|This article needs additional citations for verification. (September 2013) (Learn how and when to remove this template message)|
Ecological collapse refers to a situation where an ecosystem suffers a drastic, possibly permanent, reduction in carrying capacity for all organisms, often resulting in mass extinction. Usually, an ecological collapse is precipitated by a disastrous event occurring on a short time scale.
Ecosystems have the ability to rebound from a disruptive agent. The difference between collapse or a gentle rebound is determined by two factors —- the toxicity of the introduced element and the resiliency of the original ecosystem.
Through natural selection the planet's species have continuously adapted to change through variation in their biological composition and distribution. Mathematically it can be demonstrated that greater numbers of different biological factors tend to dampen fluctuations in each of the individual factors.
Scientists can predict tipping points for ecological collapse. The most frequently used model for predicting food web collapse is called R50[disambiguation needed], which is a reliable measurement model for food web robustness.
Causes and examples
Although, there is no single cause for ecological collapse, attributing factors include asteroid impacts, extremely large volcanic eruptions, and abrupt climate change. The snowball effect of these attributing factors and ecological collapse are demonstrated within the fossil record. Prehistoric examples include the Carboniferous Rainforest Collapse, the Cretaceous–Paleogene extinction event, the Permian–Triassic extinction event, and other mass extinctions. For example, effects of climate change as a contributing factor towards ecological collapse are demonstrated in the Ordovician–Silurian extinction events. A possible cause of the Ordovician Extinction was global cooling which affected the habitats of marine life. Consequently, sea creatures such as trilobites, brachiopods, and graptolites became extinct. Furthermore, Karabonov and colleagues conducted a study to show how during the Last Glacial Maximum (LGM), alternations in the environment and climate led to ecological collapse in Lake Baikal and Lake Hovsgol which then led to species evolution in these systems. The collapse of Hovsgol's ecosystem during the LGM brought forth a new ecosystem, with limited biodiversity in species and low levels of endemism, in Hovsgol during the Holocene. Karabonov's also study shows that ecological collapse during LGM in Lake Hovsgol led to higher levels of diversity and higher levels of endemism as a byproduct of evolution following the ecological collapse of the LGM. The Ordovician Extinction event and Lake Baikal and Hovsgol demonstrate two effects of ecological collapse on prehistoric environments.
Important pressures contributing to current and future ecological collapse include habitat loss, degradation, and fragmentation, overgrazing, overexploitation of ecosystems by humans, human industrial growth and overpopulation, climate change, ocean acidification, pollution, and invasive species.
Rainforest collapse refers to the actual past and theoretical future ecological collapse of rainforests. It may involve habitat fragmentation to the point where little rainforest biome is left, and rainforest species only survive in isolated refugia. Habitat fragmentation can be caused by roads. When humans start to cut down the trees for logging, secondary roads are created that will go unused after its primary use. Once abandoned, the plants of the rainforest will find it difficult to grow back in that area. Forest fragmentation also opens the path for illegal hunting. Species have a hard time finding a new place to settle in these fragments causing ecological collapse. This leads to extinction of many animals in the rainforest.
In the Carboniferous period, coal forests, great tropical wetlands, extended over much of Euramerica (Europe and America). This land supported towering lycopsids which fragmented and collapsed abruptly. The collapse of the rainforests during the Carboniferous has been attributed to multiple causes, including climate change. Specifically, at this time climate became cooler and drier, conditions that are not favourable to the growth of rainforests and much of the biodiversity within them. This sudden collapse affected several large groups including lycopsids and amphibians. Reptiles prospered in the new environment due to adaptations that let them thrive in drier conditions.
A classic pattern of forest fragmentation is occurring in many rainforests including those of the Amazon, specifically a 'fishbone' pattern formed by the development of roads into the forest. This is of great concern, not only because of the loss of a biome with many untapped resources and wholesale death of living organisms, but also because plant and animal species extinction is known to correlate with habitat fragmentation.
Overgrazing was found to cause land degradation, specifically in Southern Europe, which is another driver of ecological collapse and natural landscape loss. Proper management of pastoral landscapes can mitigate risk of desertification.
In 2010 roughly 170 million gallons of oil was dumped into the Gulf of Mexico when BP's Deepwater Horizon oil rig exploded. The effects of the BP oil spill are still being felt today, more than 8,000 marine birds, sea turtles and marine mammals were found dead or injured within months of the clean up effort. The impact of this disaster has unbalanced the food web of the environment. The oil spill occurred at the height of breeding season and as result affected egg and larval animals to the worst extent wiping entire age classes. This loss of a generation down the line will prove dire for future predators of the ecosystem.
In addition, a major concern for marine biologists is the effects of ecological collapse on the coral reefs (who based on fossil evidence are more vulnerable to extinction but also demonstrate greater resilience) . An effect of global climate change is the rising sea levels which can lead to reef drowing or Coral bleaching. Human activity, such as fishing, mining, deforestation, etc., serves as a threat for coral reefs by affecting the niche of the coral reefs. For example, Edinger and colleagues  demonstrate a correlation between a loss in diversity of coral reefs by 30-60% and human activity such as sewage and/or industrial pollution.
The ocean is in great danger of collapse, In a study of 154 different marine fish species, David Byler found out that many factors such as overfishing, climate change, and fast growth of fish populations will cause ecosystem collapse. When humans fish, they usually will fish the populations of the higher trophic levels such as salmon and tuna. The depletion of these trophic levels allow the lower trophic level to overpopulate, or populate very rapidly. For example, when the population of catfish is depleting due to overfishing, plankton will then overpopulate because their natural predator is being killed off. This causes an issue called eutrophication. Since the population all consumes oxygen the dissolved oxygen(DO) levels will plummet. The DO levels dropping will cause all the species in that area to have to leave, or they will suffocate. This along with climate change, and ocean acidification can cause the collapse of an ecosystem.
Although global climate change and human dominance are inevitable, humans can institute greater self-awareness in order to aid the habits of creatures such as coral reefs.
Scientists predict that a global ecological collapse will occur after 50% of the natural landscape is gone due to human development.
Although the causes of ecological collapse are due to factors unique to their environment, they all for the most part share similar ramifications such as loss in biodiversity, trophic cascades, and even extinction. For example, the urbanization and deforestation of the South east Asian Pacific has led to the extinction of three plant species and eight animal species in 2003.
- Environmental degradation
- Overshoot (ecology)
- Arctic shrinkage
- Global catastrophic risks § Ecological disaster
- Gopi (2010). Basic Civil Engineering. India: Pearson Education.
- Jonsson, Tomas; Berg, Sofia; Pimenov, Alexander; Palmer, Catherine; Emmerson, Mark (2015-04-01). "The reliability of R50 as a measure of vulnerability of food webs to sequential species deletions". Oikos 124 (4): 446–457. doi:10.1111/oik.01588. ISSN 1600-0706.
- "BBC Nature". Retrieved 2015-10-29.
- "BBC Nature". Retrieved 2015-10-29.
- Karabanov, Eugene; Williams, Douglas; Kuzmin, Mikhail; Sideleva, Valentina; Khursevich, Galina; Prokopenko, Alexander; Solotchina, Emilia; Tkachenko, Lilia; Fedenya, Svetlana (2004-07-06). "Ecological collapse of Lake Baikal and Lake Hovsgol ecosystems during the Last Glacial and consequences for aquatic species diversity". Palaeogeography, Palaeoclimatology, Palaeoecology. High Latitude Eurasian Palaeoenvironments 209 (1–4): 227–243. doi:10.1016/j.palaeo.2004.02.017.
- "On Overpopulation and Ecosystem Collapse | EcoInternet - Earth Blog". Retrieved 2015-10-30.
- "Living Planet Report". World Wildlife Fund.
- Kleinschroth, Fritz; Gourlet-Fleury, Sylvie; Sist, Plinio; Mortier, Fréderic; Healey, John R. (2015-04-01). "Legacy of logging roads in the Congo Basin: How persistent are the scars in forest cover?". Ecosphere 6 (4): art64. doi:10.1890/ES14-00488.1. ISSN 2150-8925.
- Sahney, S., Benton, M.J. & Falcon-Lang, H.J. (2010). "Rainforest collapse triggered Pennsylvanian tetrapod diversification in Euramerica" (PDF). Geology 38 (12): 1079–1082. doi:10.1130/G31182.1.
- Fielding, C.R.; Frank, T.D.; Birgenheier, L.P.; Rygel, M.C.; Jones, A.T.; and Roberts, J. (2008). "Stratigraphic imprint of the Late Palaeozoic Ice Age in eastern Australia: A record of alternating glacial and nonglacial climate regime". Geological Society of London Journal 165: 129–140. doi:10.1144/0016-76492007-036.
- Rosenzweig, Michael L. (1995). Species diversity in space and time. Cambridge, United Kingdom: Cambridge University Press.
- Kairis, Orestis; Karavitis, Christos; Salvati, Luca; Kounalaki, Aikaterini; Kosmas, Kostas (2015-07-03). "Exploring the Impact of Overgrazing on Soil Erosion and Land Degradation in a Dry Mediterranean Agro-Forest Landscape (Crete, Greece)". Arid Land Research and Management 29 (3): 360–374. doi:10.1080/15324982.2014.968691. ISSN 1532-4982.
- "How Does the BP Oil Spill Impact Wildlife and Habitat?". National Wildlife Federation. 2015-10-28. Retrieved 2015-10-28.
- Knowlton, Nancy (2001-05-08). "The future of coral reefs". Proceedings of the National Academy of Sciences 98 (10): 5419–5425. doi:10.1073/pnas.091092998. ISSN 0027-8424. PMC 33228. PMID 11344288.
- Edinger, Evan N; Jompa, Jamaluddin; Limmon, Gino V; Widjatmoko, Wisnu; Risk, Michael J (1998-08-01). "Reef degradation and coral biodiversity in indonesia: Effects of land-based pollution, destructive fishing practices and changes over time". Marine Pollution Bulletin 36 (8): 617–630. doi:10.1016/S0025-326X(98)00047-2.
- Pinsky, Malin L.; Byler, David (2015-08-22). "Fishing, fast growth and climate variability increase the risk of collapse". Proc. R. Soc. B 282 (1813): 20151053. doi:10.1098/rspb.2015.1053. ISSN 0962-8452. PMID 26246548.
- "Scientists Fear Global Ecological Collapse Once 50% of the Natural Landscape is Gone". TreeHugger. Retrieved 2015-10-29.
- Sodhi, Koh, Brook, Ng, Navjot, Lian, Barry, Peter (December 2004). "Southeast Asian Biodiversity and impending disaster". Trends in Ecology and Evolution 19 (12): 654–660. doi:10.1016/j.tree.2004.09.006.