The multidisciplinary analysis of a profile discovered by the winter storms on the coast of the Donana National Park has allowed us to reconstruct the evolution of its western sector during the Late Holocene. Three phases have been defined, which reflect the transition from a brackish water marsh (FA-1) to a freshwater lagoon transformed into peat bog (FA-2), to end with the deposit of dune systems (FA-3).
1.Univ Atacama, Copayapu 485, Copiapo, Chile 2.Univ Huelva, Dept Ciencias Integradas, Avda Tres de Marzo S-N, Huelva 21071, Spain 3.Univ Huelva, Dept Ciencias Tierra, Avda Tres de Marzo S-N, Huelva 21071, Spain 4.Univ Lisbon, Inst Super Tecn, C2TN, P-2695066 Bobadela, Portugal 5.Univ Seville, Dept Cristalog Mineral & Quim Agr, C Prof Garcia Gonzalez 1, E-41012 Seville, Spain 6.Univ Autonoma Madrid, Dept Geol & Geoquim, E-28049 Madrid, Spain 7.Univ Huelva, CIPHCN, Fac Humanidades, Avda Tres Marzo S-N, Huelva 21071, Spain
Recommended Citation:
Abad, M.,Munoz, A. F.,Gonzalez-Regalado, M. L.,et al. Palaeoenviromental evolution of a Late Holocene peat bog in the southwestern sector of the Donana National Park (SW Spain)[J]. ESTUDIOS GEOLOGICOS-MADRID,2019-01-01,75(1)