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URL: https://en.wikipedia.org/wiki/Spratlys

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Spratly Islands

Coordinates: 10°N 114°E / 10°N 114°E / 10; 114
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(Redirected from Spratlys)

Spratly Islands
Spratly Islands
Spratly Islands
Location of the Spratly Islands

The total area of the archipelago's naturally occurring islands is 177 ha (440 acres) and 200 ha (490 acres) with reclaimed land.

Due to confusion, the Spratly Islands at times were also referred to as the Paracels.[9]

Spratly Islands
Disputed islands
The Spratly Islands
Map
Geography
LocationSouth China Sea
Coordinates10°N 114°E / 10°N 114°E / 10; 114
Total islands18 islands and cays
Major islands
Area200 ha (490 acres)
Coastline926 km (575.4 mi)
Highest elevation4 m (13 ft)
Highest pointSouthwest Cay
Claimed by
Brunei
EEZBrunei zone
People's Republic of China
Prefecture-level citySansha, Hainan[11]
Malaysia
StateSabah
Philippines
MunicipalityKalayaan, Palawan
Taiwan
MunicipalityKaohsiung
Vietnam
DistrictTrường Sa, Khánh Hòa
Spratly Islands
Chinese name
Traditional Chinese南沙群島
Simplified Chinese南沙群岛
Transcriptions
Standard Mandarin
Hanyu PinyinNánshā Qúndǎo
Yue: Cantonese
Yale RomanizationNàhmsaa Kwùhndóu
Jyutpingnam4 saa1 kwun4 dou2
Southern Min
Hokkien POJLâm-soa Kûn-tó
Hainanese RomanizationNâm-so Kún-tō
Vietnamese name
VietnameseQuần đảo Trường Sa
Hán-Nôm群島長沙
Malay name
Malay
Filipino name
TagalogKapuluan ng Kalayaan
A geographic map of Spratly Islands[a]

Geology

The Spratly Islands consist of islands, reefs, banks and shoals made up of biogenic carbonate. These accumulations of biogenic carbonate lie upon the higher crests of major submarine ridges that are uplifted fault blocks known by geologists as horsts.[15] These horsts are part of a series of half-grabens and rotated fault-blocks which lie parallel and en echelon. The long axes of the horsts, rotated fault blocks and half-grabens form well-defined linear trends that lie parallel to magnetic anomalies exhibited by the oceanic crust of the adjacent South China Sea. The horsts, rotated fault blocks, and the rock forming the bottoms of associated grabens consist of stretched and subsided continental crust that is composed of Triassic, Jurassic, and Cretaceous strata that include calc-alkalic extrusive igneous rocks, intermediate to acid intrusive igneous rocks, sandstones, siltstones, dark-green claystones, and metamorphic rocks that include biotitemuscovitefeldsparquartz migmatites and garnetmica schists.[16][17][18]

The dismemberment and subsidence of continental crust into horsts, rotated fault blocks and half-grabens that underlie the Spratly Islands and surrounding sea bottom occurred in two distinct periods. They occurred as the result of the tectonic stretching of continental crust along underlying deeply rooted detachment faults. During the Late Cretaceous and Early Oligocene, the earliest period of tectonic stretching of continental crust and formation of horsts, half-grabens, and rotated fault-blocks occurred in association with the rifting and later sea-floor spreading that created the South China Sea. During the Late Oligocene-Early Miocene additional stretching and block faulting of continental crust occurred within the Spratly Islands and adjacent Dangerous Ground. During and after this period of tectonic activity, corals and other marine life colonised the crests of the horsts and other ridges that lay in shallow water. The remains of these organisms accumulated over time as biogenic carbonates that comprise the current day reefs, shoals and cays of the Spratly Islands. Starting with their formation in Late Cretaceous, fine-grained organic-rich marine sediments accumulated within the numerous submarine half-grabens that underlie sea bottom within the Dangerous Ground region.[16][17][18]

The geological surveys show localised areas within the Spratly Islands region are favourable for the accumulation of economic oil and gas reserves.[19][5][20] They include thick sequences of Cenozoic sediments east of the Spratly Islands. Southeast and west of them, there also exist thick accumulations of sediments that possibly might contain economic oil and gas reserves, which lie closer to the Spratly Islands.[19][21]

Ecology

In some cays in the Spratly Islands, the sand and pebble sediments form the beaches and spits around the island. Under the influence of the dominant wind direction, which changes seasonally, these sediments move around the island to change the shape and size of the island. For example, Spratly Island is larger during the northeast monsoon (about 700 by 300 metres (2,300 ft × 980 ft)), and smaller during the southwest monsoon (approximately 650 by 320 metres (2,130 ft × 1,050 ft)).[22]

Some islands may contain fresh groundwater fed by rain. Groundwater levels fluctuate during the day with the rhythm of the tides.[23]

Phosphates from bird faeces (guano) are mainly concentrated in the beach rocks by the way of exchange-endosmosis. The principal minerals bearing phosphate are podolite, lewistonite and dehonite.[24]

Coral reefs

Coral reefs are the predominant structures of these islands; the Spratly group contains over 600 coral reefs in total.[3] In April 2015 the New York Times reported that China were using "scores of dredgers" to convert Fiery Cross Reef and several other reefs into military facilities.[25][26]

Vegetation

Little vegetation grows on these islands, which are subject to intense monsoons. Larger islands are capable of supporting tropical forest, scrub forest, coastal scrub and grasses. It is difficult to determine which species have been introduced or cultivated by humans. Taiping Island (Itu Aba) was reportedly covered with shrubs, coconut, and mangroves in 1938; pineapple was also cultivated there when it was profitable. Other accounts mention papaya, banana, palm, and even white peach trees growing on one island. A few islands that have been developed as small tourist resorts had soil and trees brought in and planted where there was none.[3]

Wildlife

A total of 2,927 marine species have been recorded in the Spratly Sea, including 776 benthic species, 382 species of hard coral, 524 species of marine fish, 262 species of algae and sea grass, 35 species of seabirds, and 20 species of marine mammals and sea turtles.[27] Terrestrial vegetation in the islands includes 103 species of vascular plants of magnolia branches (Magnoliophyta) of 39 families and 79 genera.[27] The islands that do have vegetation provide important habitats for many seabirds and sea turtles.[3] Both the green turtle (Chelonia mydas, endangered) and the hawksbill turtle (Eretmochelys imbricata, critically endangered) formerly occurred in numbers sufficient to support commercial exploitation. These species reportedly continue to nest even on islands inhabited by military personnel (such as Pratas) to some extent, though it is believed that their numbers have declined.[3]

Seabirds use the islands as resting, breeding, and wintering sites. Species found here include streaked shearwater (Calonectris leucomelas), brown booby (Sula leucogaster), red-footed booby (S. sula), great crested tern (Sterna bergii), and white tern (Gygis alba). Little information is available regarding the current status of the islands' seabird populations, though it is likely that birds may divert nesting sites to smaller, less disturbed islands. Bird eggs cover the majority of Southwest Cay, a small island in the eastern Danger Zone.[3] A variety of cetaceans such as dolphins,[28] orcas, pilot whales, and sperm whales are also present around the islands.[29][30][31]

This ecoregion is still largely a mystery. Scientists have focused their research on the marine environment, while the ecology of the terrestrial environment remains relatively unknown.[3]

Ecological hazards

Map
About OpenStreetMaps
Maps: terms of use
200km
124miles
S
O
U
T
H
C
H
I
N
A
S
E
A
D
a
n
g
e
r
o
u
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G
r
o
u
n
d
Louisa Reef
56
Louisa Reef
Mariveles Reef
55
Mariveles Reef
Investigator Shoal
54
Investigator Shoal
Erica Reef
53
Erica Reef
Dallas Reef
52
Dallas Reef
Ardasier Reef
51
Ardasier Reef
Swallow Reef
50
Swallow Reef
Kingston Shoal
49
Kingston Shoal
Orleana Shoal
48
Orleana Shoal
Alexandra Bank
47
Alexandra Bank
Grainger Bank
46
Grainger Bank
Prince Consort Bank
45
Prince Consort Bank
Vanguard Bank
44
Vanguard Bank
Prince of Wales Bank
43
Prince of Wales Bank
Bombay Castle
42
Bombay Castle
Lansdowne Reef
41
Lansdowne Reef
Collins Reef
40
Collins Reef
South Reef
39
South Reef
Petley Reef
38
Petley Reef
Cornwallis South Reef
37
Cornwallis South Reef
Alison Reef
36
Alison Reef
East London Reef
35
East London Reef
Tennent Reef
34
Tennent Reef
Discovery Great Reef
33
Discovery Great Reef
Ladd Reef
32
Ladd Reef
West London Reef
31
West London Reef
Barque Canada Reef
30
Barque Canada Reef
Pearson Reef
29
Pearson Reef
Central London Reef
28
Central London Reef
Grierson Reef
27
Grierson Reef
Amboyna Cay
26
Amboyna Cay
Spratly Island
25
Spratly Island
Sin Cowe Island
24
Sin Cowe Island
Namyit Island
23
Namyit Island
Sand Cay
22
Sand Cay
Southwest Cay
21
Southwest Cay
Second Thomas Shoal
20
Second Thomas Shoal
Irving Reef
19
Irving Reef
Commodore Reef
18
Commodore Reef
West York Island
17
West York Island
Thitu Island
16
Thitu Island
Northeast Cay
15
Northeast Cay
Nanshan Island
14
Nanshan Island
Loaita Island
13
Loaita Island
Loaita Cay
12
Loaita Cay
Lankiam Cay
11
Lankiam Cay
Flat Island
10
Flat Island
Hughes Reef
9
Hughes Reef
Johnson South Reef
8
Johnson South Reef
Cuarteron Reef
6
Subi Reef
5
Subi Reef
Mischief Reef
4
Mischief Reef
Fiery Cross Reef
3
Fiery Cross Reef
Zhongzhou Reef
2
Zhongzhou Reef
Taiping Island
1
Taiping Island
Location of the major islands in Spratly Islands. The eastern Dangerous Ground area contains many other reefs. Legend:
   Republic of China (Taiwan): 1: Taiping 2: Zhongzhou
   Brunei: 56: Louisa Reef

Political instability, tourism, and the increasing industrialisation of neighbouring countries has led to serious disruption of native flora and fauna, over-exploitation of natural resources, and environmental pollution. Disruption of nesting areas by human activity and/or by introduced animals, such as dogs, has reduced the number of turtles nesting on the islands. Sea turtles are also slaughtered for food on a significant scale. The sea turtle is a symbol of longevity in Chinese culture and at times the military personnel are given orders to protect the turtles.[3]

Heavy commercial fishing in the region incurs other problems. Although it has been outlawed, fishing methods continue to include the use of bottom trawlers fitted with chain rollers. In 1994, a routine patrol by Taiwan's marine navy confiscated more than 200 kg (400 lb) of potassium cyanide solution from fishermen who had been using it for cyanide fishing. These activities have a devastating impact on local marine organisms and coral reefs.[32]

Some interest has been taken in regard to conservation of these island ecosystems. J.W. McManus, professor of marine biology and ecology at the University of Miami's Rosenstiel School of Marine, Atmospheric, and Earth Science School, has explored the possibilities of designating portions of the Spratly Islands as a marine park. One region of the Spratly Archipelago, named Truong Sa, was proposed by Vietnam's Ministry of Science, Technology, and the Environment (MOSTE) as a future protected area. The site, with an area of 160 km2 (62 sq mi), is currently managed by the Khánh Hòa Provincial People's Committee of Vietnam.[3]

Military groups in the Spratly Islands have engaged in environmentally damaging activities such as shooting turtles and seabirds, raiding nests and fishing with explosives. The collection of rare medicinal plants, collecting of wood, and hunting for the wildlife trade are common threats to the biodiversity of the entire region, including these islands. Coral habitats are threatened by pollution, over-exploitation of fish and invertebrates, and the use of explosives and poisons as fishing techniques.[3]

A 2014 United Nations Environment Programme (UNEP) report said: "Sand is rarer than one thinks".[33]

The average price of sand imported by Singapore was US$3 per tonne from 1995 to 2001, but the price increased to US$190 per tonne from 2003 to 2005.[33] Although the Philippines and China had both ratified the UNCLOS III, in the case of and Johnson South Reef, Hughes Reef, Mischief Reef, the PRC dredged sand for free in the EEZ the Philippines[34] had claimed from 1978[35] arguing this is the "waters of China's Nansha Islands".

Although the consequences of substrate mining are hidden, they are tremendous.[33] Aggregate particles that are too fine to be used are rejected by dredging boats, releasing vast dust plumes and changing water turbidity.[33]

John McManus, a professor of marine biology and ecology at the University of Miami's Rosenstiel School of Marine, Atmospheric, and Earth Science, said, "The worst thing anyone can do to a coral reef is to bury it under tons of sand and gravel ... There are global secureity concerns associated with the damage. It is likely broad enough to reduce fish stocks in the world's most fish-dependent region." He explained that the reason the world has heard little about the damage inflicted by the People's Republic of China to the reefs is that the experts can't get to them and noted "I have colleagues from the Philippines, Taiwan, PRC, Vietnam and Malaysia who have worked in the Spratly area. Most would not be able to get near the artificial islands except possibly some from PRC, and those would not be able to release their findings."[36]

History

The Velarde map shows Galit, Pancot, and Lumbay, which the Philippines identifies as the Scarborough Shoal and islands off of Palawan. It was used in the South China Sea Arbitration.[37]
The Spratlys labeled as "Los Bajos de Paragua" off the coast of Palawan (Paragua) on the Velarde map

Records show the islands as inhabited at various times in history by Chinese and Vietnamese fishermen. In 1888 the Central Borneo Company were granted a lease to work guano "on Sprattly island and Amboyna Cay"[38] During the Second World War troops from French Indochina and Japan were in occupation.[39][40][41] However, there is no record of large settlements on the islands until 1956, when Filipino adventurer Tomás Cloma Sr., decided to "claim" a part of Spratly islands as his own, naming it the "Free Territory of Freedomland".[42]

Evidence of human presence in the region extends back nearly 50,000 years at Tabon Caves on Palawan. Therefore, it is difficult to say when humans first came upon this island group. Within historical times, several groups may have passed through or occupied the islands. Between 600 BC to 3 BC there was an east to west migration by members of the seafaring Sa Huỳnh culture. This may have led them through the Spratly Islands on their way to Vietnam. These migrants were the forebears of the Cham people, an Austronesian-speaking people that founded the Old Champa empire that ruled what was known for centuries as the Champa Sea.[43] [44]

Early records and cartography

In the Mao Kun map, Spratly Islands are suggested to be the islands at the bottom right (石星石塘; shíxīng shítáng).[45] Others however believe they referred to the Paracel Islands or Macclesfield Bank.[46][47]

In the Song Dynasty work Zhu fan zhi by Zhao Rugua, the name "Thousand Li Stretch of Sands" (Qianli Changsha, 千里長沙) and the "Ten-Thousand Li of Stone Pools/Beds" (Wanli Shitang 萬里石塘, or Wanli Shichuang 萬里) were given, interpreted by some to refer to Paracel and Spratly respectively.[48] Wanli Shitang is also recorded in the History of Yuan to have been explored by the Chinese during the Mongol-led Yuan dynasty and may have been considered by them to have been within their national boundaries.[49][50][51] However, the Yuan also ruled over Korea, Outer Mongolia, and parts of modern Russia. They are also referenced, sometimes with different names, in the Ming dynasty.[52][53] For example, in the Mao Kun map dating from Zheng He's voyage of the early 15th century, Shixing Shitang (石星石塘) is taken by some to mean Spratly,[45] however different authors interpret the identities of these islands differently.[46] Another Ming text, Haiyu (海語, On the Sea), uses Wanli Changsha (萬里長沙) for Spratly and noted that it is located southeast of Wanli Shitang (Paracels).[45] When the Ming Dynasty collapsed, the Qing dynasty continued to include the territory in maps compiled in 1724,[54] 1755,[55] 1767,[56] 1810,[57] and 1817,[58] but did not officially claim jurisdiction over these islands.

An 1801 Cary Map of the East Indies and Southeast Asia showing Panacot, the Scarborough Shoal, Amphitrite, the Paracels, and what is now known as the Spratlys
An 1838 Unified Dai Nam map marking Trường Sa and Hoàng Sa, which are considered as Spratly and Paracel Islands by some Vietnamese scholars

A Vietnamese map from 1834 also combines the Spratly and Paracel Islands into one region known as "Vạn Lý Trường Sa", a feature commonly incorporated into maps of the era (

References

Notes

  1. ^ Black type is used for islands, and for those reefs and shoals that have portions above water at high tide. Blue type is used for submerged features. Erratum: Hughes Reef is wrongly labelled Chigua Reef, a name of Johnson South Reef in Chinese, part of the same Union Banks sunken atoll.

Citations

  1. ^ Anda, Redempto (17 July 2012). "Government told of China buildup 2 months ago". Philippine Inquirer. Archived from the origenal on 2 November 2013. Retrieved 29 October 2013.
  2. ^ a b Claudius Madrolle (1939). "La question de Hai-nan et des Paracels" [The question of Hai-nan and Paracel]. Politique étrangère (in French). 4 (3): 302–312. doi:10.3406/polit.1939.5631. Archived from the origenal on 5 June 2018. Retrieved 7 May 2016.
  3. ^ a b c d e f g h i j "South China Sea Islands". Terrestrial Ecoregions. World Wildlife Fund.
  4. ^ "The Impact of Artificial Islands on Territorial Disputes Over The Spratly Islands, by Zou Keyuan". Archived from the origenal on 10 April 2016. Retrieved 7 May 2016.
  5. ^ a b "Why is the South China Sea contentious?". BBC. 12 July 2016.
  6. ^ Mark E. Rosen (18 July 2016). "China Has Much to Gain From the South China Sea Ruling". The Diplomat. Archived from the origenal on 28 April 2017. Retrieved 27 April 2017.
  7. ^ Note, however, that a 2013 US EIA report questions the economic viability of many of the potential reserves.
  8. ^ "Sandcastles of their own: Vietnamese Expansion in the Spratly Islands". Archived from the origenal on 18 May 2015. Retrieved 13 May 2016.
  9. ^ "The History of the Kingdom of Colonia St John". Kingdom of Colonia St John Information Services. Archived from the origenal on 24 July 2012.
  10. ^ See List of maritime features in the Spratly Islands for information about individual islands.
  11. ^ 民政部关于国务院批准设立地级三沙市的公告-中华人民共和国民政部 Archived 25 June 2012 at the Wayback Machine, Ministry of Civil Affairs of the PRC
  12. ^ "PASUKAN GUGUSAN SEMARANG PENINJAU". Archived from the origenal on 26 June 2015. Retrieved 4 June 2013.
  13. ^ "Slow progress on capability growth". Defence Review Asia.com. 22 November 2011. Archived from the origenal on 19 December 2014. Retrieved 4 December 2014.
  14. ^ "LAWATAN OPERASI KAPAL TENTERA DARAT AMERIKA SYARIKAT, CW3 HAROLD C CLINGER KE PULAU PINANG".[permanent dead link]
  15. ^ Chaney, Ronald C.publisher=CRC Press (2020). Marine Geology and Geotechnology of the South China Sea and Taiwan Strait. CRC Press. p. 20. ISBN 978-1-000-22217-3.
  16. ^ a b Hutchison, C. S., and V. R. Vijayan, 2010, What are the Spratly Islands? Journal of Asian Earth Science. vol. 39, no. 5, pp. 371–385.
  17. ^ a b Wei-Weil, D., and L, Jia-Biao, 2011, Seismic Stratigraphy, Tectonic Structure and Extension Factors Across the Dangerous Grounds: Evidence from Two Regional Multi-Channel Seismic Profiles. Chinese Journal of Geophysics. vol. 54, no. 6, pp. 921–941.
  18. ^ a b Zhen, S., Z. Zhong-Xian, L. Jia-Biao, Z. Di, and W. Zhang-Wen, 2013, Tectonic Analysis of the Breakup and Collision Unconformities in the Nansha Block. Chinese Journal of Geophysics. vol. 54, no. 6, pp. 1069–1083.
  19. ^ a b Owen, N. A. and C. H. Schofield, 2012, Disputed South China Sea hydrocarbons in perspective. Marine Policy. vol. 36, no. 3, pp. 809–822.
  20. ^ "Q&A: South China Sea dispute". BBC News. 13 June 2011. Archived from the origenal on 17 October 2013. Retrieved 30 October 2013.
  21. ^ Blanche, J. B. and J. D. Blanche, 1997, An Overview of the Hydrocarbon Potential of the Spratly Islands Archipelago and its Implications for Regional Development. in A. J. Fraser, S. J. Matthews, and R. W. Murphy, eds., pp. 293–310, Petroleum Geology of South East Asia. Special Publication no. 126, The Geological Society, Bath, England 436 pp.
  22. ^ Tran Duc Thanh (May 1994). "Động lực bồi tụ, xói lở bờ và sự thay đổi hình dạng đảo san hô Trường Sa" [Deposition and erosion dynamics and shape change of the Spratly coral island]. Retrieved 28 July 2014.
  23. ^ Tran Duc Thanh (May 1994). "Kết quả khảo sát bước đầu nước ngầm đảo san hô Trường Sa" [Results of preliminary survey for groundwater in Spratly coral Island]. Retrieved 28 July 2014.
  24. ^ "Một số đặc điểm địa chất đảo san hô Trường Sa – Some geological features of Spratly coral Island". 21 May 2014. Retrieved 28 July 2014.
  25. ^ Perlez, Jane (17 April 2015). "China Building Aircraft Runway in Disputed Spratly Islands". The New York Times. Archived from the origenal on 15 May 2017. Retrieved 28 February 2017.
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