Yosmel Sanchez-Hernandez scite author profile

C of ~5‰). However, a low enrichment of redox-sensitive trace elements indicates that the basin did not achieve anoxic conditions. The results also suggest that a shallower-phase of the basin, coeval with platform progradation, may have increased ventilation of the basin at the same time that heightened sedimentation rates and additional input of organic matter from terrestrial sources increased the burial and preservation rate of TOC in the sediment.

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A Consistent Carbon Isotope Trend as a Potential Tool to Reduce Biostratigraphic Uncertainties at the Barremian – Aptian Boundary

Maurrasse¹,

Sanchez-Hernandez²

2016

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Yosmel Sanchez-Hernandez

The influence of regional factors in the expression of oceanic anoxic event 1a (OAE1a) in the semi-restricted Organyà Basin, south-central Pyrenees, Spain

Geochemical characterization and redox signals from the latest Barremian to the earliest Aptian in a restricted marine basin: El Pui section, Organyà Basin, south-central Pyrenees

Assessing the factors controlling high sedimentation rates from the latest Barremian–earliest Aptian in the hemipelagic setting of the restricted Organyà Basin, NE Spain

Characterization of the negative carbon isotope shift in segment C2, its global implications as a harbinger of OAE1a

Paleoenvironments and Geochemical Signals from the Late Barremian to the Middle Aptian in a Tethyan Marginal Basin, Northeast Spain: Implications for Carbon Sequestration in Restricted Basins

A Consistent Carbon Isotope Trend as a Potential Tool to Reduce Biostratigraphic Uncertainties at the Barremian – Aptian Boundary

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