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The Iberian ibex (Capra pyrenaica), also known as the Spanish ibex, Spanish wild goat and Iberian wild goat, is a species of ibex endemic to the Iberian Peninsula. [3] Four subspecies have been described; two are now extinct. The Portuguese ibex became extinct in 1892, and the Pyrenean ibex became extinct in 2000.
Capra pyrenaica pyrenaica taxidermy specimen – MHNT. The Pyrenean ibex (Capra pyrenaica pyrenaica), Aragonese and Spanish common name bucardo, Basque common name bukardo, Catalan common name herc and French common name bouquetin, was one of the four subspecies of the Iberian ibex or Iberian wild goat, a species endemic to the Pyrenees.
Species of wild goats that are called ibex are: The Asian ibex also known as the Siberian ibex (Capra sibirica) is a wild goat inhabiting long mountain systems in central Asian deserts and the northwestern Himalayas. The animal is 80–100 cm high at shoulder, and weighs an average 60 kg.
The Portuguese ibex (Capra pyrenaica lusitanica) is an extinct subspecies of Iberian ibex that inhabited the north mountainous zones of Portugal, Galicia, Asturias and western Cantabria. In size and colouration it was much like the Spanish animals, though inclining towards brown rather than black markings.
De-extinction (also known as resurrection biology, or species revivalism) is the process of generating an organism that either resembles or is an extinct species. [1] There are several ways to carry out the process of de-extinction. Cloning is the most widely proposed method, although genome editing and selective breeding have also been considered.
The Siberian ibex (Capra sibirica), also known using regionalized names including Altai ibex, Asian ibex, Central Asian ibex, Gobi ibex, Himalayan ibex, Mongolian ibex or Tian Shan ibex, [2] is a polytypic species of ibex, a wild relative of goats and sheep. It lives in Central Asia, and is, by far, the most widely-distributed species in the ...
Permian–Triassic boundary at Frazer Beach in New South Wales, with the End Permian extinction event located just above the coal layer [2]. Approximately 251.9 million years ago, the Permian–Triassic (P–T, P–Tr) extinction event (PTME; also known as the Late Permian extinction event, [3] the Latest Permian extinction event, [4] the End-Permian extinction event, [5] [6] and colloquially ...
The worst Phanerozoic event, the Permian–Triassic extinction, devastated life on Earth, killing over 90% of species. Life seemed to recover quickly after the P-T extinction, but this was mostly in the form of disaster taxa, such as the hardy Lystrosaurus. The most recent research indicates that the specialized animals that formed complex ...