Chapter 1: Mass Extinctions
In the following chapters, we will encounter several taxonomic terms like species, genus or order. Let’s clarify this with two classification examples human vs buttercup:
So, any life-form can be categorized in the taxonomic tree according to the seven taxa it belongs to: species, genus, family, order, class, phylum and kingdom. If fact, it's a bit more complicated than that with numerous subcategories like subphylum or subfamily, but for our purpose this level of details is useless.
After this short preamble, let’s address the main topic: mass extinctions. Far from the gradualist uniformitarian paradigm held by mainstream science, the history of our planet shows a recurring pattern of catastrophic destruction.
Rather than being an exception catastrophe-induced mass extinctions are the rule. So far Earth has officially experienced 5 major mass extinctions:
• Ordovician–Silurian extinction that occurred 450–440 Mya[1]. It obliterated 60% to 70% of all species[2].
• Late Devonian extinction that happened 375–360 Mya, which eliminated at least 70% of all species.[3]
• Permian–Triassic extinction, 252 Mya, during which 90% to 96% of all species[4] died. This is the largest known mass extinction[5].
• Triassic–Jurassic extinction, 201 Mya when about 70% of all species disappeared[6].
• Cretaceous–Paleogene extinction, 66 Mya, the wipe out the dinosaurs. In total about 75% of all species became extinct[7].
This count of five mass extinctions is arbitrary and rather conservative. Actually, our planet experienced way more than those five mass extinctions usually recognized by mainstream literature if one factors in the following event:
• The above mentioned late-Devonian mass extinction is actually constituted of three distinct extinction events[8]: the Taghanic Event, the Kellwasser Event and the Hangenberg Event spread over almost 30 Mya as indicated by the three black dots in the diagram below.
• The three major Cambrian extinctions[9], as shown by the three black arrows in the diagram below. The latest one was the Cambrian–Ordovician extinction event ca. 488 Mya. It was preceded by the less documented Dresbachian extinction event about 502 Mya, which annihilated approximately 40% of marine genera[10] and the End-Botomian extinction event ca. 517 Mya which removed up to 80% of marine genera[11]
• The mid-Ordovician extinction, also known as the Ordovician Meteor Event[12] happened ca. 467 Mya and wiped out about 15% of genera. It is shown by the white arrow in the graph below.
• The end-Silurian extinction also known as the Silurian-Devonian boundary. Made of three minor extinctions closely interspaced, namely the Lau event ca. 424 Mya[13], the Mulde event ca. 427 Mya[14] and the Ireviken event ca. 433 Mya. These three events caused high extinction rates among conodonts[15], graptolites[16] and trilobites[17].
• The extinction known as the late Middle Permian extinction ca. 270 Mya, as shown by the light grey arrow, that preceded the Permian-Triassic extinction by about 20 million and erased between 25 and 47% genera extinction rate[18]
• The dozen or so milder extinctions that interspersed the major ones:
- the end-Eocene extinction[19] ca. 34 Mya, which eradicated 60% of Africa primates[20]
- The Cenomanian-Turonian boundary event[21] ca. 93 Mya as shown by the gradient arrow in the diagram below. This event caused the demise of several type of dinosaurs and the extinction of 27% marine invertebrates[22]
- the Jurassic-Cretaceous extinction[23] ca. 145 Mya that eliminated about 15% of the species
- the Carboniferous-Permian extinction ca. 305 Mya also known as the Carboniferous rainforest collapse[24], shown by the dark grey arrow in the diagram below
- the mid-Carboniferous extinction[25] ca. 325 Mya which killed about 25% of the genera
- the end-Silurian extinction[26] about 420 Mya, that was particularly hard on brachiopods[27] and conodonts[28].
• The extinctions that predate the Cambrian. According to researcher Andrew Rhys Jones, before the Cambrian (ca. 540 Mya) there were four mass extinctions:
Prior to the evolution of macroscopic multicellular eukaryotes and the first metazoans, there may have been four mass extinctions of an unknown number of prokaryotic and microscopic eukaryotic species (Elewa & Joseph, 2009, Joseph 2009a). These have been referred to as the Paleoproterozoic (2.3 to 1.8 bya), the Sturtian (725 mya to 670 mya), the Marinoan/Gaskiers (640 to 580 mya), and the Ediacaran extinctions (540 mya), and with the exception of the latter, each was related to worldwide periods of prolonged glaciation that developed over millions of years of time.[29]
If one counts the extinction events described above, the real number of mass extinctions experienced by our planet is not 5 but more likely comprised between 20 and 30.
A few numbers might convey the astounding rate of replacement of life-forms: according to estimates between 5 and 50 billion species have lived on the Earth and humans have only found evidence of about 50 million of them[30]. Based on these figures, about 99.9% of all species that ever lived on Earth have now disappeared. Part of these 99.9% extinction occurred during mass extinction, as illustrated by the difference between the extinction rate during mass extinction (15-50%) and the background extinction rate of about 4% shown in the diagram below:
[1] Million years Ago
[2] Baez, John. (2006). “Extinction”. University of California, Riverside, Department of Mathematics
[3] Briggs, Derek; Crowther, Peter R. (2008). “Palaeobiology II”. John Wiley & Sons. p. 223
[4] Baez, 2006.
[5] Ibid
[6] Ibid
[7] Raup, D.; Sepkoski Jr, J. (1982). "Mass extinctions in the marine fossil record". Science. 215 (4539): 1501–03.
[8] Britannica, The Editors of Encyclopaedia. (2021). "Devonian Period". Encyclopedia Britannica
[9] National Geographics Editors. (2020). ”The Cambrian Period”. National Geographics
[10] David P.G. Bond et al. (2017). “On the causes of mass extinctions”. Palaeogeography, Palaeoclimatology, Palaeoecology, Volume 478, Pages 3-29.
[11] Signor, Philip W. (1992). "Taxonomic diversity and faunal turnover in the Early Cambrian: Did the most severe mass extinction of the Phanerozoic occur in the Botomian stage?". The Paleontological Society Special Publications. 6: 272.
[12] Korochantseva, Ekaterina; et al. (2007). "L-chondrite asteroid breakup tied to Ordovician meteorite shower by multiple isochron 40 Ar- 39 Ar dating". Meteoritics & Planetary Science. 42 (1): 113–130.
[13] Urbanek, A. (1993). "Biotic crises in the history of Upper Silurian graptoloids: a palaeobiological model". Historical Biology. 7: 29–50.
[14] Jeppsson, L.; Calner, M. (2007). "The Silurian Mulde Event and a scenario for secundo—secundo events". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 93 (02): 135–154.
[15] Jarochowska, et al. (2017). "Harnessing stratigraphic bias at the section scale: Conodont diversity in the Homerian (Silurian) of the Midland Platform, England". Palaeontology. 61: 57–7
[16] Urbanek, A. (1993). "Biotic crises in the history of Upper Silurian graptoloids: a palaeobiological model". Historical Biology. 7: 29–50.
[17] Munnecke, A. et al. (2003). "The Ireviken Event in the lower Silurian of Gotland, Sweden-relation to similar Palaeozoic and Proterozoic events". Palaeogeography, Palaeoclimatology, Palaeoecology. 195 (1): 99–124.
[18] Hecht, Jeff . (2014). “Missing' disaster led to all-time worst extinction”. New Scientist
[19] Prothero, D. R. (1994). “The Late Eocene-Oligocene Extinctions”. Annual Review Of Earth And Planetary Sciences, Volume 22, pp. 145-165.
[20] Dorien de Vries et al. (2021) “Widespread loss of mammalian lineage and dietary diversity in the early Oligocene of Afro-Arabia”, Communications Biology
[21] Martin A. Pearce et al. (2009). “ The Cenomanian–Turonian boundary event, OAE2 and palaeoenvironmental change in epicontinental seas: New insights from the dinocyst and geochemical records”. Palaeogeography, Palaeoclimatology, Palaeoecology, Volume 280, Issues 1–2, Pages 207-234
[22] New Scientist Editors (2008). "Submarine eruption bled Earth's oceans of oxygen". New Scientist.
[23] Tennant, J.P. et al. (2017), “Biotic and environmental dynamics through the Late Jurassic–Early Cretaceous transition: evidence for protracted faunal and ecological turnover”. Biol Rev, 92: 776-814.
[24] Sahney, S. et al. (2010). "Rainforest collapse triggered Pennsylvanian tetrapod diversification in Euramerica". Geology. 38 (12): 1079–1082.
[25] W. B. Saunders, W.H.C. Ramsbottom. (1986). The mid-Carboniferous eustatic event. Geology. 14 (3): 208–212.
[26] Calner, Mikael. (2005). “A Late Silurian extinction event and anachronistic period”. Geology. 33. 10.1130/G21185.1.
[27] Colloquial called sea shells. Phylum containing about 400 living species grouped into over 120 genera.
[28] Extinct group of vertebrates resembling eels.
[29] Jones, Andrew. (2009), “The Next Mass Extinction: Human Evolution or Human Eradication”. Journal of Cosmology, Vol 2, pp. 316-333.
[30] Prothero, Donald. (2013). “Bringing Fossils to Life: An Introduction to Paleobiology”. Columbia University Press.
Attachments
Last edited: