The morphology and systematics of the clam shrimp Platyestheria gen. nov. abaetensis (Cardoso) (Crustacea, Spinicaudata) from the Lower Cretaceous of the Sanfranciscana Basin, southeast Brazil

Abstract

New specimens of the clam shrimp 'Pseudestheria' abaetensis Cardoso, 1971 (Spinicaudata) are described. The material was collected from the Quiric o Formation (Lower Cretaceous of the Sanfranciscana Basin), at the same locality as the type series of the species. The carapaces are very large, oval and elongated, with anteriorly located and slightly projected umbo, straight dorsal margin, with flattened growth bands and 15e20 serrated growth lines. Details of the microscopic structure of the carapace were analysed under scanning electron microscope for the first time, disclosing a unique reticular pattern of ornamentation. This species is similar to some Early Cretaceous taxa from South America, Africa and China. Yet, the peculiarities in the shape and ornamentation of the carapace support its reassignment to a new genus (Platyestheria gen. nov.), within the Superfamily Eosestherioidea. In addition, an energy-dispersive X-ray spectroscopy analysis of the multiple stacked growth bands revealed that the valves are enriched in calcium and phosphorus, similar to those of modern spinicaudatans. Minor amounts of silicon, iron and aluminium suggest that the carapaces were preserved partly through the input of ions from the environment during the diagenesis.

Preliminary Report on the Lacustrine Strata of the Sanfranciscana Basin in Northern Minas Gerais, Brazil

“….J.S. Bittencourt et al / Geonomos, 27(1), 1-10, 2019 www.igc.ufmg.br/geonomos The geological and paleontological research in the Sanfranciscana Basin is increasing in the last few years (Bi encourt et al, 2015(Bi encourt et al, , 2017(Bi encourt et al, , 2018Mescolo , 2015Mescolo , , 2017Carvalho & Santucci, 2018;Leite et al, 2018). Yet, the outcrops in northern Minas Gerais are less studied than those in southern locali es.…”

“…The Areado Group is especially no ceable due to its fossil record. The paleobiota of the Quiricó Forma on includes so far charophytes, con nental palynomorphs, g y m n o s p e r m s a n d a n g i o s p e r m s , o s t r a c o d s , ' c o n c h o s t r a c a n s ' , i n s e c t s , e l a s m o b r a n c h s , ac nopterygians, the coelacanthiform Mawsonia and dinosaurs (Scorza & Silva Santos, 1955;Barbosa, 1965;Cardoso, 1971;Santos, 1971;Lima, 1979;Silva Santos, 1985;Mar ns-Neto, 1996;Duarte, 1997;Carvalho & Ka ah, 1998;do Carmo et al, 2004;Carvalho & Maisey, 2008;Zaher et al, 2011;Bi encourt et al, 2015Bi encourt et al, , 2018Carvalho & Santucci, 2018;Leite et al, 2018). Fossils recovered from the Três Barras Forma on include enigma c marine microfossils, notably radiolarians, in very restricted horizons (Ka ah & Koutsoukos, 1992;Pessagno Jr. & Dias-Brito, 1996;Dias-Brito et al, 1999), and dinosaur footprints (Carvalho & Ka ah, 1998).…”