In the past, there were five major extinction events (a widespread and rapid decrease in the biodiversity on Earth), and a lot of minor ones. Now, unfortunately, we are in the middle of the sixth major extinction event, called “Holocene extinction event”. And the cause is… guess what? Humans.
According to the WWF’s (World Wildlife Fund) new Living Planet Report (2016), now we are in the middle of the biggest mass extinction on Earth, since the dinosaurs, which was around 65 million years ago. And the world set to lose two-thirds of its wildlife by as close as 2020.
The situation is really, really bad. WWF published a declaration on their web site titled “Urgent Action Needed” and said that:
Global biodiversity is declining at an alarming rate, putting the survival of other species and our own future at risk. The latest edition of WWF’s Living Planet Report brings home the enormity of the situation – and how we can start to put it right. The Living Planet Index reveals that global populations of fish, birds, mammals, amphibians and reptiles declined by 58 per cent between 1970 and 2012. We could witness a two-thirds decline in the half-century from 1970 to 2020 – unless we act now to reform our food and energy systems and meet global commitments on addressing climate change, protecting biodiversity and supporting sustainable development.
Major Extinction Event List
- Ordovician–Silurian extinction events (450–440 Ma(1)): 60% to 70% of all species were gone. Possible causes: global cooling and sea level drop; and/or a Gamma-ray burst.
- Late Devonian extinction (375–360 Ma): The second largest extinction in Earth’s history. At least 70% of all species were gone. Possible causes: bolide impact, plant evolution and its effects on weather and CO2 levels, or magmatism(2).
- Permian–Triassic extinction event (252 Ma): Dubbed as the “mother of all extinctions”, it is the biggest extinction event ever, 90% to 96% of all species were gone. Possible causes: bolide impact, volcanism, methane hydrate gasification, widespread ocean anoxia (severe deficiency of oxygen) and euxinia (presence of hydrogen sulfide), the formation of Pangaea, microbes.
- Triassic–Jurassic extinction event (201.3 Ma): 70% to 75% of all species became extinct. Dinosaurs’ age begins: most non-dinosaurian archosaurs, most therapsids, and most of the large amphibians were eliminated, leaving dinosaurs with little terrestrial competition. Possible causes: bolide impact, Ggradual climate change, sea-level fluctuations or a pulse of oceanic acidification, massive volcanic eruptions.
- Cretaceous–Paleogene extinction event (66 Ma): 75% of all species, including dinosaurs (except avian dinosaurs) became extinct. Possible cause: bolide impact (Chicxulub impactor).
- Holocene extinction event (c. 10,000 BCE – Ongoing): two-thirds of the world’s wildlife will be extinct by 2020. Cause: humans.
- Traditionally, geologists have used different abbreviations for ages (time before present) and duration (amount of time elapsing between two different events). Ages are abbreviated from Latin: Ga (giga-annum) is a billion years, Ma (mega-annum) is a million years, ka (kilo-annum) is a thousand years.
- Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. Volcanism is the surface expression of magmatism.