RECLASSIFICATION OF ACTAEA TO INCLUDE CIMICIFUGA AND SOULIEA (RANUNCULACEAE) - PHYLOGENY INFERRED FROM MORPHOLOGY, NRDNA ITS, AND CPDNA TRNL-F SEQUENCE VARIATION
Ja. Compton et al., RECLASSIFICATION OF ACTAEA TO INCLUDE CIMICIFUGA AND SOULIEA (RANUNCULACEAE) - PHYLOGENY INFERRED FROM MORPHOLOGY, NRDNA ITS, AND CPDNA TRNL-F SEQUENCE VARIATION, Taxon, 47(3), 1998, pp. 593-634
Phylogenetic analyses using parsimony were performed on three independ
ent data sets to test generic relationships between Actaea, Cimicifuga
, and Souliea. Analyses of morphology and nuclear ribosomal DNA ITS we
re performed on 23 species of Cimicifuga, 4 species of Actaea, and the
single species of Souliea. Analysis of chloroplast DNA tmL-F was appl
ied to the same species, less two of Cimicifuga. The outgroup taxa Era
nthis and Anemonopsis both resolved outside the ingroup in all parsimo
ny analyses, whereas Souliea resolved within it. Jukes-Cantor pairwise
sequence distances confirm Eranthis and Anemonopsis to be most distan
t. Souliea distances are comparable with those of taxa within the Acta
ea-Cimicifuga assemblage. A strongly supported monophyletic clade incl
uding all studied species of Actaea, Cimicifuga, and Souliea was found
in all analyses. Evidence presented here allows a broader concept of
Actaea to be adopted, reverting to the circumscription of Linnaeus in
1753. Seven sections, based on clades found in the total analysis, cou
ld be defined by morphological characters: A, sect. Actaea, sect. Podo
carpae, sect. Cimicifuga, sect. Dichanthera, sect. Oligocarpae, sect.
Pilyrosperma, and sect. Souliea. One species, A. taiwanensis, is newly
described and 23 new combinations are made in the ranks of section, s
pecies, and variety. Keys are provided to identify taxa at all ranks w
ithin the revised circumscription of Actaea. Maps showing the distribu
tions of all seven sections and their constituent species are presente
d. Phytogeographic patterns suggest a Tertiary origin for the newly re
defined genus, with species surviving in refugia during the glacial pe
riods of the Pleistocene.