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Abstract Developments in the theory of continental drift and its general acceptance during the 1960s and 1970s confirmed the idea that disjunct biotic patterns and corresponding geological patterns are due to the same events in earth history. That the earth, including relative sizes and composition of land masses, constantly changes means that many, if not all, migration or dispersal solutions to biogeographic questions are wrong, or, at least, overstated. To us, a more realistic solution came when Brundin (1966) applied Hennig’s (1950) definition of phylogenetic relationship to the problems of vicariant distribution of southern hemisphere chironomid midges.Keywords:
Vicariance
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Continental drift
Ten North Temperate taxa representing diverse angiosperm lineages were analyzed for biogeographic histories using the dispersal‐vicariance analysis method to gain insights into the origin and evolution of disjunct distributions in the Northern Hemisphere. Results indicate four general biogeographic patterns: (1) origin and speciation in eastern Asia with subsequent expansion into North America and/or Europe (e.g., Aralia sect. Aralia, Symplocarpus, and possibly Asarum, Aesculus, and Chrysosplenium); (2) origin in eastern Asia and western North America with subsequent spread into eastern North America (e.g., Calycanthus and Boykinia); (3) a disjunct origin in eastern Asia and eastern North America with subsequent dispersal from eastern Asia into eastern North America (e.g., Panax); and (4) a widespread origin in the Northern Hemisphere with subsequent fragmentation by intercontinental vicariance (e.g., Cornus and Trautvetteria). Although there are caveats, the results indicate that the disjunct distributions of angiosperm lineages in the Northern Hemisphere cannot be explained with a simple vicariance model. Most lineages may have been restricted ancestrally to one or two adjacent areas and then secondarily expanded their ranges via dispersal. A noteworthy finding was the one‐way intercontinental plant exchange from the Old World to the New World and biased dispersal within each continent. There was more dispersal from the west to the east in North America but more dispersal from the east to the west in Eurasia. Such asymmetrical dispersal has also been documented in animals. The results also indicate that eastern Asia and western North America were the centers of origin for a majority of lineages examined, implying that these two areas were important sources of temperate angiosperm evolution in the Northern Hemisphere. The results further support a complex evolutionary history of angiosperms in the Northern Hemisphere and suggest pseudocongruence among lineages in phylogenetic relationships and distributional patterns.
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Disjunct distributions among wet-zone taxa of the Indian subcontinent have intrigued biologists for decades. Most authors have invoked variations of either the dispersal or the vicariance model to explain disjunct distribution. However, some have noted that incorrect taxonomy, due to convergence in morphological characters, can erroneously suggest disjunct distribution. An appropriate approach to test these models (vicariance, dispersal and convergence) is to use molecular phylogenetic methods. A survey of recent molecular phylogenetic studies on Indian systems with disjunct distribution suggests that convergence may be quite common. Therefore, I propose that the first step in studying disjunct distributions is to determine if the observed pattern is real (true disjunct) and not due to convergence, i.e. an artifact of incorrect taxonomy (false disjunct).
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Vicariance
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Genetic algorithm
Disjunct distribution
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Insular biogeography
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Population disjunctions, as a first step toward complete allopatry, present an interesting situation to study incipient speciation. The geological formation of the Baja California Peninsula currently divides 19 species of fish into disjunct populations that are found on its Pacific Coast and in the northern part of the Gulf of California (also called the Sea of Cortez), but are absent from the Cape (Cabo San Lucas) region. We studied the genetic makeup of disjunct populations for 12 of these 19 fish species. Phylogeographic patterns for the 12 species can be separated into two major classes: a first group (eight species) showed reciprocal monophyly and high genetic divergence between disjunct populations. A second group (four species) displayed what appeared to be panmictic populations. Population structure between Pacific Coast populations, across the Punta Eugenia biogeographic boundary, was also evaluated. While dispersal potential (inferred by pelagic larval duration) was a poor predictor of population structure between Gulf of California and Pacific populations, we found that population genetic subdivision along the Pacific Coast at Punta Eugenia was always positively correlated with differentiation between Pacific and Gulf of California populations. Vicariant events, ongoing gene flow, and ecological characteristics played essential roles in shaping the population structures observed in this study.
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Aim To illustrate the use of natural historical data to evaluate vicariance and dispersal as hypotheses competing to explain disjunct populations. Location Nine disjunct areas on the margin of the Tyrrhenian basin of the Mediterranean Sea. Methods First describe how each hypothesized mechanism might explain the observed morphological variation in the model species complex, Genista ephedroides (Fabaceae); then confront the hypotheses with natural historical data including geology, oxygen isotopes, palynology, macro‐, micro‐ and nano‐fossils, and sea level changes, and with the ecological tolerances of the model species complex. Results Dispersal seems the more credible explanation. Main conclusion Patterns of morphological (or other) variation among related disjunct taxa can fit both vicariance and dispersal hypotheses. However they can possibly be distinguished by considering natural historical data.
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Abstract The present paper reviews advances in the study of two major intercontinental disjunct biogeographic patterns: (i) between Eurasian and western North American deserts with the Mediterranean climate (the Madrean–Tethyan disjunctions); and (ii) between the temperate regions of North and South America (the amphitropical disjunctions). Both disjunct patterns have multiple times of origin. The amphitropical disjunctions have largely resulted from long‐distance dispersal, primarily from the Miocene to the Holocene, with available data indicating that most lineages dispersed from North to South America. Results of recent studies on the Mediterranean disjuncts between the deserts of Eurasia and western North America support the multiple modes of origin and are mostly consistent with hypotheses of long‐distance dispersal and the North Atlantic migration. Axelrod's Madrean–Tethyan hypothesis, which implies vicariance between the two regions in the early Tertiary, has been favored by a few studies. The Beringian migration corridor for semiarid taxa is also supported in some cases.
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Oceans, or other wide expanses of inhospitable environment, interrupt present day distributions of many plant groups. Using molecular dating techniques, generally incorporating fossil evidence, we can estimate when such distributions originated. Numerous dating analyses have recently precipitated a paradigm shift in the general explanations for the phenomenon, away from older geological causes, such as continental drift, in favour of more recent, long-distance dispersal (LDD). For example, the ‘Gondwanan vicariance’ scenario has been dismissed in various studies of Indian Ocean disjunct distributions. We used the gentian tribe Exaceae to reassess this scenario using molecular dating with minimum (fossil), maximum (geological), secondary (from wider analyses) and hypothesis-driven age constraints. Our results indicate that ancient vicariance cannot be ruled out as an explanation for the early origins of Exaceae across Africa, Madagascar and the Indian subcontinent unless a strong assumption is made about the maximum age of Gentianales. However, both the Gondwanan scenario and the available evidence suggest that there were also several, more recent, intercontinental dispersals during the diversification of the group.
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Vicariance biogeography seeks geo-physical explanations for disjunct distributions of organisms. Optimally, vicariance hypotheses are tested on the basis of the comparison of unrelated lineages of organisms that share geographic arenas. The fundamental approach is to marry geology and biology in the study of current and historical patterns of biodiversity. As a science, vicariance biogeography grew out of a synthesis of Alfred Wegener’s continental drift as realized by the plate-tectonic mechanism, Léon Croizat’s track analyses, and Willi Hennig’s phylogenetic systematics into a discipline with more readily testable hypotheses than those from classical dispersal biogeography. Vicariance biogeography, at the time of its emergence in the mid-1960s, offered a common explanation for many of the most puzzling disjunct-distribution patterns across the globe. From the 1960s to the early 21st century, vicariance biogeography dominated the field, marginalizing inquiries into geographic distributions on the basis of dispersal explanations, in part because center-of-origin ideas had fallen into disrepute. However, with the realization that vicariance hypotheses fail to explain an array of biogeographic patterns, including both isolated biotas on oceanic islands and many groups spread over previously connected landmasses, dispersal’s role in disjunct distributions of living things has been resurrected. The current consensus is that both processes play key roles in shaping the distribution of organisms through time.
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Population disjunctions, as a first step toward complete allopatry, present an interesting situation to study incipient speciation. The geological formation of the Baja California Peninsula currently divides 19 species of fish into disjunct populations that are found on its Pacific Coast and in the northern part of the Gulf of California (also called the Sea of Cortez), but are absent from the Cape (Cabo San Lucas) region. We studied the genetic makeup of disjunct populations for 12 of these 19 fish species. Phylogeographic patterns for the 12 species can be separated into two major classes: a first group (eight species) showed reciprocal monophyly and high genetic divergence between disjunct populations. A second group (four species) displayed what appeared to be panmictic populations. Population structure between Pacific Coast populations, across the Punta Eugenia biogeographic boundary, was also evaluated. While dispersal potential (inferred by pelagic larval duration) was a poor predictor of population structure between Gulf of California and Pacific populations, we found that population genetic subdivision along the Pacific Coast at Punta Eugenia was always positively correlated with differentiation between Pacific and Gulf of California populations. Vicariant events, ongoing gene flow, and ecological characteristics played essential roles in shaping the population structures observed in this study.
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