Carbonate REE + Y signatures from the restricted early marine phase of South Atlantic Ocean (late Aptian – Albian) : The influence of early anoxic diagenesis on shale-normalized REE + Y patterns of ancient carbonate rocks
Sergio Caetano-Filho, Gustavo M. Paula-Santos, Dimas Dias-Brito
ARTIGO
Inglês
Agradecimentos: This study was supported by the project “Carbonate rocks of Brazil”, a partnership between São Paulo State University (UNESP) and PETROBRAS (grant #0050.0051732.09.9 Petrobras/Unesp/Fundunesp). The first author currently holds a São Paulo Research Foundat
Rare earth elements plus yttrium have been extensively applied in paleoenvironmental studies of ancient carbonate successions due to their fractionation in the marine environment. However, in modern marine anoxic environments, seawater REE + Y signatures
FUNDAÇÃO DE AMPARO À PESQUISA DO ESTADO DE SÃO PAULO - FAPESP
2016/11496-5
fechado
Carbonate REE + Y signatures from the restricted early marine phase of South Atlantic Ocean (late Aptian – Albian) : The influence of early anoxic diagenesis on shale-normalized REE + Y patterns of ancient carbonate rocks
Sergio Caetano-Filho, Gustavo M. Paula-Santos, Dimas Dias-Brito
Carbonate REE + Y signatures from the restricted early marine phase of South Atlantic Ocean (late Aptian – Albian) : The influence of early anoxic diagenesis on shale-normalized REE + Y patterns of ancient carbonate rocks
Sergio Caetano-Filho, Gustavo M. Paula-Santos, Dimas Dias-Brito
Fontes
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Palaeogeography, palaeoclimatology, palaeoecology (Fonte avulsa) |