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Vicariance

About: Vicariance is a research topic. Over the lifetime, 2527 publications have been published within this topic receiving 117155 citations.


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Journal ArticleDOI
TL;DR: This work presents a new biogeographic method, dispersal-vicariance analysis, which reconstructs the ancestral distributions in a given phylogeny without any prior assumptions about the form of area relationships, and describes the algorithms that find the optimal reconstruction.
Abstract: Quantification in historical biogeography has usually been based on the search for a single branching relationship among areas of endemism. Unlike organisms, however, areas rarely have a unique hierarchical history. Dispersal barriers appear and disappear and may have differ- ent effects on different species. As a result, the biota of an area may consist of several components with separate histories, each of which may be reticulate rather than branching. In an attempt to address these problems, I present a new biogeographic method, dispersal-vicariance analysis, which reconstructs the ancestral distributions in a given phylogeny without any prior assumptions about the form of area relationships. A three-dimensional step matrix based on a simple biogeo- graphic model is used in the reconstruction. Speciation is assumed to subdivide the ranges of widespread species into vicariant components; the optimal ancestral distributions are those that minimize the number of implied dispersal and extinction events. Exact algorithms that find the optimal reconstruction(s) are described. In addition to their use in taxon biogeography, the in- ferred distribution histories of individual groups serve as a basis for the study of general patterns in historical biogeography, particularly if the relative age of the nodes in the source cladograms is known. (Cladistic biogeography; comparative phylogeography; dispersal; extinction; historical biogeography; optimization; vicariance; widespread species.) In historical biogeography, whether fo- cused on patterns below the species level (comparative phylogeography) or above the species level, there is a need for quan- titative methods to assess the likelihood of alternative hypotheses. Most methods used today are based on the assumption that there is a single branching pattern among areas of endemism caused by vi-

1,529 citations

Journal ArticleDOI
27 Mar 1998-Science
TL;DR: This paper examined the evolutionary radiation of Anolis lizards on the four islands of the Greater Antilles and found that the same set of habitat specialists, termed ecomorphs, occurs on all four islands.
Abstract: The vagaries of history lead to the prediction that repeated instances of evolutionary diversification will lead to disparate outcomes even if starting conditions are similar. We tested this proposition by examining the evolutionary radiation of Anolis lizards on the four islands of the Greater Antilles. Morphometric analyses indicate that the same set of habitat specialists, termed ecomorphs, occurs on all four islands. Although these similar assemblages could result from a single evolutionary origin of each ecomorph, followed by dispersal or vicariance, phylogenetic analysis indicates that the ecomorphs originated independently on each island. Thus, adaptive radiation in similar environments can overcome historical contingencies to produce strikingly similar evolutionary outcomes.

958 citations

Journal ArticleDOI
TL;DR: The results confirm the hybrid origin of the South American biota: there has been surprisingly little biotic exchange between the northern tropical and the southern temperate regions of South America, especially for animals.
Abstract: The Southern Hemisphere has traditionally been considered as having a fundamentally vicariant history. The common trans-Pacific disjunctions are usually explained by the sequential breakup of the supercontinent Gondwana during the last 165 million years, causing successive division of an ancestral biota. However, recent biogeographic studies, based on molecular estimates and more accurate paleogeographic reconstructions, indicate that dispersal may have been more important than traditionally assumed. We examined the relative roles played by vicariance and dispersal in shaping Southern Hemisphere biotas by analyzing a large data set of 54 animal and 19 plant phylogenies, including marsupials, ratites, and southern beeches (1,393 terminals). Parsimony-based tree fitting in conjunction with permutation tests was used to examine to what extent Southern Hemisphere biogeographic patterns fit the breakup sequence of Gondwana and to identify concordant dispersal patterns. Consistent with other studies, the animal data are congruent with the geological sequence of Gondwana breakup: (Africa(New Zealand(southern South America, Australia))). Trans-Antarctic dispersal (Australia southern South America) is also significantly more frequent than any other dispersal event in animals, which may be explained by the long period of geological contact between Australia and South America via Antarctica. In contrast, the dominant pattern in plants, (southern South America(Australia, New Zealand)), is better explained by dispersal, particularly the prevalence of trans-Tasman dispersal between New Zealand and Australia. Our results also confirm the hybrid origin of the South American biota: there has been surprisingly little biotic exchange between the northern tropical and the southern temperate regions of South America, especially for animals.

868 citations

Journal ArticleDOI
TL;DR: Congruence of biological and geological area-cladograms at a high confidence level means that specified events of paleogeography can be adopted as an explanation of the biological patterns, and distributions of sedentary organisms have the potential to falsify dispersal theories as applied tovagile organisms, but distributions of vagile organisms cannot falsify vicariance theories as applications to sedentary ones.
Abstract: Rosen, D. E. (Department of Ichthyology, American Museum of Natural History, New York, New York 10024) 1978. Vicariant patterns and historical explanation in biogeography. Syst. Zool. 27:159-188.-Geographic coincidence of animal and plant distributions to form recognizable patterns suggests that the separate components of the patterns are historically connected with each other and with geographic history. To seek evidence of these historical connections, cladograms of geographic areas, representing sequences of disruptive geologic, climatic, or geographic events, may be compared with biological cladograms, representing sequences of allopatric speciation events in relation to those geographic areas. Such comparisons, when they meet the minimum requirements of being among dichotomized threetaxon cladograms, can resolve similar or dissimilar historical factors; two-taxon statements do not distinguish between groups with different histories. Congruence of biological and geological area-cladograms at a high confidence level (such as congruence of a five-taxon cladogram or four three-taxon cladograms with a geological cladogram, where the confidence level can be shown in cladistic theory to be 99%o) means that specified events of paleogeography can be adopted as an explanation of the biological patterns. In such a cause and effect relationship, where the earth and its life are assumed to have evolved together, paleogeography is taken by logical necessity to be the independent variable and biological history, the dependent variable. Drawing a mathematical simile, the biological cladogram y (dependent variable), is a function of the geological cladogram x (independent variable), as in a simple regression of effect y on cause x where we are given no free choice as to which is the independent variable. Such a view implies that any specified sequence in earth history must coincide with some discoverable biological patterns; it does not imply a necessary converse that each biological pattern must coincide with some discoverable paleogeographic pattern, because some biological distributions might have resulted from stochastic processes (chance dispersal). Determining that all discoverable biological patterns conflict with a given corroborated or observed sequence of geologic, climatic, or geographic change (i.e., that y is not a function of x), in theory, therefore should falsify vicariance biogeography. Because dispersal biogeography presupposes stochastic processes, and any failure to meet the expectation of a postulated dispersal is explained by an additional dispersal, dispersal biogeography is immune to falsification. Without resort to paleontology or earth history, whether a given historical relationship implied by congruence of biological area-cladograms is the result of dispersal or vicariance can also be thought of in terms which minimize the number of necessary assumptions: did the sedentary organisms disperse with the vagile ones or did the vagile organisms vicariate with the sedentary ones? Cladistic congruence of a group of sedentary organisms with a group of vagile ones rejects dispersal for both. Hence, distributions of sedentary organisms have the potential to falsify dispersal theories as applied to vagile organisms, but distributions of vagile organisms cannot falsify vicariance theories as applied to sedentary ones. The problems that arise in various kinds of historical explanation are exemplified by several specific distributions of fishes and other organisms in North and Middle America and in the larger context of Pangaean history, and are discussed in relation to current species concepts. [Vicariance; species concepts; biocladistics; biohistory; geocladistics; geohistory; Neotropics; Gondwanaland.]

786 citations


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Performance
Metrics
No. of papers in the topic in previous years
YearPapers
202350
2022171
2021104
202087
2019100
2018123