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The dromedary's karyotype is similar to that of the Bactrian camel. [5] As an adult, dromedary camels can weigh up to six times as much as a llama; as such, the hybrid needs to be produced by artificial insemination. Insemination of a female llama with sperm from a male dromedary camel has been the only successful combination.
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.
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.
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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
Adelie penguins in Antarctica. This is a list of the bird species recorded in Antarctica.The avifauna of Antarctica include a total of 63 species, of which 1 is endemic.This list's taxonomic treatment (designation and sequence of orders, families and species) and nomenclature (common and scientific names) follow the conventions of The Clements Checklist of Birds of the World, 2022 edition.
Camelops is an extinct genus of camel that lived in North and Central America from the middle Pliocene (from around 4-3.2 million years ago) to the end of the Pleistocene (around 13-12,000 years ago). It is more closely related to living camels than to lamines (llamas, alpacas, vicuñas, and guanacos), making it a true camel of the Camelini tribe.
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.