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Geochemical evidence from the Givetian–Frasnian stages indicates photic zone euxinia persisted on both the Lennard Shelf and Barbwire Terrace margins of the Fitzroy Trough. This research dataset, published in Marine and Petroleum Geology in 2018, analyzes biomarker assemblages like hopanes, steranes, and carotenoids to correlate oils with potential source rocks. It provides insights into the conditions for organic-rich shale deposition and petroleum generation in a confined Late Devonian basin.
The dataset appears to be the underlying data for a specific 2018 journal article; primary data may not be in a standard machine-readable format like CSV. License information is not provided.