The Riachuelo Formation is a geologic formation of the Early to Late Cretaceous (Late Aptian to Cenomanian) age in northeastern Brazil's Sergipe-Alagoas Basin. It is the first Formation of the Basin to contain sediments deposited under fully marine conditions. The formation is subdivided into three members: Angico, Taquari and Maruim.[1]
There are three members of this formation: Angico Member, whose environment has been interpreted as costal areas consisting of the basin margins and grabens, deltaic fans formed, and the coarse sediments they carried, the Maruim Member, in the lower sedimentation areas, with carbonate ramps and dolomitized oolite/oncolite banks deposited under fluctuating sea level conditions, and the Taquari Member, corresponding to calcareous mudstone and shale from lagoonal and slope environments.[5][11]
Ammonites are particularly plentiful and have provided a firm biocronostratigraphic control for the basin. The succession of ammonites is divided in five zones: The Epicheloniceras-Diadochoceras-Eodouvilleiceras zone, from the Aptian, the Douvilleiceras zone, from the lower Albian, the Oxytropidoceras zone, from the middle Albian, and the Elobiceras and Mortoniceras-Neokentroceras zones, both from the late Albian.[1]
History
The name Riachuelo Formation was used for the first time in the geological literature by Moraes Rego in 1929. Then, in 1959, Bender made a new interpretation, separating the upper part of the Riachuelo Formation from the lower one, naming it Maruim. This lower unit described by Bender was considered by Beurlen K. in 1963 as only one facies of the Riachuelo-Maruim Complex. In 1970, Schaller analyzed the unit again and segmenting it into four members: Angico, Taquari, Maruim and Aguilhada. Feijó, in 1994, classified the formation as a siliciclastic-carbonatic platform complex and divided it into the members: Angico, Taquari and Maruim, which is the classification currently used.[4]
^ abMANSO, C. L. de C.; SOUZA-LIMA, Wagner (2012). "NOVOS EQUINÓIDES PARA O INTERVALO APTIANO-ALBIANO (CRETÁCEO INFERIOR) DA SUB-BACIA DE SERGIPE, NORDESTE DO BRASIL". Geociências. 31 (4): 584–605.
^ abda Silva, C. R. M.; Barros, S. D. S. (2017). "AVALIAÇÃO DO POTENCIAL DE FOSFATO NO BRASIL – PARTE III: BACIA SERGIPE-ALAGOAS, ÁREA SUB-BACIA SERGIPE ESTADO DE SERGIPE". Serviço Geológico do Brasil (20).
^ abcdBeurlen, G. (1967). "Ammonoidea do complexo Riachuelo-Maruim, Sergipe". Boletim da Sociedade Brasileira de Geologia. 16 (2): 79–106.