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HYPERTHERMAL EVENT

  • Hyperthermal event
  • Sudden warming of the planet on a geologic time scale

    A hyperthermal event corresponds to a sudden warming of the planet on a geologic time scale. The consequences of this type of event are the subject of

    Hyperthermal event

    Hyperthermal event

    Hyperthermal_event

  • Latest Danian Event
  • Hyperthermal event at the end of the Danian stage

    The Latest Danian Event (LDE) was a hyperthermal event that occurred at the end of the Danian age. The LDE is believed to have lasted around 200,000 years

    Latest Danian Event

    Latest_Danian_Event

  • Paleocene–Eocene thermal maximum
  • Global warming about 55 million years ago

    Earth. Other hyperthermals clearly occurred around 53.7 million years ago (now called ETM-2 and also referred to as H-1, or the Elmo event) and around

    Paleocene–Eocene thermal maximum

    Paleocene–Eocene thermal maximum

    Paleocene–Eocene_thermal_maximum

  • Permian–Triassic extinction event
  • Earth's most severe extinction event

    evolution of carbonate platforms during the Permian–Triassic boundary hyperthermal event". Palaeogeography, Palaeoclimatology, Palaeoecology. 654 112455. Bibcode:2024PPP

    Permian–Triassic extinction event

    Permian–Triassic extinction event

    Permian–Triassic_extinction_event

  • Weissert Event
  • Hyperthermal event during the Early Cretaceous epoch

    The Weissert Event, also referred to as the Weissert Thermal Excursion (WTX), was a hyperthermal event that occurred in the Valanginian stage of the Early

    Weissert Event

    Weissert_Event

  • Eocene Thermal Maximum 3
  • Hyperthermal event

    Eocene Thermal Maximum 3 (ETM3), also known as the K or X event, was a hyperthermal event that occurred during the middle of the Ypresian stage of the

    Eocene Thermal Maximum 3

    Eocene_Thermal_Maximum_3

  • Toarcian Oceanic Anoxic Event
  • Largest anoxic event in the Jurassic period and Phanerozoic eon

    "Extinction cascades, community collapse, and recovery across a Mesozoic hyperthermal event". Nature Communications. 15 (1): 8599. Bibcode:2024NatCo..15.8599D

    Toarcian Oceanic Anoxic Event

    Toarcian_Oceanic_Anoxic_Event

  • Late Lutetian Thermal Maximum
  • Late Lutetian Thermal Maximum (LLTM), also known as the C19r Event, was a hyperthermal event that occurred during the Lutetian epoch. The LLTM occurred

    Late Lutetian Thermal Maximum

    Late_Lutetian_Thermal_Maximum

  • Faraoni Thermal Excursion
  • Hyperthermal event during the Early Cretaceous

    The Faraoni Thermal Excursion (FTX) was a hyperthermal event that occurred during the Hauterivian stage of the Early Cretaceous period, being induced by

    Faraoni Thermal Excursion

    Faraoni_Thermal_Excursion

  • 2026 in paleobotany
  • palynofloral assemblage indicative of ecological stress during the Toarcian hyperthermal event, is published by Galasso, Foster & van de Schootbrugge (2026). Yang

    2026 in paleobotany

    2026_in_paleobotany

  • Dissacus
  • Genus of extinct mammals

    faunivore that consumed relatively few bones. During and after the hyperthermal event, dental microwear patterns resembled more of lions and bone-crunching

    Dissacus

    Dissacus

    Dissacus

  • Eocene Thermal Maximum 2
  • Transient period of global warming that occurred approximately 54 million years ago

    of global warming that occurred around 54 Ma. It was the second major hyperthermal that punctuated long-term warming from the Late Paleocene through the

    Eocene Thermal Maximum 2

    Eocene_Thermal_Maximum_2

  • Danian
  • First age of the Paleocene Epoch

    Danian age. Close to the end of the Danian, around 62.2 Ma, occurred a hyperthermal, similar to but smaller in magnitude compared to the more famous Palaeocene-Eocene

    Danian

    Danian

  • Paleocene
  • First epoch of the Paleogene Period

    "Long-term resilience decline in plant ecosystems across the Danian Dan-C2 hyperthermal event, Boltysh crater, Ukraine". Journal of the Geological Society. 172

    Paleocene

    Paleocene

    Paleocene

  • Background extinction rate
  • Standard rate of extinction

    years. These species face extinction in cases of glaciation events, hyperthermal events, and climate change.[citation needed] Cenozoic Bivalves: These

    Background extinction rate

    Background_extinction_rate

  • Sinsk Event
  • which probably released large volumes of volcanic CO₂ and triggered a hyperthermal interval, promoting ocean warming and deoxygenation. An additional tectonic

    Sinsk Event

    Sinsk_Event

  • Ostrea jibananandai
  • Extinct species of mollusc

    evolutionary flexibility, is believed to have evolved in response to the hyperthermal events of the Early Eocene. Halder, Kalyan; Mitra, Aniket (2021). "Facultative

    Ostrea jibananandai

    Ostrea_jibananandai

  • 2021 in paleomalacology
  • accompanying size reduction of belemnites during an Early Jurassic hyperthermal event modulated by life history". Scientific Reports. 11 (1) 14480. Bibcode:2021NatSR

    2021 in paleomalacology

    2021_in_paleomalacology

  • Early Eocene Climatic Optimum
  • Climatic period during the Eocene epoch

    Palaeocene and Early Eocene. It was initiated by a series of intense hyperthermal events in the Early Eocene, including Eocene Thermal Maximum 2 (ETM2) and

    Early Eocene Climatic Optimum

    Early_Eocene_Climatic_Optimum

  • 2026 in paleomalacology
  • evidence indicating that peaks of molluscan biodiversity coincided with hyperthermal events. Bellosi et al. (2026) revise the age and distribution of the molluscan

    2026 in paleomalacology

    2026_in_paleomalacology

  • Magnetofossil
  • Fossils produced by magnetotactic bacteria

    associated with hyperthermal (period of warming, usually between 4-8 degrees Celsius) periods in the Earth's history. These hyperthermal events, such as the

    Magnetofossil

    Magnetofossil

    Magnetofossil

  • 2022 in paleontology
  • temperature estimates across the Eocene Thermal Maximum 2 and the hyperthermal event that occurred approximately 2 million years after the Paleocene–Eocene

    2022 in paleontology

    2022_in_paleontology

  • 2024 in paleontology
  • "Extinction cascades, community collapse, and recovery across a Mesozoic hyperthermal event". Nature Communications. 15 (1). 8599. Bibcode:2024NatCo..15.8599D

    2024 in paleontology

    2024_in_paleontology

  • Waiau Toa / Clarence River
  • River in Canterbury, New Zealand

    Maximum (PETM), Eocene Thermal Maximum 2 (ETM-2), and other Paleogene hyperthermal events. The geography of the Clarence is also affected by New Zealand's

    Waiau Toa / Clarence River

    Waiau Toa / Clarence River

    Waiau_Toa_/_Clarence_River

  • Eocene
  • Second epoch of the Paleogene Period

    analysis of and research into these hyperthermals in the early Eocene has led to hypotheses that the hyperthermals are based on orbital parameters, in

    Eocene

    Eocene

    Eocene

  • Cretaceous
  • Third and last period of the Mesozoic Era

    Thermal Event occurred around 110 Ma, followed shortly by the l'Arboudeyesse Thermal Event a million years later. Following these two hyperthermals was the

    Cretaceous

    Cretaceous

    Cretaceous

  • Giant magnetofossils
  • Microscopic magnetic minerals

    Larrasoana; L. Jovane; A.R. Muxworthy (2012). "Giant Magnetofossils and hyperthermal events". Earth and Planetary Science Letters. 351–352: 258–269. Bibcode:2012E&PSL

    Giant magnetofossils

    Giant magnetofossils

    Giant_magnetofossils

  • 2018 in paleontology
  • are any substantial differences between the hyperthermal events during the Triassic–Jurassic extinction event and Toarcian turnover and the periods of normal

    2018 in paleontology

    2018 in paleontology

    2018_in_paleontology

  • Allison Guyot
  • Seamount in the Pacific Ocean

    (Allison Guyot, ODP Site 865): Greenhouse climate and superimposed hyperthermal events". Paleoceanography. 31 (3): 346–364. Bibcode:2016PalOc..31..346A

    Allison Guyot

    Allison_Guyot

  • 2026 in paleontology
  • undergo significant changes of composition during those early Eocene hyperthermals that did not result in sea surface temperatures rising more than approximately

    2026 in paleontology

    2026_in_paleontology

  • 2020 in paleontology
  • ~700 thousand years. A study on the impact of the early Cenozoic hyperthermal events on shallow marine benthic communities, based on data from fossils

    2020 in paleontology

    2020_in_paleontology

  • Ames Research Center
  • NASA research facility in Northern California

    is an advanced thermophysics facility where sustained hypersonic- and hyperthermal testing of vehicular thermoprotective systems takes place under a variety

    Ames Research Center

    Ames Research Center

    Ames_Research_Center

  • Inostrancevia
  • Extinct genus of therapsids

    pone.0089165. PMC 3937355. PMID 24586565. Benton, Michael J. (2018). "Hyperthermal-driven mass extinctions: killing models during the Permian–Triassic mass

    Inostrancevia

    Inostrancevia

    Inostrancevia

  • 2025 in paleontology
  • (2025). "Microbial metabolism amplified warming in three Phanerozoic hyperthermal events". Nature Communications. 16 (1) 11372. Bibcode:2025NatCo..1611372W

    2025 in paleontology

    2025_in_paleontology

  • Gorgonopsia
  • Extinct group of saber-toothed therapsids from the Permian

    1016/j.palaeo.2024.112044. S2CID 267080711. Benton, Michael J. (2018). "Hyperthermal-driven mass extinctions: killing models during the Permian–Triassic mass

    Gorgonopsia

    Gorgonopsia

    Gorgonopsia

  • Saber-toothed predator
  • Group of extinct animals

    1016/j.palaeo.2024.112044. S2CID 267080711. Benton, Michael J. (2018). "Hyperthermal-driven mass extinctions: killing models during the Permian–Triassic mass

    Saber-toothed predator

    Saber-toothed predator

    Saber-toothed_predator

  • Triassic Boreal Ocean Delta Plain
  • Largest known delta plain in Earth's geological history

    google.com. Retrieved 2025-05-27. Benton, Michael J. (2018-09-03). "Hyperthermal-driven mass extinctions: killing models during the Permian–Triassic mass

    Triassic Boreal Ocean Delta Plain

    Triassic Boreal Ocean Delta Plain

    Triassic_Boreal_Ocean_Delta_Plain

  • Pavel Banya
  • Town in Stara Zagora, Bulgaria

    mineralization (low quantity of dry matter per liter, about 2 grams) and hyperthermality – 57 to 59 degrees Celsius at the spring. The water is rich of hydrocarbon

    Pavel Banya

    Pavel Banya

    Pavel_Banya

  • Formiciinae
  • Extinct subfamily of ants

    dispersal of giant thermophilic ants across the Arctic during early Eocene hyperthermals". Proceedings of the Royal Society B. 278 (1725): 3679–86. doi:10.1098/rspb

    Formiciinae

    Formiciinae

    Formiciinae

  • Geology of Cape Town
  • dunes for 90% of the last 2 million years. Warm interglacial periods (hyperthermals), have lasted only about 10 000 years and we are part way through the

    Geology of Cape Town

    Geology of Cape Town

    Geology_of_Cape_Town

  • Neutron capture therapy of cancer
  • Nonsurgical treatment for locally invasive malignant tumors

    RA-6 nuclear reactor in Bariloche. The neutron beam has a mixed thermal-hyperthermal neutron spectrum that can be used to treat superficial tumors. The In-Hospital

    Neutron capture therapy of cancer

    Neutron capture therapy of cancer

    Neutron_capture_therapy_of_cancer

  • 2019 in paleontology
  • survival and proliferation during the late Paleocene and early Eocene hyperthermals". Paleoceanography and Paleoclimatology. 34 (2): 252–274. Bibcode:2019PaPa

    2019 in paleontology

    2019_in_paleontology

  • 2011 in arthropod paleontology
  • dispersal of giant thermophilic ants across the Arctic during early Eocene hyperthermals". Proceedings of the Royal Society B. 278 (1725): 3679–3686. doi:10

    2011 in arthropod paleontology

    2011_in_arthropod_paleontology

  • 2020 in reptile paleontology
  • and their role in understanding the effects of the Permian-Triassic hyperthermal". PeerJ. 8 e10522. doi:10.7717/peerj.10522. PMC 7751423. PMID 33384899

    2020 in reptile paleontology

    2020_in_reptile_paleontology

  • 2023 in paleoentomology
  • (2023). "Eocene giant ants, Arctic intercontinental dispersal, and hyperthermals revisited: discovery of fossil Titanomyrma (Hymenoptera: Formicidae:

    2023 in paleoentomology

    2023_in_paleoentomology

  • Table Mountain National Park Marine Protected Area
  • Marine conservation area around the Cape Peninsula in South Africa

    dunes for 90% of the last 2 million years. Warm interglacial periods (hyperthermals), have lasted only about 10 000 years and we are part way through the

    Table Mountain National Park Marine Protected Area

    Table Mountain National Park Marine Protected Area

    Table_Mountain_National_Park_Marine_Protected_Area

  • 2023 in paleomammalogy
  • Primatomorpha colonized Ellesmere Island (Arctic Canada) during the hyperthermal conditions of the early Eocene climatic optimum". PLOS ONE. 18 (1). e0280114

    2023 in paleomammalogy

    2023_in_paleomammalogy

  • Paleofauna of the Eocene Okanagan Highlands
  • (2023). "Eocene giant ants, Arctic intercontinental dispersal, and hyperthermals revisited: discovery of fossil Titanomyrma (Hymenoptera: Formicidae:

    Paleofauna of the Eocene Okanagan Highlands

    Paleofauna_of_the_Eocene_Okanagan_Highlands

  • Allenby Formation
  • Sedimentary rock formation in British Columbia, Canada

    (2023). "Eocene giant ants, Arctic intercontinental dispersal, and hyperthermals revisited: discovery of fossil Titanomyrma (Hymenoptera: Formicidae:

    Allenby Formation

    Allenby Formation

    Allenby_Formation

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