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Reply: Biogenic structures of unioniform bivalves in wet-interdune deposits (late miocene-warly pliocene, Argentina)
(Society for Sedimentary Geology (SEPM), 2019)
Reply: Biogenic structures of unioniform bivalves in wet-interdune deposits (Late Miocene-Early Pliocene, Argentina)
(Society for Sedimentary Geology, 2019-03)
The Discussion of our paper by Martínez is very welcome because it supports our finding that bivalves may colonize wet-interdune settings and thus, trace fossils produced by them may record environmental changes—this is ...
Biogenic structures of unioniform bivalves in wet-interdune deposits (Late Miocene-early Pliocene, Argentina)
(Society for Sedimentary Geology, 2018-09)
Environmental changes within a Neogene coastal dune system are recorded by endobenthic unioniform bivalves that lived in muddy or sandy interdune pond sediments. These bivalves were suspension-filter feeders that formed ...
Intermontane Eolian Sand Sheet Development, Upper Tulum Valley, Central-western Argentina
(SOC BRASILEIRA GEOLOGIASAO PAULO, 2015)
Fácies e associação de fácies da Formação Piramboia na região de Descalvado (SP)
(2015-12-01)
The Piramboia Formation is a lithostratigraphic unit of the Paraná Basin that has been the focus of several studies due to its great importance as an essential component in the Guarani Aquifer System and the Irati-Piramboia ...
Internal anatomy of an erg sequence from the aeolian-fluvial system of the De La Cuesta Formation (Paganzo Basin, northwestern Argentina)
(Universidad de Barcelona, 2010-12)
Permian red beds of the De La Cuesta Formation in the Sierra de Narváez (Paganzo Basin, northwestern Argentina) are essentially composed of sandstones associated with mudstones and subordinate conglomerates. Facies ...
Facies, Facies Association and Depositional Model of Eolian Sandstones - Botucatu Formation (Lower Cretaceous) in Southern Santa Catarina State, BrazilFácies, Associação de Fácies e Modelo Deposicional dos Arenitos Eólios da Formação Botucatu (Cretáceo Inferior) na Região Sul de Santa Catarina
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 2000)