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How distinctive are flood-triggered turbidity currents?

Catharina J. Heerema; Matthieu J.B. Cartigny; Ricardo Silva Jacinto; Stephen M. Simmons; Ronan Apprioual; Peter J. Talling
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Paleoenvironmental insights from the deposition and diagenesis of Aptian pre-salt magnesium silicates from the Lula Field, Santos Basin, Brazil

Nívea G. Carramal; Daniel M. Oliveira; Alessandra S.M. Cacela; Matheus A.A. Cuglieri; Natasha P. Rocha; Samuel M. Viana; Sérgio L.V. Toledo; Saulo Pedrinha; Luiz F. de Ros
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The late Miocene eolian record at the eastern margin of the Puna Plateau, NW Argentina: Evidence of upper-tropospheric paleocirculation

Jonathan Ledesma; Cecilia E. Del Papa; Patricio Payrola
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Oyster shells, bulk carbonate sediment, and meteoric calcite cement as recorders of oceanic and radiogenic 87Sr/86Sr in mixed heterozoan carbonates and terrigenous sediment

Gunnar Sælen; Juan Carlos Braga; Fernando Sola
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    COVER EXPLANATION.—Proximal deposits from dilute pyroclastic currents from the Ramadas Eruptive Unit (∼ 6.4 Ma) that seal the eolian deposits from the Corte Blanco Member, San Antonio de los Cobres Formation. See Ledesma et al., this issue.

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