Paleoendemism along with neoendemism is one of two sub-categories of endemism. Paleoendemism refers to species that were formerly widespread but are now restricted to a smaller area. Neoendemism refers to species that have recently arisen, such as through divergence and reproductive isolation or through hybridization and polyploidy in plants.
The first part of the word, paleo, comes from the Greek word palaiós, meaning "ancient". The second part of the word, endemism is from New Latin endēmicus, from Greek ενδήμος, endēmos, "native". Endēmos is formed of en meaning "in", and dēmos meaning "the people".
Changes in climate are thought to be the driving force in creating endemic species, generally due to habitat loss. Regions where past climate change has been relatively stable with low extinction rates are more like to be endemic hotspots today. To qualify as hotspot, geographical areas have to have more than 0.5% of the world's plant species endemic to the region. These causes apply to both neoendemism and paleoendemism. However, paleoendemism differs as it does not require additional factors such as barriers and ecological opportunities as it does not rely on adaptive radiation like neoendemism does. It instead relies on the instability of other regions' climate, which may limit the range of a species to a more stable region, thus turning that species paleoendemic. Limited ability for dispersal is also important in the creation of endemic species. The two terms can essentially be defined as "cradles" of new species (neoendemism), or "museums" of old species (paleoendemism).
There are also several human related causes to paleoendemism. Anthropogenic deforestation can severely restrict a species' habitat. In countries like Madagascar, a biodiversity hotspot with extreme proportions of endemism, where only 10% of the island's original forest cover is still intact, this can also lead to extinctions. Pollution, urbanization, and agricultural growth may also turn areas inhabitable for certain species, restricting their habitat in a similar way as deforestation. Human introduction of new predators, whether it be accidental or not, destabilizes ecosystems and can lead to the creation of paleoendemic species in undisturbed regions. In many cases today, paleoendemism is essentially a stepping stone into extinction, especially for those caused by anthropogenic disturbances.
Endemism as a whole is often used to measure biodiversity. While this is not entirely correct, high levels of endemism is one of the required components of a biodiversity hot spot. Conservation efforts tend to be focused around these hot spots, and as result, endemic species reap many of the benefits. This association between biodiversity and endemism also works in the opposite way, where many conservation groups tend to pick areas to focus on based on their endemism rate.
It is not always clear whether a particular species is paleoendemic or neoendemic. For example, kiwis, which are confined to New Zealand, were cited as examples of paleoendemism, this has since been proven to be untrue. Kiwis are ratites (a group of flightless birds). Most parts of the former supercontinent Gondwana have ratites, or did have until the fairly recent past. The traditional account of ratite evolution has the group emerging in flightless form in Gondwana in the Cretaceous, then evolving in their separate directions as the continents drifted apart. More recently, it has been suggested that ratites lost the ability to fly multiple times, and the proto-kiwi developed an inability to fly after arrival in New Zealand. “Overwater dispersal” has been hypothesised for the arrival of the kiwis' ancestor in New Zealand.
Islands offer classic examples of paleoendemism. For this purpose, an island is an area of habitat that is suitable for an organism surrounded on all sides by habitat that is unsuitable. Islands as harbors for endemic species are explained by the Theory of Island Biogeography. However, in order to be considered a paleoendemic on an island, the species must have had a widespread distribution previously, thus eliminating newly formed islands as potential refuges of paleo-endemics.
For example, on the Canary Islands, there are a large number of relict plant species that were formerly distributed in Europe and North Africa. Of the 88 critically endangered species on the Canary Islands, many are the result of range reductions on the islands. The island of New Caledonia is also a prime example as many of the species on the island are paleoendemics. The palm species on New Caledonia grow in areas that are likely former Pleistocene refugia of lowland rainforests. Islands are also a refuge for relict lineages of animals. Bermuda has a high diversity of species and home to one species of terrestrial vertebrate, the skink Plestiodon longirostris, which is the only extant lineage of mainland North American Plestiodon lineages.
The Scorpion of Montecristo (Euscorpius oglasae) from the small Italian island of the same name is likely a paleoendemic species. Glaciations during the Pleistocene are unlikely to have created land bridges between the 10.39 km2 island and the Italian mainland, isolating the species for tens of thousands of years.
Many soil types harbor diverse and endemic plant species. Specific soil types act as “islands” of fertility and the distribution of these soils leads to high rates of paleo- and neoendemism. The primary example of this is serpentine soils. These soils are found in Balkan Peninsula, Turkey, Alps, Cuba, New Caledonia, the North American Appalachians, and a scattered distribution in California, Oregon, and Washington and elsewhere For example in the serpentine soil patches in the Pacific Northwest, Steptanthus glandulosus subsp. glandulosus is a paleoendemic, though the closely related members of the species complex are widely distributed.
Mountains can also be “islands” and harbors of paleoendemism because species that live on mountain peaks are geographically isolated. For example, in the Maritime Alps, Saxifraga florulenta, is an endemic plant that evolved in the Late Miocene and was once widespread across the Mediterranean Basin. Additionally, Piper’s bellflower (Campanula piperi) in the Olympic Mountains in Northern Washington is suspected to be a paleoendemic because the closest related species is located over 1,000 km away. Another example is Stroganowia tiehmii which is endemic to a single mountain range in Nevada  and all other members of the genus are in Central Asia.
Endemism is the ecological state of a species being unique to a defined geographic location, such as an island, nation, country or other defined zone, or habitat type; organisms that are indigenous to a place are not endemic to it if they are also found elsewhere. The extreme opposite of endemism is cosmopolitan distribution. An alternative term for a species that is endemic is precinctive, which applies to species (and subspecific categories) that are restricted to a defined geographical area.Neoendemism
Neoendemism is one of two sub-categories of endemism, the ecological state of a species being unique to a defined geographic location. Specifically, neoendemic species are those that have recently arisen, through divergence and reproductive isolation or through hybridization and polyploidy in plants. Paleoendemism, the other sub-category, refers to species that were formerly widespread but are now restricted to a smaller area.Tasmanian coniferous shrubbery
The vegetation in Tasmania's alpine environments is predominately woody and shrub-like. One vegetation type is coniferous shrubbery, characterised by the gymnosperm species Microcachrys tetragona, Pherosphaera hookeriana, Podocarpus lawrencei, and Diselma archeri. Distribution of these species is relevant with abiotic factors including edaphic conditions and fire frequency, and increasingly, the threat of climate change towards species survival exists. Conservation and management of coniferous shrubbery are necessary considering that the paleoendemic species, Microcachrys, Pherosphaera and Diselma, have persisted in western Tasmanian environments for millions of years