ⓘ Agulhas Basin

Agulhas Basin

ⓘ Agulhas Basin

The Agulhas Basin is an oceanic basin located south of South Africa where the South Atlantic Ocean and south-western Indian Ocean meet. Part of the African Plate, it is bounded by the Agulhas Ridge to the north and the Southwest Indian Ridge to the south; by the Meteor Rise to the west and the Agulhas Plateau to the east. Numerous bathymetric anomalies hint at the basins dynamic tectonic history.


1. Geology

In a Late Paleocene 59-56 Ma reconstruction of the opening of the South Atlantic Ocean i.e. the separation of South America and Africa during the Gondwana break-up the Meteor Rise lies conjugate to the Islas Orcadas Rise east of the Falkland Plateau. The separation of the Meteor Rise and the Islas Orcadas Rise marks the beginning of the formation of the Agulhas Basin.

The Agulhas Ridge extends from the northern tip of the Meteor Rise towards the Agulhas Bank south of South Africa. The ridge, however, ends abruptly in a small plateau at 40°S 15°E where it intersects a northeastward-trending spreading centre the Agulhas Rift that was abandoned during the Early Paleocene 61 Ma. The presence of a short-lived tectonic plate between these structures was first proposed by LaBrecque & Hayes 1979. They named it the Malvinas Plate and proposed that it was active from 90 Ma until the spreading ceased in the Agulhas Basin at 65 Ma. The plate is located at a proto-Bouvet Triple Junction.

Marks & Stock 2001 found that Late Cretaceous 100-66 Ma fracture zones generated on the Agulhas Rift do not align with those north of the Agulhas Fracture Zone and cannot therefore have been formed by the spreading of South America and Africa. Furthermore, magnetic anomalies on the Malvinas Plate do not align with their conjugates on the African Plate if the spreading rates and directions of South America and Africa are used as a guide. They also noted that the Agulhas Fracture Zone do not lay perpendicular to traces of the South America-Africa spreading north of it and cannot, therefore, have been generate by this spreading.

The Agulhas Rift is the abandoned Malvinas-Africa ridge crest. 97 Ma the plate boundary in the Agulhas Basin was reorganised when the Mid-Atlantic Ridge made an eastward jump. This brought the boundary towards the Agulhas Plateau where excessive volcanism was building a large igneous province. The inception of the Malvinas Plate accompanied this shortening of the Agulas Fracture Zone. 61 Ma, the Malvinas Plate was finally incorporated into the African Plate when the Malvinas-Africa ridge was abandoned as the result of a westward ridge jump along the Agulhas-Falkland Fracture Zone. This second ridge jump reduced one of the most spectacular fracture zones in Earths history - 1.200 km 750 mi in length - to 180 km 110 mi.


2. Oceanography

The Agulhas Current flows south along the African east coast. When it reaches the southern tip of Africa, it retroflects back into the Indian Ocean. At this retroflection it leakes warm core eddies known as Agulhas rings into the South Atlantic. This mesoscale anti-cyclonic rings feed the Atlantic meridional overturning circulation AMOC and are therefore believed to affect the global climate, although the connection between the leakage, AMOC, and climate change is still poorly understood. In the Agulhas basin, half of these rings are subdivided one or several times. A majority of the subdivided rings split at or near the bathymetric obstacles on the western side of the Agulhas Basin but almost a quarter of them also merge there either because of the obstacles or because of intense interaction with other rings.

Antarctic Bottom Water AABW originated in the Oligocene with the opening of the Drake Passage and the Tasmanian Seaway and resulted in the thermal insulation of Antarctica. AABW mixes with other masses in the Antarctic Circumpolar Current ACC to form the Circumpolar Deep Water CDW. In the Agulhas Basin CDW flows northward and is deflect mostly westward by the Agulhas Ridge. A branch of CDW, however, enters the Cape Basin west of the ridge from where it flows west along the northern side of the ridge before being deflected north-east along the Walvis Ridge at the eastern end of the ridge. This long detour in the Cape Basin and mixing with North Atlantic Deep Water NADW results in warmer water than other CDW masses. Antarctic Intermediate Water AAIW flows above the CDW in the Agulhas Basin in an anti-cyclonic path in contrast to the cyclonic path followed by CDW.

  • Madagascar 35 Sv The net transport of the Agulhas Current is estimated as 100 Sv. The flow of the Agulhas Current is directed by the topography. The
  • The Agulhas Passage is an abyssal channel located south of South Africa between the Agulhas Bank and Agulhas Plateau. About 50 km 31 mi wide, it connects
  • Current. The Agulhas Current follows the continental shelf of the African east - coast, pass through the Agulhas Passage until it leaves the Agulhas Bank and
  • between the Agulhas Bank south of South Africa and the Agulhas passage south of the bank typical for a continent - ocean transition. The Agulhas Passage
  • The Agulhas Bank əˈɡʌləs from Portuguese for Cape Agulhas Cabo das Agulhas Cape of Needles is a broad, shallow part of the southern African continental
  • flow northwards through the Agulhas Basin and then east through the Agulhas Passage and over the southern margins of the Agulhas Plateau from where it is
  • the Black Needles peak Pico das Agulhas Negras The higher part of the park contains the origins of 12 river basins that supply the Rio Grande Grand
  • Hyphessobrycon agulha also known as the red - tailed flag tetra is a species of tetra in the family Characidae. As a freshwater fish, it inhabits the basin of the
  • Water AABW enters the Cape Basin between the Agulhas Bank and the Agulhas Ridge after which it flows west north of the Agulhas Ridge. AABW then retroflects
  • and mass extinction in the ocean basins Campbell Plateau South Pacific Challenger Plateau South Pacific Agulhas Plateau Southwest Indian Caribbean - Colombian