Talk:Extinction event

references

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Vendian Extinction

What about the extinction that killed the Vendian (precambrian) biota? Should that be included? —Preceding unsigned comment added by Maurajbo (talk • contribs) 15:17, 11 May 2009 (UTC)

K-T Extinction

From the K-T extinction blurb: " including the dinosaurs." I personally feel that the evolutionary lineage of birds from dinosaurs is clear, so feel that this should be amended to say "including the non-avian dinosaurs." I realize that this may be contentious for some, so, before doing so, I wanted to hear what the community felt. Baryonyx 04:25, Sep 28, 2004 (UTC)

Electricity/Industrial Revolution

I didn't notice anyone mention the advent of electricity and the industrial revolution playing very real roles in the acceleroration of such a hypothetical instance as extinction occurring now. As with all else pertaining to the development of society, the advent of electricity and the industrial revolution has hastened the process.... in which ever directions a person chooses to recognize it as having proceded.

The Oxygen Revolution Extinctions

I remember having read about a (widely accepted?) theory that the second (or the first) mass extincting was caused by the development of photsynthesis in the evolution of life: The new organism capable of doing photosynthesis thrived and rapidly increases the abundance of oxygen in the atmosphere from only traces before to several tens of percents as now. As oxygen is highly corrosive (remember: there was no oxidation before) most organism died expect for those that developped protection against oxidation in time.

Does anybody know details? Is this correct? If so there should it go? -- sanders_muc

The original poster is talking about the idea that many of the original microbes of the Earth's early life evolved in the near complete abscene of oxygen in the atmosphere, and hence the oceans. The rise and expansion of the cyanobacteria would have posed a significant evolutionary pressure upon these organisms as oxygen began to increase in the oceans and in the atmosphere. It is believed that the Oxygen Revolution, as the buildup of oxygen during the Archean and Proterozoic is called, would have led to the extinction of organisms that could not cope with this oxygen-rich world, at least those that did not successfully move to anoxic areas or adapt. I have not seen it cited as counting as one of the Big Five, though. I would argue that it is an evolutionarily significant extinction: even if not Big Five material, it marks an important change in the history of life. As such, it probably merits mention.Baryonyx 04:25, Sep 28, 2004 (UTC)

The Sixth Mass Extinction?

Some people claim that we are living in the middle of another, man-made extinction event right now. However, humanity's effects are trivia compared with the extinction events shown in the fossil record.

Is that a fact? I've seen estimates on damage that are comparable to the smaller or intermediate sized mass extinctions, if nothing like the boundaries that end the Mesozoic and Palaeozoic eras.

If those are the same estimates that I've seen -- that something like 50,000 species a year are dying out -- they are not particularly reliable. The ones I've seen have all been created by organizations like the Sierra Club and people like Al Gore and Paul Ehrlich who have large, flaming political agenda that such figures are constructed to support. Over the past 500 years, almost 90 per cent of the forest along the Atlantic coast of Brazil has been cleared. However, no one has found a single known species that could be declared extinct. According to the "mass extinction" figures, about half the known species in that Brazilian forest should have been lost.

But if you can cite figures commonly accepted by paleontologists -- figures that, say, appeared in a peer-reviewed journal -- feel free to enter them! --The Epopt

Do a search for something like "current mass extinction" in google, and you will find a great number of hits, including articles in Nature and Science. It looks to me like the mass extinction view is closer to a consensus than to a minority of politically motivated views. At the very least there is enough here to remove the sentence from the article, which I'm doing.

We should move this discussion to Holocene extinction event anyway.

It should also be noted that some scientists have begun to refer to the period from 18th century forward as a new geological epoch, the Anthropocene, mainly because of the impact we are having on the planet. It is by no means in common use though, but wanted to note it.Baryonyx 04:25, Sep 28, 2004 (UTC)

So, do we actually have a common unbiased point of view that there is, in fact, another extinction event currently going on? If so, is there a wikipedia entry or other material we could link to? Because I, frankly, remain skeptical and would like to see more scientific evidence (on both sides of the argument). Cema 22:39, 12 Nov 2004 (UTC)

At present (Dec 2006) the "Holocene extinction" gets more space in this article than the P-Tr and K-T extinctions, which is ridiculous. A lot of the material about the debate and evidence should be moved to Holocene extinction event. My own inclination would be to qualify the "Holocene extinction" in this article as "suggested", because it appears from Holocene extinction event that a different method is being used to assess its severity (attempting to allow for undocumented extinctions) and that this method is likely to produce a higher extinction rate than the traditional fossil-counting method.Philcha 13:36, 8 December 2006 (UTC)

strongly disagree with philcha's comments. Holocene should not be watered down with words like "suggested". this is one article we ont need more weasel words. as for the coverage i think we need more coverage of Holocene in this article, not less. Anlace 15:08, 8 December 2006 (UTC)

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Recently, 24.7.97.222 removed this section:

Other scientists view this estimate as exaggerated, however. For example it can be noted that only 9 species of mammals have gone extinct in North America since Columbus' discovery. Of these, 7 are small rodents [1]. Compared to a background global extinction rate of roughly 2 mammal species per millenia, this is quite high, but probably not enough by itself to make dire predictions about. The most species rich environment on Earth are the rainforest, and their destruction could lead to major losses. However, though 12.5% of the amazon rainforest have been cleared, studies suggest that only a far smaller fraction of its diversity has been destroyed. Because animals and plants can frequently be found in many distant locales within the rainforest, it may be possible to preserve most of the rainforest's diversity in an area 1/3 to 1/2 its original size. Hence conservation efforts may be able to save a majority of these species.

and replaced it with:

A survey by the American Museum of Natural History in 1998 found that the vast majority of biologists agreed with Wilson's assessment, and numerous confirmatory studies in the years since then-- led by the IUCN's annual "Red List" of threatened species-- have now produced a scientific concensus on the subject.[2]

Obviously this is a change in perspective for that section of the article and not one I am entirely happy about. I don't doubt that there is a "mass extinction" ongoing in terms of humanity's reorganization of the environment and ensuing loss of diversity. However, from a paleontological perspective, the extinctions we have caused are no where near the scale of any of the major mass extinctions listed in the article. Maybe our impact could reach that level, but in my honest opinion, most of the near-term dire predictions are grossly overblown. In particular, they frequently apply the species-area relation in a context that has never been empirically verified. In doing so, they predict a number of extinctions based solely on the amount of habitat that was destroyed. However, I have never seen a single field study that concluded that the actual impact even approached the level predicted.

Frankly, this article has a problem in that it only talks about the truly major extinction events, which had profound effects even on global disperse and well-adapted taxa. While the Holocene extinctions might well qualify as a man-made event, to date, they simply aren't in the same category as the major mass extinctions. Perhaps we can discuss extinctions as having a gradiation between local/regional extinction events to those of global scale, and also discuss more of the minor/moderate mass extinctions that have occured in the past. In my opinion, the Holocene extinctions are basically minor so far. Whether they can graduate to major is obviously a matter of debate and should be portrayed as such.

Dragons flight 22:52, Dec 31, 2004 (UTC)

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I'm the one (24.7.97.222) who made the change you just described. Did you look at the reference link I provided?[3] The issue is not the extinctions that humans have caused so far-- it is the extinctions that are about to take place as a result of the staggering growth in human population and consumption over the past two centuries. It is this impending mass extinction that the world's biologists are warning about. And it certainly does rival the great mass extinctions of the past: the most recent estimate I heard at the California Academy of Sciences two weeks ago was that half of all species will be extinct in 50 years-- i.e., twice as fast as E.O. Wilson's estimate.

Check the list in the ref provided by our anonymous poster, it is quite impressive. I've upped the ante a bit by including the current or Holocene extinction event as #7. No doubt some skeptics will be unhappy and probably claim that its all some large, flaming political agenda as someone so eloquently put it earlier. So be it. Vsmith 03:17, 1 Jan 2005 (UTC)

Vsmith, you cited IUCN, without realizing that their own rate estimate of 2300 species extinctions a year predicts the extinction of only 1% of species in the next 50 years. (This compares with Wilson's 27000 - 100000 species extinctions a year, which is certainly on the high side of views held by scientists). Secondly, the 1998 AMNH study only showed that most biologists agreed that the current rate of extinction is historically very high, not that they endorsed Wilson's position. And they are right, a 1% turn over would be phenomenally high since 1% would be more typical of a million years. I don't disagree that the extinction rate is currently enormous. But I don't believe there exists a consensus that the current rate is high enough to lead to a MAJOR mass extinction in the near term.

Wilson holds an extreme position in a field where the scale of the problem is still being actively debated. I will provide more documentation for the more moderate position before updating this further. Dragons flight 03:58, Jan 1, 2005 (UTC)

Dragons flight (this is 24.7.97.222 speaking!): The AMNH study said "The majority (70%) polled think that during the next thirty years as many as one-fifth of all species alive today will become extinct, and one third think that as many as half of all species on the Earth will die out in that time."[4] And the IUCN estimates that one in four mammals, one in three amphibians, and one in eight birds are now threatened with extinction.[5] I don't know where you got your figure for the IUCN estimating "2300 species extinctions a year." Can you give a reference? I don't recall the IUCN ever giving an estimate of the total number of species they believe are going extinct per year-- in fact, they seem to systematically avoid such global estimates, carefully limiting themselves to talking only about the groups of species (mammals, birds, and now amphibians) that they have fully evaluated.

Maybe what you're talking about is the increase of 3,300 threatened species between the 2003 and 2004 Red Lists (from 12,259 to 15,589). However, this figure of 3,300 is not even remotely the total number of species that the IUCN scientists think might be going extinct per year-- it is simply the increase between 2003 and 2004 in the number of species that the IUCN was able to fully evaluate and to conclude are threatened. But the number of species the IUCN has fully evaluated is only a microscopic fraction of the total number of species on earth. As the Executive Summary of the 2004 Red List says, "this figure (15,589) is an underestimate of the total number of threatened species as it is based on an assessment of less than 3% of the world’s 1.9 million described species"[6]-- and even the 1.9 million "described species" are only a small fraction (roughly 10%) of the total number of species on earth, which the IUCN estimates as being between 10 and 30 million.

A good example of how far the figure of 15,589 understates the magnitude of the extinction crisis is found in the fact that the 2004 Red List evaluated only 771 insect species out of the almost 1,000,000 insect species it says have been described[7] (by the way, of these 771 insect species, 559-- 73%-- were found to be threatened). And the 1,000,000 insect species that have been described are only a small fraction of the total number of insect species, which is now estimated at between 4 and 6 million[8]

So let's do the math (just a rough ballpark figure): the IUCN says 15,589 species are threatened, but it has evaluated only 3% of described species-- and described species are only about 10% of the total number of species on earth. So that means the IUCN has evaluated about .3% of the total number of species on earth, and has found that roughly 15,000 of those are threatened with extinction. So if we extrapolate to a ballpark figure, 15,000 X 300 = 4,500,000 species threatened with extinction. Granted that's just a ballpark figure, but the order of magnitude shows why the IUCN scientists and almost every other biologist in the world now think we're facing a mass extinction on the same scale as the other great extinction events in the earth's history.

New edit: Think of processes, of a graph with the numbers of species going down from 100% to 98% over millennia and then rapidly to about 95% in 2000. Then think of the momentum that such a 'system' posesses - to coast along to 90%, to 80%, to 50%, could be easy - do nothing new. The extinction debate should be about what counter forces can Humans begin to apply now so as not only to equal the forces driving extinctions, but to reverse the trend. Only then will the graph bottom out, and a painful, slow recovery begin.

I've made a small 'change of balance' edit and hope to do more. This first point is to reinstate the 'taxonomy' of the sixth extinction. The person who carefully, and I assume factually, records 1/, 2/ ... 6/ and 7/ mass extinction events, with 7/ being the sixth extinction should be - well the word is close to the tip of my tongue )- That person was being devious. I would be grateful to him for removing this confusion from the Article.

I've also removed a line that implied that someone (or more) had received a science research grant to search for a past total extinction! I hope he was alone when he earned his reward. Stanskis 04:10, 12 July 2005 (UTC)

• • • I think there might be a Possible Link between unexplained events such as those experienced in a mass extinction in conjunction with where the sun and local planets lie within their travels across the galactic cycle. The Sun rotates around what we guess is a black hole, or a big bar of stars. we only preceve it as fixed because we have traveled such a short leg of this cycle since the age of scientific discovery. It could be that at points during its 65 million year cycle, that we come close to 'galactic clouds' or pulsars or whatnot, which may be the source of some random elements found in various layers of strata. —Preceding unsigned comment added by 8.15.176.177 (talk) 01:30, 23 August 2008 (UTC)

Other Issues

Out of curiosity, is "extinction event" really the standard biological terminology here? Anyone know where the phrase originated? --Ryguasu 22:31 Dec 2, 2002 (UTC)

Yes "extinction event" is what biologists and geologists use. I don't think there is any special story behind the origin of the term since scientists often speak of "events." --mav

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Although many life forms may become extinct, this does not necessarily imply that all life ceases to exist…

This seems like an awfully weak statement. If I'm not mistaken, no recorded or even theorized extinction event has ever implied that "all life cease[d] to exist". Sure, it could happen, but even a man-made nuclear winter or other catastrophic climate change would probably leave quite a bit of life, even if it destroyed all of our favorite genera. Surely this could be rephrased more meaningfully. -- Jeff Q 04:07, 19 May 2004 (UTC)

I'd vote for it to be removed. The summaries of the extinctions should make this pretty clear. If there really is a need to note this type of sentiment, it should be something more describing the sheer impossibility of wiping out all forms of life, because of life's resilience and the variability already shown on Earth. Remove oxygen... anoxic forms will take over. Nuclear winter? Bacteria, many arthropods, and probably a great deal of deep sea or chemical-processing organisms will be just fine. Hell... blow up the entire planet, and odds are most bacteria will adapt. This comment only begins to address the problem with viewing everything from a megafaunal PoV. Baryonyx 04:25, Sep 28, 2004 (UTC)

Remove verneshot paragraph

I removed the following questionable material. Verneshot is more untested hypothesis or wild speculation than theory. Google search brings up some bizzare sites. Don't think it belongs here.

An even more recent theory, which is still being evaluated, is that periodic large scale vulcanism along continental rifts may include eruption events named verneshots which launch gigatonnes of rock into sub-orbital trajectories. The consequent impacts are expected to have very similar effects to asteroid impacts. This theory explains the periodicity of extinction events as well as the apparently coincidental occurrence of large-scale impacts and vulcanism for at least three of the extinction events without relying on coincidence in the way that the asteroid impact theory does.

Vsmith 15:03, 31 Dec 2004 (UTC)

If this has a good Reference, use it, and the item can stay in place. It's a long-shot theory to help balance peoples' views against the inevitability of the processes that we take for granted as right an proper - CO₂, and all that. Stanskis 04:16, 12 July 2005 (UTC)

We're missing one.

The Eocene Mass Extinction, about 36(?) million years ago. I don't know too many details, but I do know there was a drop in average temperature and a die-off of some mammal groups. Somebody who knows more could fill it in.--Rob117 03:48, 3 September 2005 (UTC)

Missing more than that (though the Eocene is minor on geological time scales). Raup and Sepkoski's Big 5 are End Ordovician, Late Devonian, End Permian, End Triassic, and End Cretaceous. To that one could easily add End Eocene, End Jurassic, End Middle Permian, End Silurian, Middle Carboniferous, Dresbachian (late Cambrian), and Botomanian (middle Cambrian). Depending on which author one chooses to cite there may be more than 20 discernable extinction "events" since the start of the Phanerozoic. Wiki's coverage of extinction events in general is just plain weak (not that I presently have the time to improve it). Dragons flight 05:13, September 3, 2005 (UTC)

Its weak...but you can't do anything about it. Thanks for stopping by. RealityCheck 06:23, 3 September 2005 (UTC)

Timeframes

I have seen various figures for how many years ago each event happened. There seems to be a rough margin of error of about 1 - 3%. And also, some events occured over a few million years, so I think there should be some way to clearly note this on the page. Phaldo December 12, 2005

Extinction events vs Mass extinctions

Geologic time periods and mass extinction events.

I agree with Phaldo that there should be a note in the article drawing attention to the margin of error for estimates of when extinction events occurred. In the External links section, The Sixth Extinction by Niles Eldredge (American Institute of Biological Sciences) puts the dates of the five previous mass extinctions at circa 65, 210, 245, 370 and 440 million years ago. The University of Hawaii's College of Natural Sciences says 65, 208, 245, 360 and 438 mya. A History of the Universe timeline on the University of California's website says 67, 205, 251, 370 and 440 mya. I've also seen a variety of alternative names for the most recent geologic periods. I think these discrepancies should be noted and explained. Non-specialist visitors might feel confused if the article seeks to establish one set of event dates and period/epoch names as difinitive when they've already seen alternative dates and names on other websites which they consider authoritative (universities, encyclopedias).

I found this article after a Google search for info on the five major mass extinctions. I was redirected from Wikipedia's superseded "Mass extinction" article. This article addresses Extinction events in general and includes a list of seven events. I feel there should be a specific section on the five major mass extinctions. I'm not well versed on the subject, which is why I resorted to Wikipedia for a quick summary. There are probably many non-scientists and highschool students who arrive at this article for the same reason.

I was trying to find reliable dates for the five major mass extinctions to include in a chart. I've included the current version of the chart, which I donated to Wikipedia. -- Bookish 12:40, 17 May 2006 (UTC)

Timeline graphic

I just removed Image:MassExtinctionTimeline.png from the article and restored the EasyTimeline version it had replaced. I figured I should elaborate on my reasoning. The EasyTimeline version is much easier to edit, the layout can be customized to different presentation formats (printed versions, for example, or link maps) with arbitrary resolution, and even as it currently stands it's more precice - the image version has a scale marked only at hundred million year intervals whereas the EasyTimeline is set to ten million year intervals. Bryan 07:24, 15 February 2006 (UTC)

Wilkes Land Crater

Added detail on recent report of putative P-T linked crater/mascon finding in Wilkes Land, Antarctica.

Extinction Theory Fallacy

The following text was inserted by [[::User:72.195.144.113|72.195.144.113]] ([[::User talk:72.195.144.113|talk]] · [[::Special:Contributions/72.195.144.113|contribs]]). It is not suitable for a scientific discussion of extinction, but it is cogent and might be suitable for some philosophical or metaphysical article, so I am preserving it here in case anyone knows a suitable place for it. Dragons flight 04:31, 27 June 2006 (UTC)

==Extinction Theory Fallacy==

Certain geotheorists and vitalistic philosophers (vide Buffon, Lamarck, de Luc, Pareto, Sorel, Deleuze, et al) have elaborated theories of eternal life-sustainability or infinite life-resilience in the process of constructing a philosophical problematics of life on earth (vide geosophy). Many of these theories maintain a common speculative or propositional assertion or claim of faith that life in all its manifestations, stages, and permutations is a "permanent integer," an inexpugnable factor in the quanta that envelope, permeate, embody, and constitute all energy. All of these theories contend that all theories of species (as opposed to population) extinction constitute non-malicious fallacies based on the dependence in the biological sciences on empirical proofs of presence or being. These theorists contend that life in its individual instance leaves an eternel, inerradicable, energetic presence-print or residue on the dimensions of time and space, one which grants each cell and thus each creature eternal presence in time and space– essentially eternal life. Such a presence or life would of course not be entirely equatable or identical to the life of, for example, new-born animals, for the simple reason that new-born animals would not have passed through the psychic, systemic, and energetic "trauma" of physical disintegration known as death, but it would nevertheless constitute a continuation of individual presence, not to mention an envolving state of energetic existence, another phase of life. The process of energy utilization would be different in both cases, and this difference would result in post-thanatic (vide thanatos) life being largely removed from and invisible to pre-thanatic life, although it would leave the possibility, if perhaps not the probability, of pre-thanatic life's detection of post-thanatic beings.

A related theory holds that all animals (and one assumes plants) that ever existed from the earliest unicellular life form, to the dinosaurs, to the latest mutant strain of avian flu, continue to exist in some zone or area of the planet and will continue to do so (although perhaps in greatly diminished numbers) until the earth itself ceases to exist. This theory contends that once life assumes a certain form through the processes of evolutionary change that form will eternally abide as an inerradicable part of the biological diversity of the earth through the organism's own undefeatable processes of preservation either as cellular or mitochondrial memory in the body of another organism or by actually finding the most impenetrable enviromental niches permitting its continued survival as a living relic, in certain cases with a relic population consisting of two individuals, or simply a pregnant female or even just a hermaphroditic specimen.

List of doomsday scenarios

Could use votes to save this article, thanks MapleTree 22:26, 28 September 2006 (UTC)

Need to restructure set of pages about mass extinctions

I think the set of pages about mass extinctions needs to be restructured, and in particular detailed discussion of particular extinctions should be removed from the general "mass extinction" page:

• Before I recently edited it, the general "mass extinction page" presented just 1 theory for the P/T and K/T extinctions. i.e. it was not objective.
• Adding further theories about P/T and K/T has made the page too long but the analysis of causes is still superficial and not very objective.
• Meanwhile the page is unbalanced because there's no mention of causes of other extinctions.
• The length of the page and the space taken up by the causes pf particular extinctions squeezes out disussion of other topics and makes it difficult to add other mass extinctions.

Topics that should be added to the general "mass extinction page" include:

• The role of mass extinctions in evolution - competitive displacement of dominant groups appears to be rare and mass extinctions create openings for new or previously obscure groups of organisms. The P/T and K/t extinctions are spectacular examples of this.
• The role of extinctions in evolutionary theory - supporters of punctuated equilibrium place more emphasis on mass extinctions than gradualists do.
• The distinction between mass extinctions that change ecosystems and mass extinctions that simply kill a lot of species. I remember seeing a web page where a researcher argued that the late Devonian extinction(s) did not change the ecosystem. On the other hand the P/T and K/T extinctions did, even more in the seas than on land - before P/T 67% of known marine organisms were sessile, during the Mesozoic 50% were sessile, after K/T only 33% are sessile.
• The related concept of key species (I can't remember if that's the right term) - if a lot of key species die the ecosystem changes, otherwise there's a temporary reduction in species but the ecosystem remains much the same.
• The fact that the background extinction rate appears to have declined over time. Is this real or is it an artefact of e.g. fossilisation or how fossils are discovered?
• The difficulty of deciding whether an extinction was abrupt or gradual because of the Signor-Lipps effect. This is a large feature of debates about the K/T extinction.
• A list of all the proposed mass extinctions, including those whose status is under debate. This provides an opportunity to link to pages about each one, and to invite contributions for those which have no detail pages. One good example is the late Pre-Cambrian extinction which killed off the Ediacaran biota (this one is important for both the history and the theory of evolution - see for example Gould's Wonderful Life).
• A list of hypothetical mass extinctions, i.e. those where we can see adequate causes but have little / no paleontological evidence. For example the O2 extinction and the extinction(s) likely to have been caused by the supercontinent Rodinia.

I also suggest that the "Marine genus diversity" diagram should be reversed - I've seen many presentations with time runing left to right and no other ones with time running right to left, and I think Wikipedia runs the risk of confusing readers if it remains the odd one out. Philcha 07:50, 6 October 2006 (UTC)

I agree, the text you added is much too long and the detail should appear in the specific articles, not here. I do think however, that is there is a leading cause (or causes) then it should be mentioned here, but all the details about what effect it would have or argument about different explanations should be at the subpage not here. Dragons flight 18:27, 6 October 2006 (UTC)

Discussion on end of civilization

Editors input would be appreciated at Talk:End_of_civilization. There seems to be some disagreement what the end of civilization actually means. nirvana2013 17:44, 10 November 2006 (UTC)

Need to include mid-Cambrian (Botomian) extinction

I've seen articles that say this had a major-league extinction percentage, and the "marine biodiversity" diagram agrees with this. It might also be important in terms of biodiversity and ecosystems - I'd have to check how many of the Cambrian explosion's "weird wonders" became extinct.Philcha 14:11, 14 January 2007 (UTC)

Update: Signor thinks a greater % of genera died out than in the end-Permian catastrophe [9], but the main victims appear to have been the small shelly fauna and the archaeocyathids.Philcha 16:44, 21 August 2007 (UTC)

Remove "Magnitude and rate of loss for current extinction"?

This section is in the wrong place within the the article and is as long as all the summaries of past mass extinctions put together. It also looks more like a "talk" item than a contribution to an article, especially the 2 references to Vreugdenhil's blog.

I therefore suggest that the person who added it ([[User:Stevenmitchell | Stevenmitchell) if I've read the history correctly) should move it either to the Holocene extinction event article to to the talk page about that article. That's better than someone else doing it because then the relevant history would show the real author's name.Philcha 17:44, 9 March 2007 (UTC)

I've moved it to Holocene extinction event. Philcha 00:37, 20 April 2007 (UTC)

Well, I won't waste my time again trying to write a serious contribution and then seeing it being completely deleted by knowbetters. I have real work to do to actually try and prevent as much as possible . I thought that it would interest people what the current expectations could be on the basis of a never contested biological curve. I only mentioned a blog because wikipedia asks for references. over and out, Daan Vreugdenhil —Preceding unsigned comment added by Dr. Daan Vreugdenhil (talk • contribs) 11:39, 1 March 2008 (UTC)

Most widely-supported explanations: Sustained global cooling

Section "Most widely-supported explanations: Sustained global cooling" says, "The glaciation cycles of the current ice age are believed to have had only a very mild impact on biodiversity ...". I've tried to find citations to support this and the first relevant material I found ([10]) contradicted it, saying that the long cooling beginning 3.2MYA in the run-up to the glaciations caused marine and terrestrial extinctions all over the world. Can any one supply citations (a) to support what the article currently says; and / or (b) to contradict it, as the one I found does. Philcha 13:58, 20 April 2007 (UTC)

Cosmic radiation

There's another interesting hypothesis for a 62 million year extinction cycle based on Cosmic Radiation effects when the Sun travels out of the Milky Way plane along the (northern) leading edge of the galaxy's collective motion.[11] It sounds at least somewhat plausible. — RJH (talk) 20:41, 20 April 2007 (UTC)

The Timeline...

Is upside down. Negative numbers need to be used: I'd fix it myself if I had time...

I've been thinking of whipping up an SVG version of it anyway, I'll fix it when I do that. Bryan Derksen 02:41, 14 July 2007 (UTC)

There, how's that? Bryan Derksen 03:16, 14 July 2007 (UTC)

Much better! Thanks! The only down side with using a graphic is that it is harder for people to update. That said, extinction events are now precisely enough dated that this oughtn't to be in issue. Cheers, Verisimilus T 13:44, 14 July 2007 (UTC)

On the other hand if people do update it there will be many more options than there would be with EasyTimeline. It's a tradeoff, and the old EasyTimeline code is still in the article history so we can always dig it up again if need be. Bryan Derksen 17:41, 14 July 2007 (UTC)

Incidentally, could I ask what program you used to create the SVG? I've tried a few but can't find anything satisfactory... Verisimilus T

I used Inkscape. Sorry, neglected to mark that on the Commons page. Bryan Derksen 17:41, 14 July 2007 (UTC)

Just a quibble, but being unconventional isn't the same as wrong. It never really bothered me to show it the way it was, though I'm fine with the current one too. Dragons flight 17:50, 14 July 2007 (UTC)

Conventions do exist for a reason - once you're used to time going upwards, anything else can be disorienting (for me, at least)! Verisimilus T 19:20, 14 July 2007 (UTC)

The things I don't like about this orientation is that now the text list goes in the opposite direction from the graphical timeline (easily fixable by reordering the text list) and the order of the period names is opposite from how they're used in the article (Tertiary-Cretaceous vs. Cretaceous-Tertiary). But if there's a convention to have timelines run a particular way I don't feel strongly enough about it to go against that. Unless perhaps a horizontal timeline would work better? Bryan Derksen 05:57, 15 July 2007 (UTC)

In terms of a horizontal timeline, the diversity chart already fulfils this role in a perhaps more informative way... You're right though, I hadn't picked up on those weaknesses with the right-way-up timeline. Hmm... Verisimilus T 09:13, 15 July 2007 (UTC)

Evolutionary importance of mass extinctions

Someone has inserted extraneous material into the 1st para of this section. I propose to remove the extraneous material, leaving only the 1st and last sentences.

Someone has added a "POV" tag to to the 2nd para, which represents AFAIK the current consesus and whose purpose is simply to provide a well-known example of how extinctions can open the door for evolution. I propose to remove the "POV" tag.Philcha 09:27, 19 July 2007 (UTC)

I've now removed the extraneous material and "POV" tag.Philcha 00:53, 3 August 2007 (UTC)

Implication of the title

I wonder if the article should also give some material or reference to events which could cause complete extinction of all life on earth, say an impact by a large asteroid which would destroy all life on earth including bacteria. The article seems to emphasise 'extinction' more than 'event'. AshLin 15:31, 19 July 2007 (UTC)

OMG, now an electrical engineers is becoming interested in extinctions!!!! You know, this is interesting. Last night, while eating dinner, I watched a program on Discovery Channel HD about a massive extinction event. Though probably very low probability now, because it would require an almost planet to planet collision, researchers believe that bacteria would survive in some very isolated deep earth pockets. If all life were destroyed, I would suggest that that would be it. Abiogenesis is an extraordinarily rare event--I personally believe that life outside of earth, if it does exist, is so rare that there is probably no chance for us to find it. My next project is touching up the Permian-Triassic extinction article, then keep going back. I think a total extinction event is either speculative (so not sure how we can create an article) or happened so far in the past that we may not have sufficient fossil evidence. Each extinction event going further back in time, becomes more and more difficult to analyze.Orangemarlin 17:02, 19 July 2007 (UTC)

Indeed, as bacteria live and multiply in rocks several kilometers below the surface, it would take an almost-complete destruction of the planet to remove all life from Earth. Tim Vickers 17:37, 19 July 2007 (UTC)

Thats really interesting. Do we have a wiki on such bacteria? I was under the impression that a 200km dia comet would be enough to wipe out all life. Shades of Deep Impact with its reference to 'Ellie'!

BTW, this electrical engineer started Wikipedia:WikiProject Lepidoptera and has an ambitious project of tackling 1000 Indian butterflies and 10,000 moths besides about 400 odd snakes! ;-) Nope, not a single edit about my electrical engineering - my craft or trade and just one GA review on soldiering my chosen profession. Hobbies rule on Wikipedia!AshLin 18:17, 19 July 2007 (UTC)

Atomic powered bacteria 2.8 km down. [12]. What would we call such an event? Meggar 18:29, 19 July 2007 (UTC)

Thanks for the url, very interesting!AshLin 14:00, 21 July 2007 (UTC)

We'd call it, We're Up The Creek without a Paddle Extinction Event. I could simplify that title, but I might offend someone.  :) Orangemarlin 20:06, 19 July 2007 (UTC)

BTW, Mr. Electrical Engineer, actually bacteria can survive some very harsh conditions. On the program that resurrected some Permian (I'm not sure if that's what he said, but I swear it was) bacteria locked in pockets of water within salt crystals. I'm not sure how wise it is to resurrect Permian bacteria (life on earth has no resistance to such an ancient microbe), but that wasn't he point. 200 million year old bacterial spores is quite impressive. Also, bacteria survive in some very hot locations (look at thermal hot springs, for example). The program stated that even a planet to planet collision would not cause heat to be equally distributed across the planet. Some deep earth locations (2000-5000 m below the surface) would be cool enough to allow bacteria to survive. But cockroaches would definitely not.  :) Orangemarlin 20:06, 19 July 2007 (UTC)

I'd say, fine. But such an event which extinguishes all (including cockroaches) but may leave some life behind also needs a paragraph to tell it like it is. More people have seen Deep Impact and had the words 'ELE' impacted on their memories and believe it to be completely true than ever looked at this article in Wikipedia. But some will definitely come this way. As the major article on extinction events, such large, though low-probability events deserve to be dealt with - NPOV and all that jazz.AshLin 13:40, 21 July 2007 (UTC)

I may have an overactive imagination but do all WP Extinction articles suggest feminine names, fitrst Katie now Ellie, ;-).AshLin 13:40, 21 July 2007 (UTC)

Ediacarian/Cambrian

Isn't the loss of Ediacarian life a mass extinction? 70.51.8.110 (talk) 08:48, 14 March 2008 (UTC)

Find a reliable source that classes it as such, and we can add it. --Anticipation of a New Lover's Arrival, The 14:04, 1 April 2008 (UTC)

Best known claim?

The line, "the best-known of these claims is the 26M to 30M year viral cycle in extinctions proposed by Raup and Sepkoski (1986)," made me somewhat suspicious. I hadn't heard of this claim, and yet I'd heard of some of the others. So, I followed the citations to see if it backed up this claim, and there was noting in that paper that made any claims to breadth of familiarity. -Miskaton (talk) 22:28, 2 April 2008 (UTC)

Gamma Ray Bursts

The article says that a burst within 8000 light years of Earth would destroy organisms and the O-Zone layer. While the article on GRB's agrees on the first point, that a burst within 6000 light years would cause a mass extinction, it differs on the latter, in that the burst wouldn't destroy the ozone layer, but rather that it would destroy half of the O-Zone layer, because the other side would be in the 'shadow' of the burst, and basic physics agrees with that, because any GR's that hit the Earth would be stopped by the Earth itself, in the same way that a tennis ball wouls stop the light from a flashlight. Also it would take a birst of at least 10 seconds for it to do that much damage, so its not like a quarter second burst would wipe out the world as we know it. Perhaps a re-wording of the article is needed to make it clear that there would be some O-Zone left and also to make it a little clearer that it would only be a mass extinction, not a total one, which is what I thought it said the first time I read it. 82.21.111.208 (talk) 19:57, 10 April 2008 (UTC)

Ozone is destroyed by the nitrous oxides and other reactive chemicals in the atmosphere created by the burst, so it consumes the ozone on the other side too. Dragons flight (talk) 21:16, 10 April 2008 (UTC)

Image:Phanerozoic Biodiversity.svg

This could be useful for explaining the difference between "extiction" and "change in diversity". I've asked the image's author if he can turn the image round so that time runs left to right and if he can remove thetext so it can be added via Template:Annotated image -- Philcha (talk) 12:54, 13 September 2008 (UTC)

Wouldn't have to turn the image, if people had left "Extinction event" in the orientation it was published in to begin with. Dragons flight (talk) 15:12, 13 September 2008 (UTC)

Left-to-right time is a bit more intuitive, at least for laypeople. -- Beland (talk) 07:39, 15 September 2008 (UTC)

Graphics

Consider that:

• Image:Extinction Intensity.png lists both major and minor events, but can't link to articles because it is a flat graphic.
• {{Annotated image/Extinction}} has links to articles, but only the major ones because it would be cumbersome to add in-graphic links to all the minor events.
• {{ExtEvent nav}} has serious layout problems, doesn't show the "extinction intensity", and doesn't include many of the minor events.

I think it would be useful to have a new graphic that would show all the minor events on a vertical axis (putting the oldest events at the bottom, to match the period-to-period navigation convention). It could have the columns: Mya, Period, Event name/link, Extinction intensity (bar graph). Does that sound like the best approach? -- Beland (talk) 07:52, 15 September 2008 (UTC)

Or a table with the same info. I'd include all the known events, so users don't have to scroll around and then merge the info in their heads. I think we could still make the backgrounds of the "period" cells match the standard colours, although I'm not keen on that since the period names don't stand out so well as they are usually wikilinked. OTOH we might use the period colours as bg but give the labels white bg, if that doesn't make it look like measles.

Biggest problem would be the 3-pulse Late Devonian extinction - AFAIK no single pulse was huge but the cumulative effect was severe. P-Tr might also be tricky: elevated rate througout 2nd half of P, then 2 pulses - but we could summarise the total of the 2 final pulses, as they were close together. -- Philcha (talk) 10:23, 15 September 2008 (UTC)

Proposed merger of The Big Five

It has been proposed that The Big Five be merged into this article.

• qualified support The Big Five duplicates content in this article, which should be merged with this article. However it also contains more detail about some of "The Big Five" than is appropriate for this overview article. The more detailed content should be merged into the articles on the specific extinctions. -- Philcha (talk) 10:29, 15 September 2008 (UTC)

Even though I am the one who created the The Big Fivearticle, I must agree--Dale S. Satre 22:08, 17 September 2008 (UTC) —Preceding unsigned comment added by Dale S. Satre (talk • contribs)

• a weak oppose, instead move The Big Five to list of extinction events. Reason: Extinction event is becoming too large and unwieldy. If you merge The Big Five hereto, the need to make a list of events will soon become obvious anyways. Said: Rursus (☻) 09:46, 23 September 2008 (UTC)

I implemented the proposed mergers, though some post-merge cleaning up of the target articles may be in order. -- Beland (talk) 20:50, 30 September 2008 (UTC)

Set of extinctions described

We need to sort out how this article lists extinctions:

• The "Marine extinction intensity through time" diagram highlights the Big Five, although others are visible and the end-Botomian and end-Dresbachian have % scores higher than some of the Big Five. Perhaps we should note the Big Five for historical reasons, but otherwise de-emphasise the term as obsolescent.
• Section "Major extinction events" lists 7. Those not highlighted in the "Marine extinction intensity through time" diagram are Tr-J and Holocene. I'm happy about including Tr-J as it may have been the dinos' lucky break, see Superiority, Competition, and Opportunism in the Evolutionary Radiation of Dinosaurs. The Holocene extinction is tricky: there's a fair amount of WP:RS literature about it; but its method of counting / estimating differs significantly from that used in the earlier ones. I'd move the sentence "Some paleontologists, however, question whether the available data support a comparison with mass extinctions in the past" to 2nd sentence so readers can see up front that theres' a difference.
• A recently-added section "Minor events" sprawls far too much and the only cited source is "Partial list from Image:Extinction_Intensity.png". I think this is clearly WP:OR. The list is also a real mixed bag. For example the end-Botomian and end-Dresbachian have % scores higher than some of the Big Five and I already know a source or 2 for end-Botomian; but Ireviken event cites only one locality, so at present that article offers no evidence that it was wide-spread.

Since known significant extinctions are likely to increase as paleo knowledge increases, I propose a "List of extinction events" artilce to summarise all known extinctions. I suggest its main content should be a table: date (range); name; impact; notes, which can cover how wide-spread, severity, very brief description with internal link to further details in same article if necessary.

That leaves the question of which event should be mentioned specifically in Extinction event. I suggest:

• Holocene, but possibly with stronger qualifications about difference in counting.
• The Big Five.
• Tr-J
• end-Botomian and end-Dresbachian. High % extinction rate. One (can't remember which) has been described as a significant change in composition of Cambrian fauna.

That list has some implicit criteria - an extinction should be included if it satisfies one of:

• wide-spread and % extinction rate at least 70% of Big Five - 70% is a rough guess, we may have to adjust to avoid having too many borderline cases; a "list of" article will help in showing the frequency distribution of % extinction rate.
• significant change in ecosystems. It's hard to define "significant" up front, and we may need tohandle this case by case.

-- Philcha (talk) 11:16, 15 September 2008 (UTC)

List split?

So it's been proposed to create List of extinction events, but we already have Timeline of extinctions. But that only covers historical extinctions on a per-species basis, whereas here we cover both historic and pre-historic extinctions en masse. Should we have Timeline of extinction events with links to "event" articles from a big long table, as proposed above, or something else? -- Beland (talk) 21:04, 30 September 2008 (UTC)

As you point out, the timescale and extinction scale are totally different. A full list of paleo mass extinctions would still be a good idea, I think. -- Philcha (talk) 22:05, 30 September 2008 (UTC)

But where does one draw the line when deciding what qualifies as a mass extinction? Don't Template:Extinction events and The big five fulfil the role already? Martin (Smith609 – Talk) 03:20, 1 October 2008 (UTC)

All genera

"Well-defined" genera

Trend line

"Big Five" mass extinctions

Other mass extinctions

Million years ago

Thousands of genera

Phanerozoic biodiversity as shown by the fossil record

Benton M.J. and Harper.D.A.T "Basic Palaeontology" (1997; Addison Wesley Longman) allegedly defines "mass extinction" as "the loss of 10% or more of families, and 40% or more of species, in a short time"

A timeline diagram gives some perspective to the dates and period names, but that's all, and runs out of space quickly. For example Template:Extinction events graphical timeline would need considerable rearrangement to accommodate the PETM extinction or the apparently three Cambrian extinctions, which have an apparent % loss in the Big Five range, although the decline in total recorded biodiversity was apparently small and the end-Botomian extinction may have been an artefact due to the sharp decline of phosphatic preservation - which is the kind of info that could go in a "notes" column in a table. -- Philcha (talk) 07:05, 1 October 2008 (UTC)

Oxygen catastrophe?

Why is the oxygen catastrophe of ~2.7 bya and its associated massive extinctions not included? Vultur (talk) 23:35, 1 December 2008 (UTC)

These were only ever hypothetical, there is no actual evidence of mass extinctions after the oxgen content of the atmosphere started rising. A recent paper (Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry, Royal Society, 2008) summarises current ideas about the issue. The idea of an oxygen catastrophe is based on ideas about the evolution of the biosphere that originated in the 1970s. Evidence found by microbiologists and geochemists since the 1990s paints a different picture, although the oxygen catastrophe hypothesis is still widely written about by scientists who are not specialists in these fields (Google Scholar give tons of hits for "oxygen catastrophe" but only a few for "oxygen catastrophe" evidence). The biological evidence consists of the existence of non-aerobic eucaryotes throughout the eucaryote family tree, not just in a few "primitive" groups - some plants and fungi are obligate (full-time) anerobes, and some plants, fungi and animals are facultative anerobes (can live without oxygen if circumstances require it). The geochemical evidence indicates that until about 600 million years ago the oceans remained anoxic and sulphidic, except possibly in the top 100-200 meters where there was enough light to support photosynthesis. (end of summary of paper). IMO it's very likely that oxygenation had effects on life from the start, but these were nowhere near as massive and abrupt as the phrase "oxygen catastrophe" implies. --Philcha (talk) 08:51, 2 December 2008 (UTC)

To paraphrase Butterfield 2007, pre-Phanerozoic communities were stable and didn't really undergo "mass extinctions". I agree that this should be noted in the article, though! Martin (Smith609 – Talk) 22:53, 2 December 2008 (UTC)

Holocene extinction

I undid this edit because:

• Paleontologists' "Big Five" does not include the Holocene extinction and AFAIK the O-S extinction is still rated the 2nd largest in % terms (after P-Tr).
• The estimating methods for the "Big Five" and the Holocene extinction are different - for the "Big Five" it's taxa in the fossil record before and after the extinction, and Holocene extinction event is unclear about how extinction rates for the Holocene extinction are estimated. Note the statement (with citation) "Some paleontologists, however, question whether the available data support a comparison with mass extinctions in the past."
• Any further statments that claim that the Holocene extinction is comparable with the "Big Five" will need citations that define the estimating metohds clearly, otherwise this article will wind up comparing apples and oranges. --Philcha (talk) 14:11, 27 December 2008 (UTC)

Period of Sun's orbit around the galaxy wrong?

In the section titled "Passage through galactic spiral arms" a value of 700 million years is given for the orbital period of the Sun around the galaxy. There are a number of sources that place this value closer to 200-250 million years. One is the Wikipedia enter titled Milky Way. "It takes the Solar System about 225–250 million years to complete one orbit of the galaxy (a galactic year),[37] " Amazedbyitall (talk) 06:33, 29 January 2009 (UTC)

The Earth orbits the center of mass of the galaxy every 225 Myr, give or take, but the spiral arms are also orbiting, albeit at a different rate. The time required to pass through all of the spiral arms is thus determined by the difference in these two rates of rotation and consequently much longer. Dragons flight (talk) 06:38, 29 January 2009 (UTC)

Reference needs to be added

Are periodic mass extinctions driven by a distant solar companion? Whitmire, D. P.; Jackson, A. A. Nature (ISSN 0028-0836), vol. 308, April 19, 1984, p. 713-715. (Nature Homepage) 04/1984 http://adsabs.harvard.edu/abs/1984Natur.308..713W --aajacksoniv 19:30, 27 April 2009 (UTC) —Preceding unsigned comment added by Aajacksoniv (talk • contribs)

gnome work

the major and minor timescales go in opposite directions. Needs fixing Andrewjlockley (talk) 01:29, 11 August 2009 (UTC)

Volcanism

Is a major Impact event triggering the the volcainsm ? as both are often associated with a mass extinction ? Photnart 04:24, 20 November 2009 (UTC)

Sea-level falls - Clarification

The article mentions:

"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."

When one discusses the mid-ocean ridges, the first question that pops into my mind is where is it going?

The way I'm thinking about it is a shift in mass from the ocean seabed to the continents, or processes that would make the continents smaller and taller would tend to cause the sea level to fall. This would include the sequestration of water in the form of ice

Processes that transfer mass from on the continents to the sea such as erosion or melting of ice would tend to make the sea level rise.

So, if a force such as subduction moved mass from under the seabed to depositing the material in with the Cascade Mountain Volcanoes, then that would be equivalent to removing the equivalent amount of mass displaced by the mountains from the ocean.

If, on the other hand, India collides with Asia, the Himalayan mountains are pushed up, and essentially the continental area is decreased and the oceans levels could fall.

Anyway, it seems as if the concept of transferring matter from the ocean to the continents needs clarification.--Keelec (talk) 19:05, 21 February 2010 (UTC)