The Paleo-Tethys or Palaeo-Tethys Ocean was an ocean
located along the northern margin of the paleocontinent Gondwana
that started to open during the Middle Cambrian
, grew throughout the Paleozoic
, and finally closed during the Late Triassic
; existing for about 400 million years.
Paleo-Tethys was a precursor to the Tethys Ocean
(also called the Neo-Tethys) which was located between Gondwana and the Hunic terranes
(continental fragments that broke-off Gondwana and moved north). It opened as the Proto-Tethys Ocean
subducted under these terranes and closed as the Cimmerian terranes
(that also broke-off Gondwana and moved north) gave way to the Tethys Ocean. Confusingly, the Neo-Tethys is sometimes defined as the ocean south of a hypothesised mid-ocean ridge separating Greater Indian from Asia, in which case the ocean between Cimmeria and this hypothesised ridge is called the Meso-Tethys, i.e. the "Middle-Tethys".
The so-called Hunic terranes are divided into the ''European Hunic'' (today the crust
under parts of Europe – called Armorica
– and Iberia
) and ''Asiatic Hunic'' (today the crust of parts of southern Asia). A large transform fault
separated the two terrane
The role the Paleo-Tethys played in the supercontinent cycle
, and especially the break-up of Pangaea
, is unresolved. Some geologists argue that the opening of the North Atlantic was triggered by the subduction of Panthalassa
under the western margins of the Americas while other argue that the closure of the Paleo-Tethys and Tethys resulted in the break-up. In the first scenario, mantle plume
s caused the opening of the Atlantic and the break-up of Pangaea and the closure of the Tethyan domain was one of the consequences of this process; in the other scenario, the longitudinal forces that closed the Tethyan domain were transmitted latitudinally in what is today the Mediterranean region, resulting in the initial opening of the Atlantic.
[[Image:249 global.png|200px|The Cimmerian plate starts to move northward, closing the Paleo-Tethys Ocean, while the Tethys Ocean begins to open from the south. ~249 mya (Permian-Triassic boundary).
The Paleo-Tethys Ocean began to form when [[Back-arc basin|back-arc spreading separated the European Hunic terranes from Gondwana in the late [[Ordovician, to begin moving toward [[Euramerica (also known as the Old Red Sandstone Continent) in the north. In the process, the plate under the Rheic Ocean
between Euramerica and the European Hunic terranes subducted and rift
s in this plate resulted in the formation of a small Rhenhercynian Ocean
which lasted until Late Carboniferous time.
In the Early Devonian
, the eastern part of Paleo-Tethys opened up, when the Asiatic Hunic terranes, including the North
and South China
microcontinents, moved northward.
These events caused Proto-Tethys Ocean
, a precursor of Paleo-Tethys, to shrink, until the Late Carboniferous
, when the Chinese blocks collided with Siberia
In the Early Carboniferous however, a subduction zone
developed south of the European Hunic terranes consuming Paleo-Tethys oceanic crust
Gondwana started moving north, in the process the western part of the Paleo-Tethys would close.
In the Carboniferous continental collision
took place between the Old Red Sandstone Continent and the European Hunic terrane, in North America
this is called the Alleghenian orogeny
, in Europe
the Variscan orogeny
. The Rheic Ocean
had completely disappeared, and the western Paleo-Tethys was closing.
By the Late Permian
, the small elongated Cimmerian plate
(today's crust of Turkey
and parts of South-East Asia
) broke away from Gondwana (now part of Pangaea
). South of the Cimmerian continent a new ocean, the Tethys Ocean
, was created. By the Late Triassic
, all that was left of the Paleo-Tethys Ocean was a narrow seaway.
In the Early Jurassic
epoch, as part of the Alpine Orogeny
, the oceanic crust of the Paleo-Tethys subducted under the Cimmerian plate, closing the ocean from west to east. A last remnant of Paleo-Tethys Ocean might be an oceanic crust under the Black Sea
, to the sea's south, is a part of the original Cimmerian continent that formed the southern boundary of the Paleo-Tethys.)
The Paleo-Tethys Ocean sat where the Indian Ocean
and Southern Asia
are now located. The Equator
ran the length of the sea, giving it a tropical climate. The shores and islands probably supported dense coal forest
Late Carboniferous Map
- at ''PaleoMap Project''; a good picture of Paleo-Tethys Ocean before the Cimmerian Plate
Paleo-Tethys and Proto-Tethys