Talk:Great Oxidation Event

Wiki Education Foundation-supported course assignment

This article was the subject of a Wiki Education Foundation-supported course assignment, between 2 April 2019 and 28 June 2019. Further details are available on the course page. Student editor(s): PLin AB. Peer reviewers: Lmfifer.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 21:57, 17 January 2022 (UTC)

Wiki Education Foundation-supported course assignment

This article was the subject of a Wiki Education Foundation-supported course assignment, between 7 January 2019 and 9 April 2019. Further details are available on the course page. Student editor(s): Aseja Dava.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 22:40, 16 January 2022 (UTC)

Too Technical, Missing Points?

I have an MSc in Physics and I think this page is way too technical, or unfortunately is written in a way that makes it much less interesting. (no offence to the hard working souls who created it). There is a huge middle section that goes off on a technical tangent about a time lag, and only near the end do we get to the explanation of what actually happened. It also seems that there is no mention at all of the Snowball Earth or how the snowball earth was eventually broken by more microbes that evolved to consume oxygen and create carbon dioxide. I found the DamnInteresting page on this event to be much more readable. It follows events chronologically and explains cause and effect in less technical language, as opposed to explaining one or two technical points in verbose detail. (http://www.damninteresting.com/?p=673#more-673) 69.156.113.62 04:35, 3 December 2006 (UTC)

The Snowball Earth was several billion years later, so I don't see that it's directly relevant to the Oxygen Catastrophe. But yes, this article could certainly do with some work, I'll try a rewrite if I have time. -- Danny Yee 08:09, 3 December 2006 (UTC)

Also, the story on the DamnInteresting page is highly speculative. It goes into details that are certainly not known but simply guessed at. -- Danny Yee 08:10, 3 December 2006 (UTC)

Before a hyper-technical term like "oxy-photosynthesis" appears in a sub-title, it MUST be defined! I myself am shakey as to what the writer here actually meant by this difficult-to-pronounce scientistic term. Dr.Bastedo (talk) 01:20, 27 June 2010 (UTC)

Dr.Bastedo, please do not SHOUT!

When I refer to an article or or page, I provide a link - please do the same.

The article used "oxy-photosynthesis" only as a heading, not in text. Photosynthesis#Evolution is interesting but that section has no citations. Microbial mat is also very interesting, but the sources have limitations: Nisbet describes his one as speculative, and Krumbein and co get too enthusiastic and and I doubt their objectivity (I wrote the WP article).

If you find any good sources for any of this, please ensure that the citations have the required parameters: last1, first1, etc.; pages for all except pure web pages; url and accessdate if a url is available for a non-web source; etc. --Philcha (talk) 00:37, 28 June 2010 (UTC)

Introductory color visual or graph

The "Great Oxygenation Event" (G.O.E.) has the SAME colored visual or line-graph that appears at the START of the "Geological history of oxygen", a much-better and more readable Wiki article.

However, we need some illustrations for G.O.E. So either we should (1) colorfully revise the current graphic as -- say -- a differently-colored histogram/barchart, or (2) come up with better alternative illustrations -- e.g., a diagram, flow-chart, photo, cartoon, artwork, or colorful data.

The illustrated subject could be Cyanobacteria, fossil Stromatolites, Aerial castrophe, Oxygenation, Banded iron formations, Oxidation, Extinction events, or whatever...

For more ideas, I recommend Prof. Edward Tufte's colorful how-to books on how to present statistics, science and history.

In short, we should avoid redundancy, plagiarism, dejavu, and confusion with the other article(s). And I'm way too old and too retired to fuss with all the details... Dr.Bastedo (talk) 02:07, 27 June 2010 (UTC)

Cyanobacteria

It would be useful to mention that the cause of the oxygen build up was the evolution of photosynthesising cyanobacteria from earlier photosynthesising sulphur bacteria. Photosynthesising sulphur bacteria use sunlight to split Hydrogen Sulphide (H2S) molecules to produce sulphur, but cyanobacteria modified this process to split water (H20)molecules to produce oxygen. RV 4 March 2007

The oxygenation of the atmosphere and oceans

This 2006 paper by Heinrich Holland lucidly reviews the subjects covered in this article. Professor Holland has kindly released figure 10 from his article under GFDL, for us to be able to use it in Wikipedia. These graphs illustrate the estimated evolution of atmospheric $\ P_{O_{2}}$ and the concentration of O₂ in the shallow and deep oceans. Your assistance is now needed to adapt these graphs for use in Wikipedia, and update our articles with the information provided in the said paper. Regards, Lior 17:03, 11 June 2007 (UTC)

• The presentation of information D.I. End of Life here, deleted as "blogspam" [sic] might prove useful in improving the presentation in this Wikipedia article. --Wetman 17:14, 18 June 2007 (UTC)

When did ozone layer appear?

I thought that ozone layer appeared 500 millions years ago, when land became habitable (see Timeline of evolution). However this article relates its appearance with the much earlier Oxygen Catastrophe. Is it a real discrepancy, or are we talking about two different phases in its forming (i.e. for a stable 21% oxygen atmosphere one needs a much thinner ozone layer compared to the one needed for the land to become habitable)? Dan Gluck 09:41, 17 September 2007 (UTC)

Capitalization

• The use of capitals in phrases like "Oxygen catastrophe" is unwarranted. --Wetman 18:56, 7 October 2007 (UTC)
• I'm proposing moving the page to the non-capitalized version (which redirects here). - tameeria (talk) 20:09, 30 December 2007 (UTC)
• There was only one oxgen catastrophe, so the expression may as well have capitals as a proper name of a specific event. Anthony Appleyard (talk) 21:10, 30 December 2007 (UTC)

I agree that it was a specific event that can have this title.

IceDragon64 (talk) 20:22, 2 February 2009 (UTC)

Me too. -- Dr.Bastedo (talk) 01:26, 27 June 2010 (UTC)

Image caption

What does 'A', 'B', and 'C' in the image caption refer to? There are no such labels in the image itself. —Preceding unsigned comment added by 85.228.39.223 (talk) 08:28, 16 November 2007 (UTC)

The source paper of the diagram does not seem to suggest these time frames either (PDF available here). Strangely, the phases A, B,C are in addition to the stages 1-5, which are not linear in time. Linear time scale is indicated at the bottom of illustration. --83.76.186.14 (talk) 21:08, 9 December 2007 (UTC)

The image caption refers to the old image (see right) that was replaced apparently without updating the image caption as well. - tameeria (talk) 20:00, 30 December 2007 (UTC)

Requested Move

Oxygen Catastrophe to oxygen catastrophe

• Oppose as it refers to a specific and not a generic event. 70.51.11.191 (talk) 00:48, 2 January 2008 (UTC)
• Oppose, probably. The stuff I can find usully doesnt have a capital 'C', but if we dont write it like that people will think its about a general phenomenon, not a specific event. Callmederek (talk) 19:18, 4 January 2008 (UTC)
• Oppose per comments above; specific event --Lox (t,c) 12:55, 5 January 2008 (UTC)
• Looks like the consensus is not to move the page, so I'm removing the move tag. - tameeria (talk) 16:33, 5 January 2008 (UTC)

What exactly was the "catastrophe" ?

I didn't find anything that actually explained what was so catastrophic to justify the title. What/how much actually happened ? Did existing lifeforms disappear, move underground, evolve ? Anaerobic organisms still exist. The availability of O2 seems more like a great opportunity than a catastrophe.Rcbutcher (talk) 02:53, 18 January 2008 (UTC)

The rising oxygen levels wiped out a huge portion of Earth's inhabitants at the time. From their perspective it was a catastrophe. Cyanobacteria were essentially responsible for probably the largest extinction event in Earth's history. Eris Discord | Talk 02:35, 29 February 2008 (UTC)

Eris, do you have any source for that statement? If so, exactly what would have killed off the previous species? What were the previous species? --Mlewan (talk) 15:34, 11 March 2010 (UTC)

Now that's exactly what should be in the article! ;) BenJury (talk) 13:15, 10 September 2008 (UTC)

The catastrophe was 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) 12:03, 2 December 2008 (UTC)

That link doesn't work for me, BTW. --Michael C. Price ^talk 08:28, 4 February 2010 (UTC)

'Catastrophe' doesn't refer to mass extinction but to the abrupt rise in oxygen levels (compare ultraviolet catastrophe; the reference is to how the graph looks, not to disastrous events speifically). 165.91.174.196 (talk) 07:31, 4 February 2010 (UTC)

Not quite. The UV catastrophe refers to the diaster implied by the shape of the graph. Similarly the reference here is to the associated mass extinction (real or imaginary) of the anerobes. --Michael C. Price ^talk 08:24, 4 February 2010 (UTC)

'Catastrophe' can be read both ways: A lethal event and a "sudden shift in behavior arising from small changes in circumstances" (see Catastrophe theory). As a name for what happened to the oxygen levels I find it apt. -- Zirconscot (talk) 23:10, 3 December 2011 (UTC)

I feel that the article still needs to speak about the name Oxygen Catastrophe- if it is true that for years it was percieved as a catastrophic death etc, then we need to say something about realising that this is not known, since books and other media have long called it a Catastrophe. Don't get me wrong, I was one of those who wanted it to have another name etc, I just feel that if only in a historical context the common word Castastrophe needs explaining.

IceDragon64 (talk) 23:17, 1 January 2013 (UTC)

The specific catastrophe, though not mentioned here, was the systematic extinction of all species that used amino alcohols, favoring a switch to the more oxygen-stable amino acids. Amino alcohols are simple prebiotic compounds formed by the reaction of methane, ammonia, and water. They can polymerize into a variety of functional proteins and catalyze reactions, and there should be a whole branch of the tree of life that uses them, but oxygen causes amino alcohols to break down, and so any life trying to use amino alcohols on Earth was doomed to have their proteins fall apart. The mechanism of conversion to amino acids is surprisingly simple: all you have to do is add formic acid (HCOOH). Life solvated by ammonia or methane (like on Titan) uses amino alcohols and oxygen is toxic to them, but hydrogen cyanide is essential for them, since it condenses into nucleobases like adenine. Life solvated by water uses amino acids and the mitochondria use oxygen, but hydrogen cyanide is toxic to them, since the cyanide ion inhibits hemoglobin and cytochrome c oxidase. You get some, you lose some. See Hemiaminal for a list of geminal amino alcohols that can be converted into amino acids by condensation reactions with formic acid. See Alkanolamine for a slightly biased view of amino alcohols with a note on the Great Oxygenation Event that will probably end up being deleted. There's no way to prove that there was ever life that used amino alcohols on Earth, since any fossils necessarily don't contain proteins and certainly don't contain monomers like amino alcohols, but the life that used amino acids had to come from somewhere, and evolving from amino alcohol using life, adapting by converting their amino alcohols to amino acids using formic acid is really the only logical explanation for the species that survived the Great Oxidation Event. Zuloo37 (talk) 05:45, 3 November 2014 (UTC)

Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry — Preceding unsigned comment added by Pedro Lamo (talk • contribs) 07:17, 23 April 2017 (UTC)

Sources

Recent publications suggest we need to re-examine the whole idea of an "oxygen catastrophe". I'm going to start collecting sources here, with brief notes. If we get enough, it may be necessary to re-organise the list into sub-sections. Please contribute, using a similar format. If you wish to discuss any of these items, please do so in separate sections, so that this remains a simple list.--Philcha (talk) 12:14, 2 December 2008 (UTC)

• Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry (Mentel & Martin; Phil. Trans. Royal Society, 2008) - The existence of non-aerobic eucaryotes throughout the eucaryote family tree, not just in a few "primitive" groups, and the very narrow range of energy-producing chemical paths eucaryotes possess, suggest that eucaryotes acquired mitochondria / hydrogenosomes / mitosomes in a single endosymbiosis event that happened in an anerobic environment. Geochemical evidence suggests the oceans remained anoxic and probably sulphidic until about 600 million years ago, except for the photic zone in the top 100-200 metres.
• Dating the rise of atmospheric oxygen (Bekker, Holland, Wang et al; Nature, 2004) - Oxygenation of atmosphere started about 2,450 million years ago and reached 10^-5 PAL (present atmospheric level), enough to become significant, by 2,320 million years ago.
• The oxygenation of the atmosphere and oceans (Holland; Philos Trans R Soc Lond B Biol Sci., 2006) - Stages: 3,850 to 2,450 million years ago atmosphere and oceans anoxic, except possibly "oxygen oases" in shallow oceans; 2,450 to 1,850 million years ago atmospheric oxygen levels rose to between 0.02 and 0.04 PAL, shallow oceans became mildly oxygenated, deep oceans remained anoxic; 1,850 to 850 million years ago (the "boring billion") little change in atmospheric oxygen levels, surface and deep oceans mildly oxygenated, anoxic or euxinic deep oceans not inevitable; 850 to 540 million years ago atmospheric oxygen rose to about 0.2 atm, shallow oceans oxygenated, deep oceans anoxic at least some of the time(three major Neoproterozoic glaciations); 540 million years ago to present show atmospheric oxygen rising to 30% in Carboniferous ("wood crisis") then declining to present level (about 18%), shallow oceans were oxygenated, oxygen levels in deep oceans fluctuated, possibly sharply at times.
• The loss of mass-independent fractionation in sulfur due to a Palaeoproterozoic collapse of atmospheric methane (Zahnle, Claire, Catling; Geobiology 2006) - Collapse of atmos methane level a prerequisite for oxygenation; collapse of methane greenhouse enabled Proterozioc glaciations; stable oxygen level restored methane greenhouseby protecting it from UV with ozone layer.
• Did the Proterozoic ‘Canfield Ocean’ cause a laughing gas greenhouse? (Buick; Geobiology 2007) - not sure how serious, but start and finish are amusing (deliberately).
• Oxygen and life in the Precambrian (Catling, Buick; Geobiology 2006) - Summarise all the other Geobiology 2006 papers.
• Bistability of atmospheric oxygen and the Great Oxidation (Goldblatt, Lenton & Watson; Nature, 2006) - Oxygenic photosynthesis evolved about 2,700 million years ago but the "Great Oxidation" was about 2,400 million years ago; man yexplanation so fthis lag have been proposed. Possible explanation - atmospheric oxygen level is bistable: below 10^-5 PAL there is too little O2 to form an ozone layer, and UV drive oxidisation of methane; above 10^-5 PAL, ozone form and blocks UV, so O2 and methane levels rise again. This model predicts a sharp fall inmethane levels during the transtion, setting the scene for glaciations.
• The Emerging Aerobic Earth System through Archaean-Palaeoproterozoic Transition: Problems and Perspectives (Melezhik, Fallick, et al; Geophysical Research Abstracts, 2006) - some puzzles, including first appearance of petroleum about 2,000 million years ago}.
• The rise of atmospheric oxygen (Kump; Nature, 2008) - A failed oxygenation event about 3,200 million years ago ago?

--Philcha (talk) 14:24, 2 December 2008 (UTC)

• http://www.bbc.com/earth/story/20170125-there-is-one-animal-that-seems-to-survive-without-oxygen three species of loricefrans living in the anoxic and sulfidic mud of the soil of the L'Atlante basin seem to be the first obligate anaerobic metazoans. They have hidrogenosomes instead of current mithocondrias, Obviously their evolutive origin and importance is not well understood, so far. They could be a sign of that early complex eukaryota lived in anoxic conditions. Other theories point to lateral gene transference. --Pedro Lamo (talk) 09:02, 14 May 2017 (UTC)

Article title

Atmospheric oxygenation event is free, what about a move to a less dramatic title? Tim Vickers (talk) 21:10, 15 January 2009 (UTC)

That's better, but I'm not sure "event" is right for a 16,00M yr process. How about Atmospheric oxygenation? That leaves the options open, whichever way the geochemists jump.--Philcha (talk) 21:41, 15 January 2009 (UTC)

No, that might be an ambiguous title that could also refer to the oxygen cycle. This is something that happened once, within defined boundaries (however long these were), so I think "event" is technically accurate. Tim Vickers (talk) 21:56, 15 January 2009 (UTC)

Good point about the oxygen cycle. Re "event", the boundaries are not so well defined. In fact there's a series of events, see File:Oxygenation-atm.svg and the cited article. How about History of atmospheric oxygenation? --Philcha (talk) 22:28, 15 January 2009 (UTC)

Sounds good, but you'd then have to expand the article a bit to include later fluctuations after the initial reducing/oxidising switch, since that title covers a broader subject area. I'd be happy with that as a solution though. I wonder if anybody else watching this page will comment? Tim Vickers (talk) 22:53, 15 January 2009 (UTC)

I think that if we can settle that there was not a Catastrophe, then the bulk of the article, describing what actually happened, should move to Atmospheric oxygenation event. It doesn't really matter whether anyone has used it before or anything, so long as it establishes the truth as accurately as we know. I think that a small article should remain here about the original idea, that it was "The biggest extinction in history" or whatever, and showing any key research which discredits this- linked to a main article over there. I have been bold and created the page, in brief, wikidragon fashion.

IceDragon64 (talk) 20:34, 2 February 2009 (UTC)

I don't think we can (or should) settle that there wasn't a catastrophe.

BTW, there is an interesting take in New Scientist on it - claims that the GOE triggered a much earlier snowball Earth episode. See First breath: Earth's billion-year struggle for oxygen. A rare high quality article from NS. --Michael C. Price ^talk 17:32, 7 February 2010 (UTC)

I do not understand, why the Title here is "Great Oxygenation Event", while specialists like H. Holland (in ref.1) call it Great Oxidation Event" - my english is not the best (sorry for this) but shouldn't we call things like this as Specialists do it? -- Hartmann Schedel ^cheers 12:14, 16 May 2013 (UTC)

Graph Lines?

Am I missing something? There are two different coloured lines on the graph and only one atmostpheric constituant discussed, so what does the other line mean and which is which?

IceDragon64 (talk) 21:03, 2 February 2009 (UTC)

One of them is O2 pressure, the other is O2 concentration in ocean surface waters. But which is which? 131.111.85.79 (talk) 15:19, 16 March 2009 (UTC)

Drake Equation

This is intended as a stub until either I or anyone else can fully illustrate the significance of this portion.

By many accounts, the Drake Equation is roughly 13 to 14 orders of magnitude higher than we are experiencing, taken even for when the anecdotially reported myriad forms of intelligent extraterrestrial life are accounted, totalling roughly more than one, perhaps 10, and far fewer than 100 distinctly differeing species. In order to rectify the Equation, I postulate that the condition of the earliest times of the planetary evolutionary cycles be admitted as another variable to the Drake Equation, somewhere between fℓ and fi, considering the exegesis of particularly protozoan life from those same conditions on early planet Earth.

This is not necessarily a case of making the equation fit the data results, although it appears to be exactly so.

It is my hypothesis that this hypothetical Great Oxygenation Event, which seems to have formed the Ozone Layer, atmospheric and oceanic oxygen, and many useful minerals for life on Earth, could happen only extremely rarely, and could perhaps wholly account for the remaining roughly 1/10,000,000,000,000 (1 in 10 quadrillion) chance that life evolved here and not everywhere else. The quantification of the rarity of this event would help to define one element of the proposed additional variable to establish a realistic number for the Drake Equation. The additional rarity of the progression of life on Earth to anti-photosynthetic form could possibly have been predicated by a disruption of another extremely large impactor into the atmosphere, and is also deserved another element of this proposed variable, although these two do not comprise the exclusivity of that variable.

This other part of the entire hypothesis is that it appears to me that the entirety of the Canadian Shield, including Greenland, seems to be formed from a giant impactor which formed the crater now known as most of the Hudson Bay area. I would like it if more research was done to confirm or deny whether or not the Hudson Bay area in general, and the Canadian Shield at large is the result of a rather large and early (c.2,700M-3,400M years ago) impactor against the surface and early atmosphere of the Earth. When one compares the Canadian Shield to the Hellas Basin on the surface of Mars, the geological similarities are convincingly striking, albeit in roughly half the size, and although certainly not conclusive. More work, specifically using core samples from various locations surrounding the Hudson Bay area, would be requisite to begin to either confirm or deny this hypothesis.

The number for this variable may be revised upward if we do find through telescopic radiometry and spectrography a larger prevalence of oxygenated worlds in other solar systems within the galaxy.

This section in its entirety is being cited as an original derivative work, from my own making.

This is all posted as a postualtive, and not under copyright, although attribution would be appreciated under Creative Commons License.

IllegalKnowledge (talk) 14:02, 2 June 2010 (UTC)Michael Oatman (IllegalKnowledge@gmail.com)

Your speculations are nonsense and will be removed as they violate 2 policies of WP, No original research and Verification. --Philcha (talk) 17:54, 2 June 2010 (UTC)

2,400 million years ago?

Why not 2.4 billion? —Preceding unsigned comment added by 96.230.200.94 (talk) 20:59, 28 October 2010 (UTC)

Atmospheric composition

The article does not make clear what the current consensus is about the total atmospheric composition before, during, and after the event. Meaning percentage of nitrogen, carbon oxides, hydrogen, methane, ammonia, noble gases, etc., as well as the rise in free oxygen. It's odd to see, for example, a paragraph about the reduction in atmospheric nickel without actual numbers for the much larger constituents. --173.76.64.248 (talk) 21:40, 19 November 2012 (UTC)

Volcanism

This article does not address the theory that this event was caused by volcanic changes rather than cyanobacteria. For example, see this article in Nature http://www.nature.com/nature/journal/v478/n7368/full/nature10460.html or the studies of H.D. Holland (Harvard). It appears that there is some debate in the scientific literature over what actually caused this event. — Preceding unsigned comment added by 99.135.168.103 (talk) 15:48, 24 April 2013 (UTC)

Timeline formatting problem

In the timeline in the "Role in mineral diversification" section, the Quaternary period spills over onto its own row (at least in my browser), where it is aligned with a large chunk of the early Paleoproterozoic era. This is obviously very misleading, but I don't understand the timeline template well enough to fix it. Can someone help? Ravi12346 (talk) 21:03, 27 May 2013 (UTC)

Most of the information under "Timing" is covered again immediately afterword in the "Time Lag Theory" section. Can these sections be combined, or else differentiated more?67.51.110.77 (talk) 15:41, 29 May 2013 (UTC)

table broken?

{{Horizontal timeline}}

perhaps I've just misunderstood it (in which case it could do with more labels). EdwardLane (talk) 12:24, 30 May 2013 (UTC) Quaternary is definitely in the wrong place in this drawing as displayed on my browser - it is shown on the far left, at the most distant time from the present, which doesn't make any sense if you follow the links. Perhaps it has wrapped around? Jintian (talk) 19:13, 23 June 2013 (UTC)

eons

Palæoproterozoic

Mesoproterozoic

Neoproterozoic

Palæozoic

Mesozoic

Cenozoic

periods

Siderian

Rhyacian

Orosirian

Statherian

Calymmian

Ectasian

Stenian

Tonian

Cryogenian

Ediacaran

Cambrian

Ordovician

Silurian

Devonian

Carboniferous

Permian

Triassic

Jurassic

Cretaceous

Paleogene

Neogene

Quaternary

ok looks like periods is the template that has gone wrong, documentation is not present, so here's my best attempt at fixing it so far but it's still not right as, for example 'The Cenozoic is divided into three periods: The Paleogene, Neogene, and Quaternary;' but those are not lined up.

{{Horizontal timeline}}

looks like this is beyond my skills, so I've put a request on Wikipedia_talk:WikiProject_Templates#Template_horizontal_timelines . EdwardLane (talk) 07:54, 29 June 2013 (UTC)

Effects on Life

Oxygen started appearing in the atmosphere around 2.3 billion years ago, yet the Cambrian Explosion did not occur until much later around 550 million years ago. This page says oxygenation allowed diversification, but does not mention the time gap between the two. It would be helpful just to have a little clarification with that. Kkennedy657 (talk) 22:13, 1 October 2014 (UTC)

New study

Quote: It took 100 million years for oxygen levels in the oceans and atmosphere to increase to the level that allowed the explosion of animal life on Earth about 600 million years ago - See more at: http://www.ucl.ac.uk/news/news-articles/1215/181215-earth-oxygenation prokaryotes (talk) 21:45, 18 December 2015 (UTC)

"Homogenization of the marine sulfur pool"?

In the section "Late evolution of oxy-photosynthesis theory", a term is introduced yet not explained. I Googled this term, and found that it has its origin in this Wikipedia article, and that all references to the "marine sulfur pool" anywhere on the Web are clones of this article. If anyone knows what is meant by "homogenization of the marine sulfur pool" and can rewrite this paragraph using less-obscure wording, they would do the world a favor. The cited article from PNAS uses the term "homogenization of the S pool"; unfortunately that article is beyond my comprehension, and the term "homogenization of the S pool" is unique to this article.--97.120.35.87 (talk) 18:47, 17 July 2016 (UTC)

"Oxygen holocaust"?

Is there at least a source for that name being in even occasional use? It seems like a ludicrous appropriation of a phrase that specifically refers to intentional genocide.86.149.158.184 (talk) 10:47, 30 July 2016 (UTC)

I did a search and immediately found a Wikipedia echo chamber, repeating what's written here. This word has legs we should not facilitate without the strongest source. — MaxEnt 16:31, 17 July 2017 (UTC)

Fixed via Margulis, Lynn; Sagan, Dorion (1986). "Chapter 6, "The Oxygen Holocaust"". Microcosmos: Four Billion Years of Microbial Evolution. California: University of California Press. p. 99. ISBN 9780520210646. -- atropos235 ✄ (blah blah, my past) 18:33, 4 September 2017 (UTC)

Page is misnamed: GOE is defined by leading researchers in this area as Great Oxidation Event in the scientific literature

In 1999, the late Heinrich Holland (then a Professor at Harvard University) named the first rise of oxygen in the Paleoproterozoic the "Great Oxidation Event" and this is the common usage by virtually all of other scientists in this area. Later, Holland (2006) specifically defines it: "the period between 2.4 and 2.0 Ga has become known as the Great Oxidation Event". A recent review in Nature by Lyons et al. says the step increase is "now popularly know as the Great Oxidation Event or GOE". In another scholarly review of the topic by Catling (2014), "Great Oxidation Event" is used in the title (which is a dead giveaway as to what the correct name is). Surely, it is unacceptable that this wikipedia page, written by people who have done none of the original research on the topic (unlike Holland or Lyons et al. or Catling or others), decide to rename the GOE the Great Oxygenation Event? I also agree with the comment above about questioning use of the phrase "oxygen holocaust", which is similarly unjustified. In fact, the over-emphasis on "oxygen catastrophe" on the page is unsupported by evidence. But my main point is that the page name needs to be changed to Great Oxidation Event as a matter of accuracy and to reflect the common, consensus definition of 'GOE' in the scientific literature. This point has been made earlier (see Hartmann Schedel) above and was ignored. I'm adding to his argument to say that what he said is obviously and unequivocally correct. Charliecat1 (talk) 04:51, 22 September 2016 (UTC)

It is mentioned in the lede and there is a redirect to this article from "Great Oxidation Event", agree about "oxygen holocaust" and "oxygen catastrophe". More "scholarly articles" on Google for "oxidation" than oxygenation. I don't know how to move a page or I'd do it. Raquel Baranow (talk) 19:46, 22 September 2016 (UTC)

The link given to the article "Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry", was broken. This one works for me Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry — Preceding unsigned comment added by Pedro Lamo (talk • contribs) 07:13, 23 April 2017 (UTC)

References

Not appropriate language

The increased production of oxygen set Earth's original atmosphere off balance.

In my experience, "balance" has more truck in Humorism than in geophysics or ecology. A more precise word is "equilibrium". By virtue of being more precise, one can immediately see why it shouldn't be used here (to usefully discuss an "equilibrium" requires a broadly accepted mathematical framework, which I doubt we have concerning the earth's conditions at 3 Gya).

"Brought a new dynamic into play" would be a rough order of magnitude less grievous, which perhaps brings it into the territory of the barely palatable. — MaxEnt 16:29, 17 July 2017 (UTC)

External links modified

Hello fellow Wikipedians,

I have just modified 2 external links on Great Oxygenation Event. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:

• Added archive https://web.archive.org/web/20110106141826/http://ptc-cam.blogspot.com/2010/02/first-breath-earths-billion-year.html to http://ptc-cam.blogspot.com/2010/02/first-breath-earths-billion-year.html
• Added archive https://web.archive.org/web/20110106141826/http://ptc-cam.blogspot.com/2010/02/first-breath-earths-billion-year.html to http://ptc-cam.blogspot.com/2010/02/first-breath-earths-billion-year.html

When you have finished reviewing my changes, you may follow the instructions on the template below to fix any issues with the URLs.

This message was posted before February 2018. After February 2018, "External links modified" talk page sections are no longer generated or monitored by InternetArchiveBot. No special action is required regarding these talk page notices, other than regular verification using the archive tool instructions below. Editors have permission to delete these "External links modified" talk page sections if they want to de-clutter talk pages, but see the RfC before doing mass systematic removals. This message is updated dynamically through the template {{source check}} (last update: 5 June 2024).

• If you have discovered URLs which were erroneously considered dead by the bot, you can report them with this tool.
• If you found an error with any archives or the URLs themselves, you can fix them with this tool.

Cheers.—InternetArchiveBot (Report bug) 01:46, 23 October 2017 (UTC)

Water/atmosphere

"Before the GOE, any free oxygen they produced was chemically captured by dissolved iron or organic matter. The GOE was the point in time when these oxygen sinks became saturated, at which point oxygen, produced by the cyanobacteria, was free to escape into the atmosphere."

It looks like there must have been two overlapping phases to the oxidation event: oxidation of minerals dissolved in water, and oxidation of land minerals. The paragraph above discusses water, while another paragraph discusses land rock, but there doesn't seem to be anything joining the two, so that if you don't notice you may think that the oxidation only applied to one. Scott McNay (talk) 18:31, 18 December 2017 (UTC)

New Findings

"Two-billion-year-old salt rock reveals rise of oxygen in ancient atmosphere". Princeton. 22 March 2018. 2001:BB6:4703:4A58:ED30:9F33:3B3:D255 (talk) 16:07, 24 March 2018 (UTC)

Was the great oxygenation event a mass extinction?

Although many biology sources state this as a fact, the evidence isn't that strong. Nick Lane put it like this[1]:

"Microbes are not equivalent to large animals: their population sizes are enormously larger, and they pass around useful genes (such as those for antibiotic resistance) by lateral transfer, making them very much less vulnerable to extinction. There is no hint of any microbial extinction even in the aftermath of the Great Oxygenation Event. The 'oxygen holocaust', which supposedly wiped out most anaerobic cells, can't be traced at all; there is no evidence from either phylogenetics or geochemistry that such an extinction ever took place. On the contrary, anaerobes prospered."

I think this viewpoint should be mentioned Robert Walker (talk) 16:45, 7 April 2018 (UTC)

Looks like a reliable source and an important viewpoint. WP:BOLD. --Kent G. Budge (talk) 01:06, 8 April 2018 (UTC)

Regarding the latest 'citation needed' tag: an alternative explanation to an 'oxygen holocaust' might be that the anaerobic cells were less efficient at survival, in the face of competition from the cyanobacteria. In the face of the competitive advantage of the cyanobacteria over a billion years, the niches for anaerobic cells might have been simply outnumbered after a loss of habitat, from the development of multicellular organisms, according to Schirrmeister et.al. (2015) "Cyanobacteria and the Great Oxidation Event: evidence from genes and fossils". Might this possibility, of an indirect result, be included in the article. --Ancheta Wis   (talk | contribs) 12:53, 3 July 2018 (UTC)

I still maintain that a lot of literature etc. was created with the idea that it was a Catastrophe and an Extinction, so some clear reference to this piece of scientific history- an explanation of why they thought it was and why we don't think it is now, should be made, with a subtitle of one or other of these titles. IceDragon64 (talk) 23:47, 14 February 2024 (UTC)

Requested move 10 June 2019

The following is a closed discussion of a requested move. Please do not modify it. Subsequent comments should be made in a new section on the talk page. Editors desiring to contest the closing decision should consider a move review after discussing it on the closer's talk page. No further edits should be made to this discussion.

The result of the move request was: moved  — Amakuru (talk) 08:06, 18 June 2019 (UTC)

---

Great Oxygenation Event → Great Oxidation Event – Great Oxidation Event is the commonly used term in scientific paper and sources PLin AB (talk) 06:04, 10 June 2019 (UTC)

This is a contested technical request (permalink) by PLin AB. Steel1943 (talk) 18:51, 10 June 2019 (UTC)

Needs discussion since this is a WP:COMMONNAME claim that is not inherently obvious. Steel1943 (talk) 18:51, 10 June 2019 (UTC)

• Support per GScholar hits 4870 for "Great Oxidation Event" v. 1330 for "Great Oxygenation Event". Shyamal (talk) 14:40, 12 June 2019 (UTC)

• Please note that in earlier talk (item 23 in the Talk Table of Contents) there is discussion under the heading "Page is misnamed: GOE is defined by leading researchers in this area as Great Oxidation Event in the scientific literature". In that earlier discussion, the point was made that the event was originally named the "Great Oxidation Event" by Heinrich Holland (Professor of Geochemistry at Harvard University) in 1999 (in this article - http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.452.6871&rep=rep1&type=pdf ). If you restrict the date range in GScholar, you can verify the claim (taking account of mis-hits that inadvertently bring up post-1999 citations). It appears that one group in 2001 then called the phenomenon the Great Oxygenation Event (Rae et al., 2001), perhaps in error, but it didn't catch on much, with Great Oxidation Event outnumbering the alternative name about 5 to 1 in the next 5 years. Since then, the oxygenation name has gained slightly, but researchers have gone with the original name of Great Oxidation Event by more than 3 to 1 overall as Shyamal noted. It seems clear cut, so if this is "contested" request, contested by whom and with what justification? DCCProf (talk) 06:50, 13 June 2019 (UTC)

---

The above discussion is preserved as an archive of a requested move. Please do not modify it. Subsequent comments should be made in a new section on this talk page or in a move review. No further edits should be made to this section.

Dubious

The abstract of the paywalled source does not say rise in O2 caused extinctions. Rather, it notes that an extinction is observed in the fossil record, and suggests that hiccups in phosphorous availability was to blame. NewsAndEventsGuy (talk) 12:32, 5 September 2019 (UTC)

I partially agree. The source abstract suggests that rise in O2 set in motion other changes - that led to restricted phosphorous availability - which then caused the extinctions. At minimum, the sentence needs elaboration, to give a plausible chain of consequences from increased atmospheric O2, to extinctions. I haven't read the source, so I don't know whether it has those details, or references a source that explains a possible mechanism. ToolmakerSteve (talk) 22:46, 5 September 2019 (UTC)

It was recently added here, I think it should be deleted. Raquel Baranow (talk) 05:02, 3 January 2020 (UTC)

Missing details about land sinks and productiviy collapse

First issue: https://wiki.riteme.site/wiki/File:Oxygenation-atm-2.svg refers in stage 3 to the absorption of oxygen after outgassing. However, there are virtually no further details about this in the main text. Second issue: https://www.pnas.org/doi/full/10.1073/pnas.1900325116 finds large decrease in nutrients supplied to the biosphere that, in turn, marked the conclusion of the GOE. There is also no description of this in the main text. — Preceding unsigned comment added by 2A02:2454:8D55:500:CE2:26BF:E8DB:6FDE (talk) 07:02, 24 June 2023 (UTC)