TY - JOUR
T1 - Historical biogeography, divergence times, and diversification patterns of bumble bees (Hymenoptera: Apidae: Bombus)
AU - Hines, Heather M.
N1 - Funding Information:
ACKNOWLEDGMENTS I extend my deepest gratitude to Sydney Cameron and Paul Williams for their advice and support. I would like to thank Sean Brady, Dickson Cunningham, Dave Hillis, Michael Knapp, Pierre Rasmont, Richard Ree, Fredrik Ronquist, Isabel Sanmartin, Jeff Thorne, Jim Whitfield, and Matt Yoder for helpful comments regarding data analysis and interpretation. I also extend my gratitude to Andy Deans, Claus Rasmussen, Josephine Rodriguez, and Jim Whitfield for additional comments on the manuscript. This project was supported by a USDA grant awarded to S. A. Cameron (NRI, CSREES 2004-35302-15077).
PY - 2008/2
Y1 - 2008/2
N2 - Bumble bees (Bombus) are a cold-adapted, largely alpine group that can elucidate patterns of Holarctic historical biogeography, particularly in comparison to the alpine plants with which they likely coevolved. A recently published molecular phylogeny of bumble bees provides uniquely comprehensive species sampling for exploring historical patterns of distribution and diversification. Using this phylogeny and detailed data on extant distributions, I reconstruct the historical distribution of bumble bees in a temporal framework, estimating divergence times using fossil data and molecular rates derived from the literature. The nearly comprehensive phylogeny allows assessment of the tempo of diversification within the bumble bees using lineage-through-time plots and diversification statistics, which have been performed with special consideration to confidence intervals. These analyses reveal movements of Bombus concordant with geographic and climatic events of the late Cenozoic. The initial diversification of extant bumble bee lineages was estimated at around 25 to 40 Ma, near the Eocene-Oligocene boundary 34 Ma, a period of dramatic global cooling. Dispersal-vicariance analysis (DIVA) predicted an Old World Bombus ancestor, with early diversification events largely restricted to the eastern Old World. The numerous intercontinental dispersal events occurred mostly in the direction of OldWorld to NewWorld and North America to South America. Early movements from the Palearctic into the Nearctic most likely took place after 20 Ma and may have coincided with a period of Miocene cooling that gave rise to taiga habitat across Beringia. Subsequent dispersal between these regions is estimated to have occurred among boreal and tundra-adapted species mostly in the last 5 million years. Radiations are estimated in both Nearctic and Neotropical regions at ~6 to 8 Ma and after 3.5 Ma, concordant with the opening of land corridors between the continents.
AB - Bumble bees (Bombus) are a cold-adapted, largely alpine group that can elucidate patterns of Holarctic historical biogeography, particularly in comparison to the alpine plants with which they likely coevolved. A recently published molecular phylogeny of bumble bees provides uniquely comprehensive species sampling for exploring historical patterns of distribution and diversification. Using this phylogeny and detailed data on extant distributions, I reconstruct the historical distribution of bumble bees in a temporal framework, estimating divergence times using fossil data and molecular rates derived from the literature. The nearly comprehensive phylogeny allows assessment of the tempo of diversification within the bumble bees using lineage-through-time plots and diversification statistics, which have been performed with special consideration to confidence intervals. These analyses reveal movements of Bombus concordant with geographic and climatic events of the late Cenozoic. The initial diversification of extant bumble bee lineages was estimated at around 25 to 40 Ma, near the Eocene-Oligocene boundary 34 Ma, a period of dramatic global cooling. Dispersal-vicariance analysis (DIVA) predicted an Old World Bombus ancestor, with early diversification events largely restricted to the eastern Old World. The numerous intercontinental dispersal events occurred mostly in the direction of OldWorld to NewWorld and North America to South America. Early movements from the Palearctic into the Nearctic most likely took place after 20 Ma and may have coincided with a period of Miocene cooling that gave rise to taiga habitat across Beringia. Subsequent dispersal between these regions is estimated to have occurred among boreal and tundra-adapted species mostly in the last 5 million years. Radiations are estimated in both Nearctic and Neotropical regions at ~6 to 8 Ma and after 3.5 Ma, concordant with the opening of land corridors between the continents.
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U2 - 10.1080/10635150801898912
DO - 10.1080/10635150801898912
M3 - Article
C2 - 18275002
AN - SCOPUS:47749083186
SN - 1063-5157
VL - 57
SP - 58
EP - 75
JO - Systematic Biology
JF - Systematic Biology
IS - 1
ER -