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Wildlife of Great Britain |
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The island of Great Britain, along with the rest of the archipelago known as the British Isles, has a largely temperate climate. It contains a relatively small fraction of the world's wildlife. The biota was severely diminished in the last ice age, and shortly (in geological terms) thereafter was separated from the continent by the English Channel's formation. Since then, humans have hunted the most dangerous forms (the wolf, [Notes 1] the brown bear and the wild boar) to extinction, though domesticated forms such as the dog and the pig remain. The wild boar has subsequently been reintroduced as a meat animal. [2]
In most of Great Britain there is a temperate climate, with high levels of precipitation and medium levels of sunlight. Further northwards, the climate becomes colder and coniferous forests appear, replacing the largely deciduous forests of the south. There are a few variations in the generally temperate British climate, with some areas of subarctic conditions, such as the Scottish Highlands and Teesdale, and even sub-tropical in the Isles of Scilly. Plants have to cope with seasonal changes across the British Isles, such as in levels of sunlight, rainfall and temperature, as well as the risk of snow and frost during the winter.
Since the mid 18th century, Great Britain has gone through industrialisation and increasing urbanisation. A DEFRA study from 2006 suggested that 100 species became extinct in the UK during the 20th century: about 100 times the background extinction rate. [3] This has had a major impact on indigenous animal populations. Song birds in particular are becoming scarcer, and habitat loss has affected larger mammalian species. Some species have however adapted to the expanding urban environment, particularly the red fox, which is the most successful urban mammal after the brown rat, and other creatures such as common wood pigeon.
There are 220 species of non-marine molluscs that have been recorded as living in the wild in Britain. Two of them ( Fruticicola fruticum and Cernuella neglecta ) are locally extinct. In addition there are 14 gastropod species that live only in greenhouses. [4]
The species of amphibian native to Britain are the great crested newt, smooth newt, palmate newt, common toad, natterjack toad, common frog and the pool frog. Several other species have become naturalised.
Like many temperate areas, Great Britain has few snake species: the European adder is the only venomous snake to be found there. The other notable snakes found in Great Britain are the barred grass snake and the smooth snake. Great Britain has three native species of lizard: slowworms, sand lizards and viviparous lizards. There are also turtles, such as leatherback turtles to be found in the Irish Sea, although these are rarely seen. Other reptile species exist but are not native: aesculapian snake, wall lizard and green lizard.
In general the avifauna of Britain is similar to that of Europe, consisting largely of Palaearctic species. As an island, it has fewer breeding species than continental Europe. Some species, like the crested lark, breed as close as northern France, but have not colonised Britain. The mild winters mean that many species that cannot cope with harsher conditions can winter in Britain, and also that there is a large influx of wintering birds from the European continent and beyond. There are about 250 species regularly recorded in Great Britain, and another 350 that occur with varying degrees of rarity.
Large mammals are not particularly numerous in Great Britain. Many of the large mammal species, such as the grey wolf and the brown bear, were hunted to extinction many centuries ago. However, in recent times some of these large mammals have been tentatively reintroduced to some areas of Britain. The largest wild mammals that remain in Britain today are predominantly members of the deer family. The red deer is the largest native mammal species, and is common throughout England, Scotland and Wales.
The other indigenous species is the roe deer. The common fallow deer was not naturally present Britain during the Holocene, having been brought over from France by the Normans in the late 11th century. It has become well established, [5] though the fallow deer was naturally present in Britain during the previous Eemian interglacial. [6] The sika deer is another small species of deer which is not indigenous, originating from Japan. It is widespread and expanding in Scotland from west to east, with a strong population in Peeblesshire. Bands of sika exist across the north and south of England though the species is absent in Wales. [7]
There are also several species of insectivore found in Britain. The hedgehog is probably the most widely known as it is a regular visitor to urban gardens. The mole is also widely recognised and its subterranean lifestyle causes much damage to garden lawns. Shrews are also fairly common, and the smallest, the pygmy shrew, is one of the smallest mammals in the world. There are also seventeen species of bat found in Britain: the pipistrelle is the smallest and the most common.
Rodents are also numerous across Britain, particularly the brown rat which is by far the most abundant urban mammal after humans. Some however, are becoming increasingly rare. Habitat destruction has led to a decrease in the population of dormice and bank voles found in Britain. Due to the introduction of the North American grey squirrel, the red squirrel had become largely extinct in England and Wales, with the last populations existing in parts of North West England and on the Isle of Wight. European rabbit and European hare were introduced in Roman times, [8] [9] while the indigenous mountain hare remains only in Scotland and a small re-introduced population in Derbyshire. [10]
Eurasian beavers were formerly native to Britain before becoming extinct by the early 16th century due to hunting. Efforts are being made to reintroduce beavers. [11]
There are a variety of carnivores, especially from the weasel family (ranging in size from the weasel, stoat and European polecat to the European badger, pine marten, recently introduced mink and semiaquatic otter). In the absence of the locally extinct grey wolf and brown bear the largest carnivores are the badger, red fox, the adaptability and opportunism of which has allowed it to proliferate in the urban environment, and the European wildcat whose elusiveness has caused some confusion over population numbers, and is believed to be highly endangered, partly by hybridisation with the domestic cat.
Various species of seal and dolphin are found seasonally on British shores and coastlines, along with harbour porpoises, orcas, and many other sea mammals.
Great Britain has about forty species of native freshwater fish, of which the largest is the salmon. The saltwater fish include some larger species such as sharks.
During the previous Eemian Interglacial (130-115,000 years ago) when Britain had a similar or slightly warmer temperate climate as it does today, [12] the large mammal fauna of Britain was considerably more diverse than it is at present or earlier in the Holocene. Large herbivore species present during the Eemian not present in Britain during the Holocene include the large straight-tusked elephant, [12] the narrow-nosed rhinoceros, [13] the hippopotamus, [14] Irish elk and bison, in addition to the currently present roe, fallow and red deer. [15] Large carnivores present during this time include hyenas ( Crocuta spelaea ) and lions ( Panthera spelaea ) in addition to wolves and brown bears. [15] During the Holocene, Britain was inhabited by the aurochs (the wild ancestor of modern domestic cattle) until its extinction around 3,500 years ago. [16] The Eurasian lynx was also formerly native to Britain during the Holocene, with its youngest records dating to around 1,500 years ago during the early Medieval period. [17] The moose/elk was present in Britain during the early Holocene, but became extinct by around 5600 years ago. [18] The European pond turtle was also present in Britain during the Holocene (as it had been during the Eemian [12] ), with the youngest radiocarbon-dated records dating to around 5,500 years ago. [19]
The Cenozoic is Earth's current geological era, representing the last 66 million years of Earth's history. It is characterized by the dominance of mammals, birds, conifers, and angiosperms. It is the latest of three geological eras, preceded by the Mesozoic and Paleozoic. The Cenozoic started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor.
The fauna of Australia consists of a large variety of animals; some 46% of birds, 69% of mammals, 94% of amphibians, and 93% of reptiles that inhabit the continent are endemic to it. This high level of endemism can be attributed to the continent's long geographic isolation, tectonic stability, and the effects of a unique pattern of climate change on the soil and flora over geological time. A unique feature of Australia's fauna is the relative scarcity of native placental mammals. Consequently, the marsupials – a group of mammals that raise their young in a pouch, including the macropods, possums and dasyuromorphs – occupy many of the ecological niches placental animals occupy elsewhere in the world. Australia is home to two of the five known extant species of monotremes and has numerous venomous species, which include the platypus, spiders, scorpions, octopus, jellyfish, molluscs, stonefish, and stingrays. Uniquely, Australia has more venomous than non-venomous species of snakes.
The Irish elk, also called the giant deer or Irish deer, is an extinct species of deer in the genus Megaloceros and is one of the largest deer that ever lived. Its range extended across Eurasia during the Pleistocene, from Ireland to Lake Baikal in Siberia. The most recent remains of the species have been radiocarbon dated to about 7,700 years ago in western Russia. Its antlers, which can span 3.5 metres (11 ft) across are the largest known of any deer. It is not closely related to either living species called the elk, with it being widely agreed that its closest living relatives are fallow deer (Dama).
The steppe bison or steppe wisent is an extinct species of bison. It was widely distributed across the mammoth steppe, ranging from Western Europe to eastern Beringia in North America during the Late Pleistocene. It is ancestral to all North American bison, including ultimately modern American bison. Three chronological subspecies, Bison priscus priscus, Bison priscus mediator, and Bison priscus gigas, have been suggested.
During the Last Glacial Maximum, the mammoth steppe, also known as steppe-tundra, was once the Earth's most extensive biome. It stretched east-to-west, from the Iberian Peninsula in the west of Europe, across Eurasia to North America, through Beringia and Canada; from north-to-south, the steppe reached from the arctic islands southward to China. The mammoth steppe was cold and dry, and relatively featureless, though topography and geography varied considerably throughout. Some areas featured rivers which, through erosion, naturally created gorges, gulleys, or small glens. The continual glacial recession and advancement over millennia contributed more to the formation of larger valleys and different geographical features. Overall, however, the steppe is known to be flat and expansive grassland. The vegetation was dominated by palatable, high-productivity grasses, herbs and willow shrubs.
The Late Pleistocene is an unofficial age in the international geologic timescale in chronostratigraphy, also known as the Upper Pleistocene from a stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between c. 129,000 and c. 11,700 years ago. The late Pleistocene equates to the proposed Tarantian Age of the geologic time scale, preceded by the officially ratified Chibanian. The beginning of the Late Pleistocene is the transition between the end of the Penultimate Glacial Period and the beginning of the Last Interglacial around 130,000 years ago. The Late Pleistocene ends with the termination of the Younger Dryas, some 11,700 years ago when the Holocene Epoch began.
India is the world's 8th most biodiverse region with a 0.46 BioD score on diversity index, 102,718 species of fauna and 23.39% of the nation's geographical area under forest and tree cover in 2020. India encompasses a wide range of biomes: desert, high mountains, highlands, tropical and temperate forests, swamplands, plains, grasslands, areas surrounding rivers, as well as island archipelago. Officially, three out of the 36 Biodiversity Hotspots in the world are present in India: the Himalayas, the Western Ghats, and the Indo-Burma region. To these may be added the Sundarbans and the Terrai-Duar Savannah grasslands for their unique foliage and animal species. These hotspots have numerous endemic species. Nearly 5% of India's total area is formally classified under protected areas.
The European wild ass or hydruntine is an extinct equine from the Middle Pleistocene to Late Holocene of Europe and West Asia, and possibly North Africa. It is a member of the subgenus Asinus, and closely related to the living Asiatic wild ass. The specific epithet, hydruntinus, means from Otranto.
The Calamian deer, also known as Calamian hog deer, is an endangered species of deer found only in the Calamian Islands of Palawan province in the Philippines. It is one of three species of deer native to the Philippines, the other being the Philippine sambar and the Visayan spotted deer.
The fauna of the United States of America is all the animals living in the Continental United States and its surrounding seas and islands, the Hawaiian Archipelago, Alaska in the Arctic, and several island-territories in the Pacific and in the Caribbean. The U.S. has many endemic species found nowhere else on Earth. With most of the North American continent, the U.S. lies in the Nearctic, Neotropic, and Oceanic faunistic realms, and shares a great deal of its flora and fauna with the rest of the American supercontinent.
Pleistocene rewilding is the advocacy of the reintroduction of extant Pleistocene megafauna, or the close ecological equivalents of extinct megafauna. It is an extension of the conservation practice of rewilding, which aims to restore functioning, self-sustaining ecosystems through practices that may include species reintroductions.
The fauna of Europe is all the animals living in Europe and its surrounding seas and islands. Europe is the western part of the Palearctic realm. Lying within the temperate region, the wildlife is not as rich as in the hottest regions, but is nevertheless diverse due to the variety of habitats and the faunal richness of Eurasia as a whole.
The Late Pleistocene to the beginning of the Holocene saw numerous extinctions of predominantly megafaunal animal species, which resulted in a collapse in faunal density and diversity across the globe. The extinctions during the Late Pleistocene are differentiated from previous extinctions by the widespread absence of ecological succession to replace these extinct megafaunal species, and the regime shift of previously established faunal relationships and habitats as a consequence. The timing and severity of the extinctions varied by region and are thought to have been driven by varying combinations of human and climatic factors. Human impact on megafauna populations is thought to have been driven by hunting ("overkill"), as well as possibly environmental alteration. The relative importance of human vs climatic factors in the extinctions has been the subject of long-running controversy.
The fauna of England is similar to that of other areas British Isles and lies within the Palearctic realm. England's fauna is mainly made up of small animals and is notable for having few large mammals, but in similarity with other island nations; many bird species.
Fauna of Wales includes marine and land animals, birds and reptiles that are resident, visitors or have been introduced to Wales.
Bubalus murrensis, also known as European water buffalo, is an extinct buffalo species native to Europe during the Pleistocene epoch.
Microtus (Tyrrhenicola) henseli is an extinct species of vole belonging to the genus Microtus that was endemic to Sardinia and Corsica during the Pleistocene and Holocene.
The wood-pasture hypothesis is a scientific hypothesis positing that open and semi-open pastures and wood-pastures formed the predominant type of landscape in post-glacial temperate Europe, rather than the common belief of primeval forests. The hypothesis proposes that such a landscape would be formed and maintained by large wild herbivores. Although others, including landscape ecologist Oliver Rackham, had previously expressed similar ideas, it was the Dutch researcher Frans Vera, who, in his 2000 book Grazing Ecology and Forest History, first developed a comprehensive framework for such ideas and formulated them into a theorem. Vera's proposals, although highly controversial, came at a time when the role grazers played in woodlands was increasingly being reconsidered, and are credited for ushering in a period of increased reassessment and interdisciplinary research in European conservation theory and practice. Although Vera largely focused his research on the European situation, his findings could also be applied to other temperate ecological regions worldwide, especially the broadleaved ones.