Conservation gaps and priorities of range-restricted birds in the Northern Andes. [PDF]
Medina W, Pimm SL, Huang RM.
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Dispersal of Late Triassic clam shrimps across Pangea linking northwestern Gondwana and central Pangea rift basins. [PDF]
Alarcón CM +4 more
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Future glacio-hydrological changes in the Andes: a focus on near-future projections up to 2050. [PDF]
Caro A +4 more
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Ten new species of <i>Selaginella</i> (Lycopodiopsida, Selaginellaceae) from northern South America, primarily Venezuela, with a new status and combination, and distributional updates. [PDF]
Valdespino IA, López CA, Ceballos JI.
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The ants of the genus Rhopalothrix Mayr, 1870 (Hymenoptera, Formicidae, Myrmicinae) in Colombia. [PDF]
Guerrero RJ +5 more
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Chagas Disease: Comparison of Therapy with Nifurtimox and Benznidazole in Indigenous Communities in Colombia. [PDF]
Kann S +7 more
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The savannization of moist forests in the Sierra Nevada de Santa Marta, Colombia
Journal of Biogeography, 1998In the Rio Ranchería watershed of the Sierra Nevada de Santa Marta, between 500 and 1500 m, savanna vegetation is interspersed with moist forests. The savannas are composed of native savanna grasses like Aristida adscensionis L., Arundinella sp., Panicum olyroides Kunth, and Schyzachyrium microstachyum (Desv.) Roseng., Arrill & Izag and the African
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Geologic Evolution of the Sierra Nevada de Santa Marta, Northeastern Colombia
Bulletin of the Geological Society of America, 1974New geologic, petrographic, and radiometric evidence (52 ages) from the Sierra Nevada suggest that plate tectonics controlled the complex Mesozoic evolution of the Caribbean continental margin. The triangular Sierra Nevada massif is bounded by the Oca fault, Santa Marta–Bucaramanga fault, and Cesar lineament. During the Tertiary, dextral and sinistral
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Abstract The Santa Marta Fault System (SMFS) is a NNW-striking major structural feature that controls the western foothills of the Sierra Nevada de Santa Marta (SNSM), the world’s highest coastal relief. Morphotectonically, the SMFS exhibits an arrangement of parallel to subparallel fault traces.
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