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- McGhee et al. (2013), a paper which primarily focused on ecological effects of mass extinctions, also published new estimates of extinction severity based on Alroy’s methods. Many extinctions were significantly more impactful under these new estimates, though some were less prominent.[43] - Source: Internet
- A 2008 study, published in the journal Nature, established a relationship between the speed of mass extinction events and changes in sea level and sediment.[108] The study suggests changes in ocean environments related to sea level exert a driving influence on rates of extinction, and generally determine the composition of life in the oceans.[109] - Source: Internet
- It may be necessary to consider combinations of causes. For example, the marine aspect of the end-Cretaceous extinction appears to have been caused by several processes that partially overlapped in time and may have had different levels of significance in different parts of the world.[92] - Source: Internet
- Another theory is that the creation of the super-continent Pangaea contributed to the End-Permian mass extinction. Pangaea was almost fully formed at the transition from mid-Permian to late-Permian, and the “Marine genus diversity” diagram at the top of this article shows a level of extinction starting at that time, which might have qualified for inclusion in the “Big Five” if it were not overshadowed by the “Great Dying” at the end of the Permian.[133] - Source: Internet
- Alroy also elaborated on three-timer algorithms, which are meant to counteract biases in estimates of extinction and origination rates. A given taxon is a “three-timer” if it can be found before, after, and within a given time interval, and a “two-timer” if it overlaps with a time interval on one side. Counting “three-timers” and “two-timers” on either end of a time interval, and sampling time intervals in sequence, can together be combined into equations to predict extinction and origination with less bias.[64] In subsequent papers, Alroy continued to refine his equations to improve lingering issues with precision and unusual samples.[65][66] - Source: Internet
- Germany is a top exporter of vehicles, machinery, chemicals, and other manufactured goods and has a highly skilled workforce. Germany, however, faces some demographic challenges to its economic growth. Its low fertility rate makes replacing its aging workforce more difficult, and its high levels of net immigration strain its social welfare system. - Source: Internet
- In a landmark paper published in 1982, Jack Sepkoski and David M. Raup identified five mass extinctions.[2] They were originally identified as outliers to a general trend of decreasing extinction rates during the Phanerozoic,[3] but as more stringent statistical tests have been applied to the accumulating data, it has been established that multicellular animal life has experienced five major and many minor mass extinctions.[4] The “Big Five” cannot be so clearly defined, but rather appear to represent the largest (or some of the largest) of a relatively smooth continuum of extinction events.[3] An earlier (first) event at the end of the Ediacaran is speculated [5] - Source: Internet
- The eventual warming and expanding of the Sun, combined with the eventual decline of atmospheric carbon dioxide, could actually cause an even greater mass extinction, having the potential to wipe out even microbes (in other words, the Earth would be completely sterilized): rising global temperatures caused by the expanding Sun would gradually increase the rate of weathering, which would in turn remove more and more CO 2 from the atmosphere. When CO 2 levels get too low (perhaps at 50 ppm), most plant life will die out, although simpler plants like grasses and mosses can survive much longer, until CO 2 levels drop to 10 ppm.[135][136] - Source: Internet
- The bio-availability of essential trace elements (in particular selenium) to potentially lethal lows has been shown to coincide with, and likely have contributed to, at least three mass extinction events in the oceans, that is, at the end of the Ordovician, during the Middle and Late Devonian, and at the end of the Triassic. During periods of low oxygen concentrations very soluble selenate (Se6+) is converted into much less soluble selenide (Se2-), elemental Se and organo-selenium complexes. Bio-availability of selenium during these extinction events dropped to about 1% of the current oceanic concentration, a level that has been proven lethal to many extant organisms.[127] - Source: Internet
- Clathrates are composites in which a lattice of one substance forms a cage around another. Methane clathrates (in which water molecules are the cage) form on continental shelves. These clathrates are likely to break up rapidly and release the methane if the temperature rises quickly or the pressure on them drops quickly—for example in response to sudden global warming or a sudden drop in sea level or even earthquakes. Methane is a much more powerful greenhouse gas than carbon dioxide, so a methane eruption (“clathrate gun”) could cause rapid global warming or make it much more severe if the eruption was itself caused by global warming. - Source: Internet
- These are often clearly marked by worldwide sequences of contemporaneous sediments that show all or part of a transition from sea-bed to tidal zone to beach to dry land – and where there is no evidence that the rocks in the relevant areas were raised by geological processes such as orogeny. Sea-level falls could reduce the continental shelf area (the most productive part of the oceans) sufficiently to cause a marine mass extinction, and could disrupt weather patterns enough to cause extinctions on land. But sea-level falls are very probably the result of other events, such as sustained global cooling or the sinking of the mid-ocean ridges. - Source: Internet
- Sepkoski formally published his marine genera compendium in 2002, prompting a new wave of studies into the dynamics of mass extinctions.[40] These papers utilized the compendium to track origination rates (the rate that new species appear or speciate) parallel to extinction rates in the context of geological stages or substages. A review and re-analysis of Sepkoski’s data by Bambach (2006) identified 18 distinct mass extinction intervals, including 4 in the Cambrian. These fit Sepkoski’s definition of extinction, as short substages with large diversity loss and overall high extinction rates relative to their surroundings.[42] - Source: Internet
- But Wignall (2001) concluded that only five of the major extinctions coincided with flood basalt eruptions and that the main phase of extinctions started before the eruptions. Sea-level falls: 12, of which seven were associated with significant extinctions. [e] - Source: Internet
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