The Pharusian Ocean (; ) is an ancient ocean that existed on

Earth Earth is the third planet from the Sun and the only astronomical object known to Planetary habitability, harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all ...

from , between the break-up of the

Rodinia Rodinia (from the Russian родина, ''rodina'', meaning "motherland, birthplace") was a Mesoproterozoic and Neoproterozoic supercontinent that assembled 1.26–0.90 billion years ago (Ga) and broke up 750–633 million years ago (Ma). wer ...

supercontinent In geology, a supercontinent is the assembly of most or all of Earth's continent, continental blocks or cratons to form a single large landmass. However, some geologists use a different definition, "a grouping of formerly dispersed continents", ...

and the start of formation of the

Pannotia Pannotia (from Greek: ''wikt:pan-, pan-'', "all", ''wikt:νότος, -nótos'', "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neo ...

supercontinent.

Opening and closure

The Pharusian Ocean opened around 800 million years ago in the

Neoproterozoic The Neoproterozoic Era is the last of the three geologic eras of the Proterozoic geologic eon, eon, spanning from 1 billion to 538.8 million years ago, and is the last era of the Precambrian "supereon". It is preceded by the Mesoproterozoic era an ...

era after rifting along the eastern margin of the

West African craton The West African Craton (WAC) is one of the five cratons of the Precambrian basement rock of Africa that make up the African Plate, the others being the Kalahari craton, Congo craton, Saharan Metacraton and Tanzania Craton.Jessell M.W., Li ...

during the breakup of

. The ocean began to close around 730 million years ago with eastward subduction of the Tilemsi arc, which was accreted against the Hoggar region of the Saharan Metacraton. The western part of the Hoggar massif is made of material from the Pharusian Ocean including oceanic basalts, arc volcanic and sedimentary rocks and sediments that were shed into the Pharusian Ocean by the West African craton and the eastern Hoggar. Closure was completed when the West African and Saharan cratons collided around 635 million years ago at the start of the

Pan-African orogeny The Pan-African orogeny was a series of major Neoproterozoic orogenic events which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago. This orogeny is also known as the Pan-Gondwanan or Saldanian Oro ...

Southern extension

The Goiás Ocean, lying to the southwest between the Amazonian craton and the Congo craton, extended into the Pharusian Ocean. The Goiás Ocean closed during the final phases of formation of West

Gondwana Gondwana ( ; ) was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia (continent), Australia, Zea ...

. The southern portion of the Trans Brazilian Lineament (TBL) marks the suture zone of this closure, while the northern Borborema portion of the TBL and the Trans-Saharan Belt, running from

Algeria Algeria, officially the People's Democratic Republic of Algeria, is a country in the Maghreb region of North Africa. It is bordered to Algeria–Tunisia border, the northeast by Tunisia; to Algeria–Libya border, the east by Libya; to Alger ...

Benin Benin, officially the Republic of Benin, is a country in West Africa. It was formerly known as Dahomey. It is bordered by Togo to the west, Nigeria to the east, Burkina Faso to the north-west, and Niger to the north-east. The majority of its po ...

, mark the suture zone of the Pharusian Ocean closure. These ocean closures and subsequent tectonic events were not simultaneous, but happened over an extended period of time. In southwestern central Africa the granulite cooling ages range between 587 and 576 Ma, while in northeast Brazil they range from 568 to 500 Ma. However, aeromagnetic and gravity data give evidence of continuity between the TBL lineament, the Sobral fault in northeastern Brazil, the Kandi fault zone in

and the Trans-Saharan Belt formed by closure of the Pharusian Ocean.

References

Sources

* * * * * * * Historical oceans {{palaeo-geo-stub