INVESTIGADORES
BERTELLI Sara Beatriz
artículos
Título:
A phylogeny of extant penguins (Aves: Sphenisciformes) combining morphology and mitochondrial sequences.
Autor/es:
BERTELLI, S.; GIANNINI, N.P.
Revista:
CLADISTICS (PRINT)
Editorial:
WILEY-BLACKWELL PUBLISHING, INC
Referencias:
Lugar: Ann Arbor, Michigan; Año: 2005 vol. 21 p. 209 - 239
ISSN:
0748-3007
Resumen:
The phylogenetic relationships among the penguins have received little attention, despite their well-known anatomy and the conspicuous nature of the group. Previous attempts have included datasets limited to few, mostly osteological characters, and one study was based on integumentary and breeding characters. We developed a morphological matrix comprising 159 morphological characters of osteology (70 characters), myology (15), digestive tract (1), integument (66), and breeding (7 characters), scored in 18 extant forms (all currently recognized species plus one distinct subspecies). A gaviiform was placed at the root, and 11 species of representative procellariiform groups completed the outgroup. A heuristic parsimony analysis under equal weights was performed. We also compiled DNA sequences available in GenBank for the mitochondrial genes 12S rDNA and cytochrome b.We included the two data partitions in a combined analysis under direct optimization. Both analyses recovered the monophyly of Sphenisciformes and all the traditional polytypic genera. Morphological characters performed optimally at the ordinal and generic nodes, also providing resolution and varying degrees of support at supra- and intrageneric nodes. The comparison of molecular and morphological results indicated that the most significant problem in the phylogeny of extant penguins is rooting the ingroup. The mutual interaction of molecular and morphological data decreases the ambiguity regarding the placement of the root, and provides a resolved, relatively well-supported phylogeny of extant penguins. Biogeographical patterns based on breeding ranges and derived from the combined analysis show that the major intercontinental vicariance events detected are consistent with cold marine current patterns of the Southern Hemisphere.