The La Pasada Formation is a geologic formation in the southern Sangre de Cristo Mountains of New Mexico . It preserves fossils dating back to the early to middle Pennsylvanian .
5-428: The formation is a cyclic carbonate consisting of alternating limestone and shale with some thin sandstones . Total thickness is 973–1,002 ft (297–305 m). The formation is more clastic towards its base (50% shale and siltstone ) than towards its upper portion (24% shale and siltstone). The shales are noncalcareous and greenish towards the base but become gray, calcareous, and often fossiliferous towards
10-577: The La Pasada Formation from the Madera Group. Cyclothem In geology , cyclothems are alternating stratigraphic sequences of marine and non-marine sediments , sometimes interbedded with coal seams. The cyclothems consist of repeated sequences, each typically several meters thick, of sandstone resting upon an erosion surface , passing upwards to pelites (finer-grained than sandstone) and topped by coal. Historically,
15-538: The term was defined by the European coal geologists who worked in coal basins formed during the Carboniferous and earliest Permian periods. Depositional sequences have been thoroughly studied by oil geologists using geophysical profiles of continental and marine basins. A general theory of basin-scale deposition has been formalized under the name of sequence stratigraphy . Some cyclothems may have formed as
20-735: The upper portion. The formation shows considerable lateral variability, grading into the Flechado Formation to the north. The lower half of the formation is interpreted as a shallow marine nearshore sequence with occasional nonmarine intervals with thin coal beds. The upper half was deposited under neritic offshore marine conditions with infrequent nonmarine intervals. The formation contains abundant fossils of Mesolobus and other brachiopods , fenestrate bryozoans , crinoid fragments, and less common pectinid bivalves , as well as small numbers of trilobites , including Ditomopyge scitula and Ameura missouriensis . The formation
25-465: Was first defined in 1963 by Patrick K. Sutherland, who considered it correlative with the lower part of the Madera Formation . However, in 2004, Barry Kues and Katherine Giles recommended restricting the Madera Group to shelf and marginal basin beds of Desmoinean (upper Moscovian) to early Virgilian age, which excluded the La Pasada Formation. Spencer G. Lucas and coinvestigators also exclude
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