Lower–Middle Ordovician carbon and oxygen isotope chemostratigraphy at Hällekis, Sweden : implications for regional to global correlation and palaeoenvironmental development
A high-resolution chemostratigraphical (coupled δ13Ccarb and δ18Ocarb) study of the topmost Floian through the middle Darriwilian (Ordovician) succession at the Hällekis quarry, Kinnekulle, southern Sweden, shows relatively steady isotopic values with overall minor changes, although some notable short- and long-term shifts are discernible. A pronounced positive shift in δ13C in the uppermost part