As. Chanderbali et al., Phylogeny and historical biogeography of Lauraceae: Evidence from the chloroplast and nuclear genomes, ANN MO BOT, 88(1), 2001, pp. 104-134
Phylogenetic relationships among 122 species of Lauraceae representing 44 o
f the 55 currently recognized genera are inferred from sequence variation i
n the chloroplast and nuclear genomes. The trnL-trnF, trnT-trnL, psbA-trnH,
and rpl16 regions of cpDNA, and the 5' end of 26S rDNA resolved major line
ages, while the ITS/5.8S region of rDNA resolved a large terminal clade. Th
e phylogenetic estimate is used to assess morphology-based views of relatio
nships and, with a temporal dimension added, to reconstruct the biogeograph
ic history of the family. Results suggest Lauraceae radiated when trans-Tet
hyean migration was relatively easy and basal lineages are established on e
ither Gondwanan or Laurasian terrains by the Late Cretaceous. Most genera w
ith Gondwanan histories place in Cryptocaryeae, but a small group of South
American genera, the Chlorocardium-Mezilaurus clade, represent a separate G
ondwanan lineage. Caryodaphnopsis and Neocinnamomum may be the only extant
representatives of the ancient Lauraceae flora documented in Mid- to Late C
retaceous Laurasian strata. Remaining genera place in a terminal Perseeae-L
aureae clade that radiated in Early Eocene Laurasia. Therein, non-cupulate
genera associate as the Persea group, and cupuliferous genera sort to Laure
ae of most classifications or Cinnamomeae sensu Kostermans. Laureae are Lau
rasian relicts in Asia. The Persea group and Cinnamomum group (of Cinnamome
ae) show tropical ampi-Pacific disjunctions here credited to disruption of
boreotropical ranges by Eocene-Oligocene climatic cooling. The Ocotea compl
ex accommodates remaining Cinnamomeae and shows a trans-Atlantic disjunctio
n possibly derived from a Madrean-Tethyan ancestral distribution. These fin
dings support Laurasian ancestry for most extant Lauraceae, with their cons
iderable neotropical representation primarily derived from Early Miocene ra
diation of the Ocotea complex upon reaching South America.