The Holocene extinction, sometimes called the Sixth Extinction, is a name proposed to describe the extinction event of species that has occurred during the present Holocene epoch (since around 10,000 BC). The large number of extinctions span numerous families of plants and animals including mammals, birds, amphibians, reptiles and arthropods. Although 875 extinctions occurring between 1500 and 2009 have been documented by the International Union for Conservation of Nature and Natural Resources, the vast majority are undocumented. According to the species-area theory and based on upper-bound estimating, up to 140,000 species per year may be the present rate of extinction.
The Holocene extinction includes the disappearance of large mammals known as megafauna, starting between 9,000 and 13,000 years ago, the end of the last Ice Age. Such disappearances are considered to be results of both climate change and the proliferation of modern humans. These extinctions, occurring near the Pleistocene–Holocene boundary, are sometimes referred to as the Quaternary extinction event. The Holocene extinction continues into the 21st century.
There is no general agreement on whether to consider more recent extinctions as a distinct event, merely part of the Quaternary extinction event, or just a result of natural evolution on a non-geologic scale of time. Only during these most recent parts of the extinction have plants also suffered large losses. Overall, the Holocene extinction can be characterised by humanity's presence.
Prehistoric extinctions 
||This section's tone or style may not reflect the encyclopedic tone used on Wikipedia. (September 2008)|
||This section needs additional citations for verification. (October 2012)|
North and South America 
There was a debate as to the extent to which the disappearance of megafauna at the end of the last glacial period can be attributed to human activities, directly, by hunting, or indirectly, by decimation of prey populations. Recent discoveries at Monte Verde in South America, and at Meadowcroft Rock Shelter in Pennsylvania have effectively ended the "clovis first" position of American Archaeology and pushed the arrival of humans in the Americas back many thousands of years. This coupled with a more complete fossil record of the extinct animals has weakened the correlation between human occupation and mega-fauna extinction in the Americas. However around the world there is often a very strong correlation between human arrival and megafauna extinction, an example being Wrangel Island in Siberia, where the extinction of Mammoths (approximately 2000 bce) coincided directly with the arrival of humans. Furthermore, the success of mega-fauna in surviving previous more severe periods of climate change suggest natural events were not entirely to blame.
The ongoing extinction seems more outstanding in light of separating recent extinctions (approximately since the industrial revolution) from the Pleistocene extinction near the end of the last glacial period. The latter is exemplified by the extinction of large herbivores such as the woolly mammoth and the carnivores that preyed on them. Therefore, the logical basis for the theory may be flawed, since it presumes that early Americans, despite being only a slight fraction of the population of industrial era America and armed with rudimentary tools, were many times more destructive than later historic humans who engaged in the often deliberate eradication of species. However it should be considered that the ecosystems encountered by the first Americans had not been exposed to human interaction and were far less resilient to man made changes than the ecosystems encountered by industrial era humans, those environments seasoned as they were, having been exposed to over 10,000 years of human interaction. Therefore the actions of the Clovis people and likewise, despite seeming insignificant by today's standards could indeed have had a profound effect on the ecosystems and wild life which was entirely unused to human influence.
New Zealand 
Circa 1500, several species became extinct after Polynesian settlers arrived, including:
- Ten species of Moa, giant flightless ratite birds.
- The giant Haast's Eagle, Harpagornis
- The flightless predatory Adzebills.
Pacific, including Hawaii 
Recent research, based on archaeological and paleontological digs on 70 different islands, has shown that numerous species went extinct as people moved across the Pacific, starting 30,000 years ago in the Bismarck Archipelago and Solomon Islands. It is currently estimated that among the bird species of the Pacific some 2000 species have gone extinct since the arrival of humans. Among the extinctions were:
- The Moa-nalos, grazing ducks from Hawaii.
- The Nēnē-nui, or Woodwalking Goose, an extinct species of goose that once inhabited Maui.
- A giant megapode from New Caledonia.
- Mekosuchine crocodiles from New Caledonia, Fiji and Samoa.
Ten species or subspecies of birds have disappeared from the Hawaiian islands since the 1980s. These include the Kaua'i O'o, Nukupu'u, 'Akialoa, Kama'o, Po'ouli, and others.
Starting with the arrival of humans around 2000 years ago, nearly all of the island's megafauna became extinct, including:
- Eight species of elephant birds, giant flightless ratites in the genera Aepyornis and Mullerornis.
- 17 species of lemur, known as giant, subfossil lemurs, including:
- Giant Aye-aye (Daubentonia robusta)
- Sloth lemurs, including chimpanzee-sized Palaeopropithecus and gorilla-sized Archaeoindris
- Koala lemurs (Megaladapis), a koala-like, orangutan-sized arboreal lemur
- Monkey lemurs, most terrestrial of lemurs, often compared to baboons or macaques.
- Pachylemur, a genus of giant ruffed lemurs
- Giant Fossa
- Plesiorycteropus, a genus containing two species of digging mammal unlike anything alive today
- Two species of Malagasy Hippopotamus
Indian Ocean Islands 
Starting c. 1500, a number of species became extinct upon human settlement of the islands, including:
- several species of giant tortoise on Seychelles and Mascarene Islands
- 14 species of birds on the Mascarene Islands, including the Dodo, the Rodrigues Solitaire, and the unrelated Réunion Solitaire.
Ongoing Holocene extinction 
One scientist estimates the current extinction rate may be 10,000 times the background extinction rate. Nevertheless most scientists predict a much lower extinction rate than this outlying estimate. Stuart Pimm stated "the current rate of species extinction is about 100 times the natural rate" for plants, and the number of extinctions that we have actually documented suggests we're on par with the background rate (1-10 species lost per year). Mass extinctions are characterized by the loss of at least 75% of species within a geologically short period of time.
Megafaunal extinctions continue into the 21st century. Modern extinctions are more directly attributable to human influences. Extinction rates are minimized in the popular imagination by the survival of captive populations of animals that are extinct in the wild (Père David's Deer, etc.), by marginal survivals of highly publicized megafauna that are ecologically extinct (the Giant Panda, Sumatran Rhinoceros, North American Black-Footed Ferret, etc.) and by extinctions among arthropods. Some examples of modern extinctions of "charismatic" mammal fauna include:
- Aurochs, Europe
- Tarpan, Europe
- Thylacine or Tasmanian Tiger, Thylacinus cynocephalus, Tasmania
- Quagga, a zebra subspecies, Southeast Africa
- Steller's Sea Cow
- Pyrenean Ibex
- Falkland Islands Wolf
- Atlas Bear
- Caribbean Monk Seal
- The closely related Bali Tiger and Javan Tiger
- Eastern Cougar
- Western Black Rhinoceros
Many birds have become extinct as a result of human activity, especially birds endemic to islands, including many flightless birds (see a more complete list under extinct birds). Notable extinct birds include:
- the Dodo, the giant flightless pigeon of Mauritius, Indian Ocean
- the Great Auk of islands in the north Atlantic
- the Passenger Pigeon of North America
- several species of Moa, giant flightless birds from New Zealand
- the Carolina Parakeet of the American southeast
The decline of amphibian populations has also been identified as an indicator of environmental degradation.
Peter Raven, past President of the American Association for the Advancement of Science (AAAS), states in the foreword to their publication AAAS Atlas of Population and Environment: "We have driven the rate of biological extinction, the permanent loss of species, up several hundred times beyond its historical levels, and are threatened with the loss of a majority of all species by the end of the 21st century."
189 countries which are signatory to the Convention on Biological Diversity (Rio Accord) have committed to preparing a Biodiversity Action Plan, a first step at identifying specific endangered species and habitats, country by country.
Human influence on extinction 
Extinction of animals, plants, and other organisms caused by human actions may go as far back as the late Pleistocene, over 12,000 years ago. There is evidence that abrupt climate change has especially played an enormous role in the extinction of larger mammals. However, while previous mass extinctions were due to natural environmental causes, research shows that wherever on Earth humans have migrated, other species have gone extinct, and human overpopulation, most prominently in the past two centuries, is regarded as one of the underlying causes of this Holocene extinction event. In terms of how humans have contributed to this mass extinction, three major factors include how humans: have increased the global concentration of greenhouse gases, affecting global climate; have been culpable for oceanic devastation, such as overfishing and contamination; and have modified and destroyed vast tracts of land and river systems around the world to meet solely human-centered ends (with 10 to 15 percent of Earth's land surface now used as urban-industrial or row-crop agricultural sites and 6 to 8 percent used as pastures), thus ruining the local ecosystems. Other, related human causes of the extinction event include deforestation, hunting, pollution, the introduction in various regions of non-native species, and the widepsread transmission of infectious diseases. At present, the rate of extinction of species is estimated at 100 to 1000 times higher than the "base" or historically typical rate of extinction (in terms of the natural evolution of the planet) and also the current rate of extinction is, therefore, 10 to 100 times higher than any of the previous mass extinctions in the history of Earth. On the other hand, this extinction concerns a large number of plants, different from previous extinctions.
The abundance of species extinctions considered anthropogenic, or due to human activity, have sometimes (especially when referring to hypothesized future events) been collectively called the "Anthropocene extinction". The Anthropocene is a term introduced in 2000. Most biologists believe that we are at the beginning of an anthropogenic mass extinction that is accelerating at a terrifying rate. In The Future of Life (2002), E.O. Wilson of Harvard calculated that, if the current rate of human disruption of the biosphere continues, one-half of Earth's higher lifeforms will be extinct by 2100. A 1998 poll conducted by the American Museum of Natural History found that seventy percent of biologists believe that we are in the midst of an anthropogenic extinction. Numerous scientific studies—such as a 2004 report published in Nature, and papers authored by the 10,000 scientists who contribute to the IUCN's annual Red List of threatened species—have since reinforced this conviction. Numerous scientific studies since then—as the 2004 report of the journal Nature, as well as the 10,000 scientists who contribute to the IUCN Red List Annual International Union for the Conservation of endangered species—have only strengthened this consensus.
The evidence of all previous extinctions is geological in nature, and shorter geological time scale is of the order of several hundred thousand to several million years. Even extinctions caused by instantaneous events such as the impact of the asteroid in Chicxulub, which is currently the best example, extend the equivalent of many human lives, due to complex ecological interactions that are triggered by the event.
Recent extinctions described are well-documented, but the nomenclature used varies. The term Anthropocene is a term that is used by few scientists, and some commentators may refer to the current and projected future extinctions as part of a longer Holocene extinction. The Holocene–Anthropocene boundary is contested, with some commentators asserting significant human influence on climate for much of what is normally regarded as the Holocene Epoch. Other commentators place the Holocene–Anthropocene boundary at the industrial revolution while also saying that "Formal adoption of this term in the near future will largely depend on its utility, particularly to earth scientists working on late Holocene successions. "
Three hypotheses have been proposed to explain the extinction of megafauna in the late Pleistocene. Of these, only two have much scientific credibility. Although Ross McPhee proposed that a hyper-disease may have been the cause of the extinction, the study by Lyons et al., demonstrated conclusively that a hyperdisease was unlikely to have caused the extinction. The two main theories to the extinction are climate change and human hunting. The climate change theory has suggested that a change in climate near the end of the late Pleistocene stressed the megafauna to the point of extinction. Most scientists favor abrupt climate change as the catalyst for the extinction of the mega-fauna at the end of the Pleistocene, but there are many who believe increased hunting from early modern humans also played a part.
See also 
- "Extinction continues apace". International Union for Conservation of Nature. 3 November 2009. Retrieved 18 October 2012.
- S.L. Pimm, G.J. Russell, J.L. Gittleman and T.M. Brooks, The Future of Biodiversity, Science 269: 347–350 (1995)
- Steadman & Martin 2003
- Steadman 1995
- J.H.Lawton and R.M.May, Extinction Rates, Oxford University Press, Oxford, UK
- Has Plant Life Reached Its Limits? September 20, 2012
- Baillie, The IUCN species survival commission ; Jonathan E. M.; Bennun, Leon A.; Baillie, Thomas M. Brooks,... [et al.] ; ed. by Jonathan E. M.; Hilton-Taylor, Craig; Brackett, Simon N. Stuart ; foreword by Hamdallah Zedan ; preface by David (2004). 2004 IUCN red list of threatened species : a global species assessment. Cambridge [etc.]: International union for conservation of nature and natural resources. ISBN 2-8317-0826-5.
- Barnosky, Anthony D.; Matzke, Nicholas; Tomiya, Susumu; Wogan, Guinevere O. U.; Swartz, Brian; Quental, Tiago B.; Marshall, Charles; McGuire, Jenny L.; Lindsey, Emily L.; Maguire, Kaitlin C.; Mersey, Ben; Ferrer, Elizabeth A. (3 March 2011). "Has the Earth’s sixth mass extinction already arrived?". Nature 471 (7336): 51–57. doi:10.1038/nature09678.
- Wilson, Edward O. (2003). The Future of life. (1st Vintage Books ed. ed.). New York: Vintage Books. ISBN 9780679768111.
- C.Michael Hogan. 2010. Edenic Period. Encyclopedia of Earth. National Council for Science and Environment. ed. Galal Hassan, ed in chief Cutler Cleveland, Washington DC
- Rubinkam, Michael (2 March 2011). "Federal researchers declare eastern cougar extinct". Salon.com. Retrieved 18 October 2012.
- "Atlas of Population and Environment". AAAS. 2000. Retrieved 2008-02-12.
- "Atlas of Population and Environment, Foreword". American Association for the Advancement of Science (AAAS). 2000. Retrieved 2008-02-12.
- Lions, tigers, big cats may face extinction in 20 years by Dan Vergano, USA Today
- Exotic animals: 18 tiger deaths a cruel blow to imperiled species October 20, 2011 LA Times
- Jaguars cling to survival in Argentina's forests by Kylie Stott Tue Oct 11, 2011 Reuters
- Poachers Drive Javan Rhino to Extinction in Vietnam by John R. Platt October 25, 2011 Scientific American
- Zalasiewicz, Jan; Williams, Mark; Smith, Alan; Barry, Tiffany L.; Coe, Angela L.; Bown, Paul R.; Brenchley, Patrick; Cantrill, David; Gale, Andrew; Gibbard, Philip; Gregory, F. John; Hounslow, Mark W.; Kerr, Andrew C.; Pearson, Paul; Knox, Robert; Powell, John; Waters, Colin; Marshall, John; Oates, Michael; Rawson, Peter; Stone, Philip (2008). "Are we now living in the Anthropocene". GSA Today 18 (2): 4. doi:10.1130/GSAT01802A.1.
- "Human Population Growth and Extinction". Center for Biological Diversity.
- Vitousek, P. M.; Mooney, H. A.; Lubchenco, J.; Melillo, J. M. (1997). "Human Domination of Earth's Ecosystems". Science 277 (5325): 494–499.
- Pimm, S. L. 2001.
- "Measuring extinction, species by species". The Economic Times. 2008-11-06. Retrieved 2010-05-20.
- Lawton, J. H. and May, R. M. (1995). Journal of Evolutionary Biology (Oxford: Oxford University Press).
- Wooldridge, S. A. (9 June 2008). "Mass extinctions past and present: a unifying hypothesis". Biogeosciences Discuss (Copernicus) 5 (3): 2401–2423. doi:10.5194/bgd-5-2401-2008.
- Jackson, J. B. C. (Aug 2008). "Colloquium paper: ecological extinction and evolution in the brave new ocean" (Free full text). Proceedings of the National Academy of Sciences of the United States of America 105 (Suppl 1): 11458–11465. Bibcode:2008PNAS..10511458J. doi:10.1073/pnas.0802812105. ISSN 0027-8424. PMC 2556419. PMID 18695220.
- American Museum of Natural History Press Release
- Study sees mass extinctions via warming. MSNBC. URL accessed July 26, 2006.
- Elewa, Ashraf M. T. "14. Current mass extinction". In Elewa, Ashraf M. T. Mass Extinction. pp. 191–194. doi:10.1007/978-3-540-75916-4_14.
- Mason, Betsy (10 December 2003). "Man has been changing climate for 8,000 years". Nature. doi:10.1038/news031208-7.
- MacPhee and Marx published their hyperdisease hypothesis in 1997. "The 40,000-year plague: Humans, hyperdisease, and first-contact extinctions." In S. M. Goodman and B. D. Patterson (eds), Natural Change and Human Impact in Madagascar, pp 169-217, Smithsonian Institution Press: Washington DC.
- Lyons, S. Kathleen; Smith, Felisa A.; Wagner, Peter J.; White, Ethan P.; Brown, James H. (2004). "Was a ‘hyperdisease’ responsible for the late Pleistocene megafaunal extinction?". Ecology Letters 7 (9): 859–868. doi:10.1111/j.1461-0248.2004.00643.x.
- Graham, R. W. and Mead, J. I. 1987. Environmental fluctuations and evolution of mammalian faunas during the last deglaciation in North America. In: Ruddiman, W. F. and H.E. Wright, J., editors. North America and Adjacent Oceans During the Last Deglaciation. Volume K-3. The Geology of North America, Geological Society of America
- Martin P. S. (1967). Prehistoric overkill. In Pleistocene extinctions: The search for a cause (ed. P.S. Martin and H.E. Wright). New Haven: Yale University Press. ISBN 0-300-00755-8.
- Lyons, S.K., Smith, F.A., and Brown, J.H. (2004). "Of mice, mastodons and men: human-mediated extinctions on four continents". Evolutionary Ecology Research 6: 339–358. Retrieved 18 October 2012.
Further reading 
- Firestone RB, West A, Kennett JP, et al. (October 2007). "Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling". Proceedings of the National Academy of Sciences of the United States of America 104 (41): 16016–21. Bibcode:2007PNAS..10416016F. doi:10.1073/pnas.0706977104. PMC 1994902. PMID 17901202.
- Kolbert, Elizabeth (May 25 2009). "The Sixth Extinction? There have been five great die-offs in history. This time, the cataclysm is us.". The New Yorker. Retrieved May 2012.
- Leakey, Richard; Lewin, Roger (1996). The Sixth Extinction: Patterns of Life and the Future of Humankind. New York: Anchor Books. ISBN 0-385-46809-1.
- Loarie, Scott R.; Duffy, Philip B.; Hamilton, Healy; Asner, Gregory P.; Field, Christopher B.; Ackerly, David D. (2009). "The velocity of climate change". Nature 462 (7276): 1052–1055. doi:10.1038/nature08649. PMID 20033047.
- Martin, P. S.; Wright, H. E. Jr. (eds.) (1967). Pleistocene Extinctions: The Search for a Cause. New Haven: Yale University Press. ISBN 0-300-00755-8.
- Marsh, Bill (1 June 2012). "Are We in the Midst Of a Sixth Mass Extinction?". The New York Times Sunday Review: Opinion Page. Retrieved 18 October 2012.
- Nihjuis, Michelle (23 July 2012). "Conservationists Use Triage to Determine Which Species to Save and Not". Scientific American.
- Ted Oakes (2003). Land of Lost Monsters: Man Against Beast--The Prehistoric Battle for the Planet. Hylas Publishing. ISBN 1-59258-005-X.
- Steadman, D. W. (1995). "Prehistoric extinctions of Pacific island birds: biodiversity meets zooarchaeology". Science 267 (5201): 1123–1131. doi:10.1126/science.267.5201.1123.
- Steadman, D. W.; Martin, P. S. (2003). "The late Quaternary extinction and future resurrection of birds on Pacific islands". Earth Science Reviews 61 (1–2): 133–147. Bibcode:2003ESRv...61..133S. doi:10.1016/S0012-8252(02)00116-2.
- World facing 'extinction crisis'[dead link] October 27, 2010 Postmedia News
- Species Selection Maintains Self-Incompatibility by Goldberg et al. Science 22 October 2010: 493-49
- The extinction risk for birds, mammals and amphibian 2010 The Christian Science Monitor
- 2010 may be the worst year ever for coral death in the Caribbean, Science 22 October 2010:Vol. 330. no. 6003, p. 437
- Early Warning for Endangered Species? 8 September 2010 Science (journal)
- Climate Change Causing Lizards to 'Wink Out of Existence' by Michael Price on 13 May 2010 Science (journal)
- "National Survey Reveals Biodiversity Crisis — Scientific Experts Believe We Are In MidstT Of Fastest Mass Extinction In Earth's History". American Museum of Natural History. Retrieved 2008-08-03.
- "An Interview with Dr. Peter Raven, director of the Missouri Botanical Garden". Retrieved 2008-08-03.
- "the current mass extinction". Retrieved 18 October 2012.
Millions of years before present