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  2. Acute respiratory distress syndrome - Wikipedia

    en.wikipedia.org/wiki/Acute_respiratory_distress...

    Adult diagnosis is based on a PaO 2 /FiO 2 ratio (ratio of partial pressure arterial oxygen and fraction of inspired oxygen) of less than 300 mm Hg despite a positive end-expiratory pressure (PEEP) of more than 5 cm H 2 O. [1] Cardiogenic pulmonary edema, as the cause, must be excluded. [4]

  3. Infant respiratory distress syndrome - Wikipedia

    en.wikipedia.org/wiki/Infant_respiratory...

    Infant respiratory distress syndrome (IRDS), also known as surfactant deficiency disorder (SDD), [2] and previously called hyaline membrane disease (HMD), is a syndrome in premature infants caused by developmental insufficiency of pulmonary surfactant production and structural immaturity in the lungs.

  4. Extinction event - Wikipedia

    en.wikipedia.org/wiki/Extinction_event

    The scientific consensus is that the main cause of the End-Permian extinction event was the large amount of carbon dioxide emitted by the volcanic eruptions that created the Siberian Traps, which elevated global temperatures. The formation of large igneous provinces by flood basalt events could have:

  5. Cretaceous–Paleogene extinction event - Wikipedia

    en.wikipedia.org/wiki/Cretaceous–Paleogene...

    It marked the end of the Cretaceous period, and with it the Mesozoic era, while heralding the beginning of the current era, the Cenozoic. In the geologic record, the K–Pg event is marked by a thin layer of sediment called the K–Pg boundary, Fatkito boundary or K–T boundary, which can be found throughout the world in marine and terrestrial ...

  6. Timeline of Cretaceous–Paleogene extinction event research

    en.wikipedia.org/wiki/Timeline_of_Cretaceous...

    June 6th: Alvarez and others published their hypothesis that an impact event cause the extinction of the dinosaurs. [40] Penfield wrote to Walter Alvarez, suggesting the Yucatan structure as the possible crater of the end-Cretaceous impactor, but received no response. [24] The spore-bearing structures of a modern fern. 1981

  7. Capitanian mass extinction event - Wikipedia

    en.wikipedia.org/wiki/Capitanian_mass_extinction...

    The impact of the Capitanian extinction event on marine ecosystems is still heavily debated by palaeontologists. Early estimates indicated a loss of marine invertebrate genera between 35 and 47%, [15] [16] while an estimate published in 2016 suggested a loss of 33–35% of marine genera when corrected for background extinction, the Signor–Lipps effect and clustering of extinctions in certain ...

  8. Near-death experience - Wikipedia

    en.wikipedia.org/wiki/Near-death_experience

    Another psychological theory is called the expectancy model. It has been suggested that although these experiences could appear very real, they had actually been constructed in the mind, either consciously or subconsciously, in response to the stress of an encounter with death (or perceived encounter with death), and did not correspond to a ...

  9. Cambrian–Ordovician extinction event - Wikipedia

    en.wikipedia.org/wiki/Cambrian–Ordovician...

    Volcanic activity, particularly that of large igneous provinces, has been speculated to have been the cause of the environmental crisis. [3] The emplacement of the Namaqualand–Garies dykes in South Africa has been dated to 485 mya, the time at which the Cambrian–Ordovician extinction event occurred, although there remains no unambiguous evidence of a causal relationship between this ...