The forest is home to some of the most distinct mammals including the orangutan, gibbons, Borneo round-leaf bat, and the endangered proboscis monkey. The mammals of the Indomalayan region: a systematic review. The most widespread glaciations in the ice age lasted for 21,000 years, and many scientists consider it to be the newest event of the bigger ice age which dates back to over 2 million years. Sunda Strait, channel, 16–70 miles (26–110 km) wide, between the islands of Java (east) and Sumatra, that links the Java Sea (Pacific Ocean) with the Indian Ocean (south). [4], The presence of a savanna corridor—even if fragmented—would have allowed for savanna-dwelling fauna (as well as early humans) to disperse between Sundaland and the Indochinese biogeographic region; emergence of a savanna corridor during glacial periods and subsequent disappearance during interglacial periods would have facilitated speciation through both vicariance (allopatric speciation) and geodispersal. [13] The fish is now found in the Kapuas River on the island of Borneo, and in the Musi and Batanghari rivers in Sumatra. [34], Before Sundaland emerged during the late Pliocene and early Pleistocene (~2.4 million years ago), there were no mammals on Java. [9], During the last glacial period, sea levels were lower and all of Sundaland was an extension of the Asian continent. Perhumid climate has existed in Sundaland since the early Miocene; though there is evidence for several periods of drier conditions, a perhumid core persisted in Borneo.
According to the most widely accepted theory, the ancestors of the modern-day Austronesian populations of the Maritime Southeast Asia and adjacent regions are believed to have migrated southward, from the East Asia mainland to Taiwan, and then to the rest of Maritime Southeast Asia. [9] Pollen records from sediment cores around Sundaland are contradictory; for example, cores from highland sites suggest that forest cover persisted throughout the last glacial period, but other cores from the region show pollen from savanna-woodland species increasing through glacial periods.
Sunda Strait, Indonesian Selat Sunda, channel, 16–70 miles (26–110 km) wide, between the islands of Java (east) and Sumatra, that links the Java Sea (Pacific Ocean) with the Indian Ocean (south). Biogeography and variation of. There are several volcanic islands within the strait, the most famous of which is Krakatoa, which erupted on August 27, 1883, causing a tsunami with waves as high as 125 feet (38 metres) that destroyed 300 towns and villages and killed about 36,000 people. The name came from Sunda Kingdom, a kingdom ruling the west part of Java. The northeastern part of the strait is the shallowest, while the western side is the deepest. Rising sea levels in three massive pulses may have caused flooding and the submerging of the Sunda continent, creating the Java and South China Seas and the thousands of islands that make up Indonesia and the Philippines today. The Most And Least Populated Provinces And Territories Of Canada? [33] Soil type, rather than long-term existence of a savanna corridor, has also been posited as an explanation for species distribution differences within Sundaland; Slik et al. [4] The northern border of Sundaland is more difficult to define in bathymetric terms; a phytogeographic transition at approximately 9ºN is considered to be the northern boundary. Omissions?
Sundaland encompasses the Sunda-shelf which is a tectonically stable extension of the continental shelf of Southeast Asia which was exposed during the last glacial era in the last 2 million years. Wilson DE, Reeder DM. The Wallace Line corresponds to a deep-water channel that has never been crossed by any land bridges.
These swamp-forests can be found in Sarawak, Malaysia, and in the Kalimantan and the Belait district of Brunei in Indonesia. Today, the Sundaland hosts 25% of Earth’s fishes and 17% of Earth’s birds.
[38] Genetic research reported in 2008 indicates that the islands which are the remnants of Sundaland were likely populated as early as 50,000 years ago, contrary to a previous hypothesis that they were populated as late as 10,000 years ago from Taiwan. Sundaland is in the tropics, and the equator passes through central Borneo and Sumatra.
[24][5] Others posit that changes in precipitation have been minimal[25] and an increase in land area in the Sunda Shelf alone (due to lowered sea level) is not enough to decrease precipitation in the region. Sarawak Museum Journal Special Issue No. The warm and shallow seas of the Sunda Shelf (averaging 28 °C or more) are part of the Indo-Pacific Warm Pool/Western Pacific Warm Pool[10] and an important driver of the Hadley circulation and the El Niño-Southern Oscillation (ENSO), particularly in January when it is a major heat source to the atmosphere. There are several volcanic islands within the strait, the most famous of which is Krakatoa, which erupted on August 27, 1883, Located in the subtropical and tropical moist broadleaf jungle biome, the swamp-forest is divided between three countries: Malaysia, Indonesia, and Brunei. [28] There is also evidence for savanna vegetation, particularly in now submerged areas of Sundaland, throughout the last glacial period. Population dispersals seem to have occurred at the same time as sea levels rose, which may have resulted in migrations from the Philippine Islands to as far north as Taiwan within the last 10,000 years. Some of the distinct fauna calling the cloud forest home include the civet, tree shrew, and orangutans among others. [22], Most recent research agrees that Indo-Pacific sea surface temperatures were at most 2-3 °C lower during the Last Glacial Maximum. The size of the Sundaland fluctuated in the last two million years and the current land is half the maximum size of Sundaland. The strait was the scene of an encounter between Allied and Japanese forces in March 1942. [7], Tropical and subtropical moist broadleaf forests, Tropical and subtropical coniferous forests, The name "Sunda" goes back to antiquity, appearing in Ptolemy's Geography, written around 150 AD. During the previous glacial maximum (the ice age), the sea level decreased by over 393.7 feet thus the whole Sunda shelf got exposed. Although the 17,000 islands of the Sundaland cover about 1% of the world’s land, this land mass hosts approximately 10% of the flowering species on Earth.
Karim, C., A.A. Tuen, Abdullah MT. (2014) suggest that Dipterocarp rainforest persisted throughout the last glacial period. After that, other animals moved in including tigers, the Indian elephant, and the Sumatran rhinoceros, among others. The Sunda Strait is an important passage connecting the Indian Ocean with eastern Asia. [3], The western and southern borders of Sundaland are clearly marked by the deeper waters of the Sunda Trench - some of the deepest in the world - and the Indian Ocean. [4], Greater portions of Sundaland were most recently exposed during the last glacial period from approximately 110,000 to 12,000 years ago.
The Wallace line is the boundary of the Sundaland. Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree.... What Indonesian city was originally named Batavia? Alfred Wallace identified the eastern border which is also the boundary of the Australasia and Indomalaya ecozones.
It also comes from the name of the Sundanese people, the native people of West Java, with the Javanese people being found mostly in Central and East Java.
Companies in more than a dozen countries and regions to carry out business.
The area of Sundaland encompasses the Sunda Shelf, a tectonically stable extension of Southeast Asia's continental shelf that was exposed during glacial periods of the last 2 million years. There are fewer birds in the Borneo mountains than in the lowlands, and the rainforest hosts some of the endemic species in Borneo. The climate and ecology of Sundaland throughout the Quaternary has been investigated by analyzing foraminiferal δ18O and pollen from cores drilled into the ocean bed, δ18O in speleothems from caves, and δ13C and δ15N in bat guano from caves, as well as species distribution models, phylogenetic analysis, and community structure and species richness analysis. The ancient drainage systems described by Molengraff were verified and mapped by Tjia in 1980[19] and described in greater detail by Emmel and Curray in 1982 complete with river deltas, floodplains and backswamps.[20][21].
The changing sea levels would have caused these humans to move away from their coastal homes and culture, and farther inland throughout southeast Asia.
Other than the Malay Peninsula and the islands of Sumatra, Borneo, and Java, Sundaland also includes part of the South China Sea, the Java Sea, and the Thailand Gulf. Explorers and scientists began measuring and mapping the seas of Southeast Asia in the 1870s, primarily using depth sounding. [31][12][3][32][17] Using the modern distribution of primates, termites, rodents, and other species, other researchers infer that the extent of tropical forest contracted—replaced by savanna and open forest —during the last glacial period. [3] Additionally, Wurster et al. [29] However, researchers disagree on the spatial extent of savanna that was present in Sundaland. It connects the Java Sea to the Indian Ocean. Of the three oceans that extend northward from the Antarctic continent, the…, Indian Ocean, body of salt water covering approximately one-fifth of the total ocean area of the world. It stretches for more than 6,200 miles (10,000 km) between the southern tips of Africa….
80: 221–234. (2011) suggest that the sandy soils of the now submerged seabed are a more likely dispersal barrier. (2010) analyzed stable carbon isotope composition in bat guano deposits in Sundaland and found strong evidence for the expansion of savanna in Sundaland. The name "Sundaland" for the peninsular shelf was first proposed by Reinout Willem van Bemmelen in his Geography of Indonesia in 1949, based on his research during the war.
6. [35] Later fauna included tigers, Sumatran rhinoceros, and Indian elephant, which were found throughout Sundaland; smaller animals were also able to disperse across the region.[7]. [6][4] The area of exposed land in Sundaland has fluctuated considerably during the past recent 2 million years; the modern land area is approximately half of the maximum extent. 2004.
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