A new Permian bivalve-dominated assemblage in the Rio do Rasto Formation, Parana Basin, Brazil: Faunal turnover driven by regional-scale environmental changes in a vast epeiric sea

Author(s)

Simoes, Marcello Guimaraes ^[1] ; Matos, Suzana Aparecida ^[2] ; Anelli, Luiz Eduardo ^[3] ; Rohn, Rosemarie ^[4] ; Warren, Lucas Verissimo ^[4] ; David, Juliana Machado ^[2]

Affiliation

^[1] Univ Estadual Paulista, Inst Biociencias, Dept Zool, BR-18618970 Botucatu, SP - Brazil

^[2] Univ Sao Paulo, Programa Posgrad Geoquim & Geotecton, Inst Geociencias, BR-05508080 Sao Paulo, SP - Brazil

^[3] Univ Sao Paulo, Dept Geol Sedimentar & Ambiental, Inst Geociencias, BR-05508080 Sao Paulo, SP - Brazil

^[4] Univ Estadual Paulista, Dept Geol Aplicada, Inst Geociencias & Ciencias Exatas, BR-13506900 Rio Claro, SP - Brazil

• Document type: Journal article
• Source: Journal of South American Earth Sciences; v. 64, p. 14-26, DEC 2015.
• Web of Science Citations: 10

Abstract

The basal portion of the Permian Rio do Rasto Formation (Serrinha Member), Passa Dois Group, Parana Basin, Brazil, records an entirely new bivalve fauna intercalated between the underlying Pinzonella neotropica assemblage (uppermost portion of the Teresina Formation) and the overlying Leinzia similis assemblage (Rio do Rasto Formation). Mollusks of these assemblages lived in marginal shallow-water habitats of an immense epeiric sea and were dominated by endemic bivalve species. Taxonomic analysis revealed the presence of Terraia curvata (60.61%), Astartellopsis prosoclina (19.70%), Cowperesia emerita (10.61%), Leinzia curta (4.55%), Terraia bipleura (3.03%) and Beurlenella elongatella (1.52%), which are associated with conchostracans and plant remains. Species composition, abundance, and dominance in this novel assemblage differ notably from the preceding ones, suggesting a substantial evolutionary turnover. Regional-scale environmental changes recognized based on taphonomy, facies analysis, and geochemical data consist of progressive freshening of the marginal habitats of the Parana Basin and taxic changes that include the following: (a) loss of genera, (b) decrease in bivalve abundance and ecological guilds, (c) disappearance of the dominant bivalve group (Pinzonellinae) and (d) diversification of Terrainae bivalves. The ecological signature also changed notably because only infaunal suspension-feeding bivalves are present, indicating a significant loss of functional diversity at the regional scale. Likely stressor factors (among others) are tied to freshening events, suggesting profound changes in (a) salinity, (b) primary productivity and (c) a lack of coarse, stable substrates coupled with high bioturbation rates. Hence, our regional example could offer valuable clues to benthic (bivalve) community responses in a habitat subjected to (a) rapid climate changes and (b) freshening events in shallow-water settings. Finally, the stratigraphic range of the dominant species (T curvata) appears to be restricted to the basal portion of the Rio do Rasto Formation. Based on the presence of this species and of C. emerita, the novel assemblage is tentatively correlated with that of the Permian Gal-As Formation in the Huab region of Namibia, thus supporting previous assumptions of a seaway connecting both basins during the Guadalupian Epoch. (C) 2015 Elsevier Ltd. All rights reserved. (AU)

• FAPESP's process: 11/01975-0 - Systematics, paleoecology and bioestratigraphy of the Permian bivalves of the Rio do Rasto (Paraná Basin, Brazil) and Waterford (Karoo basin, South Africa) formations
• Grantee: Juliana Machado David
• Support Opportunities: Scholarships in Brazil - Doctorate