2000
DOI: 10.1016/s0895-9811(00)00048-1
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First record of oligocene conchostracans (Tremembé formation, Taubaté Basin) from São Paulo, Brazil

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Cited by 12 publications
(14 citation statements)
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“…Sample 8 dates from the Cretaceous period ( ca . 85 Ma), and samples 9 and 10 are from the Oligo‐Miocene period (23 Ma, Gallego and Mesquita ). Sample 10 was analysed by ICP‐OES to obtain complementary quantitative data for selected elements.…”
Section: Methodsmentioning
confidence: 99%
“…Sample 8 dates from the Cretaceous period ( ca . 85 Ma), and samples 9 and 10 are from the Oligo‐Miocene period (23 Ma, Gallego and Mesquita ). Sample 10 was analysed by ICP‐OES to obtain complementary quantitative data for selected elements.…”
Section: Methodsmentioning
confidence: 99%
“…The world record of Cenozoic fossil spinicaudatans is limited to only a few countries: China, with many localities ranging from the late Palaeocene to the early Eocene (Hong et al . 1974; Chen 1975; Chen & Shen 1979, 1980, 1981, 1985; Shen & Chen 1979; Shen & Zhang 1979); Mongolia (late Palaeocene to early Eocene: Trusova & Badamgarav 1976); Brazil (Oligocene: Gallego & Mesquita 2000); Argentina (late Palaeocene and Miocene–Pliocene: Gallego & Mesquita 2000; Petrulevicius 2001) and North America (Eocene: Shen et al . 2006; early Oligocene: Stigall et al 2017) (see Table 1).…”
Section: Spinicaudatamentioning
confidence: 99%
“…In South America there are three ‘conchostracan'-bearing formations. Tremembeglypta saadi Gallego (in Gallego & Mesquita 2000) has been reported from the Oligocene Tremembé Formation of the Taubaté Group, São Paulo State, Brazil. Petrulevicius (2001) mentioned ‘conchostracans' ( Euestheria ?)…”
Section: Cenozoic ‘Conchostracan' Distributionmentioning
confidence: 99%
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“…On the other hand, Martins- Neto (1989) claims that the presence of larvae of Trichoptera, and palemonid crustaceans are evidences that the waters of the Tremembé Paleolake were not stagnant. Gallego & Mesquita (2000) ascribe the low diversity and abundance of conchostracans in the Tremembé Formation either to the predatory pressure by fishes, or to environmental restrictions in chemical parameters. Due to their sensitiveness to ecological parameters at the water-sediment interface, and high fossilization potential, ostracods provide invaluable data for paleoenvironmental reconstruction of lacustrine environments.…”
Section: Paleolimnological Remarksmentioning
confidence: 99%