Central America 2007
DOI: 10.1201/9780203947043.ch13
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Stratigraphy and geologic history

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Cited by 3 publications
(4 citation statements)
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“…The present-day MCKB, developed within the Paleogene carbonates of the Buena Vista Formation, lies near the northern edge of the Mesozoic-Cenozoic North Petén sedimentary basin. As mapped by Dengo, the Petén Basin of Guatemala covers a region of 110,000 km 2 and is bounded by the Chiapas massif to the west, the Polochic Fault to the South, the Maya Mountains to the east, and thins to the north over the Yucatán Platform [ 71 ]. The basin initially developed in the Late Jurassic as a rift basin evolving during the Early Cretaceous into a shallow marine basin.…”
Section: Regional Settingmentioning
confidence: 99%
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“…The present-day MCKB, developed within the Paleogene carbonates of the Buena Vista Formation, lies near the northern edge of the Mesozoic-Cenozoic North Petén sedimentary basin. As mapped by Dengo, the Petén Basin of Guatemala covers a region of 110,000 km 2 and is bounded by the Chiapas massif to the west, the Polochic Fault to the South, the Maya Mountains to the east, and thins to the north over the Yucatán Platform [ 71 ]. The basin initially developed in the Late Jurassic as a rift basin evolving during the Early Cretaceous into a shallow marine basin.…”
Section: Regional Settingmentioning
confidence: 99%
“…The La Libertad Arch separates the basin into the North Petén and South Petén sub-basins. More thorough descriptions of the structural history of northern Guatemala, the formation of the Petén Basin, and its stratigraphic fill have previously been published [ 6 , 67 , 71 73 ]. Exposed over much of the Guatemalan portion of the PP is the Buena Vista Formation, loosely correlative with the Icaiché Formation to the north.…”
Section: Regional Settingmentioning
confidence: 99%
“…A typical phenomenon observed in Costa Rica is that many closely related species pairs occur on the Caribbean and the Pacific sides (Kohlmann & Wilkinson 2007). This vicariant speciation pattern seems to be mediated by the slow emergence of the Talamanca range (Alvarado et al 2007, Hoernle et al 2008, which has divided the original continuous tropical forest into two separate areas; one on the Caribbean slope, the other on the Pacific slope (Kohlmann & Wilkinson 2007). This phenomenon has not been detected just in dung beetles (Kohlmann & Solís 1997, 2001a, 2001bKohlmann & Wilkinson 2007); many cases have also been reported for fishes, amphibians, reptiles, and birds (Fogden & Fogden 1997, Kohlmann & Wilkinson 2007.…”
Section: Taxonomic Considerationsmentioning
confidence: 99%
“…Finally, it seems that the diversification of Ramiellona has occurred mainly in the mountains of Guatemala, El Salvador and the southern Mexican state of Chiapas, where volcanic activity has been constant since the early Oligocene, ca. 32 Ma ago (Alvarado et al 2007). How much of the isolation and differentiation between species and populations has been due to the orographic changes occurred during the formation of these mountain systems, is something that should be investigated in the next years.…”
Section: Introductionmentioning
confidence: 99%