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Sequence stratigraphic analysis of four widely spaced outcrops of middle Cenomanian to middle Turonian strata deposited in the Western Interior foreland basin in southern New Mexico, USA, defines ten sequence boundaries in a marine shale-rich interval ca 200 m thick. The majority of sequence boundaries are based on basinward shifts in lithofacies characterized by either a non-Waltherian contact between distal-bar or lower shoreface sandstone and underlying lower offshore shale, or an erosional contact between distal-bar or lower shoreface sandstone and underlying upper offshore shale. The sequence boundaries commonly correlate basinward to packages of storm-deposited sandstone and to beds of sandy grainstone composed of winnowed inoceramid shell fragments. In several cases, however, the sequence boundaries pass basinward into presumably conformable successions of lower offshore shale. Maximum flooding surfaces within the sequences are represented by one or more beds of locally phosphatized globiginerid wackestone and packstone or exist within a conformable succession of lower offshore shale. Following initial south/south-westward transgression into the study area, the regional trend of palaeoeshorelines was north-west to south-east, although isopach data indicate that lobes of sandstone periodically spread south-eastward across the study area. The ten sequences in the study area are arranged into a third-order composite megasequence that is characterized by overall upward-deepening followed by upward-shallowing of sequences. The composite megasequence is similar but not identical to the previously established T-1 transgression and R-1 regression in New Mexico. Based on radioisotopic dates of bentonites, the average frequency of the sequences within the study area was ca 327 kyr, which is consistent with fourth-order cycles of ca 400 kyr interpreted in coeval marine strata elsewhere in the world. [ABSTRACT FROM AUTHOR]