Cladistic biogeography of the Mexican transition zone

By C. Marshall, J. Liebherr. 2000

258 citations recorded by the source corpus.

Subfields: Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation, Paleontology

View Paper: https://www.semanticscholar.org/paper/fafa3734d49ade9f367c973711a2394ad8e82b02

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In Ecology, Evolution, Behavior and Systematics

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Citations in the corpus

Biogeography of helminth parasites of freshwater fishes in Mexico: the search for patterns and processes (2005, background): “Mexico is recognized as a region of ‘megadiversity’, with complex biogeographical patterns (Morrone et al., 1999; Marshall & Liebherr, 2000; Morrone & Márquez, 2001).”
A historical biogeographical protocol for studying biotic diversification by taxon pulses (2005, methodology): “…by Lieberman, we suggest a general protocol for inferring biotic evolution by taxon pulses, illustrated using the extensive data set presented by Marshall & Liebherr (2000), representing 33 clades of insects, vertebrates and flowering plants, occurring throughout Mexico and parts of Central…”
Comparative phylogeography of pitvipers suggests a consensus of ancient Middle American highland biogeography (2009, background): “…has been identified as a major phylogeographical break for many taxa, including frogs (Savage, 1987; Duellman, 1999), salamanders (Parra-Olea et al., 2004), snakes (Savage, 1982; Cadle, 1985), birds (Pérez-Emán, 2005), and plants, insects and fish (Marshall & Liebherr, 2000; Halas et al., 2005).”
Historical biogeography of lowland species of toads (Bufo) across the Trans‐Mexican Neovolcanic Belt and the Isthmus of Tehuantepec (2006, background): “The TMNB has been shown to represent a barrier to gene flow in other lowland taxa (Hulsey et al., 2004; Zaldı́var-Riverón et al., 2004), while the Isthmus of Tehuantepec has been more typically invoked as a barrier for upland taxa (Marshall & Liebherr, 2000; Sullivan et al., 2000).”
Halffter’s Mexican Transition Zone, beetle generalized tracks, and geographical homology (2001, background): “…1991b, 1992b; Schuster, 1992; Lobo & Halffter, 2000; among others), Halffter's Mexican Transition Zone has been challenged because of being `anathematically dispersalist' (Thomas, 1993, p. 384) or because of `what can be called the transition zone approach' (Marshall & Liebherr, 2000, p. 204).”
Phylogeny and comparative phylogeography of Sclerurus (Aves: Furnariidae) reveal constant and cryptic diversification in an old radiation of rain forest understorey specialists (2013, background): “This barrier is important for a number of unrelated taxa (e.g. Duellman, 1999; Marshall & Liebherr, 2000; Pérez-Emán, 2005).”
Fundamental biogeographic patterns across the Mexican Transition Zone: an evolutionary approach (2010, background): “Some authors have provided cladistic biogeographic analyses of Mexico (Liebherr 1991, 1994, Marshall and Liebherr 2000, Flores Villela and Goyenechea 2001, Espinosa et al. 2006, Contreras-Medina et al. 2007b).”
The diversification of Nearctic mammals in the Mexican transition zone (2004, background): “According to Marshall & Liebherr (2000), the boundary between the Nearctic and Neotropical regions lies in the Transmexican Volcanic Belt, not in the Isthmus of Tehuantepec.”
Biogeographic areas and transition zones of Latin America and the Caribbean islands based on panbiogeographic and cladistic analyses of the entomofauna. (2006, background): “Marshall & Liebherr (68) combine the Chiapas and Yucatan Peninsula provinces in a single province.”
Distributional patterns of freshwater taxa (fishes, crustaceans and plants) from the Mexican Transition Zone (2006, methodology): “Additional data were taken from Álvarez & Aguilar (1957), Miller (1960, 1966, 1975, 1986), Rosen & Bailey (1963), Álvarez del Villar (1970), Meyer & Vogel (1981), Meyer et al.”
Historical biogeography of scarabaeine dung beetles (2002, background): “…a suggested origination from island hopping or range expansion between the Oligocene and Miocene, although a recent faunal analysis using insects, reptiles, fish and plants suggests a Pleistocene age for northern elements and a Pliocene age for southern montane elements (Marshall & Liebherr, 2000).”
Biodiversity in the Mexican highlands and the interaction of geology, geography and climate within the Trans‐Mexican Volcanic Belt (2015, background): “The Mexican highlands are inhabited by temperate-cold tolerant taxa that include species with Nearctic, Neotropical and Palaeoamerican biogeographical origins (Halffter, 1987; Marshall & Liebherr, 2000; Halffter et al., 2008; Morrone, 2010).”
Using regional comparative phylogeographic data from snake lineages to infer historical processes in Middle America (2010, background): “While many previous studies largely agree in identifying major biogeographic boundaries across Middle America (Marshall and Liebherr 2000, Perdices et al. 2005, Devitt 2006, Crawford et al. 2007, Castoe et al. 2009), there is no consensus of when these boundaries may have been relevant in splitting…”
Phylogeography of Middle American gophersnakes: mixed responses to biogeographical barriers across the Mexican Transition Zone (2011, background): “These two mountain ranges are separated by the Balsas Basin, an arid lowland depression that formed in the Pliocene and Pleistocene in response to uplift of the Transvolcanic Belt (Becerra & Venable, 1999; Marshall & Liebherr, 2000).”