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 Aquatic ecosystems in a newly formed ecospace: Early Pliocene lakes in the Central Andean Altiplano │ 2018 21 February, 2020 Paleoclimatic and paleoecological reconstruction of a middle to late Eocene South American tropical dry forest │ 2021 27 January, 2022 Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022
Aquatic ecosystems in a newly formed ecospace: Early Pliocene lakes in the Central Andean Altiplano │ 2018 21 February, 2020
Paleoclimatic and paleoecological reconstruction of a middle to late Eocene South American tropical dry forest │ 2021 27 January, 2022
Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022