The carbon cycle model GEOCARBSULF is extended by dividing the weathering of silicates into volcanic and non-volcanic rocks. The proportion of volcanic weathering is calculated as a function of time...
- Science Paper
- Science PaperNew mapping, geochronology, and geochemistry of the supracrustal enclave and associated orthogneisses at Akilia, West Greenland, support a ≥3825 ± 6 Ma age for the sequence and a chemical sedimentary...
- Science PaperThe sedimentary records of the Toarcian oceanic anoxic event display an up to 6 permil negative δ13C excursion in both carbonate and organic matter. One hypothesis to explain this excursion...