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. 2005 Aug 2;102(31):10919-23.
doi: 10.1073/pnas.0409127102. Epub 2005 Jul 20.

Timing the origin and expansion of the Mexican tropical dry forest

Affiliations

Timing the origin and expansion of the Mexican tropical dry forest

Judith X Becerra. Proc Natl Acad Sci U S A. .

Abstract

Macroevolution examines the temporal patterns of biological diversity in deep time. When combined with biogeography, it can provide unique information about the historical changes in the distribution of communities and biomes. Here I document temporal and spatial changes of diversity in the genus Bursera and relate them to the origin and expansion of the tropical dry forests of Mexico. Bursera is very old, highly adapted to warm dry conditions, and a dominant member of the Mexican tropical dry forest. These characteristics make it a useful indicator of the history of this vegetation. I used a time-calibrated phylogeny to estimate Bursera's diversification rate at different times over the last 60 million years. I also reconstructed the geographic center and time of origin of all species and nodes from information on current distributions. Results show that between 30 and 20 million years ago, Bursera began a relatively rapid diversification. This suggests that conditions were favorable for its radiation and thus, very probably for the establishment of the dry forest as well. The oldest lineages diverged mostly in Western Mexico, whereas the more recent lineages diverged in the south-central part of the country. This suggests that the tropical dry forest probably first established in the west and then expanded south and east. The timing of the radiations in these areas corresponds to that suggested for formations of the mountainous systems in Western and Central Mexico, which have been previously recognized as critical for the persistence of the Mexican dry forest.

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Figures

Fig. 1.
Fig. 1.
Distribution of the tropical dry forest in Mexico (modified from ref. 1). The black lines indicate the main axes of the Sierra Madre Occidental (A) and the Neovolcanic belt (B).
Fig. 2.
Fig. 2.
Time-calibrated phylogeny of Bursera (modified from ref. 13). Asterisks indicate species that were added to the phylogeny on the basis of their taxonomic descriptions and for which divergence time is unknown.
Fig. 3.
Fig. 3.
Number of Bursera lineages through time and 10-MY average diversification rates at different times over the last 60 MY.
Fig. 4.
Fig. 4.
Bursera's historical expansion in Mexico. (A) The distribution of Bursera was divided into 10 subareas. (B) Number of lineages that have diverged in each subarea of distribution at different time intervals. Some of the subareas have not had speciation events. (C) Diversification rates in each subarea of distribution at different time intervals.

Comment in

  • Tropical mountain cradles of dry forest diversity.
    Dick CW, Wright SJ. Dick CW, et al. Proc Natl Acad Sci U S A. 2005 Aug 2;102(31):10757-8. doi: 10.1073/pnas.0505013102. Epub 2005 Jul 26. Proc Natl Acad Sci U S A. 2005. PMID: 16046534 Free PMC article. No abstract available.

References

    1. Rzedowski, J. (1978) Vegetacion de Mexico (Limusa, Mexico).
    1. Becerra, J. X. (2003) Mol. Phylogenet. Evol. 26, 300-309. - PubMed
    1. Becerra, J. X. & Venable, D. L. (1999) Am. J. Bot. 86, 1047-1057. - PubMed
    1. Rzedowski, J. & Kruse, H. (1979) Taxon 28, 103-116.
    1. Gonzalez-Iturbe, J. A., Olmsted, I. & Tun-Dul, F. (2002) For. Ecol. Manage. 167, 67-82.

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