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Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1016/b978-0-444-59425-9.00007-xopenalex-snapshot
Strontium Isotope Stratigraphy
inferredcites →https://doi.org/10.1016/b978-0-444-59425-9.00020-2openalex-snapshot
The Ordovician Period
inferredcites →https://doi.org/10.1016/j.earscirev.2007.02.001openalex-snapshot
Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic
inferredcites →https://doi.org/10.1016/j.earscirev.2012.06.007openalex-snapshot
Phanerozoic polar wander, palaeogeography and dynamics
inferredcites →https://doi.org/10.1016/j.geobios.2007.10.006openalex-snapshot
Resolving early Mid-Ordovician (Kundan) bioevents in the East Baltic based on brachiopods
inferredcites →https://doi.org/10.1016/j.palaeo.2004.02.034openalex-snapshot
Response of Late Ordovician paleoceanography to changes in sea level, continental drift, and atmospheric pCO2: potential causes for long-term cooling and glaciation
inferredcites →https://doi.org/10.1016/j.palaeo.2005.07.010openalex-snapshot
The Ordovician biodiversification: Setting an agenda for marine life
inferredcites →https://doi.org/10.1016/j.palaeo.2006.02.033openalex-snapshot
What caused the Ordovician biodiversification?
inferredcites →https://doi.org/10.1016/j.palaeo.2008.06.012openalex-snapshot
Oxygen isotope values from high-latitudes: Clues for Permian sea-surface temperature gradients and Late Palaeozoic deglaciation
inferredcites →https://doi.org/10.1016/j.palaeo.2012.02.012openalex-snapshot
Biotic dynamics and carbonate microfacies of the conspicuous Darriwilian (Middle Ordovician) ‘Täljsten’ interval, south-central Sweden
inferredcites →https://doi.org/10.1016/j.palaeo.2015.11.003openalex-snapshot
The onset of the ‘Ordovician Plankton Revolution’ in the late Cambrian
inferredcites →https://doi.org/10.1016/s0012-8252(97)83482-4openalex-snapshot
Trilobite systematics, biostratigraphy and palaeoecology of the lower ordovician komstad limestone and huk formations, southern Scandinavia
inferredcites →https://doi.org/10.1017/s0016756809990148openalex-snapshot
Ecostratigraphical interpretation of lower Middle Ordovician East Baltic sections based on brachiopods
inferredcites →https://doi.org/10.1017/s0016756812000908openalex-snapshot
High resolution trilobite stratigraphy of the Lower–Middle Ordovician Öland Series of Baltoscandia
inferredcites →https://doi.org/10.1017/s0016756813000198openalex-snapshot
Graptoloid evolutionary rates track Ordovician–Silurian global climate change
inferredcites →https://doi.org/10.1017/s0094837300003778openalex-snapshot
A factor analytic description of the Phanerozoic marine fossil record
inferredcites →https://doi.org/10.1029/1999pa900021openalex-snapshot
Late Ordovician glaciation under high atmospheric CO2: A coupled model analysis
inferredcites →https://doi.org/10.1029/2004pa001071openalex-snapshot
A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ 18 O records
inferredcites →https://doi.org/10.1038/nature03975openalex-snapshot
Modelled atmospheric temperatures and global sea levels over the past million years
inferredcites →https://doi.org/10.1038/nature09700openalex-snapshot
Geochemical evidence for widespread euxinia in the Later Cambrian ocean
inferredcites →https://doi.org/10.1038/ngeo.2007.37openalex-snapshot
Asteroid breakup linked to the Great Ordovician Biodiversification Event
inferredcites →https://doi.org/10.1046/j.1365-3121.1999.00229.xopenalex-snapshot
Oceanic circulation as an element in palaeogeographical reconstructions: the Arenig (early Ordovician) as an example
inferredcites →https://doi.org/10.1063/1.1671982openalex-snapshot
Oxygen Isotope Fractionation in Divalent Metal Carbonates
inferredcites →https://doi.org/10.1080/08912960601151744openalex-snapshot
Baltica: A mid Ordovician diversity hotspot
inferredcites →https://doi.org/10.1080/11035897.2013.876659openalex-snapshot
Possible oceanic circulation patterns, surface water currents and upwelling zones in the Early Palaeozoic
inferredcites →https://doi.org/10.1080/11035897.2014.880507openalex-snapshot
The Volkhov–Kunda transition and the base of the Holen Limestone at Kinnekulle, Västergötland, Sweden
inferredcites →https://doi.org/10.1111/j.1502-3931.1973.tb00871.xopenalex-snapshot
Aspects of carbonate sedimentation in the Ordovician of Baltoscandia
inferredcites →https://doi.org/10.1111/j.1502-3931.2008.00115.xopenalex-snapshot
The Ordovician Biodiversification: revolution in the oceanic trophic chain
inferredcites →https://doi.org/10.1111/j.1502-3931.2008.00136.xopenalex-snapshot
The new chronostratigraphic classification of the Ordovician System and its relations to major regional series and stages and to δ 13 C chemostratigraphy
inferredcites →https://doi.org/10.1126/science.1155814openalex-snapshot
Did Cooling Oceans Trigger Ordovician Biodiversification? Evidence from Conodont Thermometry
inferredcites →https://doi.org/10.1126/science.1156963openalex-snapshot
Phanerozoic Trends in the Global Diversity of Marine Invertebrates
inferredcites →https://doi.org/10.1126/science.1161648openalex-snapshot
A Chronology of Paleozoic Sea-Level Changes
inferredcites →https://doi.org/10.1126/science.1189910openalex-snapshot
The Shifting Balance of Diversity Among Major Marine Animal Groups
inferredcites →https://doi.org/10.1130/g34962.1openalex-snapshot
Plate tectonic influences on Neoproterozoic–early Paleozoic climate and animal evolution
inferredcites →https://doi.org/10.1144/0016-76492009-080openalex-snapshot
The middle Darriwilian (Ordovician) δ 13 C excursion (MDICE) discovered in the Yangtze Platform succession in China: implications of its first recorded occurrences outside Baltoscandia
inferredcites →https://doi.org/10.1144/0016-76492011-048openalex-snapshot
Oxygen isotope variability in conodonts: implications for reconstructing Palaeozoic palaeoclimates and palaeoceanography
inferredcites →https://doi.org/10.1144/jgs2012-122openalex-snapshot
Long-period orbital climate forcing in the early Palaeozoic?
inferredcites →https://doi.org/10.1144/m38.11openalex-snapshot
Chapter 11 Biodiversity, biogeography and phylogeography of Ordovician rhynchonelliform brachiopods
inferredcites →https://doi.org/10.1144/sp325.1openalex-snapshot
Early Palaeozoic peri-Gondwana terranes: new insights from tectonics and biogeography
inferredcites →https://doi.org/10.1144/sp325.2openalex-snapshot
The Lower Palaeozoic palaeogeographical evolution of the northeastern and eastern peri-Gondwanan margin from Turkey to New Zealand
inferredcites →https://doi.org/10.1146/annurev.ea.22.050194.002033openalex-snapshot
THE INITIATION OF NORTHERN HEMISPHERE GLACIATION
inferredcites →https://doi.org/10.18261/8200376583-1995-01openalex-snapshot
Trilobite systematics, biostratigraphy and palaeoecology of the Lower Ordovician Komstad Limestone and Huk Formations, southern Scandinavia
inferredcites →https://doi.org/10.2475/ajs.278.3.257openalex-snapshot
Progressive ventilation of the oceans; an explanation for the distribution of the lower Paleozoic black shales
inferredcites →https://doi.org/10.37570/bgsd-2003-50-02openalex-snapshot
Review of the Ordovician rhynchonelliformean Brachiopoda of the East Baltic: their distribution and biofacies
inferredcites →https://doi.org/10.37570/bgsd-2003-50-03openalex-snapshot
Brachiopod macrofaunal distribution through the upper Volkhov – lower Kunda (Lower Ordovician) rocks, Lynna River, St. Petersburg region
inferredcites →https://doi.org/10.37570/bgsd-2003-50-08openalex-snapshot
Upper Arenig trilobite biostratigraphy and sea-level changes at Lynna River near Volkhov, Russia
inferredcites →https://doi.org/10.7312/webb12678-011openalex-snapshot
10. Ordovician Sea Level Changes: A Baltoscandian Perspective
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.5852/ejt.2021.774.1533zenodo-depositor-declared
Middle Ordovician Drepanoistodus (Vertebrata, Conodonta) from Baltica, with description of three new species
inferred← citeshttps://doi.org/10.1002/2016pa002928openalex-snapshot
Glacial onset predated Late Ordovician climate cooling
inferred← citeshttps://doi.org/10.1002/9781119412595openalex-snapshot
Ordovician rhynchonelliformean brachiopods from Co. Waterford, SE Ireland: Palaeobiogeography of the Leinster Terrane
inferred← citeshttps://doi.org/10.1002/9781119412595.ch1openalex-snapshot
Ordovician rhynchonelliformean brachiopods from Co. Waterford, SE Ireland: palaeobiogeography of the Leinster Terrane
inferred← citeshttps://doi.org/10.1002/essoar.10511918.3openalex-snapshot
Temperature: a key driver of Earth’s habitability over the last billion years
inferred← citeshttps://doi.org/10.1002/gj.4068openalex-snapshot
Middle to Late Ordovician carbon isotope chemostratigraphy of the Lower Yangtze Platform: Implications for global correlation
inferred← citeshttps://doi.org/10.1007/978-94-017-9600-2_4openalex-snapshot
The Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1007/s00410-020-01699-9openalex-snapshot
U–Pb geochronology of apatite and zircon from the Brent impact structure, Canada: a Late Ordovician Sandbian–Katian boundary event associated with L-Chondrite parent body disruption
inferred← citeshttps://doi.org/10.1007/s12517-020-06202-zopenalex-snapshot
Evolution of Ordovician cephalopod diversity in the Middle Yangtze region of South China and its controlling factors
inferred← citeshttps://doi.org/10.1007/s12549-016-0260-1openalex-snapshot
Heterostracan vertebrates and the Great Eodevonian Biodiversification Event—an essay
inferred← citeshttps://doi.org/10.1007/s12549-020-00426-3openalex-snapshot
Diversity patterns and palaeoecology of benthic communities of the Kanosh Formation (Pogonip Group, Utah, western USA)
inferred← citeshttps://doi.org/10.1007/s41513-025-00290-0openalex-snapshot
Gondwana platform paleoenvironment reconstruction: insights from the geochemistry of Ordovician black-grey shales in NW Iberia
inferred← citeshttps://doi.org/10.1016/bs.sats.2020.09.001openalex-snapshot
Ordovician δ13C chemostratigraphy: A global review of major excursions and their ties to graptolite and conodont biostratigraphy
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2016.08.039openalex-snapshot
Geochemistry of Campanian–Maastrichtian brachiopods from the Rørdal-1 core (Denmark): Differential responses to environmental change and diagenesis
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2016.10.012openalex-snapshot
Redox fluctuations in the Early Ordovician oceans: An insight from chromium stable isotopes
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2017.03.034openalex-snapshot
Element/Ca, C and O isotope ratios in modern brachiopods: Species-specific signals of biomineralization
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2017.06.007openalex-snapshot
Geochemistry of the brachiopod Hemithiris psittacea from the Canadian Arctic: Implications for high latitude palaeoclimate studies
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2020.119665openalex-snapshot
The impacts of land plant evolution on Earth's climate and oxygenation state – An interdisciplinary review
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.120906openalex-snapshot
A reassessment on the timing and potential drivers of the major seawater 87Sr/86Sr drop in the Ordovician Period: New evidence from conodonts in China
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2025.122859openalex-snapshot
Middle Ordovician climate modulation by enhanced continental and reverse weathering: Evidence from lithium isotopes
inferred← citeshttps://doi.org/10.1016/j.cub.2021.08.069openalex-snapshot
Bottom-up controls, ecological revolutions and diversification in the oceans through time
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.04.003openalex-snapshot
Marine oxygenation, lithistid sponges, and the early history of Paleozoic skeletal reefs
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103672openalex-snapshot
Early Paleozoic radiolarian plankton diversity and the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103748openalex-snapshot
Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions – insights from molybdenum and uranium isotopic global redox proxies
inferred← citeshttps://doi.org/10.1016/j.earscirev.2023.104400openalex-snapshot
Quantitative paleogeographical reconstructions and basin evolution of South China during the Ordovician
inferred← citeshttps://doi.org/10.1016/j.earscirev.2025.105194openalex-snapshot
Diversification to extinction: oceanic and climatic context of the Ordovician
inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117641openalex-snapshot
Role of seafloor production versus continental basalt weathering in Middle to Late Ordovician seawater 87Sr/86Sr and climate
inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117717openalex-snapshot
Understanding the early Paleozoic carbon cycle balance and climate change from modelling
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118805openalex-snapshot
Calcium isotope constraints on a Middle Ordovician carbon isotope excursion
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118891openalex-snapshot
L-chondrite body breakup in Ordovician strata in China - A time tie point globally and across the inner solar system
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118991openalex-snapshot
Evidence suggesting that earth had a ring in the Ordovician
inferred← citeshttps://doi.org/10.1016/j.epsl.2026.120043openalex-snapshot
Co-evolution of marine ecosystems and nutrient cycles during the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1016/j.gca.2017.11.015openalex-snapshot
A paired apatite and calcite clumped isotope thermometry approach to estimating Cambro-Ordovician seawater temperatures and isotopic composition
inferred← citeshttps://doi.org/10.1016/j.gca.2026.04.031openalex-snapshot
Chemical fingerprints of five modern brachiopod species and their application to support fossil geochemical studies
inferred← citeshttps://doi.org/10.1016/j.gca.2026.07.010openalex-snapshot
Suppressed upwelling during the Cambrian–Ordovician transition revealed by coupled Cr–Cd isotope systematics
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2016.12.008openalex-snapshot
Biotic immigration events, speciation, and the accumulation of biodiversity in the fossil record
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.12.010openalex-snapshot
An astronomically forced cooling event during the Middle Ordovician
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.103032openalex-snapshot
Upper Ordovician marine red limestones, Tarim Basin, NW China: A product of an oxygenated deep ocean and changing climate?
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.103069openalex-snapshot
Minor Δ33S anomalies coincide with biotic turnover events during the Great Ordovician Biodiversification Event (GOBE) in South China
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103665openalex-snapshot
The palaeogeographical impact on the biodiversity of marine faunas during the Ordovician radiations
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103917openalex-snapshot
What triggered the Late Ordovician mass extinction (LOME)? Perspectives from geobiology and biogeochemical modeling
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104183openalex-snapshot
Progressive marine oxygenation and climatic cooling at the height of the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104523openalex-snapshot
High resolution Ordovician carbon isotope chemostratigraphy in South China and its significance for global correlation
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105209openalex-snapshot
Ordovician climate changes in South China and implications for biotic turnover after the Great Ordovician Biodiversification Event (GOBE): Evidence from conodont δ18O thermometry
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105246openalex-snapshot
Oxygen isotope-based evidence for stepwise climate cooling aligns with the tripartite division of the Ordovician
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105283openalex-snapshot
Astronomically paced Katian (late Ordovician) sea-level changes: A record from Northern Yangtze Block
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105671openalex-snapshot
Coupled evolution of marine chemocline and nitrogen cycling on continental margins during the Middle Ordovician cooling
inferred← citeshttps://doi.org/10.1016/j.gr.2018.01.006openalex-snapshot
Oxygen isotope analysis of the eyes of pelagic trilobites: Testing the application of sea temperature proxies for the Ordovician
inferred← citeshttps://doi.org/10.1016/j.gr.2020.09.008openalex-snapshot
Ordovician palaeogeography and climate change
inferred← citeshttps://doi.org/10.1016/j.gr.2023.12.002openalex-snapshot
Speculations on the Paleozoic legacy of Gondwana amalgamation
inferred← citeshttps://doi.org/10.1016/j.jop.2026.100366openalex-snapshot
The last stand of an Ordovician heritage: Daedalus from the upper Silurian of the Yangtze platform, South China
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2019.02.008openalex-snapshot
Lipid biomarker and stable isotopic profiles through Early-Middle Ordovician carbonates from Spitsbergen, Norway
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.03.023openalex-snapshot
Conodonts from the Lower Ordovician of Morocco — Contributions to age and faunal diversity of the Fezouata Lagerstätte and peri-Gondwana biogeography
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.05.015openalex-snapshot
Co-evolution of oceans, climate, and the biosphere during the ‘Ordovician Revolution’: A review
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.12.016openalex-snapshot
Biostratigraphy and carbon and nitrogen geochemistry of the SPICE event in Cambrian low-grade metamorphic black shale, Southern Norway
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.06.004openalex-snapshot
Microfacies analysis of the Lower-Middle Ordovician succession at Xiangshuidong, southwestern Hubei Province, and the drowning and shelf-ramp transition of a carbonate platform in the Yangtze region
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.10.006openalex-snapshot
Dispersal in the Ordovician: Speciation patterns and paleobiogeographic analyses of brachiopods and trilobites
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.10.018openalex-snapshot
Paired isotope records of carbonate and organic matter from the Middle Ordovician of Argentina: Intrabasinal variation and effects of the marine chemocline
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.04.002openalex-snapshot
Lower and Middle Ordovician chitinozoans from Honghuayuan, South China: Biodiversity patterns and response to environmental changes
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.10.006openalex-snapshot
Influence of dissolved oxygen on secular patterns of marine microbial carbonate abundance during the past 490 Myr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.10.032openalex-snapshot
Climatic and oceanic changes during the Middle-Late Ordovician transition in the Tarim Basin, NW China and implications for the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.01.032openalex-snapshot
Middle–Upper Ordovician (Darriwilian–Sandbian) paired carbon and sulfur isotope stratigraphy from the Appalachian Basin, USA: Implications for dynamic redox conditions spanning the peak of the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.02.018openalex-snapshot
Impacts of climate-ocean-tectonic changes on early Paleozoic conodont ecology and evolution evidenced by the Canadian part of Laurentia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.03.016openalex-snapshot
Comparative Lower-Middle Ordovician conodont oxygen isotope palaeothermometry of the Argentine Precordillera and Laurentian margins
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.04.007openalex-snapshot
Late Cambrian (Furongian) to mid-Ordovician euconodont events on Baltica: Invasions and immigrations
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.05.030openalex-snapshot
First documentation of Middle Ordovician warm-water carbonates in the Mount Jolmo Lungma (Mount Everest) area, southern Xizang (Tibet), China, and its paleogeographic implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.05.034openalex-snapshot
Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109280openalex-snapshot
Revisiting the Great Ordovician Diversification of land plants: Recent data and perspectives
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109319openalex-snapshot
The glacially induced Middle Ordovician rise of the Plectambonitoidea (Brachiopoda) and the phylogenetic placement of the Baltic genus Ukoa
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109341openalex-snapshot
Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ~458 Ma)?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109521openalex-snapshot
A multidisciplinary perspective on the Great Ordovician Biodiversification Event and the development of the early Paleozoic world
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109534openalex-snapshot
Darriwilian carbon isotope stratigraphy in the Taebaeksan Basin, Korea and its implications for Middle Ordovician paleoceanography
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109584openalex-snapshot
δ30Si and δ18O of multiple silica phases in chert: Implications for δ30Siseawater of Darriwilian seawater and sea surface temperatures
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109792openalex-snapshot
Marine redox variability from Baltica during extinction events in the latest Ordovician–early Silurian
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109991openalex-snapshot
Paleo-environmental changes during the Middle–Late Ordovician transition on the Yangtze Platform, South China and their ecological implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.110116openalex-snapshot
Environmental changes revealed by Lower–Middle Ordovician deeper-water marine red beds from the marginal Yangtze Platform, South China: Links to biodiversification
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110347openalex-snapshot
Climate changes in the pre-Hirnantian Late Ordovician based on δ18Ophos studies from Estonia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110555openalex-snapshot
Ecological niche evolution, speciation, and feedback loops: Investigating factors promoting niche evolution in Ordovician brachiopods of eastern Laurentia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110564openalex-snapshot
Geochemistry of lower Ordovician microbialites on the Yangtze Platform, South China: Implications for oceanic oxygenation at the onset of the GOBE
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110715openalex-snapshot
Marine oxygenation, deoxygenation, and life during the Early Paleozoic: An overview
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111149openalex-snapshot
Biostratigraphically-controlled Darriwilian (Middle Ordovician) δ13C excursions in North China: Implications for correlation and climate change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111209openalex-snapshot
Orbital-scale climate changes detected in Lower and Middle Ordovician cyclic limestones using oxygen isotopes of conodont apatite
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111446openalex-snapshot
Coupled biostratigraphy and chemostratigraphy at Lanna, Sweden: A key section for the Floian–lower Darriwilian interval (Lower–Middle Ordovician)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111519openalex-snapshot
The Central Andean Basin as a dispersal centre: Biogeographic patterns of olenid trilobites during the late Cambrian – Early Ordovician
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111568openalex-snapshot
Hydrodynamics as a hidden abiotic factor constraining Ordovician chitinozoan morphological evolution
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111592openalex-snapshot
No (Cambrian) explosion and no (Ordovician) event: A single long-term radiation in the early Palaeozoic
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111640openalex-snapshot
Paired carbon isotope chemostratigraphy across the Ordovician–Silurian boundary in central East Baltic: Regional and global signatures
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111686openalex-snapshot
Coupled sedimentary and δ13C records of western Thailand and South China from Middle to Late Ordovician: Sea-level and climate changes prior to the Hirnantian glaciation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111738openalex-snapshot
Depositional and tectonic influences on preservation of Milankovitch record during long-term global cooling: Middle and Upper Ordovician convergent foreland, eastern USA
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111905openalex-snapshot
Diversity dynamics, faunal turnover and radiation pattern of the Middle Ordovician trilobites in South China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111906openalex-snapshot
Phosphorus cycling during the Hirnantian glaciation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112265openalex-snapshot
Middle Ordovician climatic and oceanic destabilization in a slope-setting of the Yangtze platform, South China, and its role as a regional brake on the Ordovician radiations
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112371openalex-snapshot
Persistent cooling in the Ordovician (Darriwilian–Sandbian) revealed by conodont δ18O records in the Tarim Basin, NW China: Climatic and sedimentary implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112550openalex-snapshot
Globally synchronous meteorite rain during the Middle Ordovician
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112765openalex-snapshot
Climate changes in the Middle and Late Ordovician of the tropical belt: The δ18O record from the Tunguska Basin of Siberia and its palaeogeographical relation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113227openalex-snapshot
High resolution Ordovician (Floian-Sandbian) carbon isotope stratigraphy from the Jiangnan slope, South China: The first complete record of the MDICE in δ13Corg and its global significance
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113465openalex-snapshot
Phanerozoic marine bioevents: A review with applications to stratigraphy and earth history
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114134openalex-snapshot
Species-level diversity dynamics during the Great Ordovician biodiversification event: a phylodynamic case study of Laurentian brachiopod lineages
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114220openalex-snapshot
Lithofacies control on the expression of the Middle Darriwilian carbon isotope excursion (MDICE) and the first radiolarian record from the excursion interval, western margin of the Ordos Basin, North China
inferred← citeshttps://doi.org/10.1016/j.palwor.2022.09.003openalex-snapshot
Darriwilian–Sandbian (Middle–Late Ordovician) shallow warm-water deposits in the Upper Yangtze region, South China: A case study from the Qiaojia area, northeastern Yunnan Province
inferred← citeshttps://doi.org/10.1016/j.petrol.2022.111308openalex-snapshot
Controls on organic matter accumulation on the Late-Ordovician shales in Awati Sag in northwestern Tarim Basin, NW China
inferred← citeshttps://doi.org/10.1016/j.revmic.2017.08.001openalex-snapshot
Middle Ordovician acritarchs and problematic organic-walled microfossils from the Saq-Hanadir transitional beds in the QSIM-801 well, Saudi Arabia
inferred← citeshttps://doi.org/10.1016/j.revpalbo.2017.06.008openalex-snapshot
Chitinozoan biostratigraphy and carbon isotope stratigraphy from the Upper Ordovician Skogerholmen Formation in the Oslo Region. A new perspective for the Hirnantian lower boundary in Baltica
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2021.105943openalex-snapshot
Composition and spatiotemporal evolution of the mixed turbidite-contourite systems from the Middle Ordovician, in western margin of the North China Craton
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2026.107189openalex-snapshot
Middle Darriwilian carbon isotope excursion in the Ordos Basin, North China: Geochemical constraints on paleoenvironmental change during the great Ordovician biodiversification event
inferred← citeshttps://doi.org/10.1017/jpa.2026.10259openalex-snapshot
Late Ordovician ostracods from the “butter shale” Lagerstätten of the Cincinnati Arch region, Ohio, USA
inferred← citeshttps://doi.org/10.1017/pab.2019.4openalex-snapshot
Dissecting the paleocontinental and paleoenvironmental dynamics of the great Ordovician biodiversification
inferred← citeshttps://doi.org/10.1017/pab.2020.24openalex-snapshot
Estimating dispersal and evolutionary dynamics in diploporan blastozoans (Echinodermata) across the great Ordovician biodiversification event
inferred← citeshttps://doi.org/10.1017/pab.2022.45openalex-snapshot
Insights for modern invasion ecology from biotic changes of the Clarksville Phase of the Richmondian Invasion (Ordovician, Katian)
inferred← citeshttps://doi.org/10.1017/pab.2024.7openalex-snapshot
The Fezouata Shale Formation biota is typical for the high latitudes of the Early Ordovician—a quantitative approach
inferred← citeshttps://doi.org/10.1017/pab.2025.10054openalex-snapshot
Global factors constrain body-size trends across the Great Ordovician Biodiversification Event at a regional scale: a case study from the Arbuckle Mountains of Oklahoma
inferred← citeshttps://doi.org/10.1017/s001675681700098xopenalex-snapshot
The integration of palaeomagnetism, the geological record and mantle tomography in the location of ancient continents
inferred← citeshttps://doi.org/10.1017/s0016756819000372openalex-snapshot
Katian (Upper Ordovician) carbon isotope chemostratigraphy in the Neixiang area, central China: implications for intercontinental correlation
inferred← citeshttps://doi.org/10.1017/s0016756819001298openalex-snapshot
Early Palaeozoic diversifications and extinctions in the marine biosphere: a continuum of change
inferred← citeshttps://doi.org/10.1017/s0016756820001077openalex-snapshot
Middle Ordovician (Darriwilian) conodonts from southern Tibet, the Indian passive margin: implications for the age and correlation of the roof of the world
inferred← citeshttps://doi.org/10.1017/s0016756822001078openalex-snapshot
Chitinozoan biostratigraphy of the regional Arenig Series in Wales and correlation with the global Lower–Middle Ordovician series and stages
inferred← citeshttps://doi.org/10.1017/s1755691025100947openalex-snapshot
Early Palaeozoic radiolarian macroevolutionary dynamics and possible relation to global change
inferred← citeshttps://doi.org/10.1029/2021av000563openalex-snapshot
Geochemical Records Reveal Protracted and Differential Marine Redox Change Associated With Late Ordovician Climate and Mass Extinctions
inferred← citeshttps://doi.org/10.1029/2021pa004309openalex-snapshot
A Baltic Perspective on the Early to Early Late Ordovician δ 13 C and δ 18 O Records and Its Paleoenvironmental Significance
inferred← citeshttps://doi.org/10.1038/ncomms14066openalex-snapshot
Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification
inferred← citeshttps://doi.org/10.1038/s41467-021-26396-4openalex-snapshot
Middle Ordovician astrochronology decouples asteroid breakup from glacially-induced biotic radiations
inferred← citeshttps://doi.org/10.1038/s41561-017-0024-1openalex-snapshot
Ordovician oxygen and biodiversity
inferred← citeshttps://doi.org/10.1038/s41561-023-01287-zopenalex-snapshot
Oxygenation of the Baltoscandian shelf linked to Ordovician biodiversification
inferred← citeshttps://doi.org/10.1038/s41597-022-01826-0openalex-snapshot
The PhanSST global database of Phanerozoic sea surface temperature proxy data
inferred← citeshttps://doi.org/10.1038/s41598-022-07822-zopenalex-snapshot
Contrasting Early Ordovician assembly patterns highlight the complex initial stages of the Ordovician Radiation
inferred← citeshttps://doi.org/10.1038/s43247-022-00548-wopenalex-snapshot
Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1073/pnas.1821123116openalex-snapshot
Cascading trend of Early Paleozoic marine radiations paused by Late Ordovician extinctions
inferred← citeshttps://doi.org/10.1073/pnas.2013083118openalex-snapshot
A high-resolution record of early Paleozoic climate
inferred← citeshttps://doi.org/10.1073/pnas.2400434121openalex-snapshot
Reconstruction of Phanerozoic climate using carbonate clumped isotopes and implications for the oxygen isotopic composition of seawater
inferred← citeshttps://doi.org/10.1080/11035897.2016.1181102openalex-snapshot
Darriwilian (Middle Ordovician) worms of southern Sweden
inferred← citeshttps://doi.org/10.1080/11035897.2017.1291538openalex-snapshot
Megascopic processes reflected in the microscopic realm: sedimentary and biotic dynamics of the Middle Ordovician “orthoceratite limestone” at Kinnekulle, Sweden
inferred← citeshttps://doi.org/10.1080/11035897.2018.1435561openalex-snapshot
Conodont biostratigraphy and carbon isotope stratigraphy of the Middle Ordovician (Darriwilian) Komstad Limestone, southern Sweden
inferred← citeshttps://doi.org/10.1080/14772019.2022.2042408openalex-snapshot
The Ordovician diversification of sea urchins: systematics of the Bothriocidaroida (Echinodermata: Echinoidea)
inferred← citeshttps://doi.org/10.1080/14772019.2023.2234929openalex-snapshot
Stromatoporoids of the Katian (Upper Ordovician) Beiguoshan Formation, North China
inferred← citeshttps://doi.org/10.1098/rspb.2021.1450openalex-snapshot
An early burst in brachiopod evolution corresponding with significant climatic shifts during the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1101/2025.09.11.673971openalex-snapshot
Mass Extinction Triggered the Early Radiations of Jawed Vertebrates and Relatives (Gnathostomes)
inferred← citeshttps://doi.org/10.1111/1755-6724.14257openalex-snapshot
Multiple Stratigraphy Study of the Ordovicianin SW Ordos, China
inferred← citeshttps://doi.org/10.1111/1755-6724.70033openalex-snapshot
Palaeoenvironmental Evolution During the Darriwilian Age in the Lower Yangtze Region (South China) and its Controls on Enrichment of Organic Matter
inferred← citeshttps://doi.org/10.1111/brv.12456openalex-snapshot
Climate‐driven ecological stability as a globally shared cause of Late Quaternary megafaunal extinctions: the Plaids and Stripes Hypothesis
inferred← citeshttps://doi.org/10.1111/ggr.12308openalex-snapshot
Determination of Radiogenic 87 Sr/ 86 Sr and Stable δ 88/86 Sr SRM987 Isotope Values of Thirteen Mineral, Vegetal and Animal Reference Materials by DS‐TIMS
inferred← citeshttps://doi.org/10.1111/iar.70052openalex-snapshot
A Well‐Constrained Middle Darriwilian Isotopic Carbon Excursion ( MDICE ) in South China and Its Global Implications
inferred← citeshttps://doi.org/10.1111/let.12197openalex-snapshot
The Bohemo‐Iberian regional chronostratigraphical scale for the Ordovician System and palaeontological correlations within South Gondwana
inferred← citeshttps://doi.org/10.1111/let.12216openalex-snapshot
Reprint of: The Bohemo-Iberian regional chronostratigraphical scale for the Ordovician System and palaeontological correlations within South Gondwana
inferred← citeshttps://doi.org/10.1111/let.12232openalex-snapshot
How is biodiversity produced? Examining speciation processes during the GOBE
inferred← citeshttps://doi.org/10.1111/let.12233openalex-snapshot
Ecological revolution of Oklahoma's rhynchonelliform brachiopod fauna during the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1111/let.12238openalex-snapshot
A Gondwanan perspective on the Ordovician Radiation constrains its temporal duration and suggests first wave of speciation, fuelled by Cambrian clades
inferred← citeshttps://doi.org/10.1111/let.12252openalex-snapshot
The Hirnantian (Late Ordovician) and end-Guadalupian (Middle Permian) mass-extinction events compared
inferred← citeshttps://doi.org/10.1111/let.12259openalex-snapshot
The Great Ordovician Biodiversification Event (GOBE): definition, concept and duration
inferred← citeshttps://doi.org/10.1111/let.12307openalex-snapshot
Lower–Middle Ordovician carbon and oxygen isotope chemostratigraphy at Hällekis, Sweden: implications for regional to global correlation and palaeoenvironmental development
inferred← citeshttps://doi.org/10.1111/pala.12303openalex-snapshot
Early Middle Ordovician scolecodonts from north‐western Argentina and the emergence of labidognath polychaete jaw apparatuses
inferred← citeshttps://doi.org/10.1111/pala.12348openalex-snapshot
Baltoscandian conodont biofacies fluctuations and their link to Middle Ordovician (Darriwilian) global cooling
inferred← citeshttps://doi.org/10.1111/pala.12489openalex-snapshot
Did hard substrate taxa diversify prior to the Great Ordovician Biodiversification Event?
inferred← citeshttps://doi.org/10.1111/pala.70010openalex-snapshot
Diversification and disparity in a major Palaeozoic clade of Brachiopoda: the rise and fall of the Plectambonitoidea
inferred← citeshttps://doi.org/10.1111/sed.12957openalex-snapshot
Middle Ordovician bottom current deposits in the western margin of the North China craton: Evidence from sedimentary and magnetic fabrics
inferred← citeshttps://doi.org/10.1126/sciadv.aax4184openalex-snapshot
An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body
inferred← citeshttps://doi.org/10.1126/sciadv.abd6709openalex-snapshot
Truncated bimodal latitudinal diversity gradient in early Paleozoic phytoplankton
inferred← citeshttps://doi.org/10.1126/sciadv.aeb2297openalex-snapshot
Mass extinction triggered the early radiations of jawed vertebrates and their jawless relatives (gnathostomes)
inferred← citeshttps://doi.org/10.1130/2020.2545(01)openalex-snapshot
Upper Ordovician Juniata Formation, Central Appalachian Basin, USA: A record of Milankovitch-forced eustatic oscillations originating from glaciations in polar Gondwana
inferred← citeshttps://doi.org/10.1130/abs/2020am-354845openalex-snapshot
OCEAN TEMPERATURES IN THE LATE ORDOVICIAN: A CLUMPED ISOTOPE STUDY OF BRACHIOPODS AND CEMENTS
inferred← citeshttps://doi.org/10.1130/abs/2020am-355924openalex-snapshot
ESTIMATING DISPERSAL AND EVOLUTIONARY DYNAMICS IN DIPLOPORAN BLASTOZOANS (ECHINODERMATA) ACROSS THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT
inferred← citeshttps://doi.org/10.1130/abs/2021am-366710openalex-snapshot
AN EARLY BURST IN BRACHIOPOD EVOLUTION CORRESPONDING WITH SIGNIFICANT CLIMATIC SHIFTS DURING THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT
inferred← citeshttps://doi.org/10.1130/b38311.1openalex-snapshot
High-resolution integrated conodont biostratigraphy and carbon isotope (δ13Ccarb) chemostratigraphy of the Ordovician of Sweden, with comparison to South China and North America
inferred← citeshttps://doi.org/10.1130/focus082017.1openalex-snapshot
Silicate weathering, volcanic degassing, and the climate tug of war
inferred← citeshttps://doi.org/10.1130/g38083.1openalex-snapshot
Synchronous diversification of Laurentian and Baltic rhynchonelliform brachiopods: Implications for regional versus global triggers of the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1130/g39587.1openalex-snapshot
Changes in the latitudinal diversity gradient during the Great Ordovician Biodiversification Event
inferred← citeshttps://doi.org/10.1130/g40189.1openalex-snapshot
A sea-level fingerprint of the Late Ordovician ice-sheet collapse
inferred← citeshttps://doi.org/10.1130/g45302.1openalex-snapshot
Equatorial cold-water tongue in the Late Ordovician
inferred← citeshttps://doi.org/10.1130/g49860.1openalex-snapshot
Nd isotopic evidence for enhanced mafic weathering leading to Ordovician cooling
inferred← citeshttps://doi.org/10.1130/g52533.1openalex-snapshot
Cryophilic polychaetes at the subtropical Laurentian margin of the Iapetus Ocean: Evidence for cold-water ocean circulation and upwelling
inferred← citeshttps://doi.org/10.1130/g53374.1openalex-snapshot
Upwelling-related ferruginous ooids, microbialites, and the Darriwilian tipping point of Ordovician climate
inferred← citeshttps://doi.org/10.1130/geol.s.19579441openalex-snapshot
Supplemental Material: Nd isotopic evidence for enhanced mafic weathering leading to Ordovician cooling
inferred← citeshttps://doi.org/10.1130/geol.s.19579441.v1openalex-snapshot
Supplemental Material: Nd isotopic evidence for enhanced mafic weathering leading to Ordovician cooling
inferred← citeshttps://doi.org/10.1134/s0024490226600055openalex-snapshot
The C–O Isotope Geochemistry and Chemostratigraphic Correlation of Ordovician Deposits of the Lisino-10 Borehole Section, Northwestern Russian Plate
inferred← citeshttps://doi.org/10.1139/cjes-2019-0141openalex-snapshot
Early–Middle Ordovician brachiopod diversification in the middle Yangtze region of South China
inferred← citeshttps://doi.org/10.1139/cjes-2024-0074openalex-snapshot
An unusual strophomenide brachiopod association in the Late Ordovician William Lake Lagerstätte, Williams Member of the Stony Mountain Formation (latest Katian), Manitoba
inferred← citeshttps://doi.org/10.1144/jgs2021-148openalex-snapshot
A new high-resolution palaeotemperature record during the Middle–Late Ordovician transition derived from conodont δ 18 O palaeothermometry
inferred← citeshttps://doi.org/10.1144/jgs2023-078openalex-snapshot
Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling
inferred← citeshttps://doi.org/10.1144/jgs2024-290openalex-snapshot
Hirnantian (Late Ordovician) through Aeronian (Llandovery, early Silurian) conodonts from the Whippoorwill, Brassfield and golden Brassfield formations of the North American Midwest Basins and Arches region, USA
inferred← citeshttps://doi.org/10.1144/sp450.5openalex-snapshot
Permian strontium isotope stratigraphy
inferred← citeshttps://doi.org/10.1144/sp485.3openalex-snapshot
A synopsis of Late Ordovician brachiopod diversity in the Anti-Atlas, Morocco
inferred← citeshttps://doi.org/10.1144/sp532-2022-1openalex-snapshot
The Ordovician ocean circulation: a modern synthesis based on data and models
inferred← citeshttps://doi.org/10.1144/sp532-2022-141openalex-snapshot
Ordovician of the Eastern Baltic palaeobasin and the Tornquist Sea margin of Baltica
inferred← citeshttps://doi.org/10.1144/sp532-2022-157openalex-snapshot
The Ordovician of Scandinavia: a revised regional stage classification
inferred← citeshttps://doi.org/10.1144/sp532-2022-168openalex-snapshot
Changing palaeobiogeography during the Ordovician Period
inferred← citeshttps://doi.org/10.1144/sp532-2022-258openalex-snapshot
Seawater signatures of Ordovician climate and environment
inferred← citeshttps://doi.org/10.1144/sp533-2022-128openalex-snapshot
Regional synthesis of the Ordovician geology and stratigraphy of China
inferred← citeshttps://doi.org/10.1144/sp533-2022-149openalex-snapshot
The Ordovician of the Middle East (Iran, Afghanistan, Pakistan)
inferred← citeshttps://doi.org/10.1360/tb-2021-0535openalex-snapshot
Geological evidences and mechanisms for oceanic anoxic events during the Early Paleozoic
inferred← citeshttps://doi.org/10.14770/jgsk.2016.52.6.917openalex-snapshot
A review of the middle Darriwilian carbon isotope excursion, Middle Ordovician
inferred← citeshttps://doi.org/10.1556/2065.186.2025.3.18openalex-snapshot
GOBE, a nagy ordovíciumi biodiverzitási esemény – a földi élővilág lenyűgöző diverzitásnövekedése
inferred← citeshttps://doi.org/10.18261/let.56.3.7openalex-snapshot
Cambrian and Ordovician diversity fluctuations could be resolved through a single ecological hypothesis
inferred← citeshttps://doi.org/10.18261/let.59.2.0openalex-snapshot
New data on high-latitude ecosystems from the Early Ordovician Cabrières Biota, France
inferred← citeshttps://doi.org/10.18261/let.59.4.5openalex-snapshot
Biogeographical patterns and ecological differentiation of Olenidae across the Cambrian-Ordovician transition
inferred← citeshttps://doi.org/10.2110/palo.2018.031openalex-snapshot
EXTREME HEAT IN THE EARLY ORDOVICIAN
inferred← citeshttps://doi.org/10.2139/ssrn.5258508openalex-snapshot
Atmospheric Oxygen and Paleotemperature in the Paleozoic and Triassic
inferred← citeshttps://doi.org/10.2205/2024es000946openalex-snapshot
Late Middle to Late Ordovician Phosphate Accumulation of the Moyero River Section (Siberia): A Record of Upwelling and Global Cooling
inferred← citeshttps://doi.org/10.2517/2021pr001openalex-snapshot
The Great Ordovician Biodiversification Event (GOBE) is Not a Single Event
inferred← citeshttps://doi.org/10.26879/729openalex-snapshot
RNames, a stratigraphical database designed for the statistical analysis of fossil occurrences – the Ordovician diversification as a case study
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