The formation is the richest Cenozoic fossiliferous formation of Brazil, leading to the establishment of the Parque Paleontológico de São José de Itaboraí ("São José de Itaboraí Paleontological Park") in 1995. The site is a candidate for becoming a UNESCOWorld Heritage Site.
The word "Itaboraí" is of Tupi origin, and has two possible etymologies:
"River of beautiful stones", a combination of the words itá (stone), porã (beautiful) and y (river)[3]
"River of brilliant stones", derived from the words itá (stone), berab (brilliant) and y (river)[4]
The Itaboraí Formation is restricted to the Itaboraí Basin, a minibasin stretching across an area of 1 square kilometre (0.39sqmi) of 1,400 by 500 metres (4,600ft ×1,600ft), in the vicinity of Itaboraí34 kilometres (21mi) northeast of Rio de Janeiro, southeastern Brazil.[5] Between 1933 and 1984, a local cement company exploited the rocks in the area and their workers discovered the first fossil remains in the formation.[6] The now abandoned and largely inaccessible limestone quarries of this locality have yielded a diverse mammalian fauna from early late Paleocene fissure fillings.[7] The sediments of the formation were described by Leinz in 1938.[8] Presently, the basin is filled up with water impeding any collecting activity.[9]
Basin history
The small basin, a small half-graben, is the oldest[10] and smallest[11] of several Cenozoicrift basins stretching across 1,000 kilometres (620mi) along a west-southwest to east-northeast trend between the Paraná Basin to the northwest and the Santos Basin to the southeast, separated by the Serra da Mantiqueira and Serra do Mar respectively. This Continental Rift of Southern Brazil (CRSB) comprises the Curitiba, São Paulo, Taubaté, Resende, Volta Redonda, Macacu, Barra de São João and Itaboraí Basins.[12]
An erosional surface, correlated with a 55 Ma sea-level lowstand representing the Paleocene-Eocene transition and associated with magmatism, has been recorded in the various Atlantic marginal basins along the Brazilian coast; Pelotas, Santos, Campos, Espírito Santo, Cumuruxatiba, Jequitinhonha and Mucuri Basins.[13]
Stratigraphy
The Itaboraí Formation rests unconformably on top of the PrecambrianParaíba do Sul Group, part of the Meso- to NeoproterozoicParaíba do Sul Complex.[14] The Paleogene succession of the minibasin reaches a thickness of 100 metres (330ft) and consists of three depositional sequences, with the Itaboraí Formation representing the first two;[15]
Sequence 1 (S1) - clastic limestones with travertine, grey carbonates and oolitic limestones, carbonatic shales and lignites, deposited in a lacustrineenvironment, originating from debris flows in a tectonic lake. From this sequence gastropods are abundant, while woods, reptiles and mammals are scarce.[11]
Sequence 2 (S2) - carbonates filling caverns and dissolution cracks on a karstic surface of Sequence 1, comprising fossiliferous marls, deposited in an alluvial to lacustrine environment, transported into these cavities by heavy rains and gravitational flows[11]
Sequence 3 (S3) - terrestrial siliciclastic sediments, including mudstones, sandstones and sandy conglomerates of Late Eocene to Early Oligocene age, derived from the surrounding basement gneisses, deposited by mudflows in a subaerial alluvial fan environment. These sediments, referred to as the Rio Frio Formation,[1] have been correlated with the Eocene to Oligocene Resende Formation of the eponymous basin.[13]
Thin section analysis suggests the travertine sequence went through a series of diagenetic processes: firstly, the deposition of the primary carbonate, followed by a set of percolating iron oxide enriched fluids and lastly a set of silica-rich fluids leading to the silica chalcedony and micro-crystalline deposition.[17]
Age
The Itaboraí Formation, defining the Itaboraian SALMA, was first thought to be early to mid Paleocene in age, until dating performed by Woodburne et al. in 2014 suggested as a more probable early Eocene age (53–50 Ma),[18][19] spanning polarity chron 23.[20] The overlying basalts have been dated to the Early Eocene (52.6 ± 2.4 Ma). Another very important source of data is palynological analysis of a coal-bearing horizon (lignite) interlayered with alluvial fan deposits at the northern border of the Itaboraí Basin, suggesting a Paleocene to Eocene age.[21] During this time, a biogeographical connection existed with Antarctica and, though separated by the developing South Atlantic, with Africa.[22] The deposits of the formation were formed during the Early Eocene Climatic Optimum (EECO), just after the Paleocene-Eocene Thermal Maximum.[23]
Despite its relatively small size, the São José de Itaboraí Basin comprises a diversified fossil assemblage. Among the groups found there, fossil birds are very rare, mainly due to their pneumatized bones. Only three bird species have been described up to this moment from the Itaboraí Basin. Diogenornis fragilis, a probable ratite ancestor, stands out for its good preservation and the number of specimens preserved.[25] In the Paleocene of the southern hemisphere, small terrestrial birds have only been discovered in the late Paleocene fissure fillings of the Itaboraí Formation.[7]
The relative fossil diversity of the Itaboraí Formation at family level consists of 44% mammals, 23% mollusks, 14% reptiles (lizards, chelonians, crocodyliforms), 7% birds, 5% amphibians and 7%
plants.[26] Fish are one of the few groups not found to date in the lacustrine formation.[27] The formation has provided many marsupials and related metatherians. The species Lamegoia conodonta is the largest "condylarth" at Itaboraí and approximates the size of a wolf. Ricardocifellia protocenica, originally described as Paulacoutoia protocenica, is the smallest of the "condylarth" species of Itaboraí, but the most abundant.[28] The most abundant litoptern found in the formation is Protolipterna ellipsodontoides.[29]
Because of its paleontological importance, the Itaboraí Basin area was designated as a paleontological park in 1995: Parque Paleontológico de São José de Itaboraí ("São José de Itaboraí Paleontological Park").[31] The park was established to preserve the geology and highlight the importance of the paleontological richness of the area.[32]
Castro, Luis Otavio R.; García-López, Daniel A.; Bergqvist, Lilian P.; Araújo-Júnior, Hermínio I. (2021), "A New Basal Notoungulate from the Itaboraí Basin (Paleogene) of Brazil", Ameghiniana, 58 (3): 272–288, doi:10.5710/AMGH.05.02.2021.3387
De Taranto, R.C.; Loguercio, M.F.; Bergqvist, L.P.; Rocha Barbosa, O. (2011), "Comparative analysis of the hindlimb morphology of Diogenornis fragilis (Aves, Ratites - Paleocene) and flightless extant and extinct birds", Ameghiniana, 48: R58