Carbonate-shelf evolution during the Oligocene to early Miocene: insights from shelf architecture, lithofacies, and depositional models of the Kujung Formation, offshore East Java, Indone...
The Phycosiphon Ichnofacies and the Rosselia Ichnofacies: Two new ichnofacies for marine deltaic environments
Microstructure and mineral composition of Holocene stromatolites from Lagoa Vermelha, a hypersaline lagoon in Brazil: Insights into laminae genesis
Geochemical markers of paleoenvironments, weathering, and provenance in Permian–Triassic terrestrial sediments
Late Paleozoic Ice-Age rhythmites in the southernmost Paraná Basin: A sedimentological and paleoenvironmental analysis
COVER EXPLANATION.—Schematic split-core diagram expressing the transition of ichnofacies in response to fluvial-sediment influx into a fully marine, wave-dominated environment. The succession records a muddy shelf passing into the prodelta, progressively overlain by the delta front, distributary channel-mouthbar complex, and lower delta plain during progradation of a mixed river- and wave-influenced delta (see MacEachern and Bann, this issue).
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