Biodiversity, Ecosystems, and Conservation in Northern by Jean-Luc E. Cartron, Gerardo Ceballos, Richard Stephen

By Jean-Luc E. Cartron, Gerardo Ceballos, Richard Stephen Felger

This publication describes the biodiversity and biogeography of nothern Mexico, records the organic significance of local ecosystems and the affects of human land use at the conservation prestige of vegetation and natural world. it may turn into the traditional resource record for the conservation prestige of species and ecosystems during this area, that's of bizarre organic curiosity due to its excessive biodiversity and hugely various panorama and organic zonation.

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These span nearly the entire length of the peninsula. In Baja California Sur the ranges are narrower, allowing enough space westward for a broad lowland, the Pacific Coastal Plain (<200 masl), which is widest where it forms the Vizcaíno Desert. The Peninsular Ranges and Pacific Coastal Plain make up the first two subprovinces of the peninsula (fig. 7). The Peninsular Ranges end by Bahía de La Paz, giving way southward to the La Paz–Los Cabos (Range and Upland) Subprovince. Geologic Aspect The geologic features of the northern and southern halves of the peninsula are quite different, so we describe them separately (fig.

Significant tectonic rearrangement during the Cenozoic has occurred only on the adjacent Pacific Ocean floor, involving subduction (of the Farallon Plate) and detachment of the Baja California peninsula by deep transform faults, thereby originating the Gulf of California (Ortlieb 1991a,b; Ferrari 1995; Henry and Aranda-Gómez 2000; Fletcher et al. 2003). (2) This extensional deformation seems to be genetically related to the magmatism that originated the Sierra Madre Occidental volcanic field and to the associated plutonic and volcanic bodies, which chiefly occurred in the Late Paleogene (ca.

This sector then chiefly lies east–west (i. , transverse to the Eastern Sector [hence the name]), between 24°30'–26°00' N and 100°00'–105°00' W; its area is about 68,000 km2, and it is 400 km long and 120 km wide (average). Elevation varies from 200 to slightly higher than 3000 masl, but with an uneven distribution; the 1000–2000 masl hypsometric zone is dominant. 1), 22 Historical, Geographical, and Legal Setting whereas the Transverse Sector’s climate is dominantly BWh desertic. The humid eastern slope of the Sierra Madre’s Eastern Sector is the one that has rivers.

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