In: Journal of Paleolimnology, 2015, vol. 53, no. 2, p. 233-250
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In: Aquatic Sciences, 2015, vol. 77, no. 4, p. 535-545
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In: International Journal of Earth Sciences, 2015, vol. 104, no. 6, p. 1655-1665
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In: Earth and Planetary Science Letters, 2020, vol. 545, p. 116390
Due to their large heat and moisture storage capabilities, the tropics are fundamental in modulating both regional and global climate. Furthermore, their thermal response during past extreme warming periods, such as super interglacials, is not fully resolved. In this regard, we present high-resolution (analytical) foraminiferal geochemical (δ18O and Mg/Ca) records for the last 1800 kyr from...
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In: Geobiology, 2020, vol. 18, no. 2, p. 185–206
Cold‐water coral (CWC) mounds are build‐ups comprised of coral‐dominated intervals alternating with a mixed carbonate‐siliciclastic matrix. At some locations, CWC mounds are influenced by methane seepage, but the impact of methane on CWC mounds is poorly understood. To constrain the potential impact of methane on CWC mound growth, lipid biomarker investigations were combined with...
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In: Aquatic Sciences, 2014, vol. 76, no. 1, p. 101-114
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In: International Journal of Earth Sciences, 2018, vol. 107, no. 8, p. 2907–2929
Pockmarks in Pliocene-Quaternary continental slope deposits offshore Angola show features related to: (1) fluid leakage craters that formed repeatedly, (2) authigenic methane-derived carbonates that indicate the (former) presence of hydrocarbons and (3) erosional–depositional structures that are clearly related to current activity. Depending on topography, the pockmarks show differing...
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In: Swiss Journal of Geosciences, 2008, vol. 101, no. 1, p. 99-106
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In: Swiss Journal of Geosciences, 2010, vol. 103, no. 1, p. 101-119
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In: Contributions to Mineralogy and Petrology, 2012, vol. 163, no. 6, p. 1083-1102
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