“…The initial interval, previously identi ed in several studies 40,47,48 , is attributed to distinctly continental sources, serving as a signi cant geochemical indicator supporting the interpretation of the carbonate succession as having a lacustrine origin in the Campos and Santos basins. Despite the limited understanding of the paleo-tectonic context, the notable variability in the strontium isotope signal indicates a depositional system in uenced by a range of sources, including continental cratonic rocks and contemporaneous basaltic volcanism as potential contributors 37,49 . The second interval, however, exhibits notably reduced radiogenic Sr values, predominantly around 0.709, indicating a distinct decrease in radiogenic sources entering the basin.…”