Ratification of Neogene subseries as formal units in international chronostratigraphy │ 2022 https://doi.org/10.18814/epiiugs/2022/022008 Leer más artículos Entrada anteriorPaleoenvironmental conditions over the Caribbean Large Igneous Province during the Late Cretaceous in NWof South American Margin: A sedimentological and ichnological approach │ 2022 Siguiente entradaThe relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 También podría gustarte Araceae in a High Andean Forest of the Colombian Occidental Cordillera (Natural National Park Tatamá) │ 2013 20 February, 2020 Morphological analysis of Serpocaulon (Polypodiaceae) spores from the Colombian Central Cordillera │ 2013 20 February, 2020 Climate and geological change as drivers of Mauritiinae palm biogeography │ 2021 24 January, 2022
Araceae in a High Andean Forest of the Colombian Occidental Cordillera (Natural National Park Tatamá) │ 2013 20 February, 2020
Morphological analysis of Serpocaulon (Polypodiaceae) spores from the Colombian Central Cordillera │ 2013 20 February, 2020