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Article
Open AccessShallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
The Palaeocene–Eocene Thermal Maximum (PETM) was a global warming event of 5–6 °C around 56 million years ago caused by input of carbon into the ocean and atmosphere. Hydrothermal venting of greenhouse gases p...
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Article
Open AccessMeltwater sediment transport as the dominating process in mid-latitude trough mouth fan formation
Trough mouth fans comprise the largest sediment deposits along glaciated margins, and record Pleistocene climate changes on a multi-decadal time scale. Here we present a model for the formation of the North Se...
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Article
Open AccessAuthor Correction: Glacigenic sedimentation pulses triggered post-glacial gas hydrate dissociation
The original version of this Article contained an error in the second sentence of the Abstract, which incorrectly read ‘They are stable under high pressure and low, but react sensitively to environmental chang...
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Article
Open AccessGlacigenic sedimentation pulses triggered post-glacial gas hydrate dissociation
Large amounts of methane are stored in continental margins as gas hydrates. They are stable under high pressure and low temperature, but react sensitively to environmental changes. Bottom water temperature and...
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Chapter
Erratum to: Sub-volcanic Intrusions in the Karoo Basin, South Africa
The chapter was inadvertently published without updating Table 1. The erratum chapter has been updated with the change.
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Article
Open AccessConstraining shifts in North Atlantic plate motions during the Palaeocene by U-Pb dating of Svalbard tephra layers
Radioisotopic dating of volcanic minerals is a powerful method for establishing absolute time constraints in sedimentary basins, which improves our understanding of the chronostratigraphy and evolution of basi...
