Glaciation is one factor that leads to local extinction. This was the case during the
Pleistocene glaciation event in North America. During this period, most of the native North American species of earthworm were killed in places covered by glaciation. This left them open for colonization by European earthworms brought over in soil from Europe. Species naturally become extinct from islands over time; this can be either local extinction if the species also occurs elsewhere, or in cases of
island endemism, outright extinction. The number of species an island can support is limited by its geographical size. Because many islands were relatively recently formed due to climate change at the end of the
Pleistocene when the sea level rose, and these islands most likely had the same complement of species as found on the mainland, counting the species that still survive at present on a statistically large enough number of islands will give the parameters with which certain groups of species such as plants or birds will become less biodiverse on a given island over a given period of time, depending on its size. The same calculations can also be applied to determine when species will disappear from nature parks ('islands' in many senses), mountain tops and mesas (see
sky islands), forest remnants or other such distributional patches. This research also demonstrates that certain species are more prone to extinction than others, a species has an intrinsic extinction-ability (incidence function). Some species exploit or require transient or
disturbed habitats, such as vernal pools, a human gut, or burnt woodland after
forest fires, and are characterised by highly fluctuating population numbers and shifting distributional patterns. Many natural ecosystems cycle through a standard
succession,
pioneer species disappear from a region as the ecosystem matures and reaches a
climax community. A local extinction can be useful for research: in the case of the
bay checkerspot butterfly, scientists, including
Paul R. Ehrlich, chose not to intervene as a population disappeared from an area in order to study the process. Many crocodilian species have experienced localized extinction, particularly the
saltwater crocodile (
Crocodylus porosus), which has been extirpated from Vietnam, Thailand, Java and many other areas. Major environmental events, such as volcanic eruptions, may lead to large numbers of local extinctions. Heat waves can lead to local extinction. In New Zealand, during the summer of 2017–2018,
sea surface temperatures around parts of
South Island exceeded , which was well above normal. Air temperatures were also high, exceeding . These high temperatures, coupled with small wave height, led to the local extinction of
bull kelp (Durvillaea spp.) from
Pile Bay. Lagoa Santa, a lake in
Lagoa Santa, Brazil, has lost almost 70% of the local fish species over the last 150 years. These include
Acestrorhynchus lacustris,
Astyanax fasciatus, and
Characidium zebra. This could be caused by the introduction of non-native species, such as
Tilapia rendalli, into the lagoon, changes in water level and organic pollution. Local extinctions can be reversed, in some cases artificially. Wolves are a species that have been
reintroduced into parts of their historical range. This has happened with red wolves (
Canis rufus) in the United States in the late 1980s and also grey wolves in Yellowstone National Park in the mid-1990s. There have been talks of reintroducing wolves in Scotland, Japan, and Mexico. ==Subpopulations and stocks==