Ancient DNA analysis reveals divergence of the cave bear, Ursus spelaeus, and brown bear, Ursus arctos, lineages

Citation
O. Loreille et al., Ancient DNA analysis reveals divergence of the cave bear, Ursus spelaeus, and brown bear, Ursus arctos, lineages, CURR BIOL, 11(3), 2001, pp. 200-203
Citations number
23
Categorie Soggetti
Experimental Biology
Journal title
CURRENT BIOLOGY
ISSN journal
09609822 → ACNP
Volume
11
Issue
3
Year of publication
2001
Pages
200 - 203
Database
ISI
SICI code
0960-9822(20010206)11:3<200:ADARDO>2.0.ZU;2-M
Abstract
The cave bear, Ursus spelaeus, represents one of the most frequently found paleontological remains from the Pleistocene in Europe. The species has alw ays been confined to Europe and was contemporary with the brown bear, Ursus arctos. Relationships between the cave bear and the two lineages of brown bears defined in Europe, as well as the origins of the two species, remain controversial, mainly due to the wide morphological diversity of the fossil remains, which makes interpretation difficult [1, 2]. Sequence analysis of ancient DNA is a useful tool for resolving such problems because it provid es an independent source of data [3]. We previously amplified a short DNA f ragment of the mitochondrial DNA control region (mt control region) of a 40 ,000-year-old Ursus spelaeus sample [4]. In this paper, we describe the DNA analysis of two mtDNA regions, the control region and the cytochrome b gen e. Control region sequences were obtained from ten samples of cave bears ra nging from 130,000 to 20,000 years BP, and one particularly well-conserved sample gave a complete cyt b sequence. Our data demonstrate that cave bears split largely before the lineages of brown bears around 1.2 million years ago, Given its abundance, its wide distribution in space and time, and its large morphological diversity, the cave bear is a promising model for direc t observation of the evolution of sequences throughout time, extinction per iods, and the differentiation of populations shaped by climatic fluctuation s during the Pleistocene.