Taphonomic and paleoenvironmental considerations for the concentrations of macroinvertibrate fossils in the Romualdo Member, Santana Formation, Late Aptian – Early Albian, Araripe Basin, Araripina, NE, Brazil

• Published in: Journal of South American earth sciences Vol. 62; pp. 218 - 228
• Main Authors: Prado, Ludmila Alves Cadeira Do, Pereira, Priscilla Albuquerque, Sales, Alexandre Magno Feitosa, Barreto, Alcina Magnólia Franca
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-10-2015
• Subjects: Early Cretaceous; Echinoids; Marine transgression; Molluscs; Storms; Taphofacies; Marine transgression; Taphofacies; Molluscs; Storms; Echinoids; Early Cretaceous
• ISSN: 0895-9811; 1873-0647
• DOI: 10.1016/j.jsames.2015.06.005

Benthic macroinvertebrate fossils can be seen towards to the top of the Romualdo Member of the Santana Formation, in the Araripe Basin, Northeast Brazil, and can provide paleoenvironmental and paleobiogeographical information regarding the Cretaceous marine transgression which reached the interior basins in Northeast Brazil. We analyse taphonomic characteristics of macroinvertebrate concentrations of two outcrops (Torrinha and Torre Grande) within the municipality Araripina, Pernambuco, in order to enhance our understanding of the Cretaceous paleoenvironment in the western portion of the Araripe Basin. At the outcrop Torrinha, proximal tempestitic taphofacies were identified. These predominantly consist of ceritid, cassiopid, and later, naticid gastropods as well as undetermined bivalves. Given this lack of variability it can be deduced that there were no significant paleoenvironmental changes during the successive stages tempestitic sedimentation. In the Torre Grande outcrop distal to proximal tempestitic taphofacies were identified from the base to the top respectively pointing to a decrease in paleodepth. Asides from the macroinvertebrates present in Torrinha, there are also echinoids – unequivocal evidence for marine conditions. These occurrences appear to be restricted to Romualdo Member outcrops in the Araripina municipality (the Southeast portion of the Araripe Basin) confirming a previously published hypothesis suggesting that the Cretaceous marine transgression originated from the neighbouring Parnaíba Basin to the west. This study identified marine molluscs of a similar age to those in the Romualdo Member's equivalent rock units in the Parnaíba and Sergipe-Alagoas (SE-AL) basins suggesting a marine connection between these basins and the Araripe Basin during the Early Cretaceous.
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•The identification of marine molluscs and echinoids attest to marine sedimentation.•Macroinvertebrates were deposited during storms.•Our data support the hypothesis of a marine ingression from the Parnaíba Basin.•The Parnaíba, Araripe and SE-AL basins were connected by an inland sea-way.