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M A N U S C R I P T A C C E P T E D ACCEPTED MANUSCRIPTShelf morphology worked as an indicator of these changes. Carbonate/terrigenous 59 deposition during a highstand/regressive phase coeval along the eastern Brazilian shelf, 60 either laterally and across shelf. This lateral/along coast variation in sediment supply 61 and carbonate production leads to distinct lateral facies and geometry. These spatial 62 changes in morphology and facies, with coexistence of carbonate and siliciclastic 63 sedimentation, are very important for the correlation and interpretation of the geological 64 record, especially stratigraphic surfaces and sequence units. 65 66
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