1.
Cape Peninsula
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The Cape Peninsula is a generally rocky peninsula that juts out into the Atlantic Ocean at the south-western extremity of the African continent. At the southern end of the peninsula are Cape Point and the Cape of Good Hope, on the northern end is Table Mountain, overlooking Cape Town, South Africa. The peninsula is 52 km long from Mouille point in the north to Cape Point in the south. The Peninsula has been an island on and off for the past 5 million years, as sea levels fell and rose with the ice age and interglacial global warming cycles of, particularly, the Pleistocene. The last time that the Peninsula was an island was about 1.5 million years ago, soon afterwards it was joined to the mainland by the emergence from the sea of the sandy area now known as the Cape Flats. The towns and villages of the Cape Peninsula and Cape Flats now form part of the City of Cape Town Metropolitan Municipality, the Cape of Good Hope is sometimes given as the meeting point of the Atlantic and Indian Oceans. Thus the west coast of the Peninsula is invariably referred to as the Atlantic Coast and it is at Cape Point that the ocean to the south is often said to be divided into the Atlantic Ocean to the west, and the Indian Ocean to the east. However, according to the International Hydrographic Organization agreement that defines the ocean boundaries, from there it is retroflexed in an easterly direction by the South Atlantic, South Indian and Southern Ocean currents, known as the West Wind Drift, which flow eastwards round Antarctica. The Benguela Current, on the hand, is an upwelling current which brings cold. Having reached the surface it flows northwards as a result of the prevailing wind, thus the Benguela and Agulhas currents do not strictly meet anywhere, although eddies from the Agulhas current do from time to time round the Cape to join the Benguela Current. The park comprises a part of the undeveloped area of the Cape Peninsula. The coastal waters surrounding the Cape Peninsula are proclaimed as a protected area since 2004, and include several no-take zones. The waters of this protected area are unusual in that they are parts of two fairly distinct marine bioregions, namely the Agulhas Bioregion and the South-western Cape Bioregion. The boundary is at Cape Point, the Cape Peninsula has an unusually rich biodiversity. Its vegetation consists predominantly of several different types of the unique, on the sandy Cape Flats lowlands there are a few pockets of protected Cape Flats Sand Fynbos. The Peninsulas vegetation types form part of the Cape Floral Region protected areas, many of these species, including a great many types of proteas, are endemic to these mountains and can be found nowhere else. It is a showy orchid that blooms from January to March on the Table Mountain Sandstone regions of the mountain. Although they are widespread on the Back Table, the best place to view these beautiful blooms is in the Aqueduct off the Smuts Track
2.
Shrubland
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Shrubland, scrubland, scrub or brush is a plant community characterised by vegetation dominated by shrubs, often also including grasses, herbs, and geophytes. Shrubland may either occur naturally or be the result of human activity and it may be the mature vegetation type in a particular region and remain stable over time, or a transitional community that occurs temporarily as the result of a disturbance, such as fire. A stable state may be maintained by natural disturbance such as fire or browsing. Shrubland may be unsuitable for habitation because of the danger of fire. The term shrubland was coined in 1903, shrubland species generally show a wide range of adaptations to fire, such as heavy seed production, lignotubers, and fire-induced germination. In botany and ecology a shrub is defined as a woody plant less than 8 m high. Tall shrubs are mostly 2–8 m high, small shrubs 1–2 m high, Mediterranean scrublands Mediterranean scrublands occur naturally in the Mediterranean forests, woodlands, and scrub biomes, located in the five Mediterranean climate regions of the world. Scrublands are most common near the seacoast, and have adapted to the wind. Low, soft-leaved scrublands around the Mediterranean Basin are known as garrigue in France, phrygana in Greece, tomillares in Spain, and batha in Israel. Interior scrublands Interior scrublands occur naturally in areas where soils are nutrient-poor. Florida scrub is another example of interior scrublands, dwarf shrubs Some vegetation types are formed of dwarf-shrubs, low-growing or creeping shrubs. These include the maquis and garrigues of Mediterranean climates, and the acid-loving dwarf shrubs of heathland and moorland, fynbos Maquis Prostrate shrub Semi-desert Shrub-steppe Shrub swamp Moorland
3.
Heath
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A heath is a shrubland habitat found mainly on free-draining infertile, acidic soils and is characterised by open, low-growing woody vegetation. Moorland is generally related to high-ground heaths with—especially in Great Britain—a cooler, heaths are widespread worldwide, but are fast disappearing and considered a rare habitat in Europe. They form extensive and highly diverse communities across Australia in humid and sub-humid areas where fire regimes with recurring burning are required for the maintenance of the heathlands, even more diverse though less widespread heath communities occur in Southern Africa. Extensive heath communities can also be found in the California chaparral, New Caledonia, central Chile, in addition to these extensive heath areas, the vegetation type is also found in scattered locations across all continents, except Antarctica. Heaths are dominated by low shrubs,20 centimetres to 2 metres tall, heath vegetation can be extremely plant-species rich, and heathlands of Australia are home to some 3,700 endemic or typical species in addition to numerous less restricted species. The fynbos heathlands of South Africa are second only to tropical rainforests in plant biodiversity with over 7,000 species, in marked contrast, the tiny pockets of heathland in Europe are extremely depauperate with a flora consisting primarily of heather, heath and gorse. The bird fauna of heathlands are usually species of the region. In the depauperate heathlands of Europe bird species tend to be characteristic of the community and include Montagus harrier. Australian heathlands are also home to the worlds only nectar-feeding terrestrial mammal, the bird fauna of the South African fynbos includes sunbirds, warblers and siskins. Heathlands are also an excellent habitat for insects including ants, moths, butterflies and these heaths were originally created or expanded by centuries of human clearance of the natural forest and woodland vegetation, by grazing and burning. Referring to heathland in England, Rackham says, “Heaths are clearly the product of human activities and need to be managed as heathland, in recent years the conservation value of even these man-made heaths has become much more appreciated, and consequently most heathlands are protected. However they are threatened by tree incursion because of the discontinuation of traditional management techniques such as grazing and burning that mediated the landscapes. Some are also threatened by urban sprawl, anthropogenic heathlands are maintained artificially by a combination of grazing and periodic burning, or mowing, if not so maintained, they are rapidly re-colonised by forest or woodland. The re-colonising tree species will depend on what is available as the seed source. Bolster heath Chalk heath Garrigue Maquis shrubland Matorral Scrubland The Countryside Agency information on types of open land Origin of the word heath
4.
Western Cape
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The Western Cape is a province of South Africa, situated in the south-western part of the country. It is the fourth largest of the nine provinces in terms of area and population, with an area of 129,449 square kilometres and 5.8 million inhabitants. About two-thirds of these live in the metropolitan area of Cape Town. The Western Cape was created in 1994 from part of the former Cape Province, the Western Cape Province is roughly L-shaped, extending north and east from the Cape of Good Hope, in the southwestern corner of South Africa. It stretches about 400 kilometres northwards along the Atlantic coast and about 500 kilometres eastwards along the South African south coast and it is bordered on the north by the Northern Cape and on the east by the Eastern Cape. The total land area of the province is 129,462 square kilometres and it is roughly the size of England or the State of Louisiana. Its capital city and largest city is Cape Town, and some major cities include Stellenbosch, Worcester, Paarl. The Garden Route and the Overberg are popular tourism areas. The Western Cape is the southernmost region of the African continent with Cape Agulhas as its southernmost point, the coastline varies from sandy between capes, to rocky to steep and mountainous in places. The only natural harbour is Saldanha Bay on the west coast, however a lack of fresh water in the region meant that it has only recently been used as a harbour. But fresh water coming off Table Mountain and Devils Peak allowed the early European settlers to build Cape Town on the shores of this less than satisfactory anchorage, the province is topographically exceptionally diverse. Most of the province falls within the Cape Fold Belt, a set of parallel ranges of sandstone folded mountains of Cambrian-Ordovician age. The valleys between ranges are very fertile as they contain the weathered loamy soils of the Bokkeveld mustones. The far interior forms part of the Karoo and this region of the Province is generally arid and hilly with a prominent escarpment that runs close to the Provinces most inland boundary. The Escarpment marks the edge of South Africas central plateau. The principal rivers of the province are the Berg and Olifants which drain into the Atlantic Ocean, and the Breede and Gourits which drain into the Indian Ocean. The vegetation is extremely diverse, with one of the worlds seven floral kingdoms almost exclusively endemic to the province, namely the Cape Floral Kingdom. These evergreen heathlands are extremely rich in diversity, with at least as many plant species occurring on Table Mountain as in the entire United Kingdom
5.
Eastern Cape
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The Eastern Cape is a province of South Africa. Its capital is Bhisho, but its two largest cities are Port Elizabeth and East London and it was formed in 1994 out of the Xhosa homelands of Transkei and Ciskei, together with the eastern portion of the Cape Province. Landing place and home of the 1820 settlers, the central and this resulted in several anomalies including the fact that the Province has four supreme courts and enclaves of KwaZulu-Natal in the province. The latter anomaly has fallen away with amendments to municipal and provincial boundaries. The province is made of Mpondo clan. Some of the Mpondo clan went to this province when they were running away from King Shakas war, Mpondo people are more closely related to Xhosa, as they use Xhosa as their main home language. The west is mostly semi-arid Karoo, except in the far south, the coast is generally rugged with interspersed beaches. Most of the province is hilly to very mountainous between Graaff-Reinet and Rhodes including the Sneeuberge, Stormberge, Winterberge and Drakensberg, the highest point in the province is Ben Macdhui at 3001m. Eastern Cape has a shoreline on its east which lines southward, the west is dry with sparse rain during winter or summer, with frosty winters and hot summers. The area Tsitsikamma to Grahamstown receives more precipitation, which is relatively evenly distributed. Further east, rainfall becomes more plentiful and humidity increases, becoming more subtropical along the coast with summer rainfall, the interior can become very cold in winter, with heavy snowfalls occasionally occurring in the mountainous regions between Molteno and Rhodes. Port Elizabeth, Jan Max,25 °C, Min,18 °C, Jul Max,20 °C, Min,9 °C Molteno & Barkly East, Jan Max 28 °C, Min 11 °C, Jul Max,14 °C, Min, -7 °C The landscape is extremely diverse. The western interior is largely arid Karoo, while the east is well-watered, the Addo Elephant National Park, situated 73 km from Port Elizabeth, was proclaimed in 1931. Its 743 km² offers sanctuary to 170 elephants,400 Cape buffalo and 21 black rhino of the very scarce Kenyan sub-species. The National Arts Festival, held annually in Grahamstown, is Africas largest and most colourful cultural event, every year for 11 days the towns population almost doubles, as over 50,000 people flock to the region for a feast of arts, crafts and sheer entertainment. The Tsitsikamma National Park is an 80 km long strip between Natures Valley and the mouth of the Storms River. In the park the visitor finds an almost untouched natural landscape, aliwal North, lying on a splendid agricultural plateau on the southern bank of the Orange River, is one of the countrys most popular inland resorts and is famous for its hot springs. The rugged and unspoilt Wild Coast is a place of spectacular scenery, whittlesea, Eastern Cape, situated in the beautiful Amatola Mountains, is now famous for the first wine estate in the province. The Eastern Cape is one of the poorest provinces in South Africa and this is largely due to the poverty found in the former homelands, where subsistence agriculture predominates
6.
Mediterranean climate
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A Mediterranean climate /ˌmɛdɪtəˈreɪniən/ or dry summer climate, is the climate typical of the lands in the Mediterranean Basin. The Mediterranean climate is characterised by dry summers and mild, moist winters, Mediterranean climate zones are associated with the four large subtropical high pressure cells of the oceans, the Azores High, South Atlantic High, North Pacific High, and South Pacific High. These climatological high pressure cells migrate by latitude according to the angle of the Sun, shifting north-eastward in the summer. These semi-permanent high pressure systems play a role in the formation of the worlds subtropical and tropical deserts as well as the Mediterranean Basins climate. The Azores High is associated with the Mediterranean climate found in the Mediterranean Basin, the Sahara Desert, the South Atlantic High is similarly associated with the Namib Desert and Kalahari Desert, and the Mediterranean climate of the western part of South Africa. Under the Köppen climate classification, hot climates and cool dry-summer climates are often referred to as mediterranean. Under the Köppen climate system, the first letter indicates the climate group, temperate climates or C zones have an average temperature above 0 °C, but below 18 °C, in their coolest months. The second letter indicates the precipitation pattern, Köppen has defined a dry summer month as a month with less than 30 mm of precipitation and with less than one-third that of the wettest winter month. Some, however, use a 40 mm level, the third letter indicates the degree of summer heat, a represents an average temperature in the warmest month above 22 °C, while b indicates the average temperature in the warmest month below 22 °C. Under the Köppen classification, dry-summer climates usually occur on the sides of continents. Under Trewarthas system, at least eight months must have average temperatures of 10 °C or higher, during summer, regions of mediterranean climate are dominated by subtropical high pressure cells, with dry sinking air capping a surface marine layer of varying humidity and making rainfall unlikely. In many Mediterranean climates there is a strong character to daily temperatures in the warm months. The majority of the regions with mediterranean climates have relatively mild winters, however winter and summer temperatures can vary greatly between different regions with a mediterranean climate. Or to consider summer, Athens experiences rather high temperatures in that season, in contrast, San Francisco has cool summers with daily highs around. In North America, areas with Csc climate can be found in the Olympic, Cascade, Klamath and these locations are found at high altitude nearby lower altitude regions characterized by a warm-summer mediterranean climate or hot-summer mediterranean climate. A rare instance of this occurs in the tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile, the town of Balmaceda is one of the few towns confirmed to have this climate. Small areas with a Csc climate can also be found at elevations in Corsica
7.
Ecoregion
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An ecoregion is an ecologically and geographically defined area that is smaller than a bioregion, which in turn is smaller than an ecozone. All three of these are less or greater than an ecosystem. Ecoregions cover relatively large areas of land or water, and contain characteristic, the biodiversity of flora, fauna and ecosystems that characterise an ecoregion tends to be distinct from that of other ecoregions. Three caveats are appropriate for all bio-geographic mapping approaches, firstly, no single bio-geographic framework is optimal for all taxa. Ecoregions reflect the best compromise for as many taxa as possible, secondly, ecoregion boundaries rarely form abrupt edges, rather, ecotones and mosaic habitats bound them. Thirdly, most ecoregions contain habitats that differ from their assigned biome, biogeographic provinces may originate due to various barriers. Some physical, some climatic and some ocean chemical related, the history of the term is somewhat vague as it was used in many contexts, forest classifications, biome classifications, biogeographic classifications, etc. The concept of ecoregion of Bailey gives more importance to ecological criteria, while the WWF concept gives more importance to biogeography, there is significant, but not absolute, spatial correlation among these characteristics, making the delineation of ecoregions an imperfect science. Such transition zones are called ecotones, Ecoregions can be categorized using an algorithmic approach or a holistic, “weight-of-evidence” approach where the importance of various factors may vary. An example of the approach is Robert Bailey’s work for the U. S. The intended purpose of ecoregion delineation may affect the method used, according to WWF, the boundaries of an ecoregion approximate the original extent of the natural communities prior to any major recent disruptions or changes. WWF has identified 867 terrestrial ecoregions, and approximately 450 freshwater ecoregions across the Earth, the use of the term ecoregion is an outgrowth of a surge of interest in ecosystems and their functioning. In particular, there is awareness of issues relating to spatial scale in the study and it is widely recognized that interlinked ecosystems combine to form a whole that is greater than the sum of its parts. The Global 200 is the list of ecoregions identified by WWF as priorities for conservation, Terrestrial ecoregions are land ecoregions, as distinct from freshwater and marine ecoregions. In this context, terrestrial is used to mean of land, WWF ecologists currently divide the land surface of the Earth into 8 major ecozones containing 867 smaller terrestrial ecoregions. The WWF effort is a synthesis of previous efforts to define. Many consider this classification to be decisive, and some propose these as stable borders for bioregional democracy initiatives. The eight terrestrial ecozones follow the major floral and faunal boundaries, identified by botanists and zoologists, ecozone boundaries generally follow continental boundaries, or major barriers to plant and animal distribution, like the Himalayas and the Sahara
8.
Mediterranean forests, woodlands, and scrub
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Mediterranean forests, woodlands, and scrub biome, as defined by the World Wildlife Fund, is generally characterized by dry summers and rainy winters. Summers are typically hot in low-lying inland locations but can be cool near colder seas, winters are typically mild to cool in low-lying locations but can be cold in inland and higher locations. All these ecoregions are highly distinctive, collectively harboring 10% of the Earths plant species, much of the woody vegetation in Mediterranean-climate regions is sclerophyll, which means hard-leaved in Greek. Sclerophyll vegetation generally has small, dark leaves covered with an outer layer to retain moisture in the dry summer months. This is equivalent to about 40% of the plant species of the United States and Canada combined, forests are often found in riparian areas, where they receive more summer water. Coniferous forests also occur, especially around the Mediterranean, pine and deciduous oak forest are widespread across California Woodland, Oak woodlands are characteristic of the Mediterranean Basin and in California. Pine woodlands are also present in the Mediterranean Basin, savanna and grassland, The California Central Valley grasslands are the largest Mediterranean grassland eco-region, although these grasslands have mostly been converted to agriculture. The remaining woodlands feature mainly oak, walnut and pine, the cork oak savanna in Portugal, known as montado, is a good example of a mediterranean savanna. Shrubland, Shrublands are dense thickets of evergreen shrubs and small trees. They are most common near the seacoast, and are adapted to wind. Northern coastal scrub and coastal scrub, also known as soft chaparral. In some places shrublands are of the vegetation type, and in other places are the result of degradation of former forest or woodland by logging or overgrazing. Fire, both natural and human-caused, has played a role in shaping the ecology of Mediterranean ecoregions. The hot, dry summers make much of the prone to fires. Many of the plants are pyrophytes, or fire-loving, adapted or even depending on fire for reproduction, recycling of nutrients, and the removal of dead or senescent vegetation. The plant communities in these areas adapted to the frequent human-caused fires, the European shrublands have also been shaped by anthropogenic fire, historically associated with transhumance herding of sheep and goats. Mediterranean ecoregions are some of the most endangered and vulnerable on the planet, media related to Mediterranean forests, woodlands, and scrub at Wikimedia Commons National Geographic Global 200 Ecoregions, Mediterranean Forest, Woodland and Scrub. Part of National Geographics Wild World Terrestrial Ecoregions of the World mapping project, Forest Sciences Centre of Catalonia FAO
9.
Biome
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A biome /ˈbaɪoʊm/ is a community of plants and animals that have common characteristics for the environment they exist in, and can be found over a range of continents. Spanning continents, biomes are distinct biological communities that have formed in response to a shared physical climate, biome is a broader term than habitat, any biome can comprise a variety of habitats. While a biome can cover large ares, a microbiome is a mix of organisms that coexist in a space as well. For example, the microbiome is the collection of bacteria, viruses. The biotas of the Earth make up the biosphere, the term was suggested in 1916 by Clements, originally as a synonym for biotic community of Möbius. In 1935, Tansley added the climatic and soil aspects to the idea, the International Biological Program projects popularized the concept of biome. However, in contexts, the term biome is used in a different manner. Both includes many biomes in fact and their boundaries must therefore be drawn arbitrarily and their characterization made according to the average conditions that predominate in them. A1978 study on North American grasslands found a positive correlation between evapotranspiration in mm/yr and above-ground net primary production in g/m2/yr. These findings help explain the categories used in Holdridge’s bioclassification scheme, Holdridge uses the four axes to define 30 so-called humidity provinces, which are clearly visible in his diagram. While this scheme largely ignores soil and sun exposure, Holdridge acknowledged that these were important and his scheme can be seen as a simplification of Holdridges, more readily accessible, but missing Holdridges greater specificity. Whittaker based his approach on theoretical assertions and empirical sampling and he was in a unique position to make such a holistic assertion because he had previously compiled a review of biome classifications. Physiognomy, the apparent characteristics, outward features, or appearance of communities or species. Biome, a grouping of terrestrial ecosystems on a continent that are similar in vegetation structure, physiognomy, features of the environment. Formation, a kind of community of plants on a given continent. Biome-type, grouping of convergent biomes or formations of different continents, whittakers distinction between biome and formation can be simplified, formation is used when applied to plant communities only, while biome is used when concerned with both plants and animals. Whittakers convention of biome-type or formation-type is simply a method to categorize similar communities. Whittaker considered four main ecoclines in the terrestrial realm, changes in physiognomic complexity vary with how favorable of an environment exists
10.
Biogeography
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Biogeography is the study of the distribution of species and ecosystems in geographic space and through time. Organisms and biological communities often vary in a regular fashion along geographic gradients of latitude, elevation, isolation, phytogeography is the branch of biogeography that studies the distribution of plants. Zoogeography is the branch that studies distribution of animals, Biogeography is an integrative field of inquiry that unites concepts and information from ecology, evolutionary biology, geology, and physical geography. The short-term interactions within a habitat and species of organisms describe the application of biogeography. Historical biogeography describes the long-term, evolutionary periods of time for broader classifications of organisms, early scientists, beginning with Carl Linnaeus, contributed theories to the contributions of the development of biogeography as a science. Beginning in the century, Europeans explored the world and discovered the biodiversity of life. Linnaeus initiated the ways to classify organisms through his exploration of undiscovered territories, the patterns of species distribution across geographical areas can usually be explained through a combination of historical factors such as, speciation, extinction, continental drift, and glaciation. Through observing the distribution of species, we can see associated variations in sea level, river routes, habitat. Additionally, this science considers the constraints of landmass areas and isolation. As writer David Quammen put it. biogeography does more than ask Which species, and, what is sometimes more crucial, Why not. Modern biogeography often employs the use of Geographic Information Systems, to understand the factors affecting organism distribution, often mathematical models and GIS are employed to solve ecological problems that have a spatial aspect to them. Biogeography is most keenly observed on the worlds islands and these habitats are often much more manageable areas of study because they are more condensed than larger ecosystems on the mainland. They can then apply their understanding to similar but more complex mainland habitats, Islands are very diverse in their biomes, ranging from the tropical to arctic climates. This diversity in habitat allows for a range of species study in different parts of the world. One scientist who recognized the importance of geographic locations was Charles Darwin. Two chapters in On the Origin of Species were devoted to geographical distribution, the first discoveries that contributed to the development of biogeography as a science began in the mid-18th century, as Europeans explored the world and discovered the biodiversity of life. During the 18th century most views on the world were shaped around religion and for many natural theologists, Carl Linnaeus, in the mid-18th century, initiated the ways to classify organisms through his exploration of undiscovered territories. When he noticed that species were not as perpetual as he believed, when Noah’s ark landed on Mount Ararat and the waters receded, the animals dispersed throughout different elevations on the mountain
11.
Biodiversity
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Biodiversity, a contraction of biological diversity, generally refers to the variety and variability of life on Earth. One of the most widely used definitions defines it in terms of the variability within species and it is a measure of the variety of organisms present in different ecosystems. This can refer to genetic variation, ecosystem variation, or species variation within an area, biome, terrestrial biodiversity tends to be greater near the equator, which seems to be the result of the warm climate and high primary productivity. Biodiversity is not distributed evenly on Earth, and is richest in the tropics and these tropical forest ecosystems cover less than 10 per cent of earths surface, and contain about 90 percent of the worlds species. Marine biodiversity tends to be highest along coasts in the Western Pacific, there are latitudinal gradients in species diversity. Biodiversity generally tends to cluster in hotspots, and has been increasing through time, the number and variety of plants, animals and other organisms that exist is known as biodiversity. It is a component of nature and it ensures the survival of human species by providing food, fuel, shelter, medicines. The richness of biodiversity depends on the conditions and area of the region. All species of plants taken together are known as flora and about 300,000 species of plants are known to date, all species of animals taken together are known as fauna which includes birds, mammals, fish, reptiles, insects, crustaceans, molluscs, etc. Rapid environmental changes typically cause mass extinctions, more than 99 percent of all species, amounting to over five billion species, that ever lived on Earth are estimated to be extinct. Estimates on the number of Earths current species range from 10 million to 14 million, of which about 1.2 million have been documented and over 86 percent have not yet been described. More recently, in May 2016, scientists reported that 1 trillion species are estimated to be on Earth currently with only one-thousandth of one percent described, the total amount of related DNA base pairs on Earth is estimated at 5.0 x 1037 and weighs 50 billion tonnes. In comparison, the mass of the biosphere has been estimated to be as much as 4 TtC. In July 2016, scientists reported identifying a set of 355 genes from the Last Universal Common Ancestor of all living on Earth. The age of the Earth is about 4.54 billion years old, there are microbial mat fossils found in 3.48 billion-year-old sandstone discovered in Western Australia. Other early physical evidence of a substance is graphite in 3.7 billion-year-old meta-sedimentary rocks discovered in Western Greenland. More recently, in 2015, remains of life were found in 4.1 billion-year-old rocks in Western Australia. According to one of the researchers, If life arose relatively quickly on Earth, then it could be common in the universe
12.
Endemism
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The extreme opposite of endemism is cosmopolitan distribution. An alternative term for a species that is endemic is precinctive, the word endemic is from New Latin endēmicus, from Greek ενδήμος, endēmos, native. Endēmos is formed of en meaning in, and dēmos meaning the people, the term, precinctive, has been suggested by some scientists, and was first used in botany by MacCaughey in 1917. It is the equivalent of endemism, precinction was perhaps first used by Frank and McCoy. That definition excludes artificial confinement of examples by humans in far-off botanical gardens or zoological parks, physical, climatic, and biological factors can contribute to endemism. The orange-breasted sunbird is found in the fynbos vegetation zone of southwestern South Africa. The glacier bear is found only in limited places in Southeast Alaska, political factors can play a part if a species is protected, or actively hunted, in one jurisdiction but not another. There are two subcategories of endemism, paleoendemism and neoendemism, paleoendemism refers to species that were formerly widespread but are now restricted to a smaller area. Neoendemism refers to species that have arisen, such as through divergence and reproductive isolation or through hybridization. Endemics can easily become endangered or extinct if their restricted habitat changes, particularly—but not only—due to human actions, there were millions of both Bermuda petrels and Bermuda cedars in Bermuda when it was settled at the start of the seventeenth century. By the end of the century, the petrels were thought extinct, cedars, already ravaged by centuries of shipbuilding, were driven nearly to extinction in the twentieth century by the introduction of a parasite. Bermuda petrels and cedars are now rare, as are species endemic to Bermuda
13.
Cape Floristic Region
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The Cape Floristic Region is a floristic region located near the southern tip of South Africa. It is the only region of the Cape Floristic Kingdom. Much of this diversity is associated with the fynbos biome, a Mediterranean-type, the economical worth of fynbos biodiversity, based on harvests of fynbos products and eco-tourism, is estimated to be in the region of R77 million a year. Thus, it is clear that the Cape Floristic Region has both economic and intrinsic value as a biodiversity hotspot. Covering 78,555 km², Cape Floristic Region hotspot is located entirely within the borders of South Africa and it is one of the five temperate Mediterranean-type systems on the hotspots list, and is one of only two hotspots that encompass an entire floral kingdom. Most of the region is covered with fynbos, a sclerophyllous shrubland occurring on acid sands or nutrient poor soils derived from Table Mountain Sandstones. Fynbos is home to a diversity of plant species including many members of the Protea family, Heath family. Other vegetation types are sandveld, a soft coastal scrubland found mostly on the west-facing coast of the Western Cape Province, small pockets of Afromontane forest can be found in humid and sheltered areas. According to Takhtajan, the families are endemic or subendemic to the region. The World Wildlife Fund divides the Cape floristic region into three ecoregions, the Lowland fynbos and renosterveld, Montane fynbos and renosterveld and the Albany thickets, the fynbos ecoregions are designated one of the Global 200 priority ecoregions for conservation. Conservation International declared the Cape floristic region to be a biodiversity hotspot and it is thought that the Cape Floristic Region is experiencing one of the most rapid rates of extinction in the world due to habitat loss, land degradation, and invasive alien plants
14.
Afrikaans
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Afrikaans is a West Germanic language spoken in South Africa, Namibia and, to a lesser extent, Botswana and Zimbabwe. Hence, it is a language of Dutch, and was previously referred to as Cape Dutch or kitchen Dutch. Although, it is described as a creole, a partially creolised language the least. The term is derived from Dutch Afrikaans-Hollands meaning African Dutch. It is the first language of most of the Afrikaner and Coloured people of Southern Africa, therefore, differences with Dutch often lie in the more analytic morphology and grammar of Afrikaans, and a spelling that expresses Afrikaans pronunciation rather than standard Dutch. There is a degree of mutual intelligibility between the two languages—especially in written form. With about 7 million native speakers in South Africa, or 13. 5% of the population and it has the widest geographical and racial distribution of all the eleven official languages of South Africa, and is widely spoken and understood as a second or third language. About 1. 5% of black South Africans speak it as their first language, large numbers of speakers of Bantu languages and English-speaking South Africans also speak it as their second language. It is taught in schools, with about 10.3 million second-language students and it, along with German, was among the official languages of Namibia until the country became independent in 1990, 25% of the population of Windhoek spoke Afrikaans at home. Both Afrikaans and German survive as recognised regional languages in the country, estimates of the total number of Afrikaans speakers range between 15 and 23 million. The Afrikaans language arose in the Dutch Cape Colony, through a gradual divergence from European Dutch dialects, there is a degree of mutual intelligibility between the two languages, particularly in written form. Nevertheless, Dutch speakers are confronted with fewer non-cognates when listening to Afrikaans than the way round. Mutual intelligibility thus tends to be asymmetrical, as it is easier for Dutch speakers to understand Afrikaans than for Afrikaans speakers to understand Dutch, in general, mutual intelligibility between Dutch and Afrikaans is better than between Dutch and Frisian or between Danish and Swedish. The workers and slaves who contributed to the development of Afrikaans were Asians and Malagasys, as well as the Khoi, San, and Bantu peoples who also lived in the area. African creole people in the early 18th century — documented on the cases of Hendrik Bibault, Only much later in the second half of the 19th century did the Boers adopt this attribution, too. The Khoi and mixed-race groups became collectively referred to as Coloureds, beginning in about 1815, Afrikaans started to replace Malay as the language of instruction in Muslim schools in South Africa, written with the Arabic alphabet, see Arabic Afrikaans. Later, Afrikaans, now written with the Latin alphabet, started to appear in newspapers and political, in 1925, Afrikaans was recognised by the South African government as a real language, rather than simply a slang version of Dutch proper. Before the Boer Wars, and indeed for some time afterwards, rather, Afrikaans was described derogatorily as ‘a kitchen language’ or as ‘a bastard jargon, suitable for communication mainly between the Boers and their servants
15.
Ericoid
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The word ericoid is used in modern biological terminology for its literal meanings and for extensions. Etymologically the word is derived from two Greek roots via Latin adaptations, firstly, the Ancient Greek name for plants now known in English as heather was ἐρείκη, believed to be Latinised by Pliny as Erica. Linnaeus, who wrote in Latin, used Erica as the name of the genus which still is known as such. However, when Linnaeus named an organism, using a specific epithet that described it as being like some particular thing and that was a contraction of —ο + ειδος, denoting a likeness of form. In its Latinised form it became, —oides, an example is the entry 9413 Stilbe ericoides according to Wapplers Index Plantarum to Linnaeus Species Plantarum. Further derivations emerged at need or convenience, such as —oidea, accordingly, ericoid could have more than one meaning and it has been misapplied from time to time in the literature. For example, sometimes a writer uses it where the word would be ericaceous, meaning a member of, or related to. More precisely ericoid means resembling an Erica in some relevant way, in practice the commonest use is in reference to a plants habit, in particular its leaves. The term is not precise, but ericoid leaves is a convenient way to describe small, applied to a plant, ericoid generally means that apart from its sclerophyllous leaves, it has short internodes so that the leaves more or less cover the usually slender branchlets
16.
Sclerophyll
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Sclerophyll is a type of vegetation that has hard leaves, short internodes and leaf orientation parallel or oblique to direct sunlight. The word comes from the Greek sklēros and phyllon, sclerophyllous plants occur in many parts of the world, but are most typical in the chaparral biomes. The term was coined by A. F. W, schimper in 1898, originally as a synonym of xeromorph, but later was changed. Most areas of the Australian continent able to support woody plants are occupied by sclerophyll communities as forests, common plants include the Proteaceae, tea-trees, acacias, boronias, and eucalypts. The most common sclerophyll communities in Australia are savannas dominated by grasses with an overstorey of eucalypts, acacia shrublands also cover extensive areas. These traits make the majority of plants in these woodlands largely unpalatable to domestic livestock. It is therefore important from a perspective that these woodlands support a more or less continuous layer of herbaceous ground cover dominated by grasses. Sclerophyll forests cover a smaller area of the continent, being restricted to relatively high rainfall locations. They have a eucalyptus overstory with the understory also being hard-leaved, dry sclerophyll forests are the most common forest type on the continent, and although it may seem barren dry sclerophyll forest is highly diverse. For example, a study of vegetation in Seal Creek, Victoria. Even less extensive are wet sclerophyll forests and they have a taller eucalyptus overstory than dry sclerophyll forests,30 metres or more, and a soft-leaved, fairly dense understory. They require ample rainfall — at least 1000mm, sclerophyllous plants are all part of a specific environment and are anything but newcomers. By the time of European settlement, sclerophyll forest accounted for the vast bulk of the forested areas, most of the wooded parts of present-day Australia have become sclerophyll dominated as a result of the extreme age of the continent combined with Aboriginal fire use. Deep weathering of the crust over millions of years leached chemicals out of the rock, leaving Australian soils deficient in nutrients. Such nutrient deficient soils support non-sclerophyllous plant communities elsewhere in the world, however such deficient soils cannot support the nutrient losses associated with frequent fires and are rapidly replaced with sclerophyllous species under traditional Aboriginal burning regimens. With the cessation of traditional burning non-sclerophyllous species have re-colonised sclerophyll habitat in parts of Australia. Sclerophyllous plants generally resist dry conditions well, making them successful in areas of seasonally variable rainfall, the leaves are hard due to lignin, which prevents wilting and allows plants to grow, even when there isnt enough phosphorus for substantial new cell growth
17.
Grassland
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Grasslands are areas where the vegetation is dominated by grasses, however sedge and rush families can also be found. Grasslands occur naturally on all continents except Antarctica, grasslands are found in most ecoregions of the Earth. For example, there are five terrestrial ecoregion classifications of the grasslands, savannas, and shrublands biome. Grassland vegetation can vary in height from short, as in chalk grassland, to quite tall, as in the case of North American tallgrass prairie, South American grasslands. Woody plants, shrubs or trees, may occur on some grasslands – forming savannas, scrubby grassland or semi-wooded grassland, as flowering plants and trees, grasses grow in great concentrations in climates where annual rainfall ranges between 500 and 900 mm. The root systems of perennial grasses and forbs form complex mats that hold the soil in place, graminoids are among the most versatile life forms. Existing forest biomes declined, and grasslands became much more widespread, following the Pleistocene ice ages, grasslands expanded in range in the hotter, drier climates, and began to become the dominant land feature worldwide. Grasslands often occur in areas with annual precipitation between 600 mm and 1,500 mm and average annual temperatures ranges from −5 and 20 °C. However, some occur in colder and hotter climatic conditions. Grassland can exist in habitats that are disturbed by grazing or fire. Grasslands dominated by unsown wild-plant communities can be called natural or semi-natural habitats. The majority of grasslands in temperate climates are semi-natural and these grasslands contain many species of wild plants – grasses, sedges, rushes and herbs –25 or more species per square metre is not unusual. Chalk downlands in England can support over 40 species per square metre, in many parts of the world, few examples have escaped agricultural improvement. For example, original North American prairie grasslands or lowland wildflower meadows in the UK are now rare and their associated wild flora equally threatened. Some of the worlds largest expanses of grassland are found in African savanna, grasslands may occur naturally or as the result of human activity. Grasslands created and maintained by human activity are called anthropogenic grasslands, hunting peoples around the world often set regular fires to maintain and extend grasslands, and prevent fire-intolerant trees and shrubs from taking hold. The tallgrass prairies in the U. S. Midwest may have been extended eastward into Illinois, Indiana, much grassland in northwest Europe developed after the Neolithic Period, when people gradually cleared the forest to create areas for raising their livestock. Grassland types by Schimper, meadow steppe savannah Grassland types by Ellenberg & Mueller-Dombois, terrestrial herbaceous communities A. Savannas and related grasslands B
18.
Phytochorion
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A phytochorion, in phytogeography, is a geographic area with a relatively uniform composition of plant species. Adjacent phytochoria do not usually have a boundary, but rather a soft one. The region of overlap is called a tension zone. However, some prefer not to rank areas, referring to them simply as areas. Systems used to classify vegetation can be divided in two groups, those that use physiognomic-environmental parameters and characteristics and those that are based on floristic relationships. Several systems of classifying geographic areas where plants grow have been devised, most systems are organized hierarchically, with the largest units subdivided into smaller geographic areas, which are made up of smaller floristic communities, and so on. Phytochoria are defined as possessing a large number of endemic taxons. Floristic kingdoms are characterized by a degree of family endemism, floristic regions by a high degree of generic endemism. In the late 19th century, Adolf Engler was the first to make a map with the limits of distribution of floras. His Syllabus der Pflanzenfamilien, from the third onwards, also included a sketch of the division of the earth into floral regions. Other important early works on floristics includes Augustin de Candolle, Schouw, Alphonse de Candolle, Drude, botanist Ronald Good identified six floristic kingdoms, the largest natural units he determined for flowering plants. Goods six kingdoms are subdivided into units, called provinces. The Paleotropical kingdom is divided into three subkingdoms, which are subdivided into floristic provinces. Each of the five kingdoms are subdivided directly into provinces. There are a total of 37 floristic provinces, almost all provinces are further subdivided into floristic regions. Armen Takhtajan, in a widely used scheme that builds on Goods work, identified thirty-five floristic regions, each of which is subdivided into floristic provinces, guide to Standard Floras of the World. An annotated, geographically arranged systematic bibliography of the principal floras, enumerations, checklists, 2nd ed. pp. xxiv,1100. Cambridge University Press, Cambridge
19.
Clanwilliam, Western Cape
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Clanwilliam is a town in the Olifants River valley in the Western Cape, South Africa, about 200 kilometres north of Cape Town. It is located in, and the seat of, the Cederberg Local Municipality, as of 2011 Clanwilliam had a population of 7,674. Clanwilliam is situated at an elevation of 100 metres, between the slopes of the Cederberg mountains and the east bank of the Olifants River. It is located just off the N7 national road, which runs from Cape Town to the Namibian border, and on the R364 road, Clanwilliam is 230 kilometres from Cape Town by road. The Dutch Reform Church has been a national monument since 1973. The mission there used to run a school where Harold Cressy once taught whilst studying to become the first coloured man to gain a degree in Cape Town. In 1930 District Surgeon and botanist Dr Pieter Le Fras Nortier Rhodes scholar began conducting experiments with the cultivation of the rooibos plant, Dr Nortier also saw the vast commercial potential the tea held for the region. Dr Nortier cultivated the first plants at Clanwilliam on his farm Eastside, since 2001, Clanwilliam has been the site of the Clanwilliam Arts Festival, run by Cape Town-based Magnet Theatre. During the annual arts festival, workshops in fine arts, dance, music, theatre. Clanwilliam is the birthplace of ZP Theart, former lead vocalist, Municipality — The municipal council assumed a coat of arms on 13 February 1964 and registered them with the Cape Provincial Administration in August 1964. The crest was a tree, and the motto Toujours pret. Both the motto and the ermine on the shield were dervied from the Earl of Clanwilliams arms, divisional council — The Clanwilliam divisional council registered a coat of arms at the Bureau of Heraldry in May 1976. The arms were, Or, on a pale wavy Azure, the crest was a bunch of grapes between two elephant trunks, and the motto Fide labora
20.
Port Elizabeth
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Port Elizabeth or The Bay is one of the largest cities in South Africa, situated in the Eastern Cape Province,770 km east of Cape Town. The city, often shortened to PE and nicknamed The Friendly City or The Windy City, stretches for 16 km along Algoa Bay, Port Elizabeth is the southernmost large city on the African continent, just farther south than Cape Town. Port Elizabeth was founded as a town in 1820 to house British settlers as a way of strengthening the border region between the Cape Colony and the Xhosa and it now forms part of the Nelson Mandela Bay Metropolitan Municipality, which has a population of over 1.3 million. The area around what is now called Algoa Bay was first settled by hunting and gathering people ancestral to the San at least 100,000 years ago. Around 2,000 years ago, they were displaced or assimilated by agriculturalist populations ancestral to the Xhosa. For centuries, the area was marked on European navigation charts as a landing place with fresh water. One of the goals of the Portuguese Crown in the Indian Ocean was to take over the lucrative trade of Arab. As they took over that trade, the Portuguese strengthened trading with Goa, the name Algoa means to Goa, just as the port further north in present-day Mozambique, Delagoa means from Goa. The area became part of the Cape Colony and this area had a turbulent history between its founding by the Dutch East India Company in 1652 and the formation of the Union of South Africa in 1910 as a result of the British winning the Boer War. In 1799, during the first British occupation of the Colony during the Napoleonic Wars and this fort, built to protect against a possible landing of French troops, overlooked the site of what later became Port Elizabeth. The fort is now preserved as a monument, from 1814 to 1821, the Strandfontein farm, which later became the Summerstrand beach suburb of Port Elizabeth, was owned by Piet Retief. He later became a Voortrekker leader and was killed in 1837 by Zulu king Dingane during negotiations about land, an estimated 500 men, woman and children of his party were massacred. After Retief, the Strandfontein farm was owned by Frederik Korsten, another contemporary suburb of Port Elizabeth is named for him in the 21st century. At this time the town was founded by Sir Rufane Shaw Donkin, the Acting Governor of the Cape Colony. Diplomat Edmund Roberts visited Port Elizabeth in the early 1830s and he noted that Port Elizabeth in the 1820s had contained four houses, and now it has upward of one hundred houses, and its residents are rated at above twelve hundred persons. The Apostolic Vicariate of Cape of Good Hope, Eastern District, was established in the city in 1847, the town expanded as a diverse community comprising European, Cape Malay and other immigrants. The population increased rapidly after 1873 when the railway to Kimberley was built, during the Second Boer War, the port was an important transit point for British soldiers, horses and materials headed to the front by railway. While no armed conflict took place within the city, many refugees from the war moved into the city and these included Boer women and children, who were interned by the British in a concentration camp
21.
Holarctic
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These regions are further subdivided into a variety of ecoregions. Many ecosystems, and the animal and plant communities that depend on them, are found across continents in large portions of this realm. The continuity of these results from the shared glacial history of the realm. The floristic Boreal Kingdom corresponds to the Holarctic realm, within the Holarctic realm, there are a variety of ecosystems. The type of ecosystem found in an area depends on the latitude, in the far north, a band of arctic tundra circles the shore of the Arctic Ocean. The ground beneath this land is permafrost, frozen year-round, in these difficult growing conditions, few plants can survive. South of the tundra, the boreal forest stretches across North America and this land is characterized by coniferous trees. South of here, the ecosystems become more diverse, some areas are covered in temperate grassland, while others are covered in temperate forest, dominated by deciduous trees. The southern extent of the Holarctic typically reaches into the desert, a variety of animal species are distributed across continents, throughout much of the Holarctic realm. Some of these included the brown bear, grey wolf, red fox, wolverine, moose, caribou, golden eagle, the brown bear is found in mountainous and semi-open areas distributed throughout the Holarctic. It once occupied much larger areas, but has driven out by human development. Today it is found in remaining wilderness areas. The grey wolf is found in a variety of habitats from tundra to desert. The red fox is an adaptable predator. It has the widest distribution of any terrestrial carnivore, and is adapted to a range of habitats. Like the wolf, it is distributed throughout the majority of the Holarctic, the wolverine is a large member of the weasel family found primarily in the arctic and in boreal forests, ranging south in mountainous regions. It is distributed in areas throughout Eurasia and North America. The moose is the largest member of the deer family and it is found throughout most of the boreal forest through continental Eurasia into Scandinavia, eastern North America, and boreal and montane regions of western North America
22.
Erica
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Erica is a genus of roughly 860 species of flowering plants in the family Ericaceae. The English common names heath and heather are shared by closely related genera of similar appearance. The genus Calluna was formerly included in Erica – it differs in having even smaller scale-leaves, Erica is sometimes referred to as winter heather to distinguish it from Calluna summer heather. The Latin word erica means heath or broom and it is believed that Pliny adapted erica from Ancient Greek ἐρείκη. The expected Anglo-Latin pronunciation, /ᵻˈraɪkə/, may be given in dictionaries, but /ˈɛrᵻkə/ is more commonly heard. Most of the species of Erica are small shrubs from 20–150 cm high, though some are taller, all are evergreen, with minute, needle-like leaves 2–15 mm long. Flowers are sometimes axillary, and sometimes borne in umbels or spikes. The seeds are small, and in some species may survive in the soil for decades. Dulfer published the last revision of the genus Erica, treating 605 species, many new species have subsequently been described and a further 83 have been included in Erica from former “minor genera”, such as Phillipia Klotzsch and Blaeria L. A more recent overview of Erica species is provided in an identification aid. A number of increasingly detailed phylogenetic hypotheses for Erica have been published based on nuclear ribosomal, the closest relatives of Erica are Daboecia and Calluna, representing the oldest surviving lineages of a, by inference, ancestrally Palearctic tribe Ericeae. The small number of European Erica species represent the oldest lineages of the genus, within which a single, order-of-magnitude more species rich, within the African clade, Cape and Madagascan/Mascarene species respectively represent monophyletic groups. Around 690 of the species are endemic to South Africa, the remaining species are native to other parts of Africa, Madagascar, the Mediterranean, and Europe. Like most Ericaceae, Erica species are mainly calcifuges, being limited to acidic or very acidic soils, in fact, the term ericaceous is frequently applied to all calcifuges, and to the compost used in their cultivation. Soils range from dry, sandy soils to extremely wet ones such as bog and they often dominate dwarf-shrub habitats, or the ground vegetation of open acidic woodland. Erica species are grown as landscape or garden plants for their floral effect and they associate well with conifers and are frequently seen in planting schemes as massed groundcover beneath varieties of dwarf conifers. They are capable of producing flower colour throughout the year and they can also be grown in tubs or window boxes to provide interest through autumn and into winter. Some species of sunbirds are known to visit and pollinate Erica, two such species are the southern double-collared sunbird and the orange-breasted sunbird
23.
Species description
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A species description is a formal description of a newly discovered species, usually in the form of a scientific paper. Its purpose is to give a description of a new species of organism and explain how it differs from species which have been described previously. The species description often contains photographs or other illustrations of the type material, the publication in which the species is described gives the new species a formal scientific name. Today, some 1.9 million species have been described and named and it is customary for scientists to introduce all relevant new findings and research in a scientific manuscript, which is sent to other scientists for peer review. If accepted, it is published in a journal of the appropriate discipline or in a book. Descriptions and naming of a new species or other taxa follow the same process, a name of a new species becomes valid with the date of publication of its formal scientific description. A scientific species description must fulfill several formal criteria specified by the nomenclature codes, Species names are written in the 26 letters of the Latin alphabet, but many species names are based on words from other languages, Latinized. Once the manuscript has been accepted for publication, the new name is officially created. Once a species name has been assigned and approved, it can not be changed except in the case of error. For example, a species of beetle was named by a German collector after Adolf Hitler in 1933 when he had become chancellor of Germany. It is not clear whether such a dedication would be considered acceptable or appropriate today, Species names have been chosen on many different bases. Most common is a naming for the external appearance, its origin. Examples would include a bat species named for the two stripes on its back, a named for its Bolivian origin, and an ant species dedicated to the actor Harrison Ford. A scientific name in honor of a person or persons is a known as a taxonomic patronym or patronymic, a number of humorous species names also exist. Literary examples include the genus name Borogovia, which is named after the borogove, a second example, Macrocarpaea apparata was named after the magical spell to apparate from the Harry Potter novels by J. K. Rowling, as it seemed to appear out of nowhere. For example, the genus Victoria was named in honour of Queen Victoria of Great Britain, more recently, a species of lemur was named after the actor John Cleese in recognition of his work to publicize the plight of lemurs in Madagascar. Non-profit ecological organizations may also allow benefactors to name new species in exchange for support for taxonomic research. A German non-profit organisation, BIOPAT - Patrons for Biodiversity has raised more than $450,000 for research, the International Code of Nomenclature for algae, fungi, and plants discourages this practice somewhat, Recommendation 20A
24.
Netherlands
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The Netherlands, also informally known as Holland is the main constituent country of the Kingdom of the Netherlands. It is a densely populated country located in Western Europe with three territories in the Caribbean. The European part of the Netherlands borders Germany to the east, Belgium to the south, and the North Sea to the northwest, sharing borders with Belgium, the United Kingdom. The three largest cities in the Netherlands are Amsterdam, Rotterdam and The Hague, Amsterdam is the countrys capital, while The Hague holds the Dutch seat of parliament and government. The port of Rotterdam is the worlds largest port outside East-Asia, the name Holland is used informally to refer to the whole of the country of the Netherlands. Netherlands literally means lower countries, influenced by its low land and flat geography, most of the areas below sea level are artificial. Since the late 16th century, large areas have been reclaimed from the sea and lakes, with a population density of 412 people per km2 –507 if water is excluded – the Netherlands is classified as a very densely populated country. Only Bangladesh, South Korea, and Taiwan have both a population and higher population density. Nevertheless, the Netherlands is the worlds second-largest exporter of food and agricultural products and this is partly due to the fertility of the soil and the mild climate. In 2001, it became the worlds first country to legalise same-sex marriage, the Netherlands is a founding member of the EU, Eurozone, G-10, NATO, OECD and WTO, as well as being a part of the Schengen Area and the trilateral Benelux Union. The first four are situated in The Hague, as is the EUs criminal intelligence agency Europol and this has led to the city being dubbed the worlds legal capital. The country also ranks second highest in the worlds 2016 Press Freedom Index, the Netherlands has a market-based mixed economy, ranking 17th of 177 countries according to the Index of Economic Freedom. It had the thirteenth-highest per capita income in the world in 2013 according to the International Monetary Fund, in 2013, the United Nations World Happiness Report ranked the Netherlands as the seventh-happiest country in the world, reflecting its high quality of life. The Netherlands also ranks joint second highest in the Inequality-adjusted Human Development Index, the region called Low Countries and the country of the Netherlands have the same toponymy. Place names with Neder, Nieder, Nether and Nedre and Bas or Inferior are in use in all over Europe. They are sometimes used in a relation to a higher ground that consecutively is indicated as Upper, Boven, Oben. In the case of the Low Countries / the Netherlands the geographical location of the region has been more or less downstream. The geographical location of the region, however, changed over time tremendously
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