KnowraSnowball EarthLinked fromLinked fromThe 26 pages that link to Snowball Earth, each with the reason it gives.All 26Broader topic 4Related 16Narrower topic 2Compared with 4Great Oxidation EventRelated: A proposed oxygen-related decline in greenhouse methane may have helped trigger early global cooling.AlbedoRelated: Extensive bright ice could have increased planetary albedo and reinforced global cooling.Isotope geochemistryRelated: Carbon and oxygen isotope patterns in glacial-era rocks inform reconstructions of these episodes.GeologyRelated: Geological evidence continues to refine the timing, extent, and causes of these glaciations.RodiniaRelated: Rodinia’s fragmentation has been proposed as one influence on the climate shifts behind these glaciations.Supercontinent cycleRelated: Rodsinia's low-latitude position and enhanced weathering are leading triggers proposed for the Cryogenian glaciations.Rare Earth hypothesisRelated: Global glaciations illustrate how climate instability can sharply constrain life, even on a habitable planet.Great FilterRelated: Severe climate disruption illustrates environmental hazards that life may have to survive.Oxygenation of Earth's atmosphereRelated: Some hypotheses connect oxygenation-related changes in methane to global cooling.ProterozoicRelated: Cryogenian glaciations radically altered Proterozoic climate and ocean chemistry.History of geologyRelated: Its disputed evidence reveals the difficulty of interpreting ancient climate from rocks.NeoproterozoicRelated: Neoproterozoic deposits record glaciations severe enough to motivate this hypothesis.Sturtian glaciationRelated: The Sturtian is a leading candidate for a Cryogenian near-global glaciation.History of lifeRelated: Its possible effects on survival and diversification of early complex life remain under study.Geological history of EarthRelated: Glacial deposits support extreme climate episodes, while their full extent remains disputed.Geological history of oxygenRelated: Oxygenation and carbon-cycle changes have been proposed as factors in Neoproterozoic glaciations.
KnowraSnowball EarthLinked fromLinked fromThe 26 pages that link to Snowball Earth, each with the reason it gives.All 26Broader topic 4Related 16Narrower topic 2Compared with 4Great Oxidation EventRelated: A proposed oxygen-related decline in greenhouse methane may have helped trigger early global cooling.AlbedoRelated: Extensive bright ice could have increased planetary albedo and reinforced global cooling.Isotope geochemistryRelated: Carbon and oxygen isotope patterns in glacial-era rocks inform reconstructions of these episodes.GeologyRelated: Geological evidence continues to refine the timing, extent, and causes of these glaciations.RodiniaRelated: Rodinia’s fragmentation has been proposed as one influence on the climate shifts behind these glaciations.Supercontinent cycleRelated: Rodsinia's low-latitude position and enhanced weathering are leading triggers proposed for the Cryogenian glaciations.Rare Earth hypothesisRelated: Global glaciations illustrate how climate instability can sharply constrain life, even on a habitable planet.Great FilterRelated: Severe climate disruption illustrates environmental hazards that life may have to survive.Oxygenation of Earth's atmosphereRelated: Some hypotheses connect oxygenation-related changes in methane to global cooling.ProterozoicRelated: Cryogenian glaciations radically altered Proterozoic climate and ocean chemistry.History of geologyRelated: Its disputed evidence reveals the difficulty of interpreting ancient climate from rocks.NeoproterozoicRelated: Neoproterozoic deposits record glaciations severe enough to motivate this hypothesis.Sturtian glaciationRelated: The Sturtian is a leading candidate for a Cryogenian near-global glaciation.History of lifeRelated: Its possible effects on survival and diversification of early complex life remain under study.Geological history of EarthRelated: Glacial deposits support extreme climate episodes, while their full extent remains disputed.Geological history of oxygenRelated: Oxygenation and carbon-cycle changes have been proposed as factors in Neoproterozoic glaciations.