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Liana Ecology Project
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ABSTRACT:
A phytogeographical characterization of the vine flora of the Sonoran and Chihuahuan deserts
Journal Article
Krings A
2000
Journal of Biogeography
27
1311-1319
Aim This study presents a phytogeographical characterization of the vine flora of two lower North American desert regions as a biogeographical framework for further ecological inquiry into desert vines. Location The phytogeography of the vine flora of the Sonoran and Chihuahuan Deserts was c haracterized based on 263 known species. Methods Checklists of the vines of each desert were developed. Represented genera were then grouped into 10 phytogeographical elements based on worldwide distribution patterns. To compare the floristic composition of the desert floras an index of species similarity was calculated. Results About a third more species of vines occur in the Sonoran Desert than in the Chihuahuan Desert. Based on the analysis cosmopolitan genera are the only group more numerous in absolute terms in the Chihuahuan Desert than in the Sonoran Desert. Tropical elements are represented in about the same proportion in each desert as the number of species however nearly twice as many pantropical and neotropical genera are represented in the Sonoran Desert as in the Chihuahuan Desert. Proportionately more genera of temperate elements occur in the Chihuahuan Desert than in the Sonoran desert although the absolute number of genera is slightly higher in the latter. Main conclusions As these deserts are relatively recent ecological formations and as vines evolved in forest ecosystems the composition of the desert vine floras is the result of the interaction between historical vegetation types their constituent taxa and climatic and geological history. The main differences in the vining floras of the present-day Sonoran and Chihuahuan Deserts appear to be the result of greater historical influence in the Sonoran Desert of (1) tropical vegetation types and (2) the emergence of the Gulf of California. The Chihuahuan Desert vine flora seems to be the result of (1) a more pronounced historical temperate vegetation (2) the lack of an important isolating event such as the creation of the Baja California peninsula and (3) a cooler climate with shorter growing seasons.
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