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Saint Peter and Saint Paul Archipelago

Coordinates:00°55′1″N29°20′45″W / 0.91694°N 29.34583°W /0.91694; -29.34583
From Wikipedia, the free encyclopedia
Archipelago in the Atlantic Ocean belonging to Brazil
Saint Peter and Saint Paul Archipelago
Brazilian Navy scientific station and lighthouse of the Saint Peter and Saint Paul Archipelago
Geography
LocationAtlantic Ocean
Coordinates00°55′1″N29°20′45″W / 0.91694°N 29.34583°W /0.91694; -29.34583
ArchipelagoArquipélago de São Pedro e São Paulo
Total islands15[1]
Major islandsBelmonte, Challenger, Nordeste, Cabral, South
Area1.5 ha (3.7 acres)[1]
Highest elevation17 m (56 ft)[1]
Administration
Brazil
RegionNortheast
StatePernambuco
Demographics
Population4[2]
Additional information
Official websitewww.mar.mil.br/secirm/proarq.htm
Map of the Saint Peter and Saint Paul Archipelago

TheSaint Peter and Saint Paul Archipelago (Portuguese:Arquipélago de São Pedro e São Paulo[ɐʁkiˈpɛlɐgudʒisɐ̃wˈpedɾwisɐ̃wˈpawlu]) is a group of 15 smallislets and rocks in the centralequatorialAtlantic Ocean.[3] It lies in theIntertropical Convergence Zone, a region of the Atlantic characterized by low average winds punctuated with local thunderstorms. It lies about 510 nmi (940 km; 590 mi) from the nearest point of mainlandSouth America (the northeasternBrazilian coastal town ofTouros); 625 km (388 mi) northeast of the archipelago ofFernando de Noronha; 990 km (620 mi) from the city ofNatal; and 1,824 km (1,133 mi) from the west coast ofAfrica. Administratively, the archipelago belongs toBrazil and is part of the special "state district" (Portuguese:distrito estadual) of Fernando de Noronha, in thestate ofPernambuco, in spite of the very large distance between the two island groups and the even larger distance to the state mainland.

In 1986, the archipelago was designated an environmentallyprotected area.[4] This is now part of theFernando de Noronha Environmental Protection Area.[5] Since 1998, theBrazilian Navy has maintained a permanently staffed research facility on the islands.[2] The main economic activity around the islets istuna fishing.

History

[edit]
Chart of 1839 byHMSErebus
Periscope eyeview from USSTriton (1960)

On April 20, 1511, aPortuguese Navy fleet composed of sixcaravels under the command of CaptainGarcia de Noronha discovered the islets by accident while on their journey toIndia. While navigating in the open sea late at night, theSaint Peter caravel, under the command of CaptainManuel de Castro Alcoforado, crashed against the islets. The crew was rescued by theSaint Paul caravel, forming the name given to the islets.[6]

In December 1799, the American captainAmasa Delano landed on the islets. He spent an afternoon and one night on the rocks.[7]

On the morning of February 16, 1832, the rocks were visited byCharles Darwin on the first leg of hisvoyage on HMSBeagle around the world. Darwin listed all thefauna he could find, noting that not a single plant or even a lichen could be found on the island.

The rocks, then called "St. Paul's Rocks", were visited byJames Clark Ross on 29 November 1839. He was in charge of anexpedition to the Antarctic regions with two vessels,HMSErebus andHMSTerror.Robert McCormick gave some geological and biological remarks on St. Paul's Rocks in the report on the expedition.[8]

Another famous person to visit the rocks wasErnest Shackleton, on hislast expedition toAntarctica (1921–1922).[6]

In 1942, duringWorld War II, the islets were declared to be part of the Federal Territory ofFernando de Noronha (which also included theRocas Atoll).

In early 1960, the rocks served as the starting-point and terminus for thefirst submerged circumnavigation of the world by the Americannuclear-powered submarineUSS Triton.[9]

In 1982 a wind anemometer with satellite telemetry reporting via GOES EAST satellite was installed by a team from Lamont-Doherty Geological Observatory with help from the Francais Ocean Climat Atlantique (FOCAL) and the Captain and crew of the N/O CAPRICORNE. This installation was supported by National Science Foundation Grant #OCE 82–09982.

Scientific station

[edit]
Aerial view of the islets. North is at the bottom left of the picture.

On June 25, 1998, theBrazilian Navy inaugurated the Saint Peter and Saint Paul Archipelago Scientific Station (Portuguese:Estação Científica do Arquipélago de São Pedro e São Paulo; ECASPSP). The station is staffed with fourresearchers, who are rotated in and out every 15 days.[10] By maintaining permanent occupation of the archipelago, the Brazilian Navy extendsBrazil's Exclusive Economic Zone,territorial waters andairspace into the North Atlantic Ocean.[11]

On June 5, 2006, the archipelago was shaken by anearthquake ofmagnitude 6.0 (withepicenter about 140 km to the east).[12] The strongtidal surge following the earthquake caused the battery compartment to crash against the station's outer wall, allowing sea water to flood the station. The four researchers who were on the archipelago took shelter in the lighthouse, while maintaining constant contact with the Brazilian Navy. Afishing vessel located nearby rescued the researchers, who were then transferred to a Brazilian Navypatrol boat. The incident caused considerable damage to the station and equipment.[13] The station was repaired on September 9–11, 2006, and became operational shortly after.[14]

In 2007, the Brazilian Navy started to build a new scientific station on the archipelago.[10] Construction began on July 24, 2007, and was completed on June 25, 2008.[10] The new station was built withseismic isolation, and is considerably larger and better equipped than the previous one.[15] The station is composed of a main building – equipped withreverse osmosis salt waterdesalination system,photovoltaics system andsatellite communications system; deposits and a mooring dock.[3][16]

The Brazilian Navy also maintains alighthouse, a focal light at 29 m above average sea level of 18 m lower, where the device was mounted, total height of 10.95 m, Base 2.5 m Cement, Tower 7.95 m, 3 Section of 2.65 m, Antenna 0,5 m, on the archipelago (ARLHS: SPP-001), built in 1995 to replace a previous one from 1930.[6][17] Mast Communication Besides of 15 m High.

Air France Flight 447

[edit]
Main article:Air France Flight 447

On June 1, 2009,Air France Flight 447, anAirbus A330-200 jetlineren route fromRio de Janeiro toParis, crashed in theAtlantic Ocean near the Saint Peter and Saint Paul Archipelago, killing all 228 people on board. Bodies and fragments of the aircraft were found just northwest of the archipelago.[18]

Geography

[edit]

The Saint Peter and Saint Paul Rocks are in the Atlantic Ocean, 100 km (62 mi) north of theEquator, and are the only group of Brazilian oceanic islets in theNorthern Hemisphere. The nearest point in the Brazilian coast, is Cabo do Calcanhar,Rio Grande do Norte, about 1,010 kilometres (630 mi) from the archipelago. The total emerged area is about 4.2 acres (1.7 ha) and the maximum land elevation is 18 m (59 ft), on Nordeste Island. The archipelago is composed of several rocks, five small rocky islets and four larger islets:[6][19]

  • Belmonte Islet: 5,380 square metres (1.33 acres)
  • Challenger Islet (also known as São Paulo): 3,000 square metres (0.74 acres)
  • Nordeste Islet (also known as São Pedro): 1,440 square metres (0.36 acres)
  • Cabral Islet: 1,170 square metres (0.29 acres)
  • South Islet: 943 square metres (0.233 acres).

Their base is over 3,650 metres (11,980 ft) below sea level.[6]

None of the islets have a permanentfresh water supply available.[6]

Geology

[edit]
The location of the archipelago on the junction between the African and South American plates.

The islets exposeserpentinized abyssalmantleperidotite andkaersutite-bearing ultramaficmylonite atop the world's highest and yet only second-largestmegamullion (after theParece Vela megamullion underOkinotorishima in thePacific Ocean). This grouping is the sole location in the Atlantic Ocean where the abyssal mantle is exposed above sea level.[6] Darwin noted in 1832 that, unusually, these small islands were not volcanic, but were instead formed by a geologic uplift.[6]

Abyssal morphology around the Saint Peter and Saint Paul Archipelago.

Undersea morphology

[edit]

The São Pedro and São Paulo Archipelago is located in the expansion zone between the South American Plate and the African Plate. The São Paulo Transform Fault System is one of the largest transform faults in the Atlantic Ocean., in which there is a total of 630 km of discontinuity in the segments of the mid-ocean chain. This is one of the deepest regions of the Atlantic Ocean and some locations are over 5,000 meters deep. The abyssal morphology shows that the Archipelago is located at the top of an underwater morphological elevation, with a length of 100 km, a width of 20 km and an approximate height of 3,800 meters from the ocean floor, called the Peridotitic Chain of São Pedro and São Paul. Unlike submarine volcanoes, this ledge consists of two tabular elevations oriented east–west, presenting a shape similar toBrachiosaurus dinosaur whose head faces east. On the flanks of the Archipelago, from sea level to a depth of 1,000 meters, high angle slopes occur, around 50º inclination. There is no extensive submarine platform of small depth around the Archipelago. To the south of the Archipelago there is a vertical cliff with a height greater than 2000 meters. These unstable submarine morphologies suggest that the uplift of the Archipelago originated from a recent tectonism, which continues until the present.

Biology

[edit]

Only the largest of the islets, Belmonte, is vegetated with mosses and grasses. The other rocks are mostly barren, except for some sea algae and fungi that can tolerate the salt spray. The rocks are inhabited byseabirds, including thebrown booby (Sula leucogaster),brown noddy (Anous stolidus), andblack noddy (Anous minutus), as well ascrabs (Grapsus grapsus),insects, andspiders.[20]

The islands are home to over 100 reef fishes, about 10% of which are foundnowhere else in the world, including the extremely colorfulTosanoides aphrodite.[19][21]

On his landing on the islands in 1832 Darwin found two birds, abooby and a brown noddy, a large crab that stole the fish intended for chicks, a fly that lived on the booby and a parasitic tick. He found a moth that lived on feathers, a beetle, a woodlouse that lived on dung, and numerous spiders that he thought lived on scavengers of the waterfowl. Darwin felt that these rocks represented how life first took hold on a newly formed outcrop.[22]

In literature

[edit]

St. Paul's Rocks are mentioned twice in Frank T. Bullen's 1898 semi-autobiographical travel narrative 'The Cruise of the Cachalot'.

The 1973 novelHMS Surprise byPatrick O'Brian describes a fictitious visit to one of the islands (called "St Paul's Rock" in the novel) by the character Dr Stephen Maturin. The specimens gathered by Maturin on the island are based on those historically collected by Darwin.

References

[edit]
  1. ^abcThe Scientific Station of São Pedro and São Paulo Archipelago Alvarez, Cristina; Melo, Julio; Mello, Roberto L. Retrieved on 2009-07-14.
  2. ^abPrograma Arquipélago[permanent dead link]Brazilian Navy. Retrieved on 2009-07-16.(in Portuguese)
  3. ^abThe scientific station of São Pedro and São Paulo Archipelago - BrazilArchived 2013-10-20 at theWayback Machine Alvarez, Cristina E., Melo, Julio E., Mello, Roberto L. Retrieved on June 6, 2009.
  4. ^Decree 92755 of 5 June 1986Archived 17 February 2012 at theWayback MachineLibrary of Congress. Retrieved on 2009-07-16.
  5. ^Área de Proteção Ambiental Fernando de Noronha – Rocas – São Pedro e São Paulo (in Portuguese), Parque Nacional Marinho Fernando de Noronha, archived fromthe original on 2017-01-04, retrieved2016-04-21
  6. ^abcdefghSaint Peter and Saint Paul's Archipelago - Tectonic uplift of infracrustal rocks in the Atlantic Ocean Campos, T.F.C.; Virgens Neto, J.; Srivastava, N.K.; Petta, R.A.; Harmann, L.A.; Moraes, J.F.S.; Mendes, L.; Silveira, S.R.M. In: Winge, M.; Schobbenhaus, C.; Berbert-Born, M.; Queiroz, E.T.; Campos, D.A.; Souza, C.R.G.; Fernandes, A.C.S. (Ed.),Geological and Palaeontological Sites of Brazil. Retrieved on 2017-03-20.
  7. ^Seagraves, Eleanor Roosevelt (1994).DELANO'S voyages of commerce and Discovery. Massachusetts: Berkshire House Publishers.
  8. ^Ross (1847), pp. 15–17, vol.1.
  9. ^Beach, Edward L. (2012) [1st Pub. 1962].Around the world submerged: the voyage of the Triton. New York: Holt, Rinehart and Winston. pp. 102–105, 257.ISBN 1-55750-215-3.OCLC 1292457.
  10. ^abcNova Era no Arquipélago de São Pedro e São PauloArchived 2011-09-27 at theWayback Machine Brazilian Navy. Retrieved on June 6, 2009.
  11. ^Lançamento da nova Estação Científica do Arquipélago de São Pedro e São PauloArchived 2009-12-01 at theWayback MachineBrazilian Navy. Retrieved on June 6, 2009.
  12. ^"M 6.0 - central Mid-Atlantic Ridge".Earthquake Hazards Program.USGS. Retrieved9 March 2023.
  13. ^Acidente no Arquipélago de São Pedro e São Paulo[permanent dead link]Brazilian Navy. Retrieved on 2009-07-16.(in Portuguese)
  14. ^Recuperação da Estação Científica do Arquipélago de São Pedro e São Paulo (ECASPSP)[permanent dead link]Brazilian Navy. Retrieved on 2009-07-16.(in Portuguese).
  15. ^A construção da nova Estação Científica[permanent dead link]Brazilian Navy. Retrieved on 2009-07-16.(in Portuguese)
  16. ^Manual do PesquisadorArchived 2011-09-27 at theWayback MachineBrazilian Navy. Retrieved on 2009-07-16.(in Portuguese)
  17. ^"ARLHS: SPP-001".ARLHS. 2006-06-01. Retrieved2009-06-07.
  18. ^"Total of 41 bodies recovered from Air France 447 crash".CNN.com. 2009-06-09. Archived fromthe original on June 12, 2009. Retrieved2017-06-03.
  19. ^abFeitoza, Bertran M; Rocha, Luiz A.; Luiz-Junior, Osmar J.; Floeter, Sergio R.; Gasparini, Joao L. (May 2003)."Reef fishes of St. Paul's Rocks: new records and notes on biology and zoogeography"(PDF).Aqua, Journal of Ichthyology and Aquatic Biology.7 (3):1–22. Archived fromthe original(PDF) on 2021-10-06. Retrieved2009-06-03.
  20. ^Série de reportagens sobre o arquipélago de São Pedro e São Paulo e as ilhas de Trindade e Martim VazArchived 2009-12-01 at theWayback MachineO Globo. Retrieved on 2009-07-16.(in Portuguese)
  21. ^Pinheiro, Hudson T.; Macena, Bruno C. L.; Francini‐Filho, Ronaldo B.; Ferreira, Carlos E. L.; Albuquerque, Fernanda V.; Bezerra, Natalia P. A.; Carvalho‐Filho, Alfredo; Ferreira, Romulo C. P.; Luiz, Osmar J.; Mello, Thayna J.; Mendonça, Sibele A. (2020)."Fish biodiversity of Saint Peter and Saint Paulʼs Archipelago, Mid-Atlantic Ridge, Brazil: new records and a species database".Journal of Fish Biology.97 (4):1143–1153.doi:10.1111/jfb.14484.ISSN 1095-8649.PMID 32743800.S2CID 220942252.
  22. ^Darwin's description from Voyage of the Beagle. Retrieved2009-07-16 – via www.literature.org, web.archive.org.

Further reading

[edit]
  • Andrade, F.G.G., Simões, L.S.A., Campos, T.F.C., Silva, A.J.C.A. 2007. Padrão estrutural da foliação milonígica do Arquipélago de São Pedro e São Paulo. Anais do 11º Simpósio Nacional de Estudos Tectônicos, 5th International Symposium of Tectonics of the SBG. Natal, 233. (in Portuguese)
  • Beach, Edward L. November 1960 (Vol. 118, No. 5). "Triton Follows Magellan's Wake"National Geographic Magazine. 585–615
  • Bonatti, E. 1990. Subcontinental mantle exposed in the Atlantic Ocean on St Peter-Paul islets. Nature, 345, 800–802.
  • Campos, T.F.C., Virgens Neto, J., Amorim, V.A., Hartmann, L.A., Petta, R.A. 2003. Modificações metassomáticas das rochas milonitizadas do complexo ultramáfico do Arquipélago de São Pedro e São Paulo, Atlântico Equatorial. Geochimica Brasiliensis, 17–2, 81–90. (in Portuguese)
  • Campos, T.F.C., Virgens Neto, J., Costa, L.S., Petta, R.A., Sousa, L.C., Silva, F.O. 2007. Sistema de diaclasamento do Arquipélago de São Pedro e São Paulo (Atlântico Equatorial) como indicador de movimentação destral associado à falha transformante de São Paulo. Anais do 11º Simpósio Nacional de Estudos Tectônicos, 5th International Symposium of Tectonics of the SBG. Natal, 238. (in Portuguese)
  • Hékinian, R., Juteau, T., Gracia, E., Udintsev, G., Sichler, B., Sichel, S.E., Apprioual, R. 2000. Submersible observations of Equatorial Atlantic Mantle: The St. Paul Frature Zone region. Marine Geophysical Research, 21, 529–560.
  • Melson, W.G., Jarosewich, E., Bowen, V.T., Thompsonm G. 1967. St. Peter and St. Paul rocks: a high-temperature mentle-derived intrusion. Science, 155. 1532–1535.
  • Moraes, J.F.S., Linden, E.M., Moraes, F.A.B. 1997. Planta topográfica do Arquipélago de São Pedro e São Paulo, escala 1:500. CPRM – Serviço Geológico do Brasil.
  • Motoki, A., Sichel, S.E., Campos, T.F.C., Srivastava, N.K., Soares, R.S. 2009. Taxa de soerguimento atual do Arquipélago de São Pedro e São Paulo, Oceano Atlântico Equatorial. Revista Escola de Minas, 62–3. 331–342. (in Portuguese)
  • Ross, James Ross (1847).A Voyage of Discovery and Research in the Southern and Antarctic Regions . London: John Murray – viaWikisource.
  • Sichel, S.E., Esperança, S., Motoki, A., Maia, M., Horan, M.F., Szatmari, P., Alves, E.C., Mello, S.L.M. 2008. Geophysical and geochemical evidence for cold upper mantle beneath the Equatorial Atlantic Ocean. Revista Brasileira de Geofísica, 26–1, 69–86.
  • Souza, José Eduardo Borges de: O arquipélago de São Pedro e São Paulo, Rio de Janeiro,Revista do Clube Naval, Ano 115, N° 340, Out/Nov/Dez 2006. p. 70-72, ISSN 0102-0382.
  • Thompson, Geoffrey: St. Peter and St. Paul's Rocks (Equatorial Atlantic) and the Surrounding Sea Floor, Woods Hole, Woods Hole Oceanographic Institution, 1981 (Technical Report) (Woods Hole Oceanog. Inst. Tech. Rept. WHOI-81 -98)[1]
  • Tressler, Willis L.: Rochedos São Pedro e São Paulo (St. Peter and St. Paul Rocks), Washington, U. S. Navy Hydrographic Office, 1956 (Technical Report, TR-31).
  • Virgens Neto, J., Campos, T.F.C. 2007. A influência da zona de fratura São Paulo no contexto estrutural do Arquipélago de São Pedro e São Paulo – Atlântico Equatorial. Anais do 11º. Simpósio Nacional de Estudos Tectônicos, 5th International Symposium of Tectonics of the SBG. Natal, 294–295. (in Portuguese)
  • Wiseman, J. D. H. 1966. St Paul's Rocks and the Problem of the Upper Mantle. Geophysical Journal of the Royal Astronomical Society, 11, 519–525. (in Portuguese)

External links

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