Sulawesi

Coordinates: 02°S 121°E / 2°S 121°E / -2; 121
Source: Wikipedia, the free encyclopedia.
(Redirected from
Sulawesi Island
)

Sulawesi
Topographic map of Sulawesi
Provincial division of Sulawesi
Other namesCelebes
Geography
LocationIndonesia
Coordinates02°S 121°E / 2°S 121°E / -2; 121
ArchipelagoGreater Sunda Islands
Area186,216.16 km2 (71,898.46 sq mi)
Area rank11th
Highest elevation3,478 m (11411 ft)
Highest pointLatimojong
Administration
Indonesia
Provinces
(capital)
Largest settlement
Bajau, Mongondow

Sulawesi (/ˌsləˈwsi/ SOO-lə-WAY-see),[1] also known as Celebes (/ˈsɛlɪbz, səˈlbz/ SEL-ib-eez, sə-LEE-beez),[2] is an island in Indonesia. One of the four Greater Sunda Islands, and the world's 11th-largest island, it is situated east of Borneo, west of the Maluku Islands, and south of Mindanao and the Sulu Archipelago. Within Indonesia, only Sumatra, Borneo, and Papua are larger in territory, and only Java and Sumatra are more populous.

The landmass of Sulawesi includes four peninsulas: the northern

Strait of Makassar
runs along the western side of the island and separates the island from Borneo.

Etymology

The name Sulawesi possibly comes from the words sula ("island") and besi ("iron") and may refer to the historical export of

Indonesian independence
.

The name Celebes was originally given to the island by

Portuguese explorers. While its direct translation is unclear, it might be considered a Portuguese rendering of the native name "Sulawesi".[4]

Geography

Sulawesi is the

.

The

Strait of Makassar runs along the western side of the island.[9] The island is surrounded by Borneo to the west, by the Philippines to the north, by Maluku to the east, and by Flores and Timor
to the south.

Minor islands

The

Peleng Island and the Banggai Islands form a cluster between Sulawesi and Maluku. All the above-mentioned islands and many smaller ones off the coasts of Sulawesiare administratively part of Sulawesi's six provinces.[10][11]

Geology

Mount Tongkoko
is a volcano in North Sulawesi

The island slopes up from the shores of the deep seas surrounding the island to a high, mostly non-volcanic, mountainous interior. Active volcanoes are found in the northern Minahasa Peninsula, stretching north to the Sangihe Islands. The northern peninsula contains several active volcanoes such as Mount Lokon, Mount Awu, Soputan and Karangetang.

According to

Banggai), with island arcs previously in the Pacific (forming the north and east peninsulas).[12] Because of its several tectonic origins, various faults scar the land and as a result the island is prone to earthquakes, including the deadly 2018 and 2021
quakes.

Off the eastern coast of Sulawesi, the North Banda Sea was created through subduction rollback during the early Miocene. Evidence for this tectonic event lies with the extensive interconnected fault network found in the area, a volcanic seamount with its surrounding ridges, and an accretionary wedge. Off the coast of east Selawesti and Banggai is an accumulation of carbonate rocks from the late Miocene. These carbonates are likely pinnacle reefs and the carbonate platform  has a total thickness of around 180–770 meters.[13]

Sulawesi, in contrast to most of the other islands in the

micro-continental fragments sliced from New Guinea with an active volcanic margin in West Sulawesi at different times since the Early Miocene c. 20 Mya has recently been replaced by the hypothesis that extensional fragmentation has followed a single Miocene collision of West Sulawesi with the Sula Spur, the western end of an ancient folded belt of Variscan origin in the Late Paleozoic.[14]

Bone Basin

The Bone Basin lies between the eastern and western arms of Sulawesi. According to recent studies, the basin has been opened up due to extensional forces.[15] The basin is bounded by normal faults on each side of the basin. Each side of the basin is surrounded by uplifted basement rock with young sediments found in the middle. The past geological history has allowed for a large accumulation of carbonates which could lead to a higher potential of oil and gas occurrences. However, the faults present in the basin makes it a very complicated system.

Prehistory

The oldest evidence for humans on Sulawesi are stone tools produced by archaic humans, dating from over 200,000 to 100,000 years ago, that were found at the Talepu site in southwestern Sulawesi.[16]

Before October 2014, the settlement of South Sulawesi by modern humans had been dated to c. 30,000 BC on the basis of radiocarbon dates obtained from rock shelters in Maros.[17] No earlier evidence of human occupation had at that point been found, but the island almost certainly formed part of the land bridge used for the settlement of Australia and New Guinea by at least 40,000 BC.[18] There is no evidence of Homo erectus having reached Sulawesi; crude stone tools first discovered in 1947 on the right bank of the Walanae River at Barru (now part of Bone Regency), which were thought to date to the Pleistocene on the basis of their association with vertebrate fossils,[19] are now thought to date to perhaps 50,000 BC.[20]

Dwelling

Following Peter Bellwood's model of a southward migration of Austronesian-speaking farmers (AN),[21] radiocarbon dates from caves in Maros suggest a date in the mid-second millennium BC for the arrival of a group from east Borneo speaking a Proto-South Sulawesi language (PSS). Initial settlement was probably around the mouth of the Sa'dan river, on the northwest coast of the peninsula, although the south coast has also been suggested.[22]

Subsequent migrations across the mountainous landscape resulted in the geographical isolation of PSS speakers and the evolution of their languages into the eight families of the South Sulawesi language group.

Makassarese, the closest linguistic neighbors of the Bugis are the Torajans
.

Megalith in Central Sulawesi

Pre-1200 Bugis society was most likely organized into

wet rice
may have taken place along the margins of the lakes and rivers.

In Central Sulawesi, there are more than 400 granite megaliths, which various archaeological studies have dated to be from 3000 BC to AD 1300. They vary in size from a few centimeters to approximately 4.5 meters (15 ft). The original purpose of the megaliths is unknown. Approximately 30 of the megaliths represent human forms. Other megaliths are in form of large pots (Kalamba) and stone plates (Tutu'na).[24][25]

A burial of a woman associated with the hunter-gatherer Toalean culture dating to 7,000 years ago has yielded DNA that has provided rare insight into early migrations in and through the region.[26][27]

Oldest known cave art

In October 2014, it was announced that

Stencils of right hands in Pettakere Cave in Maros are among the oldest known examples of human artwork

Dr. Maxime Aubert, of Griffith University in Queensland, Australia, said that was the minimum age for the outline in Pettakere Cave in Maros, and added: "Next to it is a pig that has a minimum age of 35,400 years old, and this is one of the oldest figurative depictions in the world, if not the oldest one."[28]

On 11 December 2019, a team of researchers led by Dr. Maxime Aubert announced the discovery of the oldest hunting scenes in prehistoric art in the world that is more than 44,000 years old from the limestone cave of Leang Bulu' Sipong 4. Archaeologists determined the age of the depiction of hunting a pig and buffalo thanks to the calcite 'popcorn', different isotope levels of radioactive uranium and thorium.[29][30][31]

In March 2020, two small stone 'plaquettes' were found by Griffith University archaeologists in the Leang Bulu Bettue cave, dated to a time between 26,000 and 14,000 years ago.[32] While one of the stones contained an anoa (water buffalo) and what may be a flower, star, or eye, another depicted astronomic rays of light.[33][34][35]

In January 2021, archaeologists announced the discovery of cave art that is at least 45,500 years old in a Leang Tedongnge cave. According to the journal Science Advances, the cave painting of a warty pig is the earliest evidence of human settlement of the region. An adult male pig, measuring 136 cm x 54 cm and what is likely a Sulawesi or Celebes warty pig (Sus celebensis), was depicted with horn-like facial warts and two hand prints above its hindquarters.[36] According to co-author Adam Brumm, there are two other pigs that are partly preserved and it appears the warty pig was observing a fight between the two other pigs.[37][38][39][40]

History

Local chief (1872)

A bronze Amaravathi statue was discovered at Sikendeng, South Sulawesi near Karama river in 1921 which was dated to 2nd–7th century AD by Bosch (1933).[41] In 1975, small locally made Buddhist statues from 10th-11th century were also discovered in Bontoharu, on the island of Selayar, South Sulawesi.[42]

Starting in the 13th century, access to prestige trade goods and to sources of iron started to alter long-standing cultural patterns and to permit ambitious individuals to build larger political units. It is not known why these two ingredients appeared together; one was perhaps the product of the other.

In 1367, several identified polities located on the island were mentioned in the Javanese manuscript

Luwu and Banggai. It seems that by the 14th century, polities in the island were connected in an archipelagic maritime trading network, centered in the Majapahit port in East Java. By 1400, a number of nascent agricultural principalities had arisen in the western Cenrana valley, as well as on the south coast and on the west coast near modern Parepare.[43]

The first Europeans to visit the island (which they believed to be an archipelago due to its contorted shape) were the

Bone
. The Dutch built a fort at Ujung Pandang, while Arung Palakka became the regional overlord and Bone the dominant kingdom. Political and cultural development seems to have slowed as a result of the status quo.

In 1905, the entire island became part of the Dutch state colony of the

Picture gallery

  • Tandako dancers and a musician in Pasere Maloku, Sulawesi.
    Tandako dancers and a musician in Pasere Maloku, Sulawesi.
  • Tandako pajogé dancers from Pasere Maloku, Celebes (now Sulawesi)
    Tandako pajogé dancers from Pasere Maloku, Celebes (now Sulawesi)
  • Padjogé dancers in Maros, Sulawesi, in the 1870s.
    Padjogé dancers in Maros, Sulawesi, in the 1870s.
  • Tandako pajogé dancers and musicians in Gorontalo, North Celebes, circa 1870s.
    Tandako pajogé dancers and musicians in Gorontalo, North Celebes, circa 1870s.

Central Sulawesi

Toraja
burial site. Tau-tau, the statue representing the buried people, can be seen in niches on the cliff.

The Portuguese were rumoured to have a fort in Parigi in 1555.[49] The Kaili were an important group based in the Palu valley and related to the Toraja. Scholars relate[citation needed] that their control swayed under Ternate and Makassar, but this might have been a decision by the Dutch to give their vassals a chance to govern a difficult group. Padbruge commented that in the 1700s the Kaili population was significantly high and were a highly militant society. In the 1850s, a civil war erupted between the Kaili groups, including the Banawa, in which the Dutch colonial government decided to intervene.[50]

In the late 19th century, the Sarasins journeyed through the Palu valley as part of a major initiative to bring the Kaili under Dutch rule. Some very surprising and interesting photographs were taken of shamans called Tadulako. Further Christian religious missions entered the area to make one of the most detailed ethnographic studies in the early 20th century.[51] A Swede by the name of Walter Kaudern later studied much of the literature and produced a synthesis. Erskine Downs in the 1950s produced a summary of Kruyts and Andrianis work: "The religion of the Bare'e-Speaking Toradja of Central Celebes," which is invaluable for English-speaking researchers. One of the most recent publications is "When the bones are left," a study of the material culture of central Sulawesi,[52] offering extensive analysis. Also worthy of study are the brilliant works of Monnig Atkinson on the Wana shamans who live in the Mori area.

Population

Population of Sulawesi by province (2020 Census)[53]

  South Sulawesi (45.60%)
  Central Sulawesi (15.01%)
  Southeast Sulawesi (13.19%)
  North Sulawesi (13.18%)
  West Sulawesi (7.13%)
  Gorontalo (5.89%)

The 2000 census population of the provinces of Sulawesi was 14,946,488, about 7.25% of Indonesia's total population.[54] By the 2010 Census the total had reached 17,371,782, and the 2020 Census produced a total of 19,896,951.[55] The official estimate for mid 2022 was 20,304,437.[56] The largest city on Sulawesi is Makassar.

Religion

Religion in Sulawesi (2022)[57]

  
Catholic (1.61%)
  Hinduism (1.30%)
  Buddhism (0.15%)
  Folk religion (0.14%)
(0.003%)

Sunnis
.

Pamona
speaking peoples of Central Sulawesi, and near Mamasa.

Though most people identify themselves as Muslims or Christians, they often subscribe to local beliefs and deities as well.

Smaller communities of

Indian
communities.

Languages

Economy

The economy of Sulawesi is heavily centered around agriculture, fishing, mining, and forestry.[59]

Administration

The island was administered as one province between 1945 and 1960. In 1960 it was divided into two provinces – North and Central Sulawesi, and South and Southeast Sulawesi. In 1964 both of these were again divided, the former into North Sulawesi and Central Sulawesi, and the latter into South Sulawesi and Southeast Sulawesi. Today, it is subdivided into six

. Among these, the newest provinces are Gorontalo, established in 2000 from part of North Sulawesi, and West Sulawesi, established in 2004 from part of South Sulawesi.

The largest cities on the island are the provincial capitals of Makassar, Manado, Palu, Kendari, and Gorontalo (the provincial capital of West Sulawesi – the town of Mamuju – is not a city); there are six other cities – Bitung, Palopo, Bau-Bau, Parepare, Kotamobagu and Tomohun.

Flora and fauna

The colorful bark of Eucalyptus deglupta

Sulawesi is part of Wallacea, meaning that it has a mix of both Indomalayan and Australasian species that reached the island by crossing deep-water oceanic barriers.[60][61] The flora includes one native eucalypt, E. deglupta. There are 8 national parks on the island, of which 4 are mostly marine. The parks with the largest terrestrial area are Bogani Nani Wartabone with 2,871 km2 and Lore Lindu National Park with 2,290 km2. Bunaken National Park, which protects a rich coral ecosystem, has been proposed as a UNESCO World Heritage Site. The coast of northern tip of Sulawesi is identified as a site of highest marine biodiversity importance in the Coral Triangle.[62]

Mammals

Early in the Pleistocene, Sulawesi had a dwarf elephant and a dwarf form of Stegodon, (an elephant relative, S. sompoensis);[63] later both were replaced by larger forms.[64][65] A giant suid, Celebochoerus, was also formerly present.[66] It is thought that many of the migrants to Sulawesi arrived via the Philippines, while Sulawesi in turn served as a way station for migrants to Flores.[67] A Pleistocene faunal turnover is recognized, with the competitive displacement of several indigenous tarsiers by more recently arriving ones and of Celebochoerus by other medium-sized herbivores like the babirusa, anoa and Celebes warty pig.[68]

The north Sulawesi babirusa is endemic to Sulawesi.

There are 127 known extant native mammalian species in Sulawesi. A large percentage, 62% (79 species) are

Strigocuscus celebensis
, which are diurnal and nocturnal, respectively).

Sulawesi is home to a large number of endemic

Rubrisciurus
.

While over 20 bat species are present on Sulawesi, only a portion of these are endemic:

Styloctenium wallacei
.

Several endemic shrews, the Sulawesi shrew, Sulawesi tiny shrew and the Sulawesi white-handed shrew, are found on the island.

Sulawesi has no

gliding mammals, being situated between Borneo with its colugos and flying squirrels, and Halmahera with its sugar gliders
.

Birds

The endemic ornate lorikeet

By contrast, Sulawesian bird species tend to be found on other nearby islands as well, such as Borneo; 31% of Sulawesi's birds are found nowhere else. One endemic (also found on small neighboring islands) is the largely ground-dwelling, chicken-sized maleo, a megapode which sometimes uses hot sand close to the island's volcanic vents to incubate its eggs. An international partnership of conservationists, donors, and local people have formed the Alliance for Tompotika Conservation,[70] in an effort to raise awareness and protect the nesting grounds of these birds on the central-eastern arm of the island. Other endemic birds include the flightless snoring rail, the fiery-browed starling, the Sulawesi masked owl, the Sulawesi myna, the satanic nightjar and the grosbeak starling. There are around 350 known bird species in Sulawesi.

Reptiles

The larger reptiles of Sulawesi are not endemic and include

Gekko iskandari
.

Sulawesi also harbours several species of freshwater chelonians, two of which are endemic. They include the

Pleistocene epoch
.

The remaining two species consist of the non-endemic

Malayan box turtle of the Wallacean subspecies, and the Asiatic softshell turtle
.

Amphibians

The amphibians of Sulawesi include the endemic frogs

.

Freshwater fish

Sulawesi is home to more than 70

undescribed species from the same region and genus also exists.[82]

Freshwater crustaceans and snails

Orange delight shrimp (Caridina loehae) from Sulawesi.

Many species of

cave-adapted species of crab known in the world".[85]

The genus Tylomelania of freshwater snails is also endemic to Sulawesi, with the majority of the species restricted to Lake Poso and the Malili Lake system.[86]

Insects

The Trigonopterus selayarensis is a flightless weevil endemic to Sulawesi.[87]

Miscellaneous

The Indonesian coelacanth and the mimic octopus are present in the waters off Sulawesi's coast.

Conservation

Sulawesi island was recently the subject of an Ecoregional Conservation Assessment, coordinated by The Nature Conservancy. Detailed reports about the vegetation of the island are available.[88] The assessment produced a detailed and annotated list of 'conservation portfolio' sites. This information was widely distributed to local government agencies and nongovernmental organizations. Detailed conservation priorities have also been outlined in a recent publication.[89]

The lowland forests on the island have mostly been removed.[90] Because of the relative geological youth of the island and its dramatic and sharp topography, the lowland areas are naturally limited in their extent. The past decade has seen dramatic conversion of this rare and endangered habitat. The island also possesses one of the largest outcrops of serpentine soil in the world, which support an unusual and large community of specialized plant species. Overall, the flora and fauna of this unique center of global biodiversity is very poorly documented and understood and remains critically threatened.

The islands of Pepaya, Mas, and Raja islands, located in Sumalata Village –

Dermochelys coriacea). In 2011, the habitat was threatened by human activities such as illegal poaching and fish bombing activities; furthermore, many coral reefs, which represent a source of food for turtles, have been damaged.[91]

Environment

Bunaken Island seen from Manado Tua island.

The largest environmental issue in Sulawesi is deforestation. In 2007, scientists found that 80 percent of Sulawesi's forest had been lost or degraded, especially centered in the lowlands and the mangroves.[92] Forests have been felled for logging and large agricultural projects. Loss of forest has resulted in many of Sulawesi's endemic species becoming endangered. In addition, 99 percent of Sulawesi's wetlands have been lost or damaged.

Other environmental threats included bushmeat hunting and mining.[93]

Parks

The island of Sulawesi has six national parks and nineteen nature reserves. In addition, Sulawesi has three marine protected areas. Many of Sulawesi's parks are threatened by logging, mining, and deforestation for agriculture.[93]

See also

Explanatory notes

  1. ^ Technically, Tomini[6] and Boni[7] are defined as gulfs by the International Hydrographic Organization, while Tolo is considered a bay of the Molucca Sea.[8]

Citations

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External links