Anatolian crested newt which prohibit capture, disturbance, killing, trade, and destruction of habitats. Anatolian crested newt The Anatolian crested newt ("Triturus anatolicus") is a newt species endemic to northern Anatolia in Turkey. Before its description in 2016, it was first considered to belong to the southern crested newt ("Triturus karelinii") and then the Balkan crested newt ("Triturus ivanbureschi"). The three species form a complex of morphologically indistinguishable cryptic species. Genetic data demonstrated the Anatolian crested newt to be distinct from the other two species, although it hybridises with the Balkan crested newt at its western range end. With its two closely related species,
Geology of the Antarctic Peninsula and was active on King George Island during most of the Tertiary. The younger system of faults, also a series of strike-slip faults, displaced the older system and formed transverse to the island arc. Movement of the fault activity was caused by the counterclockwise rotation of the Antarctic Continent with respect to the subduction zone. The last and most recent stage in the evolution of the Antarctic Peninsula subduction zone is the opening of the Bransfield Rift, creating the Bransfield back-arc basin from the Oligocene to the present day. This basin separates the inner, older magmatic arc (mainland Antarctic Peninsula)