Carbon isotope chemostratigraphy of the Late Silurian Lau Event, Gotland, Sweden
The positive δ13C excursion associated with the Late Silurian Lau Event (approximately 420 Ma) is recognized globally and considered to be one of the most prominent carbon isotope excursions of the Phanerozoic. Its maximum values are exceeded only by values from the Proterozoic. Over the last years the Lau Event has been studied in great detail on the island of Gotland, Sweden (Baltica palaeoconti
