by magmatic activity during the Late Devonian Hangenberg Crisis
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103291openalex-snapshot
Mercury anomalies and carbon isotope excursions in the western Tethyan Csővár section support the link between CAMP volcanism and the end-Triassic extinction
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103350openalex-snapshot
Persistent oxic deep ocean conditions and frequent volcanic activities during the Frasnian-Famennian transition recorded in South China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103794openalex-snapshot
Mercury enrichments of the Pyrenean foreland basins sediments support enhanced volcanism during the Paleocene-Eocene thermal maximum (PETM)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105207openalex-snapshot
Quantifying volcanism during Oceanic Anoxic Event 2 constrained by sedimentary mercury
inferred← citeshttps://doi.org/10.1016/j.gsf.2013.07.003openalex-snapshot
The Emeishan large igneous province: A synthesis
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2019.103645openalex-snapshot
Biostratigraphy and geochemistry of the Cretaceous-Paleogene (K/Pg) and early danian event (Dan-C2), a possible link to deccan volcanism: New insights from Red Sea, Egypt
inferred← citeshttps://doi.org/10.1016/j.jsames.2023.104574openalex-snapshot
Neoarchean environments associated with the emplacement of a large igneous province: Insights from the Carajás Basin, Amazonia Craton
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2008.01.048openalex-snapshot
Morphology of rubbly pahoehoe (simple) flows from the Deccan Volcanic Province: Implications for style of emplacement
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2012.04.002openalex-snapshot
Influence of volcanic gases on the epidermis of Pinus halepensis Mill. in Campi Flegrei, Southern Italy: A possible tool for detecting volcanism in present and past floras
inferred← citeshttps://doi.org/10.1016/j.lithos.2018.09.026openalex-snapshot
U-Pb Geochronology and Geochemistry of the Povungnituk Group of the Cape Smith Belt: Part of a Craton-Scale Circa 2.0 Ga Minto-Povungnituk Large Igneous Province, Northern Superior Craton
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2021.105037openalex-snapshot
Early Oligocene environment of the Central Paratethys revealed by biomarkers and pyrite framboids from the Tarcău and Vrancea Nappes (Eastern Outer Carpathians, Romania)
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.106780openalex-snapshot
Multistage dolomitization influenced by the Emeishan large igneous province: Petrographical and geochemical evidence
inferred← citeshttps://doi.org/10.1016/j.oregeorev.2012.04.007openalex-snapshot
A review of Australia's Large Igneous Provinces and associated mineral systems: Implications for mantle dynamics through geological time
inferred← citeshttps://doi.org/10.1016/j.oregeorev.2017.04.025openalex-snapshot
Transvaporite model of ore genesis and an exploration strategy for new giant ore deposits
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.08.005openalex-snapshot
Palaeoenvironmental change during the end-Guadalupian (Permian) mass extinction in Sichuan, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.05.020openalex-snapshot
Deciphering the upper Famennian Hangenberg Black Shale depositional environments based on multi-proxy record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.05.010openalex-snapshot
The Pliensbachian–Toarcian (Early Jurassic) extinction, a global multi-phased event
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.06.042openalex-snapshot
The effects of large igneous provinces on the global carbon and sulphur cycles
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.07.036openalex-snapshot
Clay mineralogical characteristics at the Permian–Triassic Shangsi section and their paleoenvironmental and/or paleoclimatic significance
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.11.005openalex-snapshot
On the causes of mass extinctions
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.03.014openalex-snapshot
How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.05.027openalex-snapshot
High-resolution clay mineral and major elemental characterization of a Permian-Triassic terrestrial succession in southwestern China: Diagenetic and paleoclimatic/paleoenvironmental significance
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111977openalex-snapshot
Mercury sequestration pathways under varying depositional conditions during Early Jurassic (Pliensbachian and Toarcian) Karoo-Ferrar volcanism
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113832openalex-snapshot
Volcanic cataclysm and the Late Devonian mass extinctions: wishful speculation or a reliable hypothesis?
inferred← citeshttps://doi.org/10.1016/j.pepi.2024.107185openalex-snapshot
Magmatic underplating, plumbing system, and carbon-enhanced electrical conductivity in the Paraná Magmatic Province
inferred← citeshttps://doi.org/10.1016/j.rgg.2016.12.001openalex-snapshot
The evolution of planets. Venus as the Earth’s probable future
inferred← citeshttps://doi.org/10.1017/cbo9780511974540.002openalex-snapshot
Integrating ecology and systematics in climate change research
inferred← citeshttps://doi.org/10.1017/cbo9780511974540.005openalex-snapshot
Global climate and extinction: evidence from the fossil record
inferred← citeshttps://doi.org/10.1017/cbo9781107415683.006openalex-snapshot
High-precision U–Pb geochronology of Phanerozoic large igneous provinces
inferred← citeshttps://doi.org/10.1017/s0016756815000199openalex-snapshot
Middle Phanerozoic mass extinctions and a tribute to the work of Professor Tony Hallam
inferred← citeshttps://doi.org/10.1017/s0016756818000481openalex-snapshot
Mercury evidence from the Sino-Korean block for Emeishan volcanism during the Capitanian mass extinction
inferred← citeshttps://doi.org/10.1017/s175569101300011xopenalex-snapshot
The links between large igneous provinces, continental break-up and environmental change: evidence reviewed from Antarctica
inferred← citeshttps://doi.org/10.1029/2008gc001994openalex-snapshot
The 40Ar/39Ar ages of the sill complex of the Karoo large igneous province: Implications for the Pliensbachian‐Toarcian climate change
inferred← citeshttps://doi.org/10.1029/2010gl045464openalex-snapshot
Aerosol size confines climate response to volcanic super‐eruptions
inferred← citeshttps://doi.org/10.1029/2011gl049032openalex-snapshot
No link between the Panjal Traps (Kashmir) and the Late Permian mass extinctions
inferred← citeshttps://doi.org/10.1029/2021gc010172openalex-snapshot
Eruption Rates, Tempo, and Stratigraphy of Paleocene Flood Basalts on Baffin Island, Canada
inferred← citeshttps://doi.org/10.1029/2021pa004392openalex-snapshot
Effects of the Pliensbachian–Toarcian Boundary Event on Carbonate Productivity of a Tethyan Platform and Slope
inferred← citeshttps://doi.org/10.1029/2024gc011464openalex-snapshot
Marine Strontium Isotope Evolution at the Triassic‐Jurassic Transition Links Transient Changes in Continental Weathering to Volcanism of the Central Atlantic Magmatic Province
inferred← citeshttps://doi.org/10.1029/2024gc012122openalex-snapshot
Mercury Deposition in South China Across the Ordovician‐Silurian Transition: Implications for Climate Change
inferred← citeshttps://doi.org/10.1038/nature09100openalex-snapshot
Massive volcanic SO2 oxidation and sulphate aerosol deposition in Cenozoic North America
inferred← citeshttps://doi.org/10.1038/s41467-019-12957-1openalex-snapshot
Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change
inferred← citeshttps://doi.org/10.1038/s41467-022-34645-3openalex-snapshot
High temperature methane emissions from Large Igneous Provinces as contributors to late Permian mass extinctions
inferred← citeshttps://doi.org/10.1038/s41561-023-01259-3openalex-snapshot
Climate extremes likely to drive land mammal extinction during next supercontinent assembly
inferred← citeshttps://doi.org/10.1038/s41598-019-53672-7openalex-snapshot
Probable basal allosauroid from the early Middle Jurassic Cañadón Asfalto Formation of Argentina highlights phylogenetic uncertainty in tetanuran theropod dinosaurs
inferred← citeshttps://doi.org/10.1073/pnas.2120441119openalex-snapshot
Continental flood basalts drive Phanerozoic extinctions
inferred← citeshttps://doi.org/10.1073/pnas.2202039119openalex-snapshot
Volume and rate of volcanic CO 2 emissions governed the severity of past environmental crises
inferred← citeshttps://doi.org/10.1080/00206814.2024.2355230openalex-snapshot
Early Jurassic (Toarcian) climate warming and correlation of continental coal-bearing basins of Siberia: problems and potential solution
inferred← citeshttps://doi.org/10.1080/08120099.2026.2700318openalex-snapshot
Magmatic evolution characteristics and heterogeneity of the outer zone of the Emeishan Large Igneous Province: a case study of basalts from the Tianquan and Huayingshan areas
inferred← citeshttps://doi.org/10.1080/08912963.2023.2190757openalex-snapshot
Early–Middle Jurassic brachiopods from Ponor Mountain, Western Balkan Mountains, Bulgaria; taxonomy, biostratigraphy and occurrence in the context of the early Toarcian Oceanic Anoxic Event
inferred← citeshttps://doi.org/10.1080/11035897.2013.799223openalex-snapshot
Palynostratigraphy of dinosaur footprint-bearing deposits from the Triassic–Jurassic boundary interval of Sweden
inferred← citeshttps://doi.org/10.1098/rspb.2007.1302openalex-snapshot
A long-term association between global temperature and biodiversity, origination and extinction in the fossil record
inferred← citeshttps://doi.org/10.1111/j.1365-246x.2008.03808.xopenalex-snapshot
The Agulhas Plateau: structure and evolution of a Large Igneous Province
inferred← citeshttps://doi.org/10.1111/j.1472-4669.2007.00130.xopenalex-snapshot
The End‐Permian mass extinction – how bad did it get?
inferred← citeshttps://doi.org/10.1111/sed.12641openalex-snapshot
Mineralogical evidence for multiple dust sources in an early Triassic loessite
inferred← citeshttps://doi.org/10.1126/sciadv.aee2277openalex-snapshot
Metamorphic sulfur release as a driver of sustained cooling and mass extinction
inferred← citeshttps://doi.org/10.1130/2014.2505(16)openalex-snapshot
Emplacement characteristics, time scales, and volcanic gas release rates of continental flood basalt eruptions on Earth
inferred← citeshttps://doi.org/10.1130/2015.2511(15)openalex-snapshot
Environmental consequences of Ontong Java Plateau and Kerguelen Plateau volcanism
inferred← citeshttps://doi.org/10.1130/2020.2544(01)openalex-snapshot
Volcanism as a prime cause of mass extinctions: Retrospectives and perspectives
inferred← citeshttps://doi.org/10.1130/2020.2544(02)openalex-snapshot
The Central Iapetus magmatic province: An updated review and link with the ca. 580 Ma Gaskiers glaciation
inferred← citeshttps://doi.org/10.1130/b30820.1openalex-snapshot
Large igneous provinces and silicic large igneous provinces: Progress in our understanding over the last 25 years
inferred← citeshttps://doi.org/10.1130/g30826c.1openalex-snapshot
Climate changes caused by degassing of sediments during the emplacement of large igneous provinces: COMMENT
inferred← citeshttps://doi.org/10.1130/g35434.1openalex-snapshot
High-precision dating of the Kalkarindji large igneous province, Australia, and synchrony with the Early–Middle Cambrian (Stage 4–5) extinction
inferred← citeshttps://doi.org/10.1144/sp514-2021-11openalex-snapshot
Impact of a northern-hemispherical cryosphere on late Pliensbachian–early Toarcian climate and environment evolution
inferred← citeshttps://doi.org/10.11606/d.44.2022.tde-28072022-080044openalex-snapshot
Magnetoestratigrafia do Geossítio K-Pg na Mina de Poty, Pernambuco, Brasil
inferred← citeshttps://doi.org/10.1180/0009855064110199openalex-snapshot
Clay mineralogy of the Permo-Triassic strata of the British Isles: onshore and offshore
inferred← citeshttps://doi.org/10.12677/ojns.2018.61015openalex-snapshot
Coupling of Permian-Triassic Volcanic Activity in Dashanbao with P-T Boundary Mass Biotic Extinction
inferred← citeshttps://doi.org/10.12789/geocanj.2014.41.060openalex-snapshot
Igneous Rock Associations 16. The Late Permian Emeishan Large Igneous Province
inferred← citeshttps://doi.org/10.18654/1000-0569/2020.07.03openalex-snapshot
Genesis of Silicic Large Igneous Provinces and effects of resources and environment
inferred← citeshttps://doi.org/10.22215/etd/2019-13791openalex-snapshot
2.0 to 1.9 Ga large igneous province magmatism in northern Quebec — U-Pb geochronology and geochemistry
inferred← citeshttps://doi.org/10.3389/feart.2024.1368342openalex-snapshot
The carbon release triggered by 1.32 Ga sill emplacement and its potential environmental implications
inferred← citeshttps://doi.org/10.3799/dqkx.2022.370openalex-snapshot
川西南乌斯河古油藏Re-Os年龄及其对峨眉山大火成岩省火山活动的响应
inferred← citeshttps://doi.org/10.4202/app.2011.0058openalex-snapshot
The Alvarez Impact Theory of Mass Extinction; Limits to its Applicability and the “Great Expectations Syndrome”
inferred← citeshttps://doi.org/10.51583/ijltemas.2025.140300050openalex-snapshot
Modeling and Development of Local Raw Materials for Automotive Brake Pad
inferred← citeshttps://doi.org/10.51583/ijltemas.2025.140300052openalex-snapshot
Reinventing the Science of Petroleum Source Rocks: A Contrarian Perspective
inferred← citeshttps://doi.org/10.5281/zenodo.36082openalex-snapshot
Large The Optimum Approximation In Generalized Time-Frequency Domains And Application To Numerical Simulation Of Partial Differential Equations
inferred← citeshttps://doi.org/10.5670/oceanog.2006.13openalex-snapshot
Large Igneous Provinces and Scientific Ocean Drilling: Status Quo and A Look Ahead
inferred← citeshttps://doi.org/10.5670/oceanog.2019.142openalex-snapshot
Contributions of Scientific Ocean Drilling to Understanding the Emplacement of Submarine Large Igneous Provinces and Their Effects on the Environment
inferred← citeshttps://doi.org/10.5710/amgh.24.01.2023.3533openalex-snapshot
Evidences of Teratology and Mutagenensis in Palynological Assemblages from the Middle Triassic Puesto Viejo Group, San Rafael Depocenter, Argentina. Implications of Volcanism and Regional Environmental Stress
inferred← citeshttps://doi.org/10.70675/276bb39az80d3z4ce0za62ez67b1a12309adopenalex-snapshot
The cuticle micromorphology of extant and fossil plants as indicator of environmental conditions : A pioneer study on the influence of volcanic gases on the cuticle structure in extant plants
inferred← citeshttps://doi.org/10.70675/47cda853z12fcz4983z9508z93920c56800dopenalex-snapshot
Element and isotope geochemistry from iron formations and carbonates : new insights into the Fe cycle and paleoenvironmental reconstructions during the Neoarchean in Carajás, Brazil
inferred← citeshttps://doi.org/10.7282/t3qv3mpsopenalex-snapshot
Interaction of the Galapagos plume with the southern Central American volcanic front
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