How To Use Tethys In A Sentence

We contrast the geological development of the Bainang terrane with that of other terranes in the region and consider this in the broader context of Neotethys evolution.
Diverse phocine seals – some apparently resembling the extant Pusa** seals – are known to have inhabited Paratethys during the Miocene (Paratethys was a brackish inland sea that covered much of south-east Europe and south-west Asia during the Miocene) and, according to the Paratethyan hypothesis, it is phocines from this region that managed to invade the Caspian Sea, later getting as far east as Lake Baikal. The most inconvenient seal
During the Pliocene, Paratethys was linked to the Arctic Ocean via a seaway just west of the Urals, apparently, and accordingly it has been proposed that the Ringed seal of the Arctic Ocean descends from a phocine that migrated north from the Paratethys (Ray 1976, Grigorescu 1977) [adjacent image shows a Ringed seal]. The most inconvenient seal
The oceans were reduced two in number; the larger by far was the enormous Panthalassa Ocean, roughly equivalent to the Pacific of today, while the smaller Tethys Ocean lay as a gigantic bight on the eastern side of Pangaea.
The family exhibited a Tethyan distribution, dispersed among epicontinental Europe, the Atlantic and Gulf Coastal Plain of North America, Africa, and the Tethys during the Eocene.

The Tethys Sea also expanded westward, splitting Pangaea into the supercontinents of Gondwana (in the South) and Laurasia (in the North).
Application of this model to the Maritimes Basin implies that this Westphalian epicontinental sea was connected to the Tethys Ocean by similarly narrow straits.
To bolster family control over the cosmetics company, Ms. Bettencourt and her daughter have agreed to appoint Ms. Bettencourt-Meyers's two sons to the board of Tethys, their holding company.
in the waters of the prehistoric Tethys ocean, a sinuous, 50-foot-long beast with gaping jaws and jagged teeth died and sank to the seafloor.
What Macey's work suggests is that each of the various taxa of agamid lizards crossed the Tethys on different continental plates, like so many groups of immigrants arriving on crowded steamers.
There is also a group of distinctive foraminifera more or less confined to the zone of the Tethys and thought to be a stenothermal tropical group.
The movement of the two resulting supercontinents was caused by sea floor spreading at the midocean ridge lying at the bottom of the Tethys Sea, the body of water between Gondwana and Laurasia.