Suvarṇabhūmi ( Sanskrit : सुवर्णभूमि ; Pali: Suvaṇṇabhūmi ) is a toponym , that appears in many ancient Indian literary sources and Buddhist texts such as the Mahavamsa , some of the Jataka tales , the Milinda Panha and the Ramayana .
155-722: Though its exact location is unknown and remains a matter of debate, Suvarṇabhūmi was an important port along trade routes that run through the Indian Ocean , setting sail from the wealthy ports in Basra , Ubullah , and Siraf , through Muscat , Malabar , Ceylon , the Nicobars , Kedah and on through the Strait of Malacca to fabled Suvarṇabhūmi. Ian Glover, Emeritus Reader in Southeast Asian Archaeology at
310-498: A Prakrit ) into Chinese. The oldest archaeological evidence of Indianized civilization in Southeast Asia comes from central Burma, central and southern Thailand, and the lower Mekong Delta . These finds belong to the period of Funan Kingdom or Nokor Phnom, present-day Cambodia, and South Vietnam including part of Burma, Laos, and Thailand, which was the first political centre established in Southeast Asia. Taking into account
465-540: A transcription from some local language into Chinese. For example, French scholar Georges Coedès advanced the theory that in using the word Funan , ancient Chinese scholars were transcribing a word related to the Khmer word bnaṃ or vnaṃ (modern: phnoṃ , meaning "mountain"). However, the epigraphist Claude Jacques pointed out that this explanation was based on a mistranslation of the Sanskrit word parvatabùpála in
620-578: A Pre-Angkorian stone inscription in the Province of Kampong Speu Baset District, which he tentatively dated to 633 CE. According to him, the inscription would “prove that Suvarnabhumi was the Khmer Empire.” The inscription, translated, read: “The great King Isanavarman is full of glory and bravery. He is the King of Kings, who rules over Suvarnabhumi until the sea, which is the border, while the kings in
775-636: A certain task ...". The Sanskrit inscription (K.5) of Tháp Mười (known as "Prasat Pram Loven" in Khmer), which is now on display in the Museum of Vietnamese History in Ho Chi Minh City , refers to a Prince Guṇavarman, younger son ( nṛpasunu—bālo pi ) of a king Ja[yavarman] who was "the moon of the Kauṇḍinya line ( ... kauṇḍi[n]ya[vaṅ]śaśaśinā ... ) and chief "of a realm wrested from
930-436: A collection of city-states that sometimes were at war with one another and at other times constituted a political unity. From archaeological evidence, which includes Roman , Chinese, and Indian goods excae centre of Óc Eo in southern Vietnam, it is known that Funan must have been a powerful trading state. Excavations at Angkor Borei in southern Cambodia have likewise delivered evidence of an important settlement. Since Óc Eo
1085-621: A divine bow to him and had directed him to embark on a large merchant junk. In the morning, he proceeded to the temple, where he found a bow at the foot of the genie's tree. He then boarded a ship, which the genie caused to land in Fúnán. The queen of the country, Liǔyè ( 柳葉 , "Willow Leaf"; Queen Soma , Middle Chinese : Iiu-iap ) wanted to pillage the ship and seize it, so Hùntián shot an arrow from his divine bow which pierced through Liǔyè's ship. Frightened, she gave herself up, and Hùntián took her for his wife. But unhappy to see her naked, he folded
1240-564: A fair amount of research on Funan sites in the lower Mekong region. Many of the mounds show evidence of material culture and landscape modification (inclusive of species-genera biological regimes) ranging from the metal age through the post-Angkorian period and later as evidenced by 13th through 16th century CE Chinese, Thai, Vietnamese, and Cham ceramics. The evidence suggests a 2000-year or longer period of urbanization, continuous activity, and relatively strong albeit indirect and multi-nodal connections to long-distance value chains. Nevertheless, it
1395-468: A global rise in sea level. Sea level also increases in the Indian Ocean, except in the south tropical Indian Ocean where it decreases, a pattern most likely caused by rising levels of greenhouse gases . Among the tropical oceans, the western Indian Ocean hosts one of the largest concentrations of phytoplankton blooms in summer, due to the strong monsoon winds. The monsoonal wind forcing leads to
1550-656: A key position with regard to the maritime trade routes, and was inevitably a port of call both for the navigators who went through the Straits of Malacca and for those – probably more numerous – who made the transit over one of the isthmuses of the Malay Peninsula. Fu-nan may even have been the terminus of voyages from the Eastern Mediterranean, if it is the case that the Kattigara mentioned by Ptolemy
1705-516: A large island which he took for the Isla del Oro . This island has not been identified although it seems likely that it is Biak , Manus or one of the Schouten Islands on the north coast of New Guinea . Indian Ocean The Indian Ocean is the third-largest of the world's five oceanic divisions, covering 70,560,000 km (27,240,000 sq mi) or approximately 20% of
SECTION 10
#17327718346061860-528: A large population of South Asians colonized Funan. Dutch historian J.C. van Leur stressed that it was the local rulers who recognized the benefits of associating with their relatively advanced social technologies and drew from the Indian traditions by encouraging migration of Brahmin clerks to help with the administration. As per O.W. Wolters, there was a mutual sharing process in the evolution of Indianized statecraft and no mass influx of Brahmans. He said that it
2015-458: A loose network of states ( Mandala ) —located in mainland Southeast Asia covering parts of present-day Cambodia, Thailand and Vietnam that existed from the first to sixth century CE. The name is found in Chinese historical texts describing the kingdom, and the most extensive descriptions a name the people of Funan gave to their polity. Some scholars argued that ancient Chinese scholars has found
2170-451: A maximum width of 175 km (109 mi). The passive margins have an average width of 47.6 ± 0.8 km (29.58 ± 0.50 mi). The average width of the slopes (horizontal distance from shelf break to foot of slope) of the continental shelves are 50.4–52.4 km (31.3–32.6 mi) for active and passive margins respectively, with a maximum width of 205.3–255.2 km (127.6–158.6 mi). In correspondence of
2325-549: A number of islands. These include those controlled by surrounding countries, and independent island states and territories. Of the non-coastal islands, there are two broad clusters: one around Madagascar, and one south of India. A few other oceanic islands are scattered elsewhere. In contrast to the Atlantic and Pacific, the Indian Ocean is enclosed by major landmasses and an archipelago on three sides and does not stretch from pole to pole, and can be likened to an embayed ocean. It
2480-470: A period of six years, except for debris that gets indefinitely stuck in the centre of the gyre. The garbage patch in the Indian Ocean will, according to a 2012 study, decrease in size after several decades to vanish completely over centuries. Over several millennia, however, the global system of garbage patches will accumulate in the North Pacific. There are two amphidromes of opposite rotation in
2635-546: A piece of material to make a garment through which he made her pass her head. Then he governed the country and passed power on to his son, who was the founder of seven cities." Nearly the same story appeared in the Jìn shū 晉書 ( Book of Jin ), compiled by Fáng Xuánlíng in 648 CE; however, in the Book of Jin the names given to the foreign conqueror and his native wife are "Hùnhuì" 混湏 and "Yèliǔ" 葉柳 . Some scholars have identified
2790-790: A process of aridification began in the southwest Indian Ocean began around 4,000 years ago. Mammalian megafauna once widespread in the MPA was driven to near extinction in the early 20th century. Some species have been successfully recovered since then — the population of white rhinoceros ( Ceratotherium simum simum ) increased from less than 20 individuals in 1895 to more than 17,000 as of 2013. Other species still depend on fenced areas and management programs, including black rhinoceros ( Diceros bicornis minor ), African wild dog ( Lycaon pictus ), cheetah ( Acynonix jubatus ), elephant ( Loxodonta africana ), and lion ( Panthera leo ). This biodiversity hotspot (and namesake ecoregion and "Endemic Bird Area")
2945-820: A rising elite and the wealthy classes at home.” Suvarṇabhūmi means 'golden land' or 'land of gold' and the ancient sources have associated it with one of a variety of places throughout the Southeast Asian region. It might also be the source of the Western concept of Aurea Regio in Claudius Ptolemy 's Trans-Gangetic India or India beyond the Ganges, and the Golden Chersonese of the Greek and Roman geographers and sailors. The Periplus of
3100-453: A ruler of Funan who in the year 357 CE sent tamed elephants as tribute to Emperor Mu of Jin (r. 344–361); personal name: Sīmǎ Dān ( 司馬聃 ): "He [Qiáochénrú] was originally a Brahmin from India. There a voice told him: 'you must go reign over Fúnán,' and he rejoiced in his heart. In the south, he arrived at Pánpán ( 盤盤 ). The people of Fúnán appeared to him; the whole kingdom rose up with joy, went before him, and chose him king. He changed all
3255-536: A significant garbage patch . Historically, the Indian Ocean has been a hub of cultural and commercial exchange since ancient times. It played a key role in early human migrations and the spread of civilizations. In modern times, it remains crucial for global trade, especially in oil and hydrocarbons. Environmental and geopolitical concerns in the region include the effects of climate change , piracy, and strategic disputes over island territories. The Indian Ocean has been known by its present name since at least 1515, when
SECTION 20
#17327718346063410-577: A single unified empire, according to some modern scholars Funan may have been a collection of city-states that sometimes warred with one another and at other times constituted a political unity. The ethnic and linguistic origins of the Funanese people have consequently been subject to scholarly debate, and no firm conclusions can be drawn based on the evidence available. The Funanese may have been Cham or from another Austronesian group, or they may have been Khmer or from another Austroasiatic group. It
3565-591: A sojourn in Java by Jayavarman II . The "Mountain Kings" of Funan were claimed as the forebears of the Malacca Sultanate and Brunei Sultanate . Keeping in mind that Funanese records did not survive in the modern period, much of what is known came from archaeological excavation. Excavations yielded discoveries of brick wall structures, precious metals and pot from southern Cambodia and Vietnam. Also found
3720-537: A sophisticated gold working technology, which relied on the import of substantial quantities of the metal. The Padang Roco Inscription of 1286 CE, states that an image of Buddha Amoghapasa Lokeshvara was brought to Dharmasraya on the Upper Batang Hari - the river of Jambi - was transported from Bhumi Java (Java) to Suvarnabhumi (Sumatra), and erected by order of the Javanese ruler Kertanegara :
3875-464: A strong coastal and open ocean upwelling , which introduces nutrients into the upper zones where sufficient light is available for photosynthesis and phytoplankton production. These phytoplankton blooms support the marine ecosystem, as the base of the marine food web, and eventually the larger fish species. The Indian Ocean accounts for the second-largest share of the most economically valuable tuna catch. Its fish are of great and growing importance to
4030-468: A study of the various literary sources for the location of Suvarṇabhūmi, Saw Mra Aung concluded that it was impossible to draw a decisive conclusion on this and that only thorough scientific research would reveal which of several versions of Suvarṇabhūmi was the original. Some have speculated that this country refers to the Kingdom of Funan . The main port of Funan was Cattigara Sinarum statio ( Kattigara
4185-467: A transcription at all. Jacques proposed that use of the name Funan should be abandoned in favour of the names, such as Bhavapura , Aninditapura , Shresthapura and Vyadhapura , which are known from inscriptions to have been used at the time for cities in the region, as opposed to Funan or Zhenla which are unknown in the Old Khmer language. The first modern scholar to reconstruct the history of
4340-507: A transcription of the " Suvaṇṇa " in “Suvaṇṇabhumī”. In December 2017, Dr Vong Sotheara, of the Royal University of Phnom Penh , discovered a Pre- Angkorian stone inscription in the Province of Kampong Speu , Basedth District, which he tentatively dated to 633 AD. According to him, the inscription would “prove that Suvarnabhumi was the Khmer Empire.” The inscription was issued in the reign of King Isanavarman I (616–637 AD) of
4495-469: A two-syllable Chinese word to transcribe a three-syllable word from another language. The story of Kaundinya is also set forth briefly in the Sanskrit inscription C. 96 of the Cham king Prakasadharma found at Mỹ Sơn . It is dated Sunday, 18 February 658 CE (and thus belongs to the post-Funanese period) and states in relevant part (stanzas XVI-XVIII): "It was there [at the city of Bhavapura] that Kauṇḍinya,
4650-761: A wide spectrum of results ranging from the late centuries BCE to the Angkorian period. A significant canal system linking the site of Oc Eo has also been researched and dated. Phon Kaseka led a Royal Academy of Cambodia and Ministry of Culture and Fine Arts team (also with Royal University of Fine Arts personnel) conducted Iron Age to Funan period burial excavations at neighboring Phnom Borei. Large landscape features, notable settlement mounds, and other sites exhibiting Funan material culture and settlement patterns extend from at least Phnom Chisor through Oc Eo and numerous sites in Vietnam. Vietnamese archaeologists have also conducted
4805-473: Is a patchwork of small forested areas, often with a unique assemblage of species within each, located within 200 km (120 mi) from the coast and covering a total area of c. 6,200 km (2,400 sq mi). It also encompasses coastal islands, including Zanzibar and Pemba, and Mafia. This area, one of the only two hotspots that are entirely arid, includes the Ethiopian Highlands ,
Suvarnabhumi - Misplaced Pages Continue
4960-513: Is centered on the Indian Peninsula. Although this subcontinent has played a significant role in its history, the Indian Ocean has foremostly been a cosmopolitan stage, interlinking diverse regions by innovations, trade, and religion since early in human history. The active margins of the Indian Ocean have an average width (horizontal distance from land to shelf break ) of 19 ± 0.61 km (11.81 ± 0.38 mi) with
5115-783: Is commonly thought to refer to the Southeast Asian Peninsula, including lower Burma and the Malay Peninsula . However there is another gold-referring term Suvarnadvipa (the Golden Island or Peninsula, where “– dvipa” may refer to either a peninsula or an island ), which may correspond to the Indonesian Archipelago , especially Sumatra . Both terms might refer to a powerful coastal or island kingdom in present-day Indonesia , possibly centered on Sumatra or Java . This corresponds to
5270-545: Is dispute among scholars. According to the majority of Vietnamese academics, for example, Mac Duong, stipulates that "Funan's core population certainly were the Austronesians, not Khmer;" the fall of Funan and the rise of Zhenla from the north in the 6th century indicate "the arrival of the Khmer to the Mekong Delta." That thesis received support from D. G. E. Hall . Recent archaeological research lends weight to
5425-647: Is impossible to assert that Funan as an area and its dominant groups were anything but Khmer". According to British Historian Robert Nichol, When Funan kingdom collapsed under Khmer invasions, during the year 680, the Sailendra Dynasty set up rump states of Funan in the small kingdoms of Sarawak in Borneo across the South China sea, from Funan. He also posited blood relations with the Visayans in
5580-701: Is located between the Bay of Bengal and the Andaman Islands. In Indonesia, the so-called Indonesian Seaway is composed of the Malacca , Sunda and Torres Straits . The Gulf of Carpentaria is located on the Australian north coast while the Great Australian Bight constitutes a large part of its southern coast. Several features make the Indian Ocean unique. It constitutes the core of
5735-552: Is mentioned that merchants of Anga (in present-day Bihar , a state of India that borders with Bengal) regularly sailed to Suvarṇabhūmi, and ancient Bengal was in fact situated very close to Anga, connected by rivers of the Ganges-Brahmaputra Delta . Bengal has also been described in ancient Indian and Southeast Asian chronicles as a "seafaring country", enjoying trade relations with Dravidian kingdoms, Sri Lanka, Java and Sumatra. Sinhalese tradition holds that
5890-1086: Is now exhibited in the National Museum of Cambodia in Phnom Penh. However, his claim and the findings are yet to be peer-reviewed, and remain in doubt with other historians and archaeology experts across the region. Mon tradition maintains that the Thaton Kingdom in Lower Myanmar was called Suvannabhumi ( Burmese : သုဝဏ္ဏဘူမိ Thuwunnabhumi ). However, dating the Thaton Kingdom independent of traditional chronicles gives an terminus post quem foundation year of 825; even this date remains unattested. There are several sites within Mon State that local archaeologists cite as Suvarṇabhūmi. Suvarnabhumi City in Bilin Township
6045-476: Is now named after India , which protrudes into it, and has been known by its current name since at least 1515. It is the only ocean named after a country. It has an average depth of 3,741 m. All of the Indian Ocean is in the Eastern Hemisphere . Unlike the Atlantic and Pacific, the Indian Ocean is bordered by landmasses and an archipelago on three sides, making it more like an embayed ocean centered on
6200-588: Is one such site with limited excavation work. The site, called Winka Old City by other archaeologists, contains 40 high-grounds of which only four have been excavated. The Winka site, along with nearby walled sites like Kyaikkatha and Kelasa, have been dated as early as the sixth century. While the archaeology of early Lower Burmese sites requires more work, other urban centres in Myanmar like the Sri Ksetra Kingdom in modern Pyay were Buddhist as early as
6355-473: Is possible that they are the ancestors of those indigenous people dwelling in the southern part of Vietnam today who refer themselves as "Khmer" or "Khmer Krom." The Khmer term "krom" means "below" or "lower part of" and is used to refer to territory that was later colonized by Vietnamese immigrants and taken up into the modern state of Vietnam. While no conclusive study to determine whether Funan's ethnolinguistic components were Austronesian or Austroasiatic, there
Suvarnabhumi - Misplaced Pages Continue
6510-469: Is projected to push the tropical Indian Ocean into a basin-wide near-permanent heatwave state by the end of the 21st century, where marine heatwaves are projected to increase from 20 days per year (during 1970–2000) to 220–250 days per year. South of the Equator (20–5°S), the Indian Ocean is gaining heat from June to October, during the austral winter, while it is losing heat from November to March, during
6665-613: Is quite evident that periods of intense production, consumption, activity, commercial and political centrality fluctuated. The Funan period seems to have been the heyday and Angkor Borei may have been Funan's premiere capital for much of that period. However, many of the settlements did not necessarily spring up out of nowhere or vanish quickly. They were certainly well integrated into pre-Funan, Funan, Zhenla [Chenla], Angkorian and post-Angkorian socio-economic and political networks. The urbanization and networking processes demonstrate significant continuity, evolution and longevity before and after
6820-410: Is the subject of much discussion among specialists. The leading hypotheses are that the Funanese were mostly Mon–Khmer , or that they were mostly Austronesian , or that they constituted a multi-ethnic society. The available evidence is inconclusive on this issue. Michael Vickery has said that, even though identification of the language of Funan is not possible, the evidence suggests that the population
6975-632: The East African Rift valley , the Socotra islands, as well as some small islands in the Red Sea and areas on the southern Arabic Peninsula. Endemic and threatened mammals include the dibatag ( Ammodorcas clarkei ) and Speke's gazelle ( Gazella spekei ); the Somali wild ass ( Equus africanus somaliensis ) and hamadryas baboon ( Papio hamadryas ). It also contains many reptiles. In Somalia,
7130-785: The International Hydrographic Organization in 1953 included the Southern Ocean but not the marginal seas along the northern rim but in 2002 the IHO delimited the Southern Ocean separately, which removed waters south of 60°s from the Indian Ocean but included the northern marginal seas. Meridionally , the Indian Ocean is delimited from the Atlantic Ocean by the 20° east meridian , running south from Cape Agulhas , South Africa, and from
7285-526: The Khmer Krom of the lower Mekong region the belief is held that they are the descendants of ancient Funan, the core of Suvarnabhumi/Suvarnadvipa, which covered a vast extent of Southeast Asia including present day Cambodia, southern Vietnam, Thailand, Laos, Burma, Malaya, Sumatra and other parts of Indonesia. In December 2017, Dr Vong Sotheara, of the Royal University of Phnom Penh, discovered
7440-818: The Mascarene Basin the CDW becomes a deep western boundary current before it is met by a re-circulated branch of itself, the North Indian Deep Water. This mixed water partly flows north into the Somali Basin whilst most of it flows clockwise in the Mascarene Basin where an oscillating flow is produced by Rossby waves . Water circulation in the Indian Ocean is dominated by the Subtropical Anticyclonic Gyre,
7595-513: The Shelf break , also known as Hinge zone, the Bouguer gravity ranges from 0 to 30 mGals that is unusual for a continental region of around 16 km thick sediments. It has been hypothesized that the "Hinge zone may represent the relict of continental and proto-oceanic crustal boundary formed during the rifting of India from Antarctica ." Australia, Indonesia, and India are the three countries with
7750-554: The University of London , has said: “It is widely accepted in the 21st century that Suvarnabhumi as reported in early Indian literature was not a specific location which can be marked on a map. Rather, it was an idealised place, perhaps equivalent to Atlantis in Western history, a distant somewhere to the east of India where traders, sailors, and Buddhist and Hindu teachers went to make their fortunes and spread their teachings and bring back gold and other exotic products desired by
7905-786: The Zambezi , Ganges - Brahmaputra , Indus , Jubba , and Murray rivers and (order 4) the Shatt al-Arab , Wadi Ad Dawasir (a dried-out river system on the Arabian Peninsula) and Limpopo rivers. After the breakup of East Gondwana and the formation of the Himalayas, the Ganges-Brahmaputra rivers flow into the world's largest delta known as the Bengal delta or Sunderbans . Marginal seas , gulfs, bays and straits of
SECTION 50
#17327718346068060-432: The runoff water to the Indian Ocean. Mainly in summer, this runoff flows into the Arabian Sea but also south across the Equator where it mixes with fresher seawater from the Indonesian Throughflow . This mixed freshwater joins the South Equatorial Current in the southern tropical Indian Ocean. Sea surface salinity is highest (more than 36 PSU ) in the Arabian Sea because evaporation exceeds precipitation there. In
8215-452: The Óc Eo culture, have supported and supplemented his conclusion. Chinese sources relate a local legend to document Funan's origin, that a foreigner named "Huntian (混填)" [pinyin: Hùntián] established the Kingdom of Funan around the 1st century CE in the Mekong Delta of southern Vietnam. Archeological evidence shows that extensive human settlement in the region may go as far back as the 4th century BCE. Though treated by Chinese historians as
8370-437: The 13th-14th centuries, the border of the new Suvarṇabhūmi or Suphannabhumi met Lavo Kingdom at the Pasak River in the east, the west to Dawei on the coast of the outer sea ( Andaman Sea ), northwest to the south of Mawlamyine , which was the sea trading harbor of the Chaliang Kingdom ( Si Satchanalai ), while the south to the tip of the Malay Peninsula , and the north to Phraek Siracha (present-day Sankhaburi ). In 1351,
8525-537: The 2nd century conquered polities on the isthmus itself, and thus may have controlled the entire trade route from Malaysia to central Vietnam. The Funanese settlement of Óc Eo , located near the Straits of Malacca, provided a port-of-call and entrepot for this international trade route. Archaeological evidence discovered at what may have been the commercial centre of Funan at Óc Eo includes Roman as well as Persian , Indian , and Greek artefacts. The German classical scholar Albrecht Dihle believed that Funan's main port,
8680-520: The 3rd century CE, beginning with the Sānguó zhì ( 三國志 , Records of the Three Kingdoms ) completed in 289 CE by Chén Shòu ( 陳壽 ; 233–297), record the arrival of two Funanese embassies at the court of Lǚ Dài ( 呂待 ), governor in the southern Chinese kingdom of Wú ( 吳 ): the first embassy arrived between 225 and 230 CE, the second in the year 243. Later sources such as the Liáng shū ( 梁書 , Book of Liang ) of Yáo Chá ( 姚察 ; 533–606) and Yáo Sīlián ( 姚思廉 , d. 637), completed in 636, discuss
8835-516: The 3rd-century king Fan Shiman ( pinyin : Fàn Shīmàn ). Fan Shiman expanded his empire's navy and improved the Funanese bureaucracy, creating a quasi-feudal pattern that left local customs and identities largely intact, particularly in the empire's further reaches. Fan Shiman and his successors also sent ambassadors to China and India to regulate sea trade. The kingdom likely accelerated the process of Indianization of Southeast Asia. Later kingdoms of Southeast Asia such as Chenla may have emulated
8990-401: The 5th century. The scholarly search for Suvannabhumi within Myanmar is attached to various nationalistic and religious narratives about Suvannabhumi. The fifteenth century legend of Shwedagon Pagoda enshrining a few hairs of the Buddha brought back by Mon merchants highlights the cultural significance placed on early Buddhist missionaries in Myanmar. In many such legends, the narrative of
9145-537: The 5th to 6th centuries, and translated several Buddhist sūtras from Sanskrit (or a prakrit ) into Chinese. Among these texts is the Mahayana Saptaśatikā Prajñāpāramitā Sūtra , also called the Mahāprajñāpāramitā Mañjuśrīparivarta Sūtra . This text was separately translated by both monks. The bodhisattva Mañjuśrī is a prominent figure in this text. Funan was Southeast Asia's first great economy. It became prosperous through maritime trade and agriculture. The kingdom apparently minted its own silver coinage, bearing
9300-453: The Arabian Sea, the violent Monsoon brings rain to the Indian subcontinent. In the southern hemisphere, the winds are generally milder, but summer storms near Mauritius can be severe. When the monsoon winds change, cyclones sometimes strike the shores of the Arabian Sea and the Bay of Bengal . Some 80% of the total annual rainfall in India occurs during summer and the region is so dependent on this rainfall that many civilisations perished when
9455-404: The Arabic Peninsula. Along the west coast of India, the Gulf of Kutch and Gulf of Khambat are located in Gujarat in the northern end while the Laccadive Sea separates the Maldives from the southern tip of India. The Bay of Bengal is off the east coast of India. The Gulf of Mannar and the Palk Strait separate Sri Lanka from India, while Adam's Bridge separates the two. The Andaman Sea
SECTION 60
#17327718346069610-493: The Cambodian Kingdom of Chenla , the successor of Funan and the predecessor of the Khmer Empire . The inscription, translated, read: “The great King Isanavarman is full of glory and bravery. He is the King of Kings, who rules over Suvarnabhumi until the sea, which is the border, while the kings in the neighbouring states honour his order to their heads”. The Inscription is the oldest found mention of Suvarṇabhūmi in Southeast Asia, identifying it with Chenla. The inscription
9765-462: The Comoros. Although both species represent an order of lobe-finned fishes known from the Early Devonian (410 mya ) and though extinct 66 mya, they are morphologically distinct from their Devonian ancestors. Over millions of years, coelacanths evolved to inhabit different environments — lungs adapted for shallow, brackish waters evolved into gills adapted for deep marine waters. Of Earth's 36 biodiversity hotspots nine (or 25%) are located on
9920-403: The East India Coastal Current to the Arabian Sea from January to April. An Indian Ocean garbage patch was discovered in 2010 covering at least 5 million square kilometres (1.9 million square miles). Riding the southern Indian Ocean Gyre , this vortex of plastic garbage constantly circulates the ocean from Australia to Africa, down the Mozambique Channel , and back to Australia in
10075-503: The Erythraean Sea refers to the Land of Gold, Chryse , and describes it as “an island in the ocean, the furthest extremity towards the east of the inhabited world, lying under the rising sun itself, called Chryse... Beyond this country... there lies a very great inland city called Thina ”. Dionysius Periegetes mentioned: “The island of Chryse (Gold), situated at the very rising of the Sun”. Or, as Priscian put it in his popular rendition of Periegetes: “if your ship… takes you to where
10230-418: The Funanese court. The Funanese established a strong system of mercantilism and commercial monopolies that would become a pattern for empires in the region. Funan's dependence on maritime trade is seen as a cause for the beginning of Funan's downfall. Their coastal ports allowed trade with foreign regions that funnelled goods to the north and coastal populations. However, the shift in maritime trade to Sumatra,
10385-437: The Funanese practised slavery and that justice was rendered through trial by ordeal , including such methods as carrying a red-hot iron chain and retrieving gold rings and eggs from boiling water. Archaeological evidence largely corresponds to Chinese records. The Chinese described the Funanese as people who lived on stilt houses , cultivated rice and sent tributes of gold, silver, ivory and exotic animals. Kang Tai's report
10540-442: The Gold and Silver Islands were constantly, so to speak, wandering towards the East. Marco Polo spoke, in the most exaggerated language, of the wealth of gold in Zipangu , situated at the extremity of this part of the world, and had thus pointed out where the precious metals should preferably be sought. Martin Behaim , on his globe of 1492, revived the Argyre and Chryse of antiquity in these regions. In 1519, Cristóvão de Mendonça ,
10695-421: The Horn of Africa. The northern end of the Red Sea terminates in the Gulf of Aqaba and Gulf of Suez . The Indian Ocean is artificially connected to the Mediterranean Sea without ship lock through the Suez Canal , which is accessible via the Red Sea. The Arabian Sea is connected to the Persian Gulf by the Gulf of Oman and the Strait of Hormuz . In the Persian Gulf, the Gulf of Bahrain separates Qatar from
10850-507: The Indian Ocean Walker circulation there are no continuous equatorial easterlies. Upwelling occurs near the Horn of Africa and the Arabian Peninsula in the Northern Hemisphere and north of the trade winds in the Southern Hemisphere. The Indonesian Throughflow is a unique Equatorial connection to the Pacific. The climate north of the equator is affected by a monsoon climate. Strong north-east winds blow from October until April; from May until October south and west winds prevail. In
11005-436: The Indian Ocean include: Along the east coast of Africa, the Mozambique Channel separates Madagascar from mainland Africa, while the Sea of Zanj is located north of Madagascar. On the northern coast of the Arabian Sea , Gulf of Aden is connected to the Red Sea by the strait of Bab-el-Mandeb . In the Gulf of Aden, the Gulf of Tadjoura is located in Djibouti and the Guardafui Channel separates Socotra island from
11160-509: The Indian Ocean includes beaches and intertidal zones covering 3,000 km (1,200 sq mi) and 246 larger estuaries . Upwelling areas are small but important. The hypersaline salterns in India covers between 5,000–10,000 km (1,900–3,900 sq mi) and species adapted for this environment, such as Artemia salina and Dunaliella salina , are important to bird life. Coral reefs, sea grass beds, and mangrove forests are
11315-481: The Indian Ocean region, or almost half of the world's mangrove habitat, of which 42,500 km (16,400 sq mi) is located in Indonesia, or 50% of mangroves in the Indian Ocean. Mangroves originated in the Indian Ocean region and have adapted to a wide range of its habitats but it is also where it suffers its biggest loss of habitat. In 2016, six new animal species were identified at hydrothermal vents in
11470-730: The Indian Ocean, during the past six decades. The tuna catch rates have also declined 50–90% during the past half-century, mostly due to increased industrial fisheries, with the ocean warming adding further stress to the fish species. Endangered and vulnerable marine mammals and turtles: 80% of the Indian Ocean is open ocean and includes nine large marine ecosystems : the Agulhas Current , Somali Coastal Current , Red Sea , Arabian Sea , Bay of Bengal , Gulf of Thailand , West Central Australian Shelf , Northwest Australian Shelf and Southwest Australian Shelf . Coral reefs cover c. 200,000 km (77,000 sq mi). The coasts of
11625-487: The Indian Ocean, probably caused by Rossby wave propagation. Icebergs drift as far north as 55° south latitude , similar to the Pacific but less than in the Atlantic where icebergs reach up to 45°S. The volume of iceberg loss in the Indian Ocean between 2004 and 2012 was 24 Gt . Since the 1960s, anthropogenic warming of the global ocean combined with contributions of freshwater from retreating land ice causes
11780-526: The Indian Ocean. While the Indian Ocean warmed at a rate of 1.2°C per century during 1950–2020, climate models predict accelerated warming, at a rate of 1.7 °C–3.8 °C per century during 2020–2100. Though the warming is basin-wide, maximum warming is in the northwestern Indian Ocean including the Arabian Sea, and reduced warming off the Sumatra and Java coasts in the southeast Indian Ocean. Global warming
11935-466: The Indian Peninsula. Its coasts and shelves differ from other oceans, with distinct features, such as a narrower continental shelf . In terms of geology, the Indian Ocean is the youngest of the major oceans, with active spreading ridges and features like seamounts and ridges formed by hotspots . The climate of the Indian Ocean is characterized by monsoons . It is the warmest ocean, with a significant impact on global climate due to its interaction with
12090-658: The Latin form Oceanus Orientalis Indicus ( lit. ' Indian Eastern Ocean ' ) is attested, named after India, which projects into it. It was earlier known as the Eastern Ocean , a term that was still in use during the mid-18th century, as opposed to the Western Ocean ( Atlantic ) before the Pacific was surmised. In modern times, the name Afro-Asian Ocean has occasionally been used. The Hindi name for
12245-407: The Malay Peninsula, Borneo and Java. Benefitting from its strategic location on the narrow Strait of Malacca , the insular theory argued that other than actually producing gold, it might also be based on such a kingdom's potential for power and wealth (hence, "Land of Gold") as a hub for sea-trade also known from vague descriptions of contemporary Chinese pilgrims to India. The kingdom referred to as
12400-536: The Monsoon failed in the past. The huge variability in the Indian Summer Monsoon has also occurred pre-historically, with a strong, wet phase 33,500–32,500 BP; a weak, dry phase 26,000–23,500 BC; and a very weak phase 17,000–15,000 BP, corresponding to a series of dramatic global events: Bølling–Allerød warming , Heinrich , and Younger Dryas . The Indian Ocean is the warmest ocean in
12555-708: The Ocean is हिंद महासागर ( Hind Mahāsāgar ; lit. transl. Ocean of India ). Conversely, Chinese explorers (e.g., Zheng He during the Ming dynasty ) who traveled to the Indian Ocean during the 15th century called it the Western Oceans. In Ancient Greek geography , the Indian Ocean region known to the Greeks was called the Erythraean Sea . The borders of the Indian Ocean , as delineated by
12710-732: The Pacific Ocean and half that of the Atlantic basin, or 30% of its ocean surface (compared to 15% for the Pacific). The Indian Ocean drainage basin is divided into roughly 800 individual basins, half that of the Pacific, of which 50% are located in Asia, 30% in Africa, and 20% in Australasia. The rivers of the Indian Ocean are shorter on average (740 km (460 mi)) than those of the other major oceans. The largest rivers are ( order 5 )
12865-647: The Pacific Ocean by the meridian of 146°49'E, running south from South East Cape on the island of Tasmania in Australia. The northernmost extent of the Indian Ocean (including marginal seas) is approximately 30° north in the Persian Gulf . The Indian Ocean covers 70,560,000 km (27,240,000 sq mi), including the Red Sea and the Persian Gulf but excluding the Southern Ocean, or 19.5% of
13020-632: The Philippines with the Vijaya of Sarawak which in turn cause them to be related to Funan people as well as the Srivijaya Empire . The "King of the mountain" was the monarch of Funan. There was a mountain regarded as holy. Mountain in Khmer sounds similar to Funan. The Java-based Sailendras claimed that the Funan monarchs were their ancestors. Cambodia was taken control of after
13175-570: The Southeast Arabian Sea salinity drops to less than 34 PSU. It is the lowest (c. 33 PSU) in the Bay of Bengal because of river runoff and precipitation. The Indonesian Throughflow and precipitation results in lower salinity (34 PSU) along the Sumatran west coast. Monsoonal variation results in eastward transportation of saltier water from the Arabian Sea to the Bay of Bengal from June to September and in westerly transport by
13330-554: The Southwest Indian Ridge, from where it continues into the Mozambique Channel and Prince Edward Fracture Zone . North of 20° south latitude the minimum surface temperature is 22 °C (72 °F), exceeding 28 °C (82 °F) to the east. Southward of 40° south latitude , temperatures drop quickly. The Bay of Bengal contributes more than half (2,950 km or 710 cu mi) of
13485-532: The Southwest Indian Ridge: a "Hoff" crab, a "giant peltospirid" snail, a whelk-like snail, a limpet, a scaleworm and a polychaete worm. The West Indian Ocean coelacanth was discovered in the Indian Ocean off South Africa in the 1930s and in the late 1990s another species, the Indonesian coelacanth , was discovered off Sulawesi Island , Indonesia. Most extant coelacanths have been found in
13640-591: The Suphannabhumi Kingdom was merged into its succeeding state, Ayuttaya , after its last ruler, Uthong , moved eastward to create a new capital Ayutthaya on present-day Ayutthaya Island. A clue referring to the Malay Peninsula came from Claudius Ptolemy 's Geography , who referred to it as Golden Chersonese (literally 'golden peninsula'), which pinpointed exactly that location in South East Asia. The term Suvarṇabhūmi ('land of gold')
13795-514: The amount of gold discovered in Butuan far exceeds that found in Sumatra, where the much better known flourishing kingdom of Srivijaya is said to have been located.” This despite that most of the gold of Butuan were already looted by invaders. A popular interpretation of Rabindranath Tagore 's poem Amar Shonar Bangla serves as the basis for the claim that Suvarṇabhūmi was actually situated in central Bengal at Sonargaon . In some Jain texts, it
13950-631: The ancient inscriptions as equivalent to the Khmer word bnaṃ and a mis-identification of the King Bhavavarman I mentioned in them as the conqueror of Funan. It has also been observed that in Chinese the character 南 ( pinyin : nán , Vietnamese : nam ) is frequently used in geographical terms to mean "South"; Chinese scholars used it in this sense in naming other locations or regions of Southeast Asia, such as Annam . Thus, Funan may be an originally Chinese word, and may not be
14105-503: The ancient polity of Funan was Paul Pelliot , who in his ground-breaking article "Le Fou-nan" of 1903 drew exclusively on Chinese historical records to set forth the sequence of documented events connecting the foundation of Funan in approximately the 1st century CE with its demise by conquest in the 6th to 7th century. Scholars critical of Pelliot's Chinese sources have expressed scepticism regarding his conclusions. First record dated 84 CE in late Han period 后汉书. Chinese records dating from
14260-457: The area dating back more than 4,000 years and the findings of 3rd-century Roman coins. The Thai government named the new Bangkok airport, Suvarnabhumi Airport , after the mythic kingdom of Suwannaphum, honouring this tradition that is still debated by scholars for the same reasons as the Burman claim. Suphan Buri (from the Sanskrit, Suvarnapura , "Golden City") in present west/central Thailand,
14415-511: The atmosphere. Its waters are affected by the Indian Ocean Walker circulation , resulting in unique oceanic currents and upwelling patterns. The Indian Ocean is ecologically diverse, with important marine life and ecosystems like coral reefs, mangroves, and sea grass beds. It hosts a significant portion of the world's tuna catch and is home to endangered marine species. It faces challenges like overfishing and pollution , including
14570-756: The austral summer. In 1999, the Indian Ocean Experiment showed that fossil fuel and biomass burning in South and Southeast Asia caused air pollution (also known as the Asian brown cloud ) that reach as far as the Intertropical Convergence Zone . This pollution has implications on both a local and global scale. Forty percent of the sediment of the Indian Ocean is found in the Indus and Ganges fans. The oceanic basins adjacent to
14725-502: The beginning of the Zhenguan era (627–649) [when Emperor Taizong of Tang ruled]." The first inscription in the Khmer language is dated shortly after the fall of Funan. A concentration of later Khmer inscriptions in southern Cambodia may suggest the even earlier presence of a Khmer population. Despite absence of compelling evidence as to the ethnicity of the Funanese, modern scholar Michael Vickery has stated that "on present evidence it
14880-400: The bordering countries for domestic consumption and export. Fishing fleets from Russia, Japan, South Korea , and Taiwan also exploit the Indian Ocean, mainly for shrimp and tuna. Research indicates that increasing ocean temperatures are taking a toll on the marine ecosystem. A study on the phytoplankton changes in the Indian Ocean indicates a decline of up to 20% in the marine plankton in
15035-417: The center of Dvaravati culture shifted to Lavo , and the people of the sacked Dvaravati moved westward and founded a new city in 807 in the area of the present-day Ladya subdistrict, Kanchanaburi (Kanchanaburi old city) while the affected area was almost left abandoned. The new settlement was named Suvarṇabhūmi and was then renamed Sri Ayutthaya and Kanchanaburi, respectively. At the peak of power around
15190-492: The center of maritime trade between China and India was Srivijaya . Due to the Chinese writing system , however, the interpretations of Chinese historical sources are based on supposed correspondences of ideograms – and their possible phonetic equivalents – with known toponyms in the ancient Southeast Asian civilizations. Hendrik Kern concluded that Sumatra was the Suvarnadvipa mentioned in ancient Hindu texts and
15345-701: The centre of the 1,500,000 km (580,000 sq mi) hotspot, the landscape is dominated by Acacia - Commiphora deciduous bushland, but also includes the Yeheb nut ( Cordeauxia edulus ) and species discovered more recently such as the Somali cyclamen ( Cyclamen somalense ), the only cyclamen outside the Mediterranean. Warsangli linnet ( Carduelis johannis ) is an endemic bird found only in northern Somalia. An unstable political situation and mismanagement has resulted in overgrazing which has produced one of
15500-643: The city of Nafuna" ( Middle Chinese : *nâ-piiidt-nâ ). The Book of Sui (complied in 636) states: "The Kingdom of Zhenla is to the southwest of Linyi and was originally subject to Funan… The surname of its [former] king was that of the Cha-li clan; his given name was Zhiduo-si-na 質多斯那. His ancestors had gradually become more powerful and flourishing until the time of Zhi-duo-sina himself, who annexed Funan and possessed it." The New Book of Tang (c. 1060) tells that "Yīshēnàxiāndài (伊奢那先代), son of Citrasena- Mahendravarman , subdued Funan and annexed Funan territory in
15655-423: The conclusion that Funan was a Mon-Khmer polity. In his Funan review, Michael Vickery expresses himself a strong supporter of Funan's Khmer predominance theory. It is also possible that Funan was a multicultural society, including various ethnic and linguistic groups. In the late 4th and 5th centuries, Indianization advanced more rapidly, in part through renewed impulses from the south Indian Pallava dynasty and
15810-524: The conqueror Hùntián of the Book of Liang with the Brahmin Kauṇḍinya who married a nāga (snake) princess named Somā, as set forth in a Sanskrit inscription found at Mỹ Sơn and dated 658 CE (see below). Other scholars have rejected this identification, pointing out that the word "Hùntián" has only two syllables, while the word "Kauṇḍinya" has three, and arguing that Chinese scholars would not have used
15965-551: The continental slopes mostly contain terrigenous sediments. The ocean south of the polar front (roughly 50° south latitude ) is high in biologic productivity and dominated by non-stratified sediment composed mostly of siliceous oozes . Near the three major mid-ocean ridges the ocean floor is relatively young and therefore bare of sediment, except for the Southwest Indian Ridge due to its ultra-slow spreading rate. The ocean's currents are mainly controlled by
16120-514: The conversion of Suvarṇabhūmi is that it Burmanizes key historical Buddhist figures. In modern Thailand, government proclamations and national museums insist that Suwannaphum was somewhere on the coast of the central plain, especially at the ancient city of U Thong , which might be the origin of the Mon Dvaravati Culture. These claims are not based on any historical records but on archaeological evidence of human settlements in
16275-612: The eastern extension of which is blocked by the Southeast Indian Ridge and the 90°E Ridge. Madagascar and the Southwest Indian Ridge separate three cells south of Madagascar and off South Africa. North Atlantic Deep Water reaches into the Indian Ocean south of Africa at a depth of 2,000–3,000 m (6,600–9,800 ft) and flows north along the eastern continental slope of Africa. Deeper than NADW, Antarctic Bottom Water flows from Enderby Basin to Agulhas Basin across deep channels (<4,000 m (13,000 ft)) in
16430-488: The epigraphic and archaeological evidence, the Suvarṇabhūmi mentioned in the early texts must be identified with these areas. Of these areas, only Funan had maritime links with India through its port at Óc Eo . Therefore, although Suvarṇabhūmi in time was broadly applied to all lands east of India, particularly Sumatra, its earliest application was probably to Funan. Furthermore, the Chinese term of “Funan” for Cambodia, may be
16585-410: The first king of Sri Lanka, Vijaya Singha , came from Bengal. Moreover the region is commonly associated with golden color - the soil of Bengal is known for its golden color (Gangetic alluvial), golden harvest ( rice ), golden fruits ( mangoes ), golden minerals (gold and clay ) and yellow-brown skinned people. Bengal is described in ancient Sanskrit texts as ' Gaud -Desh' (Golden/Radiant land). During
16740-400: The foremost among brahmins, planted the spear which he had obtained from Droṇa's Son Aśvatthāman, the best of brahmins. There was a daughter of a king of serpents, called "Somā", who founded a family in this world. Having attained, through love, to a radically different element, she lived in the abode of man. She was taken as wife by the excellent Brahmin Kauṇḍinya for the sake of (accomplishing)
16895-560: The gold production areas traditionally known in Minangkabau Highlands in Barisan Mountains , Sumatra, and interior Borneo . The eighth-century Indian text Samaraiccakaha describes a sea voyage to Suvarnadvipa and the making of bricks from the gold rich sands which they inscribed with the name “ dharana” and then baked. These pointing out to the direction of western Insular Southeast Asia, especially Sumatra,
17050-406: The human world. The nāga king drinks the sea around the island and confers the name "Kampuchea Thipdei", which is derived from the Sanskrit ( Kambujādhipati ) and may be translated into English as "the lord of Cambodia". In another version, it is stated that Preah Thaong fights Neang Neak. Kaundinya II Even if the Chinese "Hùntián" is not the proper transcription of the Sanskrit "Kaundinya",
17205-631: The image of the crested argus or hamsa bird. Funan came into prominence at a time when the trade route from India to China consisted of a maritime leg from India to the Isthmus of Kra , the narrow portion of the Malay peninsula, a portage across the isthmus, and then a coast-hugging journey by ship along the Gulf of Siam , past the Mekong Delta, and along the Vietnamese coast to China. Funanese kings of
17360-726: The immense sea he attacked more than ten kingdoms ... he extended his territory five or six thousand li ." Fan Shih-man died on a military expedition to Chin-lin, "Frontier of Gold". He was followed by Chin-cheng, Fan Chan, Ch'ang and then Fan Hsun, in successive assassinations. Before his death, Fan Chan sent embassies to India and China in 243. Around 245, Funan was described as having "walled villages, palaces, and dwellings. They devote themselves to agriculture ... they like to engrave ornaments and chisel. Many of their eating utensils are silver. Taxes are paid in gold, silver, pearls, perfumes. There are books and depositories of archives and other things." The Indianised ruler Chan-T'an
17515-517: The inscription clearly identifies Sumatra as Suvarṇabhūmi. Butuan on the southern Philippine island of Mindanao was so rich in treasures that a museum curator, Florina H. Capistrano-Baker, stated it was even richer than the more well-known western maritime kingdom of Srivijaya ; “The astonishing quantities and impressive quality of gold treasures recovered in Butuan suggest that its flourishing port settlement played an until recently little-recognized role in early Southeast Asian trade. Surprisingly,
17670-618: The island of Chryse mentioned in the Periplus of the Erythraean Sea and by Rufius Festus Avienius . The Chinese pilgrim and Buddhist scholar Yijing (義淨), visited the kingdom of Srivijaya on Sumatra in 672 and identified it with Suvarnadvipa , the Island of Gold (金洲 jin-zhou ). The interpretation of early travel records is not always easy. Javanese embassies to China in 860 and 873 CE refer to Java as rich in gold, although it
17825-593: The islands of the Indian Ocean are textbook cases of evolutionary processes; the dung beetles , day geckos , and lemurs are all examples of adaptive radiation . Many bones (250 bones per square metre) of recently extinct vertebrates have been found in the Mare aux Songes swamp in Mauritius, including bones of the Dodo bird ( Raphus cucullatus ) and Cylindraspis giant tortoise. An analysis of these remains suggests
17980-513: The large-scale Tropical Warm Pool which, when interacting with the atmosphere, affects the climate both regionally and globally. Asia blocks heat export and prevents the ventilation of the Indian Ocean thermocline . That continent also drives the Indian Ocean monsoon , the strongest on Earth, which causes large-scale seasonal variations in ocean currents, including the reversal of the Somali Current and Indian Monsoon Current . Because of
18135-579: The last few decades, and it is precisely this region that reputedly housed the capital or capitals of Funan. However, archaeological surveys and excavations were carried out by joint Cambodian (Ministry of Culture and Fine Arts; Royal University of Fine Arts) and international teams at Angkor Borei since 1994 continuing into the 2000s. The research included excavation and dating of human burials at Wat Kamnou. Numerous brick features, architectural remains, and landscape features such as mounds, canals and reservoirs have also been identified. Some have been dated with
18290-439: The laws to conform to the system of India." Keneth Hall remarks that the basic details of the Chinese legend are reiterated elsewhere in Indian and Southeast Asian folklore. The historian Gabriel Ferrand believed that some Indian merchants might have immigrated to the region and established relations with the natives and that's how the myth emerged. Some Indian historians have taken this myth to extreme length and speculate that
18445-543: The legends, the precious metals were to be gathered from the ground and did not need to be laboriously extracted from the interior of the earth. In spite of their failure, they found it difficult to give up the alluring picture. When they did not find what they sought in the regions which were indicated by the old legends and by the maps based thereon, they hoped for better success in still unexplored regions, and clutched with avidity at every hint that they were here to attain their object. The history of geography thus shows us how
18600-427: The longest shorelines and exclusive economic zones . The continental shelf makes up 15% of the Indian Ocean. More than two billion people live in countries bordering the Indian Ocean, compared to 1.7 billion for the Atlantic and 2.7 billion for the Pacific (some countries border more than one ocean). The Indian Ocean drainage basin covers 21,100,000 km (8,100,000 sq mi), virtually identical to that of
18755-511: The majority of the kingdom's population were Mon people , while Thai people arrived later, around 50 BCE. The Suvarnabhumi Kingdom was destroyed by the invasion of Funan around the 1st-2nd centuries, and most of its population was forcibly moved to Funan resulting in it being left abandoned. After Funan lost to Bhavavarman I of Chenla in 550, Suvarṇabhūmi de facto became a tributary state of Chenla as well. The kingdom's area reached Lamphakappa Nakhon (ลัมภกัปปะนคร, present-day Lampang ) in
18910-481: The margins of the Indian Ocean. The origin of this diversity is debated; the break-up of Gondwana can explain vicariance older than 100 mya, but the diversity on the younger, smaller islands must have required a Cenozoic dispersal from the rims of the Indian Ocean to the islands. A "reverse colonisation", from islands to continents, apparently occurred more recently; the chameleons , for example, first diversified on Madagascar and then colonised Africa. Several species on
19065-527: The mission of the 3rd-century Chinese envoys Kang Tai ( 康泰 ) and Zhū Yīng ( 朱應 ) from the Kingdom of Wu to Funan. The writings of these envoys, though no longer extant in their original condition, were excerpted and as such preserved in the later dynastic histories, and form the basis for much of what we know about Funan. Since the publication of Pelliot's article, archaeological excavation in Vietnam and Cambodia, especially excavation of sites related to
19220-400: The monsoon. Two large gyres , one in the northern hemisphere flowing clockwise and one south of the equator moving anticlockwise (including the Agulhas Current and Agulhas Return Current ), constitute the dominant flow pattern. During the winter monsoon (November–February), however, circulation is reversed north of 30°S and winds are weakened during winter and the transitional periods between
19375-622: The monsoons. The Indian Ocean contains the largest submarine fans of the world, the Bengal Fan and Indus Fan , and the largest areas of slope terraces and rift valleys . The inflow of deep water into the Indian Ocean is 11 Sv , most of which comes from the Circumpolar Deep Water (CDW). The CDW enters the Indian Ocean through the Crozet and Madagascar basins and crosses the Southwest Indian Ridge at 30°S. In
19530-456: The most degraded hotspots where only c. 5 % of the original habitat remains. Funan Funan ( Chinese : 扶南 ; pinyin : Fúnán ; Khmer : ហ៊្វូណន , romanized : Hvunân , Khmer pronunciation: [fuːnɑːn] ; Vietnamese : Phù Nam , Chữ Hán : 夫南 ; Sanskrit : व्याधपूर, Vyādhapūra ) was the name given by Chinese cartographers , geographers and writers to an ancient Indianized state—or, rather
19685-543: The most productive ecosystems of the Indian Ocean ;— coastal areas produce 20 tones of fish per square kilometre. These areas, however, are also being urbanised with populations often exceeding several thousand people per square kilometre and fishing techniques become more effective and often destructive beyond sustainable levels while the increase in sea surface temperature spreads coral bleaching. Mangroves covers 80,984 km (31,268 sq mi) in
19840-438: The mud". The legend of Kaundinya is paralleled in modern Khmer folklore, where the foreign prince is known as "Preah Thaong" and the queen as "Neang Neak". In this version of the story, Preah Thaong arrives by sea to an island marked by a giant thlok tree, native to Cambodia. On the island, he finds the home of the nāgas and meets Neang Neak, daughter of the nāga king. He marries her with blessings from her father and returns to
19995-436: The name "Kaundinya" [Kauṇḍinya, Koṇḍañña, Koṇḍinya, etc.] is nevertheless an important one in the history of Funan. Chinese sources mention another person of the name "Qiáochénrú" ( 僑陳如 ). A person of that name is mentioned in the Book of Liang in a story that appears somewhat after the story of Hùntián. According to this source, Qiáochénrú was one of the successors of the king Tiānzhú Zhāntán ( 天竺旃檀 , "Candana from India"),
20150-541: The national anthem of Bangladesh - Amar Shonar Bangla (My Bengal of Gold), from Tagore's poem - is a reference to this theory. The thirst for gold formed the most powerful incentive to explorers at the beginning of modern times; but although more and more extensive regions were brought to light by them, they sought in vain in the East Indian Archipelago for the Gold and Silver Islands where, according to
20305-596: The neighbouring states honour his order to their heads”. Huntian/ Kaundinya I The Book of Liang records a local legend to document Funan's origin, that of the foundation of Funan by the foreigner Hùntián ( 混塡 , Middle Chinese pronunciation /ɦwən tɦian/): "He came from the southern country Jiào ( 徼 , an unidentified location, perhaps on the Malaysian Peninsula or in the Indonesian archipelago) after dreaming that his personal genie had delivered
20460-620: The north Indian Gupta Empire . The only extant local writings from the period of Funan are paleographic Pallava Grantha inscriptions in Sanskrit of the Pallava dynasty , a scholarly language used by learned and ruling elites throughout South and Southeast Asia. These inscriptions give no information about the ethnicity or vernacular tongue of the Funanese. Funan may have been the Suvarnabhumi referred to in ancient Indian texts. Among
20615-475: The north, and was ruled in mandala style with five royal cities, including Suvarnabhumi (the present old town of Nakhon Pathom ), Ratchaburi , Singburi , Phetchaburi , and Tanintharyi . The area surrounding the old capital of Suvarnabhumi was resettled in 590 when Sri Sittichai Phromthep (ท้าวศรีสิทธิไชยพรหมเทพ) from Yossothon (possibly the city in Chenla) established the new city, Nakhon Chai Si (old name of
20770-548: The port of the Sinae ). Due to many factors, including the lack of historical evidence, and the absence of scholarly consensus, various cultures in Southeast Asia identify Suvarṇabhūmi as an ancient kingdom there, and claim ethnic and political descendancy as its successor state. As no such claim or legend existed before the translation and publication of the Edicts, scholars see these claims as based on nationalism or attempts to claim
20925-464: The present-day Nakhon Pathom ). Most of its population were Thai people from the Ngao , Yom , and Salween river basins. Lavo was also founded during such a period. Both later created a new kingdom, Dvaravati ; however, the new capital together with the other nearest settlement, Pong Tuek (พงตึก, present-day Ratchaburi) were sacked by Chenla 300 years later, around the 8th-9th centuries. After that,
21080-399: The records from Yuán Shǐ , the history records of Yuan Dynasty. "Syam Kok and Lo Hu Kok, formerly the Kingdom of Funan, were located to the west of Linyi Kok (Champa Kingdom in central Vietnam). The maritime distance was from the capital of Linyi Kok to the capital of Funan Kok. They are separated by about 3,000 li." Like the very name of the kingdom, the ethno-linguistic nature of the people
21235-590: The reign of the Bengal Sultans and the Mughal Empire , central Bengal was home to a prosperous trading town called " Sonargaon " (Golden village), which was connected to North India by the Grand Trunk Road and was frequented by Arab, Persian and Chinese travelers, including Ibn Battuta and Zheng He . Even today, Bengalis often refer to their land as ' Shonar Bangla ' (Golden Bengal), and
21390-605: The rise in the Srivijaya trade empire, and the taking of trade routes all throughout Southeast Asia by China, leads to economic instability in the south, and forces politics and economy northward. Funan was superseded and absorbed in the 6th century by the Khmer polity of the Chenla Kingdom (Zhenla). "The king had his capital in the city of T'e-mu. Suddenly his city was subjugated by Chenla, and he had to migrate south to
21545-750: The rising sun returns its warm light, then will be seen the Isle of Gold with its fertile soil.” Avienius referred to the Insula Aurea (Golden Isle) located where “the Scythian seas give rise to the Dawn”. Josephus speaks of the “ Aurea Chersonesus ”, which he equates with the Biblical Ophir , whence the ships of Tyre and Israel brought back the gold for the Temple of Jerusalem . The city of Thina
21700-471: The title of the first Buddhists in Southeast Asia. Funan (1st–7th century) was the first kingdom in Cambodian history and it was also the first Indianized kingdom that prospered in Southeast Asia. Both Hinduism and Buddhism flourished in this kingdom. According to the Chinese records, two Buddhist monks from Funan, named Mandrasena and Sanghapala , took up residency in China in the 5th to 6th centuries, and translated several Buddhist sūtras from Sanskrit (or
21855-544: The typical first to sixth century CE historic classification scheme. Funanese culture was a mixture of native beliefs and Indian ideas. The kingdom is said to have been heavily influenced by Indian culture, and to have employed Indians for state administration purposes. Sanskrit was the language at the court, and the Funanese advocated Hinduism and, after the fifth century, Buddhist religious doctrines. Records show that taxes were paid in silver, gold, pearls, and perfumed wood. Kang Tai ( 康泰 ) and Zhu Ying ( 朱應 ) reported that
22010-410: The water area of Earth's surface . It is bounded by Asia to the north, Africa to the west and Australia to the east. To the south it is bounded by the Southern Ocean , or Antarctica , depending on the definition in use. The Indian Ocean has large marginal, or regional seas, such as the Andaman Sea , the Arabian Sea , the Bay of Bengal , and the Laccadive Sea . Once called the Eastern Ocean, it
22165-426: The world's oceans; its volume is 264,000,000 km (63,000,000 cu mi) or 19.8% of the world's oceans' volume; it has an average depth of 3,741 m (12,274 ft) and a maximum depth of 7,290 m (23,920 ft). All of the Indian Ocean is in the Eastern Hemisphere and the centre of the Eastern Hemisphere, the 90th meridian east , passes through the Ninety East Ridge . Within these waters are
22320-417: The world. Long-term ocean temperature records show a rapid, continuous warming in the Indian Ocean, at about 1.2 °C (34.2 °F) (compared to 0.7 °C (33.3 °F) for the warm pool region) during 1901–2012. Research indicates that human induced greenhouse warming , and changes in the frequency and magnitude of El Niño (or the Indian Ocean Dipole ), events are a trigger to this strong warming in
22475-471: Was Khmer. However, several studies demonstrates that inhabitants of Funan probably spoke Malayo-Polynesian languages , as in neighboring Champa . The results of archaeology at Oc Eo have demonstrated "no true discontinuity between Oc Eo and pre-Angkorian levels", indicating ancient Mon-he region may have gone as far back as the 4th century BCE. Though regarded by Chinese authors as a single unified polity, some modern scholars suspect that Funan may have been
22630-534: Was a large canal system that linked the settlements of Angkor Borei and coastal outlets; this suggests a highly organised government. Funan was a complex and sophisticated society with a high population density, advanced technology, and a complex social system. On the assumption that Funan was a single unified polity, scholars have advanced various linguistic arguments about the location of its "capital". Unfortunately, only limited archaeological research has been conducted on Funan in southern Cambodia and Cochinchina in
22785-470: Was described by Ptolemy’s Geography as the capital city of the country on the eastern shores of the Magnus Sinus ( Gulf of Thailand ). The location of Suvarṇabhūmi has been the subject of much debate, both in scholarly and nationalistic agendas. It remains one of the most mystified and contentious toponyms in Asia. Scholars have identified two regions as possible locations for the ancient Suvarṇabhūmi: Insular Southeast Asia and Southern India . In
22940-420: Was founded in 877-882 as a city of the Mon-speaking kingdom of Dvaravati with the name, Meuang Thawarawadi Si Suphannaphumi ("the Dvaravati city of Suvarṇabhūmi"), indicating that Dvaravati at that time identified as Suvarṇabhūmi. According to Thai chronicles, around 241 BCE, during the times that two Buddhist monks named Sona Thera and Uttara Thera came from Magadha to spread Buddhism to Suvarṇabhūmi,
23095-405: Was given instructions to search for the legendary Isles of Gold, said to lie to "beyond Sumatra", which he was unable to do, and in 1587 an expedition under the command of Pedro de Unamunu was sent to find them in the vicinity of Zipangu (Japan). According to Antonio de Herrera y Tordesillas , in 1528 Álvaro de Saavedra Cerón in the ship Florida on a voyage from the Moluccas to Mexico reached
23250-470: Was in fact devoid of any deposits. The Javanese would have had to import gold possibly from neighbouring Sumatra, the Malay Peninsula or Borneo, where gold was still being mined in the 19th century and where ancient mining sites were located. Even though Java did not have its own gold deposits, the texts make frequent references to the existence of goldsmiths, and it is clear from the archaeological evidence such as Wonoboyo Hoard , that this culture had developed
23405-411: Was linked to a port on the coast and to Angkor Borei by a system of canals, it is possible that all of these locations together constituted the heartland of Funan. Some scholars have advanced speculative proposal regarding the origin and meaning of the word Funan . It is often said that the name Funan ( Middle Chinese pronunciation of 扶南 : /bju nậm/, Later Han pronunciation: /buɑ nəm/ ) represents
23560-498: Was rather the Indianized local Southeast Asian traders who provided the initial contact with Indian cultural traditions and the local rulers followed up. He also stated that Hindu traditions was selectively mobilized by the local rulers to strengthen the political alliances among fragile polity of the states in that period. Successive rulers following Hun-t'ien included Hun-p'an-huang, P'an-p'an, and then Fan Shih-man, "Great King of Funan", who "had large ships built, and sailing all over
23715-414: Was ruling in 357, followed by another Indianised ruler Chiao Chen-ju (Kaundinya) in the fifth century, who "changed all the laws to conform to the system of India." In 480, She-yeh-pa-mo, Jayavarman or "Protege of Victory" reigned until his death in 514. One of his sons, Rudravarman, killed the other, Gunavarman, for the throne, and became the last king of Funan. Funan reached the apex of its power under
23870-455: Was the Kattigara referred to by the 2nd century Alexandrian geographer Ptolemy as the emporium where merchants from the Chinese and Roman empires met to trade. Dihle also believed that the location of Óc Eo best fit the details given by Ptolemy of a voyage made by a Graeco-Roman merchant named Alexander to Kattigara, situated at the easternmost end of the maritime trade route from the eastern Roman Empire. Georges Coedès said: "Fu-nan occupied
24025-514: Was unflattering to Funanese civilisation, though Chinese court records show that a group of Funanese musicians visited China in 263 CE. The Chinese emperor was so impressed that he ordered the establishment of an institute for Funanese music near Nanking . The Funanese were reported to have extensive book collections and archives throughout their country, demonstrating a high level of scholarly achievements. Two Buddhist monks from Funan, named Mandrasena and Sanghapala , took up residency in China in
#605394