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Mass Extinctions and Their Aftermath

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inferred← citeshttps://doi.org/10.5281/zenodo.13175594openalex-extracted
The Late Devonian Upper Kellwasser Event and entomozoacean ostracods in the Holy Cross Mountains, Poland
inferred← citeshttps://doi.org/10.5281/zenodo.13304842openalex-extracted
The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records
inferred← citeshttps://doi.org/10.5281/zenodo.13509015openalex-extracted
Diversity dynamics of Early-Middle Jurassic brachiopods of Caucasus, and the Pliensbachian-Toarcian mass extinction
inferred← citeshttps://doi.org/10.1002/9780470015902.a0001643.pub3openalex-snapshot
Post‐Permian Radiation
inferred← citeshttps://doi.org/10.1002/9780470015902.a0001655.pub3openalex-snapshot
Extinction: End‐Triassic Mass Extinction
inferred← citeshttps://doi.org/10.1002/gj.1041openalex-snapshot
Diversity patterns of Carboniferous and Permian rugose corals in South China
inferred← citeshttps://doi.org/10.1002/gj.2552openalex-snapshot
Spectral gamma‐ray logs and palaeoclimate change? Permian–Triassic, Persian Gulf
inferred← citeshttps://doi.org/10.1002/gj.879openalex-snapshot
What are Lazarus taxa?
inferred← citeshttps://doi.org/10.1002/gj.883openalex-snapshot
Incompleteness of the Permian–Triassic fossil record: a consequence of productivity decline?
inferred← citeshttps://doi.org/10.1002/gj.897openalex-snapshot
Palaeozoic brachiopod extinctions, survival and recovery: patterns within the rhynchonelliformeans
inferred← citeshttps://doi.org/10.1002/jez.b.20006openalex-snapshot
Is telomere erosion a mechanism of species extinction?
inferred← citeshttps://doi.org/10.1002/mmng.200410003openalex-snapshot
Considerations on aBrachauchenius skeleton (Pliosauroidea) from the lower Paja Formation (late Barremian) of Villa de Leyva area (Colombia)
inferred← citeshttps://doi.org/10.1002/mmng.201000016openalex-snapshot
Temporal patterns in disparity and diversity of the Jurassic ammonoids of southern Germany
inferred← citeshttps://doi.org/10.1006/cres.2002.1019openalex-snapshot
Extinction and renewal patterns among Tethyan belemnites in the Verrucosum Subzone (Valanginian) of southeast France
inferred← citeshttps://doi.org/10.1007/3-540-25736-5_11openalex-snapshot
Continental Vertebrate Extinctions at the Triassic-Jurassic and Cretaceous-Tertiary Boundaries: a Comparison
inferred← citeshttps://doi.org/10.1007/7171_2007_116openalex-snapshot
Why Does Gunnera Do It and Other Angiosperms Don't? An Evolutionary Perspective on the Gunnera–Nostoc Symbiosis
inferred← citeshttps://doi.org/10.1007/978-1-4020-5750-2_14openalex-snapshot
Plume Winter Scenario for Biosphere Catastrophe: The Permo-Triassic Boundary Case
inferred← citeshttps://doi.org/10.1007/978-1-4020-6806-5_17openalex-snapshot
Biogeography of Kutch Ammonites During the Latest Jurassic (Tithonian) and a Global Paleobiogeograph Overview
inferred← citeshttps://doi.org/10.1007/978-1-4020-8837-7_20openalex-snapshot
Do Impacts Really Cause Most Mass Extinctions?
inferred← citeshttps://doi.org/10.1007/978-1-4419-1684-6_2openalex-snapshot
The Earth in Time
inferred← citeshttps://doi.org/10.1007/978-1-4615-0439-9_1openalex-snapshot
Evolution and Transition
inferred← citeshttps://doi.org/10.1007/978-1-4757-3486-7_1openalex-snapshot
A Photobiological History of Earth
inferred← citeshttps://doi.org/10.1007/978-1-4757-5202-1_9openalex-snapshot
Introduced Predators and Avifaunal Extinction in New Zealand
inferred← citeshttps://doi.org/10.1007/978-3-030-15989-4_9openalex-snapshot
Phanerozoic Mass Extinctions and Indian Stratigraphic Records
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/10.1007/978-3-030-53222-2_4openalex-snapshot
Brazilian Deep-Sea Corals
inferred← citeshttps://doi.org/10.1007/978-3-319-15045-1_12openalex-snapshot
Facing the Big Sixth: From Prioritizing Species to Conserving Biodiversity
inferred← citeshttps://doi.org/10.1007/978-3-319-19542-1_2openalex-snapshot
The Delaware Bay Area, U.S.A.: A Unique Habitat of the American Horseshoe Crab, Limulus polyphemus
inferred← citeshttps://doi.org/10.1007/978-3-319-22512-8_2openalex-snapshot
Phanerozoic Life and Mass Extinctions of Species
inferred← citeshttps://doi.org/10.1007/978-3-319-51412-3_13openalex-snapshot
Cretaceous Environments and Deep-Ocean Drilling
inferred← citeshttps://doi.org/10.1007/978-3-319-68009-5_15openalex-snapshot
The Missing Mass Extinction at the Triassic-Jurassic Boundary
inferred← citeshttps://doi.org/10.1007/978-3-319-68009-5_5openalex-snapshot
Distal Processes and Effects of Multiple Late Triassic Terrestrial Bolide Impacts: Insights from the Norian Manicouagan Event, Northeastern Quebec, Canada
inferred← citeshttps://doi.org/10.1007/978-3-540-33761-4_16openalex-snapshot
16 Patterns of Diversification and Extinction
inferred← citeshttps://doi.org/10.1007/978-3-540-75916-4_1openalex-snapshot
Mass Extinction - a general view
inferred← citeshttps://doi.org/10.1007/978-3-540-75916-4_8openalex-snapshot
Reexamination of the end-Triassic mass
inferred← citeshttps://doi.org/10.1007/978-3-642-10311-7_1openalex-snapshot
New Perspectives on the Evolution of Late Palaeozoic and Mesozoic Terrestrial Tetrapods
inferred← citeshttps://doi.org/10.1007/978-3-642-30425-5_3openalex-snapshot
Effects of Random and Selective Mass Extinction on Community Composition in Communities of Digital Organisms
inferred← citeshttps://doi.org/10.1007/978-3-642-56739-1_2openalex-snapshot
Der Beitrag der Paläontologie zur Biodiversitätsdebatte
inferred← citeshttps://doi.org/10.1007/978-3-642-59388-8_5openalex-snapshot
A Geographic Database Approach to the KT Boundary
inferred← citeshttps://doi.org/10.1007/978-3-662-06278-4_18openalex-snapshot
Calcareous nannoplankton evolution and diversity through time
inferred← citeshttps://doi.org/10.1007/978-3-7643-8344-2_4openalex-snapshot
The plankton turnover at the Permo-Triassic boundary, emphasis on radiolarians
inferred← citeshttps://doi.org/10.1007/978-81-322-3658-0_1openalex-snapshot
Life Through Ages: An Overview
inferred← citeshttps://doi.org/10.1007/978-90-481-2639-2_37openalex-snapshot
Mass Extinctions, Anoxic Events and Ocean Acidification
inferred← citeshttps://doi.org/10.1007/978-90-481-3428-1_24openalex-snapshot
Millennial Physical Events and the End-Permian Mass Mortality in the Western Palaeotethys: Timing and Primary Causes
inferred← citeshttps://doi.org/10.1007/978-90-481-3428-1_26openalex-snapshot
Survival, but…! New Tales of ‘Dead Clade Walking’ from Austral and Boreal Post-K–T Assemblages
inferred← citeshttps://doi.org/10.1007/978-90-481-8643-3_1openalex-snapshot
Taphonomy: Bias and Process Through Time
inferred← citeshttps://doi.org/10.1007/978-94-007-7332-5_4openalex-snapshot
Mass Extinction of Species
inferred← citeshttps://doi.org/10.1007/978-94-017-9633-0_18openalex-snapshot
Ammonoids at the Triassic-Jurassic Transition: Pulling Back from the Edge of Extinction
inferred← citeshttps://doi.org/10.1007/978-94-017-9633-0_2openalex-snapshot
Evolutionary Trends of Triassic Ammonoids
inferred← citeshttps://doi.org/10.1007/978-94-017-9633-0_3openalex-snapshot
Evolutionary Trends within Jurassic Ammonoids
inferred← citeshttps://doi.org/10.1007/978-981-13-3639-3_18openalex-snapshot
End-Paleozoic Mass Extinction: Hierarchy of Causes and a New Cosmoclimatological Perspective for the Largest Crisis
inferred← citeshttps://doi.org/10.1007/bf02875391openalex-snapshot
Periodic anoxic shelf in the Early-Middle Ordovician transition: ichnosedimentologic evidence from west-central Utah, USA
inferred← citeshttps://doi.org/10.1007/bf02988112openalex-snapshot
Some remarks on the structure and function of refugia in ecology and palaeoecology
inferred← citeshttps://doi.org/10.1007/s00015-007-1209-1openalex-snapshot
European ammonoid diversity questions the spreading of anoxia as primary cause for the Cenomanian/Turonian (Late Cretaceous) mass extinction
inferred← citeshttps://doi.org/10.1007/s00015-010-0019-zopenalex-snapshot
Bentho-planktonic evidence from the Austrian Alps for a decline in sea-surface carbonate production at the end of the Triassic
inferred← citeshttps://doi.org/10.1007/s00114-004-0515-yopenalex-snapshot
The modern theory of biological evolution: an expanded synthesis
inferred← citeshttps://doi.org/10.1007/s00114-014-1242-7openalex-snapshot
Ichthyosaurs from the French Rhaetian indicate a severe turnover across the Triassic–Jurassic boundary
inferred← citeshttps://doi.org/10.1007/s00227-007-0896-5openalex-snapshot
Cloning and expression of a tauropine dehydrogenase from the marine sponge Suberites domuncula
inferred← citeshttps://doi.org/10.1007/s00338-008-0381-8openalex-snapshot
Mass extinctions and ocean acidification: biological constraints on geological dilemmas
inferred← citeshttps://doi.org/10.1007/s00531-007-0177-zopenalex-snapshot
Comparison of taxonomic diversity, strontium isotope and sea-level patterns
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/s00531-016-1308-1openalex-snapshot
Ichnological record of the Frasnian–Famennian boundary interval: two examples from the Holy Cross Mts (Central Poland)
inferred← citeshttps://doi.org/10.1007/s005310050235openalex-snapshot
The FrasnianFamennian biotic crisis: How many (if any) bolide impacts?
inferred← citeshttps://doi.org/10.1007/s10347-004-0004-yopenalex-snapshot
Microfacies and depositional environment of an Upper Triassic intra-platform carbonate basin: the Fatric Unit of the West Carpathians (Slovakia)
inferred← citeshttps://doi.org/10.1007/s10347-004-0020-yopenalex-snapshot
Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction
inferred← citeshttps://doi.org/10.1007/s10347-005-0045-xopenalex-snapshot
Sponge communities from the Lower Liassic of Adnet (Northern Calcareous Alps, Austria)
inferred← citeshttps://doi.org/10.1007/s10347-005-0048-7openalex-snapshot
Triassic/Jurassic carbonates from the Hochfelln Mountain (Northern Calcareous Alps)—its facies, silicified fauna and implications for the end-Triassic biotic crisis
inferred← citeshttps://doi.org/10.1007/s10347-008-0164-2openalex-snapshot
Late Triassic sedimentary evolution of Slovenian Basin (eastern Southern Alps): description and correlation of the Slatnik Formation
inferred← citeshttps://doi.org/10.1007/s10347-011-0265-1openalex-snapshot
Timing and progression of the end-Guadalupian crisis in the Fars province (Dalan Formation, Kuh-e Gakhum, Iran) constrained by foraminifers and other carbonate microfossils
inferred← citeshttps://doi.org/10.1007/s10347-011-0279-8openalex-snapshot
A delayed carbonate factory breakdown during the Tethyan-wide Carnian Pluvial Episode along the Cimmerian terranes (Taurus, Turkey)
inferred← citeshttps://doi.org/10.1007/s10347-017-0500-5openalex-snapshot
Facies stacking and extinctions across the Triassic–Jurassic boundary in a peritidal succession from western Sicily
inferred← citeshttps://doi.org/10.1007/s10347-018-0538-zopenalex-snapshot
Microproblematica, calcareous algae, and microbialites at the Frasnian-Famennian boundary interval in the Šumbera section (Moravian Karst, Czech Republic) and their significance in the context of the Kellwasser Crisis
inferred← citeshttps://doi.org/10.1007/s10531-007-9261-8openalex-snapshot
Conservation of protists: is it needed at all?
inferred← citeshttps://doi.org/10.1007/s10531-015-0940-6openalex-snapshot
Vertebrate biodiversity losses point to a sixth mass extinction
inferred← citeshttps://doi.org/10.1007/s10933-021-00208-7openalex-snapshot
Late Cretaceous paleoclimate and paleoenvironment in the Songliao Basin, China
inferred← citeshttps://doi.org/10.1007/s11120-010-9593-1openalex-snapshot
The evolutionary consequences of oxygenic photosynthesis: a body size perspective
inferred← citeshttps://doi.org/10.1007/s11229-021-03254-wopenalex-snapshot
Explaining the apocalypse: the end-Permian mass extinction and the dynamics of explanation in geohistory
inferred← citeshttps://doi.org/10.1007/s11430-006-0449-7openalex-snapshot
Pioneer organisms after F-F mass extinction in Dushan region, Guizhou Province, and their significance in establishing new ecosystem
inferred← citeshttps://doi.org/10.1007/s11430-008-0128-yopenalex-snapshot
Anachronistic facies in the Lower Triassic of South China and their implications to the ecosystems during the recovery time
inferred← citeshttps://doi.org/10.1007/s11430-009-0077-0openalex-snapshot
Ecological evolution across the Permian/Triassic boundary at the Kangjiaping Section in Cili County, Hunan Province, China
inferred← citeshttps://doi.org/10.1007/s11430-009-0162-4openalex-snapshot
Dispersal events of Triassic-Jurassic boundary faunas, and paleoenvironment of Tibetan Himalaya
inferred← citeshttps://doi.org/10.1007/s11430-010-4092-yopenalex-snapshot
A comparison of the biological, geological events and environmental backgrounds between the Neoproterozoic-Cambrian and Permian-Triassic transitions
inferred← citeshttps://doi.org/10.1007/s11430-013-4749-4openalex-snapshot
Community replacement sequences and paleoenvironmental changes in reef areas of South China from Late Permian to Early Triassic exemplified by Panlongdong section in northeastern Sichuan Basin
inferred← citeshttps://doi.org/10.1007/s11434-008-0543-7openalex-snapshot
The Siberian Traps and the End-Permian mass extinction: a critical review
inferred← citeshttps://doi.org/10.1007/s11692-007-9005-4openalex-snapshot
Paleontological Patterns, Macroecological Dynamics and the Evolutionary Process
inferred← citeshttps://doi.org/10.1007/s11707-007-0057-7openalex-snapshot
Hypersaline and anoxia in the Devonian Frasnian-Famennian transition: Molecular fossil and mineralogical evidence from Guangxi, South China
inferred← citeshttps://doi.org/10.1007/s11802-020-4438-9openalex-snapshot
Astronomical Cycles of the Late Permian Lopingian in South China and Their Implications for Third-Order Sea-Level Change
inferred← citeshttps://doi.org/10.1007/s12371-021-00630-3openalex-snapshot
The Ordovician Foum Larjamme Tunnel Paleo-valleys from Bani Geopark Project—Assessment of Geological Heritage for Geo-education and Geotourism Purposes
inferred← citeshttps://doi.org/10.1007/s12542-020-00530-xopenalex-snapshot
Sedimentary factories and ecosystem change across the Permian–Triassic Critical Interval (P–TrCI): insights from the Xiakou area (South China)
inferred← citeshttps://doi.org/10.1007/s12549-018-00370-3openalex-snapshot
Devonian palaeoecosystems and palaeoenvironments of South China
inferred← citeshttps://doi.org/10.1007/s12583-010-0201-2openalex-snapshot
Reconstruction of ecosystem and biotic recovery following the end-Permian mass extinction in South China
inferred← citeshttps://doi.org/10.1007/s12583-017-0966-7openalex-snapshot
A Griesbachian (Early Triassic) Mollusc Fauna from the Sidazhai Section, Southwest China, with Paleoecological Insights on the Proliferation of Genus Claraia (Bivalvia)
inferred← citeshttps://doi.org/10.1007/s13146-020-00626-0openalex-snapshot
Episodic dolomitizations driven by sea-level fluctuations in the Permian–Triassic boundary interval: a case study from a dolomitized Changhsingian reef, Shitouzhai section, South China
inferred← citeshttps://doi.org/10.1016/b0-08-043751-6/05087-8openalex-snapshot
Soils and Global Change in the Carbon Cycle over Geological Time
inferred← citeshttps://doi.org/10.1016/b978-0-12-384719-5.00153-2openalex-snapshot
Mammals (Pre-Quaternary), Extinctions of
inferred← citeshttps://doi.org/10.1016/b978-0-12-409548-9.09216-2openalex-snapshot
Earth's Sixth Mass Extinction Event ☆
inferred← citeshttps://doi.org/10.1016/b978-0-12-409548-9.09376-3openalex-snapshot
Overview of the Cretaceous Period☆
inferred← citeshttps://doi.org/10.1016/b978-0-444-53000-4.00004-4openalex-snapshot
Pelagic Sedimentation in Modern and Ancient Oceans
inferred← citeshttps://doi.org/10.1016/b978-008044396-6/50032-0openalex-snapshot
Charophyte Gyrogonites, the Result of Enantioselective Influence 250 Million Years Ago
inferred← citeshttps://doi.org/10.1016/b978-012370518-1/50010-2openalex-snapshot
Life in Triassic Oceans: Links Between Planktonic and Benthic Recovery and Radiation
inferred← citeshttps://doi.org/10.1016/b978-012598655-7/50040-9openalex-snapshot
The interplay of physical and biotic factors in macroevolution
inferred← citeshttps://doi.org/10.1016/bs.sats.2017.07.001openalex-snapshot
A Facies-Independent Trans-European Anisian–Ladinian Marker Horizon? Significance and Impact for Sequence Stratigraphy and Intra-Tethyan Correlation
inferred← citeshttps://doi.org/10.1016/j.annpal.2011.05.004openalex-snapshot
Palaeoenvironmental setting (glaciations, sea level, and plate tectonics) of Palaeozoic major biotic radiations in the marine realm
inferred← citeshttps://doi.org/10.1016/j.annpal.2011.09.001openalex-snapshot
Taxonomic diversity structure of Silurian crinoids: Stability versus dynamism
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2005.10.010openalex-snapshot
Comparative high-resolution chemostratigraphy of the Bonarelli Level from the reference Bottaccione section (Umbria–Marche Apennines) and from an equivalent section in NW Sicily: Consistent and contrasting responses to the OAE2
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2007.03.011openalex-snapshot
Correlation and comparison of seawater δ34Ssulfate records at the permian-triassic transition
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2010.05.012openalex-snapshot
δ34SCAS and δ18OCAS records during the Frasnian–Famennian (Late Devonian) transition and their bearing on mass extinction models
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2012.03.020openalex-snapshot
U/Mo ratios and δ98/95Mo as local and global redox proxies during mass extinction events
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2012.10.034openalex-snapshot
Isotopic chemostratigraphy across the Early–Middle Frasnian transition (Late Devonian) on the South Polish carbonate shelf: A reference for the global punctata Event
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2013.07.018openalex-snapshot
Minor and trace element and Re–Os chemistry of the Upper Devonian Woodford Shale, Permian Basin, west Texas: Insights into metal abundance and basin processes
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2015.03.020openalex-snapshot
Novel 1 H -Pyrrole-2,5-dione (maleimide) proxies for the assessment of photic zone euxinia
inferred← citeshttps://doi.org/10.1016/j.cretres.2003.07.006openalex-snapshot
The Upper Jurassic–Lower Cretaceous of eastern Heilongjiang, northeast China: stratigraphy and regional basin history
inferred← citeshttps://doi.org/10.1016/j.cretres.2005.05.007openalex-snapshot
The youngest Maastrichtian ammonite faunas from Poland and their dating by scaphitids
inferred← citeshttps://doi.org/10.1016/j.cretres.2005.09.002openalex-snapshot
Status of “Trigonia ventricosa” (Bivalvia) from the Upper Jurassic–Lower Cretaceous of Kutch, western India: Kitchin's unfinished synthesis
inferred← citeshttps://doi.org/10.1016/j.cretres.2007.01.007openalex-snapshot
Ammonite-based correlations in the Cenomanian-lower Turonian of north-west Europe, central Tunisia and the Western Interior (North America)
inferred← citeshttps://doi.org/10.1016/j.cretres.2007.10.001openalex-snapshot
Upper Cretaceous depositional environments and bivalve assemblages of far-east Asia: the Himenoura Group, Kyushu, Japan
inferred← citeshttps://doi.org/10.1016/j.cretres.2008.05.021openalex-snapshot
Calcareous nannofossil biostratigraphy and paleoecology of the Cenomanian – Turonian transition in the Tarfaya Basin, southern Morocco
inferred← citeshttps://doi.org/10.1016/j.cretres.2008.05.030openalex-snapshot
Cretaceous climate, volcanism, impacts, and biotic effects
inferred← citeshttps://doi.org/10.1016/j.cretres.2009.03.005openalex-snapshot
New biostratigraphic data from the Cretaceous Bolinxiala Formation in Zanda, southwestern Tibet of China, and their paleogeographic and paleoceanographic implications
inferred← citeshttps://doi.org/10.1016/j.cretres.2010.11.005openalex-snapshot
The first definite record of a Valanginian ichthyosaur and its implications on the evolution of post-Liassic Ichthyosauria
inferred← citeshttps://doi.org/10.1016/j.cretres.2011.12.005openalex-snapshot
Early Cretaceous life, climate and anoxia
inferred← citeshttps://doi.org/10.1016/j.crpv.2004.12.007openalex-snapshot
Survival and recovery of calcareous foraminifera pursuant to the end-Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.crpv.2005.02.002openalex-snapshot
Restructuring in benthic level-bottom shallow marine communities due to prolonged environmental stress following the end-Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.crpv.2005.02.004openalex-snapshot
Ammonoid recovery from the Late Permian mass extinction event
inferred← citeshttps://doi.org/10.1016/j.crpv.2005.02.007openalex-snapshot
Recovery of gastropods in the Early Triassic
inferred← citeshttps://doi.org/10.1016/j.crpv.2005.04.003openalex-snapshot
The reorganization of reef communities following the end-Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.crpv.2005.06.004openalex-snapshot
Summary of Early Triassic carbon isotope records
inferred← citeshttps://doi.org/10.1016/j.crvi.2011.02.006openalex-snapshot
Biodiversity is not (and never has been) a bed of roses!
inferred← citeshttps://doi.org/10.1016/j.cub.2015.08.053openalex-snapshot
Life in the Aftermath of Mass Extinctions
inferred← citeshttps://doi.org/10.1016/j.dsr2.2004.06.035openalex-snapshot
Multiple colonization of the deep sea by the Asellota (Crustacea: Peracarida: Isopoda)
inferred← citeshttps://doi.org/10.1016/j.earscirev.2006.05.002openalex-snapshot
A global marine sedimentary response to the end-Permian mass extinction: Examples from southern Turkey and the western United States
inferred← citeshttps://doi.org/10.1016/j.earscirev.2007.05.002openalex-snapshot
The nonmarine Triassic–Jurassic boundary in the Newark Supergroup of eastern North America
inferred← citeshttps://doi.org/10.1016/j.earscirev.2008.07.001openalex-snapshot
Design, science and naturalism
inferred← citeshttps://doi.org/10.1016/j.earscirev.2009.04.001openalex-snapshot
Composition and similarity of global anomodont-bearing tetrapod faunas
inferred← citeshttps://doi.org/10.1016/j.earscirev.2010.07.004openalex-snapshot
The Middle Permian (Capitanian) mass extinction on land and in the oceans
inferred← citeshttps://doi.org/10.1016/j.earscirev.2014.11.008openalex-snapshot
Evidence and causes of the main extinction events in the Paleogene based on extinction and survival patterns of foraminifera
inferred← citeshttps://doi.org/10.1016/j.earscirev.2017.04.008openalex-snapshot
Permian tetrapod extinction events
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.07.012openalex-snapshot
Unusual shallow marine matground-adapted benthic biofacies from the Lower Triassic of the northern Paleotethys: Implications for biotic recovery following the end-Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.10.012openalex-snapshot
Global-ocean redox variations across the Smithian-Spathian boundary linked to concurrent climatic and biotic changes
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.10.014openalex-snapshot
Ecological persistence, incumbency and reorganization in the Karoo Basin during the Permian-Triassic transition
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.03.004openalex-snapshot
Quantitative stratigraphic correlation of Tethyan conodonts across the Smithian-Spathian (Early Triassic) extinction event
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.103060openalex-snapshot
The longest delay: Re-emergence of coral reef ecosystems after the Late Devonian extinctions
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103180openalex-snapshot
The Late Triassic Extinction at the Norian/Rhaetian boundary: Biotic evidence and geochemical signature
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103280openalex-snapshot
The latest Ordovician Hirnantian brachiopod faunas: New global insights
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103282openalex-snapshot
A two-phase end-Triassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103331openalex-snapshot
Early Triassic terrestrial tetrapod fauna: a review
inferred← citeshttps://doi.org/10.1016/j.ecocom.2008.10.013openalex-snapshot
Extinctions in a spatial model of fossil communities subject to correlated environmental disturbance
inferred← citeshttps://doi.org/10.1016/j.epsl.2004.04.034openalex-snapshot
Isotopic evidence bearing on Late Triassic extinction events, Queen Charlotte Islands, British Columbia, and implications for the duration and cause of the Triassic/Jurassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.epsl.2005.02.027openalex-snapshot
Basaltic volcanism and mass extinction at the Permo-Triassic boundary: Environmental impact and modeling of the global carbon cycle
inferred← citeshttps://doi.org/10.1016/j.epsl.2005.09.050openalex-snapshot
Anomalous iridium enrichment at the Triassic–Jurassic boundary, Blomidon Formation, Fundy basin, Canada
inferred← citeshttps://doi.org/10.1016/j.epsl.2005.12.007openalex-snapshot
Reinitialization of evolutionary clocks during sublethal environmental stress in some invertebrates
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.03.043openalex-snapshot
Two episodes of 13C-depletion in organic carbon in the latest Permian: Evidence from the terrestrial sequences in northern Xinjiang, China
inferred← citeshttps://doi.org/10.1016/j.epsl.2009.12.020openalex-snapshot
Rise and fall of the Paratethys Sea during the Messinian Salinity Crisis
inferred← citeshttps://doi.org/10.1016/j.epsl.2012.01.039openalex-snapshot
Environmental changes across the Triassic–Jurassic boundary and coeval volcanism inferred from elemental geochemistry and mineralogy in the Kendlbachgraben section (Northern Calcareous Alps, Austria)
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.08.037openalex-snapshot
40Ar/39Ar age of the Lake Saint Martin impact structure (Canada) – Unchaining the Late Triassic terrestrial impact craters
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.07.028openalex-snapshot
A chronostratigraphic assessment of the Moenave Formation, USA using C-isotope chemostratigraphy and detrital zircon geochronology: Implications for the terrestrial end Triassic extinction
inferred← citeshttps://doi.org/10.1016/j.epsl.2018.09.020openalex-snapshot
Global seawater redox trends during the Late Devonian mass extinction detected using U isotopes of marine limestones
inferred← citeshttps://doi.org/10.1016/j.gca.2019.12.019openalex-snapshot
Paleo-redox context of the Mid-Devonian Appalachian Basin and its relevance to biocrises
inferred← citeshttps://doi.org/10.1016/j.gca.2021.03.001openalex-snapshot
Resolving the age of the Puchezh-Katunki impact structure (Russia) against alteration and inherited 40Ar* – No link with extinctions
inferred← citeshttps://doi.org/10.1016/j.geobios.2007.01.007openalex-snapshot
Brachiopods and other fossils from the Permo–Triassic boundary beds of the Antalya Nappes (SW Taurus, Turkey)
inferred← citeshttps://doi.org/10.1016/j.geobios.2009.12.002openalex-snapshot
The Permian/Triassic mass extinction among brachiopods in the Northern Caucasus (northern Palaeo-Tethys): A tentative assessment
inferred← citeshttps://doi.org/10.1016/j.geobios.2010.07.004openalex-snapshot
An unusually diverse mollusc fauna from the earliest Triassic of South China and its implications for benthic recovery after the end-Permian biotic crisis
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2006.06.006openalex-snapshot
A unique carbon isotope record across the Guadalupian–Lopingian (Middle–Upper Permian) boundary in mid-oceanic paleo-atoll carbonates: The high-productivity “Kamura event” and its collapse in Panthalassa
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2006.06.011openalex-snapshot
Biostratigraphy and event stratigraphy in Iran around the Permian–Triassic Boundary (PTB): Implications for the causes of the PTB biotic crisis
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2006.06.016openalex-snapshot
Molecular and isotopic evidence for episodic environmental change across the Permo/Triassic boundary at Meishan in South China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2006.06.017openalex-snapshot
Return to Coalsack Bluff and the Permian–Triassic boundary in Antarctica
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2008.05.002openalex-snapshot
Evaluation of palaeo-oxygenation of the ocean bottom across the Permian–Triassic boundary
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2008.11.004openalex-snapshot
The effects of mid-Phanerozoic environmental stress on bryozoan diversity, paleoecology, and paleogeography
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2010.01.022openalex-snapshot
An 80 million year oceanic redox history from Permian to Jurassic pelagic sediments of the Mino-Tamba terrane, SW Japan, and the origin of four mass extinctions
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2010.03.011openalex-snapshot
Structural changes of marine communities over the Permian–Triassic transition: Ecologically assessing the end-Permian mass extinction and its aftermath
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2010.03.012openalex-snapshot
Palaeoecology and taphonomy of two brachiopod shell beds from the Anisian (Middle Triassic) of Guizhou, Southwest China: Recovery of benthic communities from the end-Permian mass extinction
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.2011.09.009openalex-snapshot
Paleoceanographic conditions following the end-Permian mass extinction recorded by giant ooids (Moyang, South China)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2012.01.002openalex-snapshot
The appearance of an oxygen-depleted condition on the Capitanian disphotic slope/basin in South China: Middle–Upper Permian stratigraphy at Chaotian in northern Sichuan
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2012.06.006openalex-snapshot
Precession-driven monsoon variability at the Permian–Triassic boundary — Implications for anoxia and the mass extinction
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.01.002openalex-snapshot
Redox conditions and marine microbial community changes during the end-Ordovician mass extinction event
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.05.008openalex-snapshot
Uppermost Permian trace fossils along a shelf to slope transect in South China and their implications for oceanic redox evolution and extinction pattern
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.10.002openalex-snapshot
Two-stage marine anoxia and biotic response during the Permian–Triassic transition in Kashmir, northern India: pyrite framboid evidence
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.01.006openalex-snapshot
A global biogeochemical perturbation during the Middle Frasnian punctata Event: Evidence from muted carbon isotope signature in the Appalachian Basin, New York State (USA)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103174openalex-snapshot
A volcanic scenario for the Frasnian–Famennian major biotic crisis and other Late Devonian global changes: More answers than questions?
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103210openalex-snapshot
Sedimentology and carbon isotope stratigraphy of the Rhaetian Hochalm section (Late Triassic, Austria)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103312openalex-snapshot
Mercury linked to Deccan Traps volcanism, climate change and the end-Cretaceous mass extinction
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103362openalex-snapshot
Smithian and Spathian (Early Triassic) conodonts from Oman and Croatia and their depth habitat revealed
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103590openalex-snapshot
Reassessing Early Triassic wrinkle structures from moderate-high latitudes: An updated interpretation of metazoan colonization in matground ecosystems after the Permian-Triassic mass extinction
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103613openalex-snapshot
Abundant conodont faunas from the Olenekian (Early Triassic) of subsurface British Columbia, Canada and diversification of the Neogondolellinae around the Smithian–Spathian boundary
inferred← citeshttps://doi.org/10.1016/j.gr.2011.08.015openalex-snapshot
Early Triassic trace fossils from Gondwana Interior Sea: Implication for ecosystem recovery following the end-Permian mass extinction in south high-latitude region
inferred← citeshttps://doi.org/10.1016/j.gr.2012.12.010openalex-snapshot
Impacts of global warming on Permo-Triassic terrestrial ecosystems
inferred← citeshttps://doi.org/10.1016/j.gr.2013.05.003openalex-snapshot
The Nebula Winter: The united view of the snowball Earth, mass extinctions, and explosive evolution in the late Neoproterozoic and Cambrian periods
inferred← citeshttps://doi.org/10.1016/j.gr.2017.05.004openalex-snapshot
Examining the Ladinian crisis in light of the current knowledge of the Triassic biodiversity changes
inferred← citeshttps://doi.org/10.1016/j.gr.2019.01.016openalex-snapshot
Exceptionally preserved soft-bodied assemblage in Ordovician carbonates of Anticosti Island, eastern Canada
inferred← citeshttps://doi.org/10.1016/j.gsf.2012.04.002openalex-snapshot
Were Late Cretaceous extinctions of gastropods selective by generic longevity?
inferred← citeshttps://doi.org/10.1016/j.gsf.2013.08.005openalex-snapshot
Flood basalt hosted palaeosols: Potential palaeoclimatic indicators of global climate change
inferred← citeshttps://doi.org/10.1016/j.gsf.2017.11.004openalex-snapshot
Episodic events in long-term geological processes: A new classification and its applications
inferred← citeshttps://doi.org/10.1016/j.gsf.2021.101146openalex-snapshot
Decoupled δ13Ccarb and δ13Corg records at Triassic–Jurassic boundary interval in eastern Tethys: Environmental implications for spatially different global response
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2005.07.015openalex-snapshot
Phanerozoic evolution of plants on the African plate
inferred← citeshttps://doi.org/10.1016/j.jfluidstructs.2020.102908openalex-snapshot
Experimental study of vortex-induced vibration of a twin-tube submerged floating tunnel segment model
inferred← citeshttps://doi.org/10.1016/j.jhevol.2014.06.016openalex-snapshot
Comparative and population mitogenomic analyses of Madagascar's extinct, giant ‘subfossil’ lemurs
inferred← citeshttps://doi.org/10.1016/j.jop.2015.08.010openalex-snapshot
End-Triassic nonmarine biotic events
inferred← citeshttps://doi.org/10.1016/j.jop.2017.10.002openalex-snapshot
Evolution of sedimentary facies and fossil communities in the Middle Permian Maokou Formation in Zigui County, Hubei Province, South China
inferred← citeshttps://doi.org/10.1016/j.jsames.2009.03.003openalex-snapshot
Triassic synthems of southern South America (southwestern Gondwana) and the Western Caucasus (the northern Neotethys), and global tracing of their boundaries
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