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Rio Negro (Amazon)

(Redirected from Guainia River)
For other uses, see Rio Negro (disambiguation).

The Rio Negro (Portuguese: Rio Negro [ˈʁi.u neɡɾu]; Spanish: Río Negro [ˈri.o ˈneɣɾo] "Black River"), or Guainía as it is known in its upper part, is the largest left tributary of the Amazon River (accounting for about 14% of the water in the Amazon basin), the largest blackwater river in the world,[8] and one of the world's ten largest rivers by average discharge. Despite its high flow, the Rio Negro has a low sediment load (5.76 million tonnes per year on average in Manaus).[4]

Rio Negro
Guainía River
Sunset over the Rio Negro, upstream from Manaus
Map showing the Rio Negro in the Amazon Basin
Native name
Location
Countries
Physical characteristics
Sourcehighlands of Colombia
 • locationGuainía Department, Amazon region, Colombia
 • coordinates1°56′50″N 70°1′55″W / 1.94722°N 70.03194°W / 1.94722; -70.03194 (approximately)
 • elevation250 m (820 ft) (approximately)
MouthAmazon River
 • location
Manaus, Amazonas State, Brazil
 • coordinates
3°08′00″S 59°54′30″W / 3.13333°S 59.90833°W / -3.13333; -59.90833
 • elevation
8 m (26 ft)[1]
LengthRio Negro–Guainía 2,250 km (1,400 mi)[2]
Basin size714,577.6 km2 (275,900.0 sq mi)[3]
Width 
 • average2,450 m (8,040 ft)[4]
Depth 
 • average20 m (66 ft) (Serrinha); 24 m (79 ft) to 31 m (102 ft) (Manaus)[3]
 • maximum60 m (200 ft) (Manaus)[4]
Discharge 
 • locationManaus
 • average(Period: 2015–2019)34,573 m3/s (1,220,900 cu ft/s)[4]
 • minimum4,240 m3/s (150,000 cu ft/s)[3]
 • maximum64,380 m3/s (2,274,000 cu ft/s)[3]
Discharge 
 • locationParicatuba (Anavilhanas)
 • average(Period: 2008–2019)34,444 m3/s (1,216,400 cu ft/s)[5]
 • minimum7,633 m3/s (269,600 cu ft/s) (2009/10)[5]
 • maximum65,510 m3/s (2,313,000 cu ft/s) (2014/06)[5]
Discharge 
 • locationSerrinha, 0°28′57.4716″S 64°49′36.6492″W / 0.482631000°S 64.826847000°W / -0.482631000; -64.826847000
 • average(Period: 1997–2015)16,845.5 m3/s (594,890 cu ft/s)[7]
 • minimum5,000 m3/s (180,000 cu ft/s)[6]
 • maximum30,000 m3/s (1,100,000 cu ft/s)[6]
Discharge 
 • locationSão Felipe, 0°22′11.8056″N 67°18′42.9948″W / 0.369946000°N 67.311943000°W / 0.369946000; -67.311943000
 • average(Period: 1997–2014)8,314.5 m3/s (293,620 cu ft/s)[7]
 • minimum1,200 m3/s (42,000 cu ft/s)[6]
 • maximum15,500 m3/s (550,000 cu ft/s)[6]
Discharge 
 • locationCucuí
 • average(Period: 1997–2014)5,113.1 m3/s (180,570 cu ft/s)[7]
 • minimum400 m3/s (14,000 cu ft/s)[6]
 • maximum10,500 m3/s (370,000 cu ft/s)[6]
Basin features
ProgressionAmazon → Atlantic Ocean
River systemAmazon River
Tributaries 
 • leftCasiquiare, Cauaburi, Marauiá, Macucuaú, Padauari, Demini, Jufari, Branco, Jauaperi, Camanaú, Baependi, Apuaú, Cuieiras, Tarumã Mirim, Tarumã Açu
 • rightGuainía (Upper Negro), Xié, Içana, Uaupés, Curicuriari, Marié, Tea, Uneiuxi, Aiuanã, Urubaxi, Ararirá, Cuiuni, Caurés, Unini, Jaú, Puduari

Geography

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Rio Negro watershed (Interactive map)

Upper course

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The source of the Rio Negro lies in Colombia, in the Department of Guainía where the river is known as the Guainía River.[9] The young river generally flows in an east-northeasterly direction through the Puinawai National Reserve, passing several small indigenous settlements on its way, such as Cuarinuma, Brujas, Santa Rosa and Tabaquén. After roughly 400 km (250 mi) the river starts forming the border between Colombia's Department of Guainía and Venezuela's Amazonas State. After passing the Colombian community of Tonina and Macanal the river turns southwest. Maroa is the first Venezuelan town the river passes. 120 km (75 mi) further downstream the river receives the Casiquiare canal from the left (north), forming a unique link between the Orinoco and the Amazon river basin. Henceforth the river is called Rio Negro.

Middle course

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The river now continues in a southeastern direction passing the Venezuelan town of San Carlos de Río Negro, its largest settlement on the river, and Colombia's San Felipe. In this stretch the river is constantly fed with tributaries from both sides, and it quickly grows in size creating large river islands, a common feature for all rivers in the Amazon basin. After forming the border between Colombia and Venezuela for 260 km (160 mi) the Rio Negro reaches the Piedra del Cocuy, an igneous rock formation from the Precambrian era, belonging to the Guyana Shield. Here the Tripoint of Colombia, Venezuela and Brazil is found in the middle of the river and it now completely enters Amazonas State, Brazil. After passing Cucuí, the river continues south, only temporarily turning west for several kilometers. In Missão Boa Vista the Içana River joins the Rio Negro and in São Joaquim the Uaupes River, the largest tributary of the Rio Negro, also enters from the right hand side. The Rio Negro now turns markedly towards the east, forming several rapids and small islets on its way. It then passes Sao Gabriel da Cachoeira an important commercial city. After several more rapids and imposing views of the Adormecida mountain chain the river leaves the Guyana shield it traversed in its upper and middle course.

Lower course

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The confluence of the Amazon River and the Rio Negro at Manaus, Brazil.

After the Marié River enters the Rio Negro the river continues its eastward course forming many large islands and becoming very wide at several locations. It passes local communities such as Santa Isabel do Rio Negro. During the wet season, the river floods the country far and wide here, sometimes to a width of 30 km (19 mi), for long distances. During this season, from April until October, it is a succession of lagoons, full of long islands and intricate channels with a lot of water wildlife. Near Carvoeiro the last major tributary of the Rio Negro, the Branco River joins the Rio Negro and the river temporarily forms the border between the state of Roraima and Amazonas State, Brazil. The river now takes a more southeastern course, becoming again very wide in many stretches before reaching the biggest city on its course Manaus.

The Anavilhanas National Park, a 350,018 ha (864,910 acres) conservation unit that was originally an ecological station created in 1981, protects part of the Anavilhanas river archipelago in this part of the river.[10] Below the archipelago, it meets the Solimões River to form the Amazon River, creating a phenomenon known as the Meeting of Waters.

Major tributaries

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List of the major tributaries of the Rio Negro (from the mouth upwards)[11][3][12][13]

Left tributary Right tributary Length Basin size Average discharge
km mi km2 sq mi m3/s cu ft/s
Rio Negro 2,362 1,468 719,216 277,691 30,640.8 1,082,070
Lower Rio Negro
Taruma-Açu 139 86 1,372 530 52.3 1,850
Cuieiras 3,441 1,329 144.2 5,090
Apuaú 3,799.1 1,466.8 153.6 5,420
Puduari 3,411.5 1,317.2 128.6 4,540
Camanaú 11,832.2 4,568.4 408 14,400
Jaú 400 250 18,896.6 7,296.0 869.2 30,700
Jauaperi 554 344 39,823.5 15,375.9 1,336.8 47,210
Unini 530 330 27,433 10,592 1,501.4 53,020
Branco 1,430 890 190,789.2 73,664.1 5,400 190,000
Jufari 311 193 12,590.5 4,861.2 446.6 15,770
Cauarés 7,332.3 2,831.0 296 10,500
Demini 39,769.6 15,355.1 1,357.9 47,950
Cuiuni 400 250 11,776.1 4,546.8 491.6 17,360
Igarapé Adairá 3,294.9 1,272.2 101.1 3,570
Ararirá 3,425 1,322 114.6 4,050
Ererê 3,251 1,255 115.7 4,090
Padauari 17,384 6,712 606.8 21,430
Daraá 3,053.3 1,178.9 114.9 4,060
Urubaxi 250 160 6,855.9 2,647.1 311.6 11,000
Aiuanã 4,590.7 1,772.5 185.2 6,540
Uneiuxi 12,474.7 4,816.5 488.3 17,240
Teá 6,365.9 2,457.9 201.4 7,110
Marauiá 6,712 2,592 255.3 9,020
Igarapé Inambu 4,618.8 1,783.3 140.6 4,970
Cauaburi 12,139.3 4,687.0 442.9 15,640
Middle Rio Negro
Marié 800 500 25,378 9,799 1,226.8 43,320
Curicuriari 14,202.2 5,483.5 916.8 32,380
Uaupés 1,375 854 64,370.4 24,853.6 4,344.9 153,440
Içana 696 432 35,675.3 13,774.3 2,278.9 80,480
Xié 8,222 3,175 488.1 17,240
Upper Rio Negro
Casiquiare 354 220 42,478 16,401 2,575.8 90,960
Guainía 617 383 28,899.5 11,158.2 2,432.7 85,910

Discharge

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Average discharge

Period Discharge Ref.
Encontro das Águas
1979–2015

30,640.8 m3/s (1,082,070 cu ft/s)

[11]
1971–2000 29,615.7 m3/s (1,045,870 cu ft/s) [12]
Manaus

3°8′19.3704″S 60°1′39.522″W / 3.138714000°S 60.02764500°W / -3.138714000; -60.02764500

2015–2019 34,573 m3/s (1,220,900 cu ft/s) [4]
1980–2006 35,943 m3/s (1,269,300 cu ft/s) [14]
1973–1992 28,400 m3/s (1,000,000 cu ft/s) [15]
1971–2000 29,607.4 m3/s (1,045,580 cu ft/s) [12]
Paricatuba

3°4′53.2848″S 60°14′0.4812″W / 3.081468000°S 60.233467000°W / -3.081468000; -60.233467000

2008–2019 34,444 m3/s (1,216,400 cu ft/s) [5]
1971–2000 29,518.2 m3/s (1,042,430 cu ft/s) [12]
Barcelos

0°58′59.6964″S 62°51′32.3892″W / 0.983249000°S 62.858997000°W / -0.983249000; -62.858997000

1971–2000 19,545.2 m3/s (690,230 cu ft/s) [12]
Serrinha

0°28′57.4716″S 64°49′36.6492″W / 0.482631000°S 64.826847000°W / -0.482631000; -64.826847000

1997–2015 16,845.5 m3/s (594,890 cu ft/s) [7]
1980–2006 18,082 m3/s (638,600 cu ft/s) [14]
1971–2000 16,611.9 m3/s (586,640 cu ft/s) [12]
São Gabriel da Cachoeira

0°8′2.9616″S 67°5′38.2956″W / 0.134156000°S 67.093971000°W / -0.134156000; -67.093971000

1971–2000 13,150.7 m3/s (464,410 cu ft/s) [12]
São Felipe

0°22′11.8056″N 67°18′42.9948″W / 0.369946000°N 67.311943000°W / 0.369946000; -67.311943000

1997–2014 8,314.5 m3/s (293,620 cu ft/s) [7]
1980–2006 7,984 m3/s (282,000 cu ft/s) [14]
1971–2000 8,244.8 m3/s (291,160 cu ft/s) [12]
Cucuí

1°11′16.7316″S 66°50′23.46″W / 1.187981000°S 66.8398500°W / -1.187981000; -66.8398500

1997–2014 5,113.1 m3/s (180,570 cu ft/s) [7]
1980–2006 4,940 m3/s (174,000 cu ft/s) [14]
1971–2000 5,065.1 m3/s (178,870 cu ft/s) [12]

History

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The river was named by the Spanish explorer Francisco de Orellana, who first came upon it in 1541. By the middle of the 17th century, Jesuits had settled along its banks in the midst of numerous tribes: Manau, Aruák, and Trumá Indians. After 1700 slaving along the river was common, and Native American populations were greatly diminished after contact with Eurasian diseases.[9] This area was the filming location for Survivor:The Amazon in 2003.

Fauna and flora

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Rio Negro near Manaus
 
Victoria amazonica

While the name Rio Negro means Black River, its waters are similar in colour to strong tea, which is typical of blackwater rivers. The dark color comes from humic acid due to an incomplete breakdown of phenol-containing vegetation from sandy clearings. The river was named because it looks black from a distance.

Much has been written on the productivity of the Rio Negro and other blackwater rivers. The older idea that these are "hunger rivers" is giving way, with new research, to the recognition that the Rio Negro, for example, supports a large fishing industry and has numerous turtle beaches. If explorers did not find many Indigenous peoples along the Rio Negro during the 17th century, it is likely that their populations were reduced because of new infectious diseases and warfare rather than low river productivity.

Rio Negro has a very high species richness. About 700 fish species have been documented in the river basin, and it is estimated that the total is 800–900 fish species, including almost 100 endemics and several undescribed species.[16] Among these are many that are important in the aquarium trade, including the cardinal tetra.[16] As a result of the Casiquiare canal, many aquatic species are found both in the Rio Negro and Orinoco. Because the Casiquiare includes both blackwater and clear- to whitewater sections, only relatively adaptable species are able to pass through it between the two river systems.[17]

In media

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The sixth season of Survivor, Survivor: The Amazon was filmed in Rio Negro in 2003.

Notes

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  1. ^ Tannenbaum, Frank (29 August 2012). TEN KEYS LAT AMER. Knopf Doubleday Publishing Group. ISBN 9780307826565. Retrieved 9 April 2018 – via Google Books.
  2. ^ Ziesler, R.; Ardizzone, G.D. (1979). "Amazon River System". The Inland waters of Latin America. Food and Agriculture Organization of the United Nations. ISBN 92-5-000780-9. Archived from the original on 8 November 2014.
  3. ^ a b c d e "Amazon basin water resources observation service".
  4. ^ a b c d e Rogério Ribeiro, Marinho; Naziano Filizola, Junior; Jean Michel, Martinez; Tristan, Harmel (2022). "Suspended sediment transport estimation in Negro River (Amazon Basin) using MSI/Sentinel-2 data". Revista Brasileira de Geomorfologia. 23. doi:10.20502/rbg.v23i1.2076.
  5. ^ a b c d Rogério Ribeiro, Marinho; Paulo Rodrigo, Zanin; Naziano Pantoja, Filizola Junior (2021). "The Negro River in the Anavilhanas Archipelago: Streamflow and geomorphology of a complex anabranching system in the Amazon". Earth Surface Processes and Landforms. 47 (4): 1108–1123. doi:10.1002/esp.5306.
  6. ^ a b c d e f Juan Gabriel, Leon; Stèphane, Calmont; F., Seyler; Marie-Paule, Bonnet; Mathilde, Cauhopé; Frédéric, Frappart; Naziano, Filizola; Pascal, Fraizy (2010). "Rating curves and estimation of average water depth at the upper Negro River based on satellite altimeter data and modeled discharges". Journal of Hydrology. 328 (3–4): 481–496. doi:10.1016/J.JHYDROL.2005.12.006.
  7. ^ a b c d e f Jamie, Towner (2019). "Assessing the performance of global hydrological models for capturing peak river flows in the Amazon basin" (PDF).
  8. ^ "Waters". Amazon Waters. 28 May 2014. Retrieved 10 October 2017.
  9. ^ a b Penn, James R (2001). Rivers of the World: A Social, Geographical and Environmental Sourcebook. Santa Barbara: ABC Clio.
  10. ^ PARNA de Anavilhanas (in Portuguese), ISA: Instituto Socioambiental, retrieved 2016-04-30
  11. ^ a b "PLANO ESTADUAL DE RECURSOS HÍDRICOS DO AMAZONAS, (PERH/AM) - RT 03 - DIAGNÓSTICO, PROGNÓSTICO E CENÁRIOS FUTUROS DO RECURSOS HÍDRICOS DO ESTADO - TOMO III" (PDF). Jan 2019. Archived from the original (PDF) on 2021-05-06. Retrieved 2021-10-03.
  12. ^ a b c d e f g h i "Amazon".
  13. ^ Emilio, Mayorga; Miles, G. Logsdon; Maria Victoria, R. Ballester; Jeffrey, E. Richey (2005). "Estimating cell-to-cell land surface drainage paths from digital channel networks, with an application to the Amazon basin". Journal of Hydrology: 167-182. doi:10.1016/j.hydrol.2005.03.023.
  14. ^ a b c d Josyane, Ronchail (2011). "Assessment of different precipitation datasets and their impacts on the water balance of the Negro River basin". Journal of Hydrology. 404 (3–4): 304–322. Bibcode:2011JHyd..404..304G. doi:10.1016/j.jhydrol.2011.04.037.
  15. ^ Théry, Hervé; Maurence, Pascale (1997). HYDROLOGIE DU BASSIN AMAZONIEN (PDF). ISBN 2-7011-1532-9.
  16. ^ a b Hales, J., and P. Petry (2013). Rio Negro. Freshwater Ecoregions of the World. Retrieved 12 February 2013
  17. ^ Staeck, W.; Schindler, I. (2015). "Description of a new Heros species (Teleostei, Cichlidae) from the Rio Orinoco drainage and notes on Heros severus Heckel, 1840" (PDF). Bulletin of Fish Biology. 15 (1–2): 121–136.

References

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  • Goulding, M., Carvalho, M. L., & Ferreira, E. J. G. (1988). Rio Negro, Rich Life in Poor Water : Amazonian Diversity and Foodchain Ecology as seen through Fish Communities. The Hague: SPB Academic Publishing. ISBN 90-5103-016-9
  • Saint-Paul, U., Berger, U., Zuanon, J., Villacorta Correa, M. A., García, M., Fabré, N. N., et al. (2000). "Fish communities in central Amazonian white- and blackwater floodplains," Environmental Biology of Fishes, 57(3), 235–250.
  • Sioli, H. (1955). "Beiträge zur regionalen Limnologie des Amazonasgebietes. III. Über einige Gewässer des oberen Rio Negro-Gebietes." Arch. Hydrobiol., 50(1), 1-32.
  • Wallace, A. R. (1853). A narrative of travels on the Amazon and Rio Negro, with an account of the native tribes, and observations on the climate, geology, and natural history of the Amazon Valley. London: Reeve.
  • Wright, R. (2005). História indígena e do indigenismo no Alto Rio Negro. São Paulo, Brazil: UNICAMP & Instituto Socioambiental. ISBN 85-7591-042-6.
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