Island

Last updated

The Hawaiian Islands, a major archipelago in the Pacific Ocean Hawaje-NoRedLine.jpg
The Hawaiian Islands, a major archipelago in the Pacific Ocean

An island or isle is a piece of subcontinental land completely surrounded by water. There are continental islands, which were formed by being split from a continent by plate tectonics, and oceanic islands, which have never been part of a continent. Oceanic islands can be formed from volcanic activity, grow into atolls from coral reefs, and form from sediment along shorelines, creating barrier islands. River islands can also form from sediment and debris in rivers. Artificial islands are those made by humans, including small rocky outcroppings built out of lagoons and large-scale land reclamation projects used for development.

Contents

Islands are host to a diverse array of plant and animal life. Oceanic islands have the sea as a natural barrier to the introduction of new species, causing the species that do reach the island to evolve in isolation. Continental islands share animal and plant life with the continent they split from. Depending on how long ago the continental island formed, the life on that island may have diverged greatly from the mainland due to natural selection.

Humans have lived on and traveled between islands for thousands of years at a minimum. Some islands became host to humans due to a land bridge or a continental island splitting from the mainland. Polynesians were the first group of humans to colonize islands at scale, dispersing over the Pacific Ocean starting near New Guinea starting as early as 1100 BC. Today, up to 10% of the world's population lives on islands. Islands are popular targets for tourism due to their perceived natural beauty, isolation, and unique cultures.

Islands became the target of colonization by Europeans, resulting in the majority of islands in the Pacific being put under European control. Decolonization has resulted in some but not all island nations becoming self-governing, with lasting effects related to industrialization, nuclear weapons testing, invasive species, and tourism. Islands and island countries are threatened by climate change. Sea level rise threatens to submerge nations such as Tuvalu and the Marshall Islands completely. Increases in the frequency and intensity of tropical cyclones can cause widespread destruction of infrastructure and animal habitats. Species that live exclusively on islands are some of those most threatened by extinction.

Definition

An island is an area of land surrounded by water on all sides that is distinct from a continent. [1] There is no standard of size that distinguishes islands and continents. Continents have an accepted geological definition -- they are the largest landmass of a particular tectonic plate. [2] Islands can occur in any body of water, including rivers, seas, and lakes. [3] Low-tide elevations, areas of land that are not above the surface during a high tide, are generally not considered islands. [4] Islands that have been bridged or otherwise joined to a mainland with land reclamation are sometimes considered "de-islanded", but not in every case. [5]

Etymology

The word island derives from Middle English iland , from Old English igland (from ig or ieg, similarly meaning 'island' when used independently, and -land carrying its contemporary meaning. Old English ieg is actually a cognate of Swedish ö and German Aue, and more distantly related to Latin aqua (water). [6]

The spelling of the word was modified in the 15th century because of a false etymology caused by an association with the Old French loanword isle, which itself comes from the Latin word insula. [1] [7]

Geology

Cross section through Earth at the Hawaii hotspot. Magma from the mantle rises into the lithosphere, creating a chain of volcanoes as the lithosphere moves over the hotspot. Hawaii hotspot cross-sectional diagram.jpg
Cross section through Earth at the Hawaii hotspot. Magma from the mantle rises into the lithosphere, creating a chain of volcanoes as the lithosphere moves over the hotspot.

Formation in oceans

Islands often are found in archipelagos or island chains, which are collections of islands. These chains are thought to form from volcanic hotspots, areas of the lithosphere where the mantle is hotter than the surrounding area. [8] [9] These hotspots would give rise to volcanoes whose lava would form the rock the islands are made of. [8] For some islands, the movement of tectonic plates above stationary hotspots would form islands in a linear chain, with the islands further away from the hotspot being progressively older and more eroded, before disappearing under the sea entirely. [10] An example is the Hawaiian Islands, [10] with the oldest island being 25 million years old, and the youngest, Hawaii, still being an active volcano. [9] However, not all island chains are formed this way. Some may be formed all at once by fractures in the tectonic plates themselves simultaneously creating multiple islands. One supporting piece of evidence is that of the Line Islands, which are all estimated to be 8 million years old, rather than being different ages. [9]

Map from Charles Darwin's 1842 The Structure and Distribution of Coral Reefs showing the world's major groups of atolls and coral reefs On the structure and distribution of coral reefs BHL40453231.jpg
Map from Charles Darwin's 1842 The Structure and Distribution of Coral Reefs showing the world's major groups of atolls and coral reefs

Other island chains form due to being separated from existing continents. The Japanese archipelago may have been separated from Eurasia due to seafloor spreading, a phenomenon where new oceanic crust is formed, pushing away older crust. [9] Islands sitting on the continental shelf may be called continental islands. [3] Other islands, like those that make up New Zealand, are what remains of continents that shrank and sunk beneath the sea. [11] It was estimated that Zealandia, the continent-like area of crust that New Zealand sits on, has had 93% of its original surface area submerged. [11]

Some islands are formed when coral reefs grow on volcanic islands that have submerged beneath the surface. [12] When these coral islands encircle a central lagoon, the island is known as an atoll. [13] The formation of reefs and islands related to those reefs is aided by the buildup of sediment in shallow patches of water. In some cases, tectonic movements lifting a reef out of the water by as little as 1 meter can cause sediment to accumulate and an island to form. [12]

A barrier island in the Outer Banks off the East Coast of the United States NOAA- Outer Banks.jpg
A barrier island in the Outer Banks off the East Coast of the United States

Barrier islands are long, sandy bars that form along shorelines due to the deposition of sediment by waves. These islands erode and grow as the wind and waves shift. Barrier islands have the effect of protecting coastal areas from severe weather because they absorb some of the energy of large waves before they can reach the shore. [14]

Formation in freshwater

A fluvial island is an island that forms from the erosion and sedimentation of debris in rivers; almost all rivers have some form of fluvial islands. [15] These islands may only be a few meters high, and are usually temporary. Changes in the flow speed, water level, and sediment content of the river may effect the rate of fluvial island formation and depletion. [15] Permanent river islands also exist, the largest of which (that is completely inland) is Bananal Island in the Tocantins of Brazil, which has a maximum width of 55 kilometers. [16]

Lakes form for a variety of reasons, including glaciers, plate tectonics, and volcanism. [17] Lake islands can form as part of these processes. [18]

Life on islands

The field of insular biogeography studies the ecological processes that take place on islands, with a focus on what factors effect the evolution, extinction, and richness of species. Scientists often study islands as an isolated model of how the process of natural selection takes place. [19] [20] Island ecology studies organisms on islands and their environment. It has yielded important insights for its parent field of ecology since the time of Charles Darwin. [20]

Endemism

The Galapagos penguin is endemic to the Galapagos Islands. Galapagos penguin (Spheniscus mendiculus) male.jpg
The Galapagos penguin is endemic to the Galápagos Islands.

In biology, endemism is defined as the phenomenon where species or genus is only found in a certain geographical area. Islands isolate land organisms from others with water, and isolate aquatic organisms living on them with land. [20] Island ecosystems have the highest rates of endemism globally. This means that islands contribute heavily to global biodiversity. [21] Areas with high lives of biodiversity are a priority target of conservation efforts, to prevent the extinction of these species. [22] Despite high levels of endemism, the total species richness, the total number of unique species in a region, is lower on islands than on mainlands. [23] The level of species richness on islands is proportional to the area of that island, a phenomenon known as the species-area relationship. This is because larger areas have more resources and thus can support more organisms. Populations with a higher carrying capacity also have more genetic diversity, which promotes speciation. [20]

Dispersal

The Seychelles fruit bat has a major role in distributing the seeds of trees between islands, a form of oceanic dispersal. Pteropus seychellensis.jpg
The Seychelles fruit bat has a major role in distributing the seeds of trees between islands, a form of oceanic dispersal.

Oceanic islands, ones that have never been connected to shore, are only populated by life that can cross the sea. This means that any animals present on the island had to have flown there, in the case of birds or bats, were carried by such animals, or were carried in a sea current in what is known as a "rafting event". This phenomenon is known as oceanic dispersal. [25] Tropical storms have the capacity to transport species over great distances. [26] Animals like tortoises can live for weeks without food or water, and are able to survive floating on debris in the sea. [27] One case study showed that in 1995, fifteen iguanas survived a 300 km journey to Anguilla in the Caribbean, an island which no iguana had lived on previously. They survived floating on a mass of uprooted trees from a storm. [28] Plant species are thought to be able to travel great distances of ocean. New Zealand and Australia share 200 native plant species, despite being separated by 1500 km. [25]

Continental islands, islands that were at one point connected to a continent, are expected to share a common history of plant and animal life up until the point that the island broke away from the continent. [25] For example, the presence of freshwater fish on an island surrounded by ocean would indicate that it once was attached to a continent, since these fish cannot traverse the ocean on their own. [20] Over the course of time, evolution and extinction changes the nature of animal life on a continental island, but only once it splits from the mainland. An example is that of the southern beech, a tree that is present in Australia, New Zealand, parts of South American, and New Guinea, places that today are geographically distant. A possible explanation for this phenomena is that these landmasses were once all part of the continent Gondwana and separated by tectonic drift. However, there are competing theories that suggest this species may have reached faraway places by way of oceanic dispersal. [25]

Evolution on island groups

Adaptive radiation of finch A (Geospiza magnirostris) into three other species of finches on the Galapagos Islands. Due to the absence of other birds, Darwin's finches adapted to new niches. Their seed-eating beaks evolved to handle foods such as nuts, fruits, and insects. Finchadaptiveradiation.png
Adaptive radiation of finch A ( Geospiza magnirostris ) into three other species of finches on the Galapagos Islands. Due to the absence of other birds, Darwin's finches adapted to new niches. Their seed-eating beaks evolved to handle foods such as nuts, fruits, and insects.

Species that colonize island archipelagos exhibit a specific property known as adaptive radiation. In this process, a species that arrives on a group of islands rapidly becomes more diverse over time, splitting off into new species or subspecies. A species that reaches an island ecosystem may face little competition for resources, or may find that the resources that they found in their previous habitat are not available. These factors together result in individual evolutionary branches with different means of survival. [29]

The classical example of this is Darwin's finches, a group of up to fifteen tanager species that are endemic to the Galápagos Islands. [30] These birds evolved different beaks in order to eat different kinds of food available on the islands. The large ground finch has a large bill used to crack seeds and eat fruit. The Genovesa cactus finch prefers cacti as a food source, and has a beak adapted for removing pulp and flowers from cacti. The green warbler-finch (in the habit of true warbler species) consumes spiders and insects that live on plants. [29] Other examples of this phenomenon exist worldwide, including in Hawaii and Madagascar, and are not limited to island ecosystems. [29]

The island rule

The extinct Dodo is an example of island gigantism. Dronte dodo Raphus cucullatus.jpg
The extinct Dodo is an example of island gigantism.

Species endemic to islands show a common evolutionary trajectory. Foster's rule (also known as the island rule), states that small mammals such as rodents evolve to become larger, known as island gigantism. One such example is the giant tortoise of the Seychelles, though it is unknown if it grew in size before or after reaching the island. Larger animals such as the hippopotamus tend to become smaller, such as in the case of the pygmy hippopotamus. This is known as insular dwarfism. [31] In the case of smaller animals, it has been hypothesized that animals on islands may have fewer predators and competitors, resulting in selection pressure towards larger animals. Larger animals may exhaust food resources quickly due to their size, causing malnutrition in their young, resulting in a selection pressure for smaller animals that require less food. Having fewer predators would mean these animals did not need not be large to survive. [31]

Darwin, the Galápagos, and natural selection

Charles Darwin formulated the theory of natural selection through the study of island ecology. [20] The species he observed on the Galápagos Islands, including tanager birds, contributed to his understanding of how evolution works. [32] He first traveled to the islands as a naturalist on the HMS Beagle in 1835, as part of a five-year circumnavigation of Earth. He wrote that "the different islands to a considerable extent are inhabited by a different set of beings". [33] Through the study of the finches and other animals he realized that organisms survive by changing to adapt to their habitat. [33] It would be over twenty years before he published his theories in On the Origin of Species. [34]

Humans and islands

History of exploration

The first evidence of humans colonizing islands probably occurred in the Paleolithic era, 100,000 to 200,000 years ago. Reaching the Indonesian islands of Flores and Timor would have required crossing distances of water of at least 29 km (18 mi). [35] The next notable island to be colonized is Australia, having been settled 10,000 years ago via a similar water crossing. [35] Some islands, such as Honshu, were probably connected to the mainland with a land bridge that allowed humans to colonize it before it became an island. [35]

Chronological dispersal of the Austronesian peoples Chronological dispersal of Austronesian people across the Pacific.svg
Chronological dispersal of the Austronesian peoples

The first people to colonize oceanic islands at scale were the Polynesians. [37] Many of the previous island settlements required traveling distances of less than 100 km (62 mi), whereas Polynesians may have traveled 2,000–3,200 km (1,200–2,000 mi) to settle islands such as Tahiti. [35] They would send navigators to sail the ocean without the aid of navigational instruments to discover new islands for settlement. [37] [38] Between 1100 and 800 BC, Polynesians sailed East from New Guinea and the Solomon Islands and reached the islands that make up the modern-day Fiji and Samoa. [39] The furthest extent of this migration would be Easter Island in the East, and New Zealand in the South, with New Zealand's first settlements between 1250 and 1300. [40] Other cultures, such as Native Americans and various populations in Africa, were also able to colonize islands. [35]

Historians have sought to understand why some remote islands have always been uninhabited, while others, especially in the Pacific Ocean, have long been populated by humans. [35] Generally, small islands that cannot sustain populations on their own can still be habitable if they are within a "commuting" distance to an island that has enough resources to be sustainable. This also implies that larger islands are more likely to be able to sustain humans and thus are more likely to have been settled. [35] Island chains may be easier for a navigator to find than a single island, since the presence of an island is marked by seabirds, differences in cloud and weather patterns, as well as changes in the direction of waves. [38] [37] It is also possible for human populations to have gone extinct on islands, evidenced by explorers finding islands that show evidence of habitation but no life. [35]

Not all islands were or are inhabited by maritime cultures. [35] [41] In the past, some societies were found to have lost their seafaring ability over time, such as the case of the Canary Islands, which were occupied by an indigenous people since the island's first discovery in the first century until being conquered by the Spanish Empire in 1496. [41] It has been hypothesized that since the inhabitants had little incentive for trade and had little to any contact with the mainland, they had no need for boats. [41]

The motivation for island exploration has been the subject of research and debate. Some early historians previously argued that early island colonization was unintentional, perhaps by a raft being swept out to sea. [42] Others compare the motivations of Polynesian and similar explorers with those of Christopher Columbus, the explorer who sailed westward over the Atlantic Ocean in search of an alternate route to the East Indies. [35] These historians theorize that successful explorers were rewarded with recognition and wealth, leading others to attempt possibly dangerous expeditions to discover more islands, usually with poor results. [35]

Lifestyle

With the exception of Greenland, islands make up 1.47% of the world's surface area. Despite this, 10% of the world's population lives on islands. [43] The study of the culture of islands is known as island studies. The interest in the study of islands is due to their unique cultures and natural environments that differ from mainland cultures. [43] This is for a few reasons: First, the obvious political and geographic isolation from mainland cultures. [43] Second, unique restraints on resources and ecology creating marine-focused cultures with a focus on fishing and sailing. [43] Third, a lasting historical and political significance of islands. [43]

A breadfruit tree in Malaysia, used in Polynesia for making an edible breadfruit paste. Breadfruit (Artocarpus altilis), Malaysia.JPG
A breadfruit tree in Malaysia, used in Polynesia for making an edible breadfruit paste.
Cultivated taro plants, a staple food for many island cultures. Cultivated Colocasia esculenta.jpg
Cultivated taro plants, a staple food for many island cultures.

Diet

The Polynesian diet got most of its protein from fishing. [44] Polynesians were known to fish close to shore, as well as in deep water. It was reported that Rapa Nui people were known to fish as far as 500 km (310 mi) from shore at coral reefs. [45] Spear, line, and net fishing were all used, [46] to catch tuna as well as sharks and stingrays. [45] Island cultures also cultivate native and non-native crops. [41] Polynesians grew the native yam, taro, breadfruit, banana, coconut and other fruits and vegetables. [47] Different island climates made different resources more important, such as the Hawaiian islands being home to irrigated fields of taro, [46] whereas in some islands, like Tahiti, breadfruit was more widely cultivated and fermented in order to preserve it. [48] There is archeological evidence that Canary Islanders would chew the roots of ferns for sustenance, a practice that wore heavily on their molars. [41] These islanders would also grow barley and raised livestock such as goats. [41]

Island nations and territories

Many island nations have little land and a restricted set of natural resources. However, these nations control some of the largest fisheries in the world, deposits of copper, gold, and nickel, as well as oil deposits. The natural beauty of island nations also makes them a magnet for tourism. Islands also have geopolitical value for naval bases, weapons testing, and general territorial control. One such example is French Polynesia, a territory that receives substantial military expenditure and aid from France. [49]

Colonization

Residents of Bikini Atoll leaving due to nuclear testing. Leaving-bikini.jpg
Residents of Bikini Atoll leaving due to nuclear testing.

Since the first discoveries of Polynesian, Micronesian, and other islands by Westerners, these nations have been the subject of colonization. [50] Islands were the target of Christian missionaries. These missionaries faced resistance, but found success when some local chiefs used European support to centralize power. Beginning in the 16th century, European states placed most of Oceania in under colonial administration. [51] Pohnpei was colonized by Spain as early as 1526. It changed hands from Germany to Japan to the United States before joining the Federated States of Micronesia in 1982, maintaining a "free association" status with the U.S. [52] Guam was a Spanish territory until 1898, and now is a unincorporated territory of the U.S. [53]

The decolonization era saw many island states achieve independence or some form of self-governance. [54] Nuclear weapons testing on the Marshall Islands left many atolls destroyed or uninhabitable, causing the forced displacement of people from their home islands as well as increases in cancer rates due to radiation. [50] Colonization has resulted in a decline of observance of traditional cultural practices in places such as Hawaii, where Native Hawaiians are now a minority. Cultural attitudes related to communal ownership of land as well as a lack of individualistic decision-making may make some island cultures less compatible with the global capitalist economy, causing these nations to experience less economic growth. [54]

Tourists are attracted to tropical beaches in large numbers, such as this one in Malapascua, the Philippines. Malapascua (island), Tropical beach, Philippines.jpg
Tourists are attracted to tropical beaches in large numbers, such as this one in Malapascua, the Philippines.

Tourism

Islands have long been a popular target for tourism, thanks to their unique climates, cultures, and natural beauty. However, islands may suffer from poor transportation connectivity from airplanes and boats and strains on infrastructure from tourist activity. [55] Islands in colder climates often rely on seasonal tourists seeking to enjoy nature or local cultures, and may only be one aspect of an island's economy. In contrast, tourism on tropical islands can often make up the majority of the local economy and built environment. These islands sometimes also require consistent foreign aid on top of tourism in order to ensure economic growth. This reliance can result in social inequality and environmental degradation. During tourism downturns, these economies struggle to make up the lost inflow of cash with other industries. [55]

Threats to islands

San Juan, Puerto Rico after Hurricane Maria. Climate change is expected to cause more frequent inland flooding on islands. Calle Loiza in San Juan, Puerto Rico after Hurricane Maria.jpg
San Juan, Puerto Rico after Hurricane Maria. Climate change is expected to cause more frequent inland flooding on islands.

Climate change threatens human development on islands due to sea level rise, more dangerous tropical cyclones, coral bleaching, and an increase in invasive species. [56] For example, in 2017 Hurricane Maria caused a loss of almost all the infrastructure in Dominica. Sea level rise and other climate changes can reduce freshwater reserves, resulting in droughts. [56] These risks are expected to decrease the habitability of islands, especially small ones. Beyond risks to human life, plant and animal life are threatened. It has been estimated that almost 50% of land species threatened by extinction live on islands. [56] Coral bleaching is expected to occur with more frequency, threatening marine ecosystems, some of which island economies are dependent on. [56]

Some islands that are low-lying may cease to exist given high enough amounts of sea level rise. Tuvalu received media attention for a press conference publicizing the ongoing submerging of the island country. [57] Tuvalu signed a cooperation agreement with Australia agreeing to annually allow 280 of its citizens to become permanent residents of Australia. The Marshall Islands, a country of 1,156 islands, have also been identified as a country that may be existentially threatened by rising seas. [57]

Increasing intensity of tropical storms also increases the distances and frequency with which invasive species may be transported to islands. Floodwaters from these storms may also wash plants further inland than they would travel on their own, introducing them to new habitats. [26] Agriculture and trade also have introduced non-native life to islands. These processes result in an introduction of invasive species to ecosystems that are especially small and fragile. One example is the apple snail, initially introduced to the U.S. by aquarium owners. It has since been transported by hurricanes across the Gulf Coast and neighboring islands. [26] These species compete for resources with native animals, and some may grow so densely that they displace other forms of existing life. [26]

Artificial islands

Kansai International Airport in Osaka is built on an artificial island. Kansai International Airport Aerial photograph.2007.jpg
Kansai International Airport in Osaka is built on an artificial island.

For hundreds of years, islands have been created through land reclamation. [58] One of the first recorded instances of this when people of the Solomon Islands created eighty such islands by piling coral and rock in the Lau Lagoon. [58] One traditional way of constructing islands is with the use of a revetment. Sandbags or stones are dropped with a barge into the sea to bring the land level slightly out of the water. The island area is then filled with sand or gravel, followed by a construction of this revetment to hold it together. [59] Islands have also been constructed with a permanent caisson, a steel or concrete structure built in a closed loop and then filled with sand. [59]

Some modern islands have been constructed by pouring millions of tons of sand into the sea, such as with Pearl Island in Qatar or the Palm Islands in Dubai. [58] These islands are usually created for real estate development, and are sold for private ownership or construction of housing. [58] Offshore oil platforms have also been described as a type of island. Some atolls have been covered in concrete to create artificial islands for military purposes, such as those created by China in the South China Sea. [58] [60] These atolls were previously low-tide elevations, landmasses that are only above water during low tide. The United Nations Convention on the Law of the Sea indicates that these islands may not have the same legal status as a naturally occurring island, and as such may not confer the same legal rights. [60]

See also

Commons-logo.svg
Wikimedia Commons has media related to:
Island (category)
Wikiquote-logo.svg
Wikiquote has quotations related to Islands .

Related Research Articles

<span class="mw-page-title-main">Oceania</span> Geographical region in the Pacific Ocean

Oceania is a geographical region including Australasia, Melanesia, Micronesia, and Polynesia. Outside of the English-speaking world, Oceania is generally considered a continent, while Australia is regarded as an island or a continental landmass contained inside of the larger continent of Oceania. Spanning the Eastern and Western Hemispheres, at the centre of the water hemisphere, Oceania is estimated to have a land area of about 9,000,000 square kilometres (3,500,000 sq mi) and a population of around 44.4 million as of 2022. When compared to the continents, Oceania is the smallest in land area and the second-least populated after Antarctica.

<span class="mw-page-title-main">Oceanian realm</span> Terrestrial biogeographic realm

The Oceanian realm is one of the eight biogeographic realms and is unique in not including any continental land mass. It has the smallest land area of any of the WWF realms.

<span class="mw-page-title-main">Pacific Islander</span> Person from the Pacific Islands

Pacific Islanders, Pasifika, Pasefika, Pacificans or rarely Pacificers are the peoples of the Pacific Islands. As an ethnic/racial term, it is used to describe the original peoples—inhabitants and diasporas—of any of the three major subregions of Oceania or any other island located in the Pacific Ocean.

Lemuria, or Limuria, was a continent proposed in 1864 by zoologist Philip Sclater, theorized to have sunk beneath the Indian Ocean, later appropriated by occultists in supposed accounts of human origins. The theory was discredited with the discovery of plate tectonics and continental drift in the 20th century.

<span class="mw-page-title-main">Ancient Hawaii</span> Period in Hawaiian history

Ancient Hawaiʻi is the period of Hawaiian history preceding the unification in 1810 of the Kingdom of Hawaiʻi by Kamehameha the Great. Traditionally, researchers estimated the first settlement of the Hawaiian islands as having occurred sporadically between 400 and 1100 CE by Polynesian long-distance navigators from the Samoan, Marquesas, and Tahiti islands within what is now French Polynesia. In 2010, a study was published based on radiocarbon dating of more reliable samples which suggests that the islands were settled much later, within a short timeframe, in about 1219 to 1266.

<span class="mw-page-title-main">Maritime Southeast Asia</span> Cultural and economic area within Southeast Asia

Maritime Southeast Asia comprises the countries of Brunei, Indonesia, Malaysia, the Philippines, Singapore, and East Timor.

<span class="mw-page-title-main">Near Oceania</span> Islands of Oceania near to Australia

Near Oceania is the part of Oceania that features greater biodiversity, due to the islands and atolls being closer to each other. The distinction of Near and Remote Oceania was first suggested by Pawley & Green (1973) and was further elaborated on in Green (1991). The distinction is based on geology, flora and fauna. Near Oceania was also settled by humans at an earlier time than Remote Oceania was. Near Oceania includes the island of New Guinea, Solomon Islands(excluding Temotu) and the Bismarck Archipelago. Sometimes Australia is also included in Near Oceania.

<span class="mw-page-title-main">Isthmus of Panama</span> Narrow landstrip in Panama

The Isthmus of Panama, also historically known as the Isthmus of Darien, is the narrow strip of land that lies between the Caribbean Sea and the Pacific Ocean, linking North and South America. It contains the country of Panama and the Panama Canal. Like many isthmuses, it is a location of great geopolitical and strategic importance.

<span class="mw-page-title-main">Indigenous peoples of Oceania</span>

The Indigenous peoples of Oceania are Aboriginal Australians, Papuans, and Austronesians. These indigenous peoples have a historical continuity with pre-colonial societies that developed on their territories. With the notable exceptions of Australia, New Zealand, Hawaii, New Caledonia, Guam, and Northern Mariana Islands, indigenous peoples make up the majority of the populations of Oceania.

<span class="mw-page-title-main">Coral island</span> Island formed from coral and associated material

A coral island is a type of island formed from coral detritus and associated organic material. It occurs in tropical and sub-tropical areas, typically as part of a coral reef which has grown to cover a far larger area under the sea. The term low island can be used to distinguish such islands from high islands, which are formed through volcanic action. Low islands are formed as a result of sedimentation upon a coral reef or of the uplifting of such islands.

<span class="mw-page-title-main">Polynesian navigation</span> Methods to navigate the Pacific Ocean

Polynesian navigation or Polynesian wayfinding was used for thousands of years to enable long voyages across thousands of kilometres of the open Pacific Ocean. Polynesians made contact with nearly every island within the vast Polynesian Triangle, using outrigger canoes or double-hulled canoes. The double-hulled canoes were two large hulls, equal in length, and lashed side by side. The space between the paralleled canoes allowed for storage of food, hunting materials, and nets when embarking on long voyages. Polynesian navigators used wayfinding techniques such as the navigation by the stars, and observations of birds, ocean swells, and wind patterns, and relied on a large body of knowledge from oral tradition. This island hopping was a solution to the scarcity of useful resources, such as food, wood, water, and available land, on the small islands in the Pacific Ocean. When an island’s required resources for human survival began to run low, the island's inhabitants used their maritime navigation skills and set sail for new islands. However, as an increasing number of islands in the South Pacific became occupied, and citizenship and national borders became of international importance, this was no longer possible. People thus became trapped on islands with the inability to support them.

<span class="mw-page-title-main">Boundaries between the continents</span>

Determining the boundaries between the continents is generally a matter of geographical convention. Several slightly different conventions are in use. The number of continents is most commonly considered seven but may range as low as four when Afro-Eurasia and the Americas are both considered as single continents. An island can be considered to be associated with a given continent by either lying on the continent's adjacent continental shelf or being a part of a microcontinent on the same principal tectonic plate. An island can also be entirely oceanic while still being associated with a continent by geology or by common geopolitical convention. Another example is the grouping into Oceania of the Pacific Islands with Australia and Zealandia.

Continental crustal fragments, partly synonymous with microcontinents, are pieces of continents that have broken off from main continental masses to form distinct islands that are often several hundred kilometers from their place of origin.

<span class="mw-page-title-main">Australia (continent)</span> One of Earths seven main divisions of land

The continent of Australia, sometimes known in technical contexts by the names Sahul, Australia-New Guinea, Australinea, Oceania, or Meganesia to distinguish it from the country of Australia, is located within the Southern and Eastern hemispheres. The continent includes mainland Australia, Tasmania, the island of New Guinea, the Aru Islands, the Ashmore and Cartier Islands, most of the Coral Sea Islands, and some other nearby islands. Situated in the geographical region of Oceania, Australia is the smallest of the seven traditional continents.

<span class="mw-page-title-main">Polynesia</span> Subregion of Oceania

Polynesia is a subregion of Oceania, made up of more than 1,000 islands scattered over the central and southern Pacific Ocean. The indigenous people who inhabit the islands of Polynesia are called Polynesians. They have many things in common, including language relatedness, cultural practices, and traditional beliefs. In centuries past, they had a strong shared tradition of sailing and using stars to navigate at night.

Island ecology is the study of island organisms and their interactions with each other and the environment. Islands account for nearly 1/6 of earth’s total land area, yet the ecology of island ecosystems is vastly different from that of mainland communities. Their isolation and high availability of empty niches lead to increased speciation. As a result, island ecosystems comprise 30% of the world’s biodiversity hotspots, 50% of marine tropical diversity, and some of the most unusual and rare species. Many species still remain unknown.

<span class="mw-page-title-main">Domesticated plants and animals of Austronesia</span> Ancient expansion of agriculture

One of the major human migration events was the maritime settlement of the islands of the Indo-Pacific by the Austronesian peoples, believed to have started from at least 5,500 to 4,000 BP. These migrations were accompanied by a set of domesticated, semi-domesticated, and commensal plants and animals transported via outrigger ships and catamarans that enabled early Austronesians to thrive in the islands of Maritime Southeast Asia, Near Oceania (Melanesia), Remote Oceania, Madagascar, and the Comoros Islands.

<span class="mw-page-title-main">Megalocnidae</span> Extinct Greater Antilles sloth family

Megalocnidae is an extinct family of sloths, native to the islands of the Greater Antilles from the Early Oligocene to the Mid-Holocene. They are known from Cuba, Hispaniola and Puerto Rico, but are absent from Jamaica. While they were formerly placed in the Megalonychidae alongside two-toed sloths and ground sloths like Megalonyx, recent mitochondrial DNA and collagen sequencing studies place them as the earliest diverging group basal to all other sloths. or as an outgroup to Megatherioidea. They displayed significant diversity in body size and lifestyle, with Megalocnus being terrestrial and probably weighing several hundred kilograms, while Neocnus was likely arboreal and similar in weight to extant tree sloths, at less than 10 kilograms.

<span class="mw-page-title-main">Peopling of Oceania</span> Early human migrations to Oceania

Oceania is a geographical region with disputed borders, but generally encompassing Australia, New Guinea, Melanesia, Micronesia and Polynesia.

References

  1. 1 2 "Island". Dictionary.com . Archived from the original on March 7, 2007. Retrieved March 5, 2007.
  2. ↑ "Continent". education.nationalgeographic.org. Archived from the original on July 16, 2019. Retrieved June 26, 2024.
  3. 1 2 "Island". education.nationalgeographic.org. Retrieved July 13, 2024.
  4. ↑ Baldacchino, Godfrey (2007). Bridging islands: the impact of fixed links. Charlottetown, Prince Edward Island: Acorn Press. ISBN   978-1-894838-24-5. OCLC   70884504.
  5. ↑ Pigou-Dennis, Elizabeth; Grydehøj, Adam (2014). "Accidental and ideal island cities: islanding processes and urban design in Belize City and the urban archipelagos of Europe". Island Studies Journal. 9 (2): 259–276. doi:10.24043/isj.305.
  6. ↑ Ringe, Donald A. (2006). A Linguistic History of English: From Proto-Indo-European to Proto-Germanic. Oxford University Press. p. 109. ISBN   0-19-928413-X.
  7. ↑ Wedgwood, Hensleigh (1855). "On False Etymologies". Transactions of the Philological Society (6): 66. Archived from the original on November 6, 2018. Retrieved September 22, 2018.
  8. 1 2 Wilson, J. Tuzo (June 1, 1963). "A Possible Origin of the Hawaiian Islands". Canadian Journal of Physics. 41 (6): 863–870. Bibcode:1963CaJPh..41..863W. doi:10.1139/p63-094. ISSN   0008-4204.
  9. 1 2 3 4 Neall, Vincent E.; Trewick, Steven A. (October 27, 2008). "The age and origin of the Pacific islands: a geological overview". Philosophical Transactions of the Royal Society B: Biological Sciences. 363 (1508): 3293–3308. doi:10.1098/rstb.2008.0119. ISSN   0962-8436. PMC   2607379 . PMID   18768382.
  10. 1 2 Jones, Anthony T (1993). "Review of the chronology of marine terraces in the Hawaiian Archipelago". Quaternary Science Reviews. 12 (9): 811–823. Bibcode:1993QSRv...12..811J. doi:10.1016/0277-3791(93)90019-I – via Research Gate.
  11. 1 2 Wallis, Graham P.; Trewick, Steven A. (2009). "New Zealand phylogeography: evolution on a small continent". Molecular Ecology. 18 (17): 3548–3580. Bibcode:2009MolEc..18.3548W. doi:10.1111/j.1365-294X.2009.04294.x. ISSN   0962-1083. PMID   19674312.
  12. 1 2 Nunn, Patrick D.; Kumar, Lalit; Eliot, Ian; McLean, Roger F. (March 2, 2016). "Classifying Pacific islands". Geoscience Letters. 3 (1): 7. Bibcode:2016GSL.....3....7N. doi: 10.1186/s40562-016-0041-8 . ISSN   2196-4092.
  13. ↑ Magazine, Smithsonian. "Why Some Geologists Say Charles Darwin's Theory of Coral Atoll Formation Is Wrong". Smithsonian Magazine. Retrieved July 13, 2024.
  14. ↑ US Department of Commerce, National Oceanic and Atmospheric Administration. "What is a barrier island?". oceanservice.noaa.gov. Retrieved June 28, 2024.
  15. 1 2 Baubinienė, Aldona (December 20, 2014). "Formation of fluvial islands and its determining factors, case study of the River Neris, the Baltic Sea basin" (PDF). Geomorphology. 231 (231): 343–352. Bibcode:2015Geomo.231..343B. doi:10.1016/j.geomorph.2014.12.025 – via Elsevier Science Direct.
  16. ↑ "Bananal Island | Amazon Rainforest, Wildlife & Conservation | Britannica". www.britannica.com. Retrieved June 27, 2024.
  17. ↑ "Lake". education.nationalgeographic.org. Retrieved June 28, 2024.
  18. ↑ "Largest And Highest Islands Of The World". WorldAtlas. May 18, 2021. Retrieved June 28, 2024.
  19. ↑ Whittaker, Robert J.; Fernández-Palacios, José María; Matthews, Thomas J.; Borregaard, Michael K.; Triantis, Kostas A. (September 2017). "Island biogeography: Taking the long view of nature's laboratories". Science. 357 (6354). doi:10.1126/science.aam8326. ISSN   0036-8075.
  20. 1 2 3 4 5 6 Graham, Natalie R.; Gruner, Daniel S.; Lim, Jun Y.; Gillespie, Rosemary G. (June 27, 2017). "Island ecology and evolution: challenges in the Anthropocene". Environmental Conservation. 44 (4): 323–335. doi:10.1017/S0376892917000315. ISSN   0376-8929.
  21. ↑ Veron, Simon; Haevermans, Thomas; Govaerts, Rafaël; Mouchet, Maud; Pellens, Roseli (August 12, 2019). "Distribution and relative age of endemism across islands worldwide". Scientific Reports. 9 (1): 11693. doi:10.1038/s41598-019-47951-6. ISSN   2045-2322.
  22. ↑ Harrison, Susan; Noss, Reed (January 7, 2017). "Endemism hotspots are linked to stable climatic refugia". Annals of Botany. 119 (2): 207–214. doi:10.1093/aob/mcw248. ISSN   0305-7364. PMC   5321063 . PMID   28064195.
  23. ↑ Kier, Gerold; Kreft, Holger; Lee, Tien Ming; Jetz, Walter; Ibisch, Pierre L.; Nowicki, Christoph; Mutke, Jens; Barthlott, Wilhelm (June 9, 2009). "A global assessment of endemism and species richness across island and mainland regions". Proceedings of the National Academy of Sciences of the United States of America. 106 (23): 9322–9327. doi:10.1073/pnas.0810306106. ISSN   0027-8424. PMC   2685248 . PMID   19470638.
  24. ↑ Gerlach, Justin (2004). "The bats of Silhouette Island, Seychelles" (PDF). Phelsuma. 12: 78–90 – via Nature Protection Trust of Seychelles.
  25. 1 2 3 4 de Queiroz, Alan (February 2005). "The resurrection of oceanic dispersal in historical biogeography" (PDF). Elsevier . 20 (2) – via Elesevier Science Direct.
  26. 1 2 3 4 "Intensifying hurricanes are helping invasive species spread across the U.S." Animals. October 27, 2020. Retrieved July 11, 2024.
  27. ↑ "How rafts helped primates rule the world". www.bbc.com. May 18, 2021. Retrieved July 13, 2024.
  28. ↑ Censky, Ellen J.; Hodge, Karim; Dudley, Judy (1998). "Over-water dispersal of lizards due to hurricanes". Nature. 395 (6702): 556–556. doi:10.1038/26886. ISSN   1476-4687.
  29. 1 2 3 Lovette, Irby (December 20, 2018). "Why Evolution Goes Wild on Islands: The Science of Adaptive Radiation". All About Birds. Retrieved July 13, 2024.
  30. ↑ Sato, Akie (March 1, 2001). "On the Origin of Darwin's Finches". academic.oup.com. doi:10.1093/oxfordjournals.molbev.a003806 . Retrieved July 13, 2024.
  31. 1 2 Tyson, Peter (November 1, 2000). "Gigantism & Dwarfism on Islands". www.pbs.org. Retrieved July 13, 2024.
  32. ↑ MacPherson, Rick (February 6, 2017). "Darwin's Islands". American Scientist. Retrieved July 11, 2024.
  33. 1 2 Magazine, Smithsonian; Helmuth, Laura. "Evolution World Tour: Galápagos Islands, Ecuador". Smithsonian Magazine. Retrieved July 14, 2024.
  34. ↑ Stix, Gary (January 1, 2009). "Darwin's Living Legacy--Evolutionary Theory 150 Years Later". Scientific American. Retrieved July 14, 2024.
  35. 1 2 3 4 5 6 7 8 9 10 11 Keegan, William F.; Diamond, Jared M. (January 1, 1987), Schiffer, Michael B. (ed.), "2 - Colonization of Islands by Humans: A Biogeographical Perspective", Advances in Archaeological Method and Theory, San Diego: Academic Press, pp. 49–92, doi:10.1016/b978-0-12-003110-8.50005-0, ISBN   978-0-12-003110-8 , retrieved July 3, 2024
  36. ↑ Chambers, Geoffrey K. (2013). "Genetics and the Origins of the Polynesians". Encyclopedia of Life Sciences . doi:10.1002/9780470015902.a0020808.pub2. ISBN   978-0470016176.
  37. 1 2 3 "Polynesia's Genius Navigators". www.pbs.org. February 15, 2000. Retrieved June 28, 2024.
  38. 1 2 Gatty, Harold (1943). The Raft Book (2nd ed.). New York City: George Grady Press. pp. 10, 48, 54–56.
  39. ↑ Lewis, David (May 1, 1994). We, the Navigators: The Ancient Art of Landfinding in the Pacific (Second Edition). University of Hawaii Press. p. 8. ISBN   978-0-8248-1582-0.
  40. ↑ "Pacific voyaging and discovery". New Zealand History. Manatū Taonga — Ministry for Culture and Heritage. November 2, 2023. Retrieved June 26, 2024.
  41. 1 2 3 4 5 6 Cornwall, Warren (February 8, 2024). "A thousand years of solitude". Science. 383 (6683): 580–584. Bibcode:2024Sci...383..580C. doi:10.1126/science.ado5092. PMID   38330134 . Retrieved June 29, 2024.
  42. ↑ Bird, Michael I.; Condie, Scott A.; O’Connor, Sue; O’Grady, Damien; Reepmeyer, Christian; Ulm, Sean; Zega, Mojca; Saltré, Frédérik; Bradshaw, Corey J. A. (June 17, 2019). "Early human settlement of Sahul was not an accident". Scientific Reports. 9 (1): 8220. doi:10.1038/s41598-019-42946-9. ISSN   2045-2322.
  43. 1 2 3 4 5 Ma, Guoqing (October 16, 2020). "Islands and the world from an anthropological perspective". International Journal of Anthropology and Ethnology. 4 (1): 12. doi: 10.1186/s41257-020-00038-x . ISSN   2366-1003.
  44. ↑ Dewailly, Eric (2008). "Fish consumption and health in French Polynesia" (PDF). Asia Pac J Clin Nutr. 17 (1).
  45. 1 2 "Polynesian culture - Kinship, Social Hierarchy | Britannica". www.britannica.com. May 8, 2024. Retrieved July 5, 2024.
  46. 1 2 Tiare Tuuhia, Hakai (November 10, 2023). "How an Ancient Practice Aids Marine Conservation". Smithsonian Magazine. Retrieved July 13, 2024.
  47. ↑ Haden, Roger (August 10, 2009). Food Culture in the Pacific Islands. Bloomsbury Publishing USA. pp. 59–67. ISBN   978-0-313-34493-0.
  48. ↑ "The island fruit that caused a mutiny". www.bbc.com. Retrieved July 13, 2024.
  49. ↑ Fairbairn, Te'o I.J. (1991). The Pacific Islands: Politics, Economics, and International Relations. University of Hawaii Press. pp. 1–11. ISBN   0-86638-140-6.
  50. 1 2 "Historical Background: Colonization of Pacific Islands". Geriatrics. March 18, 2014. Retrieved July 8, 2024.
  51. ↑ "Australia and Oceania: Human Geography". education.nationalgeographic.org. Retrieved July 13, 2024.
  52. ↑ Ragone, Diane; Lorence, David H.; Flynn, Timothy (2001). "History of Plant Introductions to Pohnpei, Micronesia and the Role of the Pohnpei Agriculture Station". Economic Botany. 55 (2): 290–324. ISSN   0013-0001.
  53. ↑ Herman, Doug (August 15, 2017). "A Brief, 500-Year History of Guam". Smithsonian Magazine. Retrieved July 13, 2024.
  54. 1 2 Fairbairn, Te'O IJ (1991). "Pacific Islands: politics, economics, and international relations". scholarspace.manoa.hawaii.edu. pp. 15, 42. Retrieved July 8, 2024.
  55. 1 2 Brown, Keith G.; Cave, Jenny (January 1, 2010). G. Brown, Keith; Cave, Jenny (eds.). "Island tourism: marketing culture and heritage – editorial introduction to the special issue". International Journal of Culture, Tourism and Hospitality Research. 4 (2): 87–95. doi:10.1108/17506181011045163. ISSN   1750-6182.
  56. 1 2 3 4 Intergovernmental Panel on Climate Change (IPCC), ed. (2023), "Small Islands", Climate Change 2022 – Impacts, Adaptation and Vulnerability: Working Group II Contribution to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge: Cambridge University Press, pp. 2043–2122, doi:10.1017/9781009325844.017, ISBN   978-1-009-32583-7 , retrieved July 9, 2024
  57. 1 2 Prete, Giovanni (January 29, 2024). "Tuvalu: Why Is the Small Island Nation Sinking?". Earth.Org. Retrieved July 9, 2024.
  58. 1 2 3 4 5 Fisher, Richard; Hirschfeld, Javier (January 6, 2022). "Why we are in 'the age of artificial islands'". www.bbc.com. Retrieved July 11, 2024.
  59. 1 2 Fang, Huacan; Duan, Menglan (2014). "3.7.3 The Artificial Island". Offshore operation facilities: equipment and procedures. Amsterdam ; Boston: Elsevier, GPP. ISBN   978-0-12-396977-4.
  60. 1 2 Mirasola, Christopher (July 15, 2015). "What Makes an Island? Land Reclamation and the South China Sea Arbitration". Asia Maritime Transparency Initiative. Retrieved July 11, 2024.
This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.