scholarly journals Transition zones and biogeographic characterization of endemism in three biogeographic provinces of central Mexico

2021 ◽  
Vol 1 (1) ◽  
Author(s):  
Enrique Ortiz-Bermúdez ◽  
José Luis Villaseñor

Background: Sites of overlap in the species distribution among regions are known as transition zones. Their floristic and biogeographic complexity is rarely discussed. Questions: Is it possible to identify transition zones amid the biogeographic provinces of Mexico? Can transition zones also be considered areas of endemism? Study species: 315 Asteraceae taxa endemic to Mexico.Study site: Volcanic Belt, Balsas Depression and Sierra Madre del Sur biogeographic provinces. Methods: For species of Asteraceae endemic to three biogeographic provinces of central Mexico, we characterized the province to which each species belonged and estimated the distance it could penetrate the neighboring province. We defined transition zones between biogeographic provinces as the average penetration distances of the species. We also evaluated the presence of species with restricted distribution to transition zones. Results: Two transition zones were identified in the Balsas Depression, first, at the junction with the Volcanic Belt with a width of 13 km, and second, with the Sierra Madre del Sur, with a width of 12.3 km. There were 45 species whose distribution was restricted to those transition zones.Conclusions: Understanding how richness and endemism are exchanged from one region to another is essential to explain how their floras have been assembling and evolving. This analysis has allowed us to better understand the relationships among regions as complex as those studied here.

Zootaxa ◽  
2017 ◽  
Vol 4277 (2) ◽  
pp. 277 ◽  
Author(s):  
JUAN J. MORRONE ◽  
TANIA ESCALANTE ◽  
GERARDO RODRÍGUEZ-TAPIA

We provide a map of the 14 biogeographic provinces of Mexico based on the ecoregions recognized for the country, which combine climatic, geological and biotic criteria. These provinces belong to the Nearctic region (Californian, Baja Californian, Sonoran, Chihuahuan Desert and Tamaulipas provinces), Neotropical region (Pacific Lowlands, Balsas Basin, Veracruzan and Yucatán Peninsula provinces) and the Mexican transition zone (Sierra Madre Occidental, Sierra Madre Oriental, Transmexican Volcanic Belt, Sierra Madre del Sur and Chiapas Highlands provinces). In order to facilitate future biogeographic analyses, we provide a file of the biogeographical regionalisation of Mexico by converting the map into a polygon shapefile and a raster file with all provinces. We also separately provide each of the provinces in vector and raster format. All the maps are in geographical and Lambert Conformal Conic projections. 


2020 ◽  
Vol 98 (4) ◽  
pp. 612-623
Author(s):  
Arturo Castro-Castro ◽  
Jonathan Gilberto Zavala-Pérez ◽  
Ramiro Cruz-Durán

Background: Manfreda includes 37 species distributed from southeastern United States to Honduras. The Pacific Lowlands and Sierra Madre del Sur biogeographic provinces and Guerrero state are the centers of species richness and endemism for the genus in Mexico. Questions: How is the geographical distribution of Manfreda in Guerrero? Some specimen does not match any known Manfreda species, could be these collections a new species? Studied species: Fourteen Manfreda species. Study site: Guerrero, Mexico. Methods: The analysis was based on specimens reviewed from 19 herbaria, fieldwork, and records in specialized literature. The richness was quantified by municipalities, biogeographic provinces, and a grid cell, using geographic information systems. The morphological descriptions and the recognition of new species are based on traditional taxonomic methods. Results: Database included 86 records for 14 species. The richness is concentrated in 10 cells located in the transition between the Balsas Basin, Transmexican Volcanic Belt and the Sierra Madre del Sur. Some specimens that could not be assigned to any of the known species in Manfreda and proposed as a new species, which is presented with illustrations, an identification key, and a distribution map. Conclusions: Given the richness, the endemism, and the low density of collections of Manfreda in Guerrero, we found that the richness is likely greater than previously estimated and it could be expected to find new species. It is advisable to focus on the collection towards the Pacific Lowlands, since there is the greatest richness in Mexico.


Author(s):  
Roberto Maciel-Flores ◽  
José Rosas-Elguera ◽  
Laura Peña-García ◽  
Celia Robles-Murguía

Conserving the geological heritage in Jalisco implies, identifying, classifying and substantiating the importance of geosites in Jalisco and its subsequent dissemination through geotourism. The above can contribute to the creation of geo-park (s), according to the definition and methodology of UNESCO, with the consequent economic benefit to the inhabitants of these regions. The disclosure of geological information encourages an appreciation and care of abiotic resources (rocks, minerals, fossils, morphology, soil and water), especially prior to productive activities, minimizing their damage or avoiding building in areas with geological hazards. Jalisco has a great geodiversity, compared to other states, its history begins approximately 200 million years ago, recorded in the Sierra Madre del Sur and in the Jalisco Block, the most recent volcanic and tectonic activity is recorded in the Volcanic Belt Mexican. The previous provinces, together with the Sierra Madre Occidental and the Central Plateau, contain a wide range of rocks, fossil areas of economic and cultural importance (most of 70 places) and relate the geological history and its dynamics. Geothermal activity, is present in 400 locations.


Zootaxa ◽  
2005 ◽  
Vol 1027 (1) ◽  
pp. 55 ◽  
Author(s):  
ROXANA ACOSTA ◽  
JUAN J. MORRONE

A new flea species, Hystrichopsylla cryptotis, is described from the Sierra Madre Oriental and Sierra Madre del Sur, Mexico. The host of this new species is the shrew Cryptotis mexicana (Coues, 1877) (Mammalia: Soricidae). This flea species is easily recognized by its large size, seven genal combs, and the slender sternum IX, with 13 pairs of thick spiniform setae of different sizes. A key to the Mexican and Guatemalan species of Hystrichopsylla is given. The cladistic analysis indicates that Mexican species of Hystrichopsylla may be arranged in two different species groups: the H. orophila species group (H. orophila Barrera 1952 and H. cryptotis) and the H. dippiei species group (H. dippiei Rotshchild 1902, H. llorentei Ayala and Morales 1990, and H. kris Traub and Johnson 1952). The resolved area cladogram based on their phylogenetic relationships indicates the following relationships: (Sierra Madre Oriental, (Sierra Madre del Sur, Transmexican Volcanic Belt)).


2016 ◽  
Vol 29 (2) ◽  
pp. 142 ◽  
Author(s):  
Guadalupe Munguía-Lino ◽  
Tania Escalante ◽  
Juan J. Morrone ◽  
Aarón Rodríguez

The tribe Tigridieae (Iridoideae: Iridaceae) is a New World group with centres of diversity in Mexico and Andean South America. North America harbours 67 of the 172 species recognised within the tribe, 54 being endemic. Our aims were to identify areas of endemism of the North American Tigridieae using endemicity analysis (EA) and to infer their relationships using parsimony analysis of endemicity (PAE). A data matrix with 2769 geographical records of Tigridieae was analysed. The EA allowed to identify six consensus areas of endemism in Mexico. The PAE resulted in one cladogram with four clades and the following five biotic components: northern Mexico, western Mexico, central Mexico, southern Mexico and central–southern Mexico. The richness analysis of these areas of endemism indicated that the greatest concentration of species is located in central Mexico, with 14 species in one grid-cell. Grid-cells with 12 species each were identified in low western Mexico, high western Mexico, southern Mexico and central–southern Mexico. This last area is characterised by the greatest endemism, including nine species. The formation of the Transmexican Volcanic Belt seems to have been a key element to explain the diversification of North American Tigridieae.


Phytotaxa ◽  
2020 ◽  
Vol 453 (1) ◽  
pp. 31-42
Author(s):  
MARÍA DEL ROSARIO GARCÍA-PEÑA ◽  
JESÚS GUADALUPE GONZÁLEZ-GALLEGOS

Recent botanical explorations in Durango, Mexico, led to the discovery of a new species endemic to this state: Cunila socorroae (Lamiaceae), which is consequently here described and illustrated. The new species is morphologically most similar to C. jaliscana and C. lythrifolia. It can be distinguished from both in having less flowers per cyme, lanceolate floral bracts, longer calyx tube, and lanceolate calyx teeth and longer. It also deviates from C. jaliscana by the fewer floral internodes, longer floral bract, and generally longer corolla tube. Also, the exfoliating bark, white corollas and internally pubescent, make a clear distinction against C. lythrifolia. The distinctive geographic distribution of these species is an additional support to their separation; the new species is exclusive of the middle portion of Sierra Madre Occidental, whereas C. jaliscana is restricted to the northernmost portion of Sierra Madre del Sur, and C. lythrifolia, though mostly occurs in eastern Tans-Mexican Volcanic Belt, has also some localities in southern Chihuahuan Desert, Sierra Madre Oriental and Sierra Madre del Sur.


Phytotaxa ◽  
2018 ◽  
Vol 372 (4) ◽  
pp. 256
Author(s):  
JERZY RZEDOWSKI ◽  
ROSAURA GRETHER

Two new species of Indigofera from central Mexico are described and illustrated. Indigofera sousae, from northwestern Michoacán, is related to I. constricta known in the Mexican states of Sinaloa to Guerrero. Indigofera uniseminalis, from northeastern Guanajuato, is similar to I. sphaerocarpa, reported from southwestern United States and northwestern Mexico, and to I. jaliscensis, of the Sierra Madre Occidental and the Transmexican Volcanic Belt.


2016 ◽  
Vol 29 (6) ◽  
pp. 489 ◽  
Author(s):  
Violeta Corral-Rosas ◽  
Juan J. Morrone

A transition zone shows the overlap between two or more regions and represents an event of biotic hybridisation, where different cenocrons assembled as a result of historical and ecological processes. The Mexican transition zone, the area where the Nearctic and Neotropical regions overlap, includes the following five biogeographical provinces: Sierra Madre Occidental, Sierra Madre Oriental, Sierra Madre del Sur, Transmexican Volcanic Belt and Chiapas Highlands. Within this transition zone, the following five cenocrons have already been recognised: Paleoamerican, Mexican Plateau, Mountain Mesoamerican, Nearctic and Typical Neotropical. We undertook three cladistic biogeographic analyses on the basis of 49 cladograms of terrestrial taxa, partitioning them into three time-slices, namely, Miocene (Mountain Mesoamerican cenocron), Pliocene (Mountain Mesoamerican plus Nearctic cenocrons) and Pleistocene (Mountain Mesoamerican, Nearctic and Typical Neotropical cenocrons). For the Miocene time-slice, we observed a close relationship of the Transmexican Volcanic Belt with the Neotropical region, whereas, for the Pliocene and Pleistocene time-slices, the closest relationship of the Transmexican Volcanic Belt was with the Nearctic region. We conclude that the Transmexican Volcanic Belt may have played a different role according to the cenocron analysed, and that the Mexican transition zone differs in its delimitation depending on the taxa analysed, strengthening the idea that it is a complex area.


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