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A portrait of P. wilsoni. Poebrotherium looked more like modern camels than its predecessor Protylopus, but at 90 centimetres (3.0 ft) in height, it was roughly the size of a modern sheep.
K2 — K2 (Kepler extended mission) catalog; KELT — Kilodegree Extremely Little Telescope (search for extrasolar planets) Kemble — Father Lucian Kemble (asterisms which could be observed through binoculars, for example: Kemble 1, aka Kemble's Cascade in Camelopardalis) Kepler — Kepler catalog; Kes — Kesteven (supernova remnants).
A cama is a hybrid between a male dromedary camel and a female llama, and has been produced via artificial insemination at the Camel Reproduction Centre in Dubai. [1] The first cama was born on January 14, 1998.
Paracamelus was named by Schlosser (1903). Its type is Paracamelus gigas. [3] P. gigas is known from the late Pliocene of China, while P. alutensis is known from the Plio-Pleistocene of Eastern Europe, P. alexejevi is known from Early Pliocene of Ukraine and P. aguirrei is known from the Early Messinian of Spain.
Bactrian camel (Camelus bactrianus) Central and Inner Asia (entirely domesticated) 300 to 1,000 kg (660 to 2,200 lb) Dromedary or Arabian camel (Camelus dromedarius) South Asia and Middle East (entirely domesticated) 300 to 600 kg (660 to 1,320 lb) Wild Bactrian camel (Camelus ferus) China and Mongolia 300 to 820 kg (660 to 1,800 lb) Lama: Llama
Aepycamelus is an extinct genus of camelids that lived during the Miocene 20.6–4.9 million years ago, existing for about 1] Its name is derived from the Homeric Greek αἰπύς, "high and steep" and κάμηλος – "camel"; [2] [3] thus, "high camel"; alticamelus in Latin.
† Western camel [4] [5] † Camelops hesternus: at least 36 individuals. A large species of camel with a generalized browsing diet. [6] Camelops, alongside the ancient bison and the western horse, is one of the most common large herbivores found in the tar pits. framless † Ancient bison [7] [8] † Bison antiquus: At least 300 individuals. [9]
Titanotylopus is an extinct genus of camel (tribe Camelini), endemic to North America from the late Hemphillian stage of the Miocene through the Irvingtonian stage of the Pleistocene. [2] It was one of the last surviving North American camels; after its extinction, only Camelops remained.
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