Cliff House Sandstone

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GEOMETRY AND DEPOSITIONAL STYLES km) zones of relatively thin (to 12 m sandstone) sheetlike OF A TRANSGRESSIVE SHORELINE: sandstone. The benches represent vertical aggradation of CLIFF HOUSE SANDSTONE (CAMPANIAN), paludal facies during temporary stabilization of shoreline SAN JUAN BASIN, NEW MEXICO positions; the intervening zones represent more rapid transgression. D.H. WOOD 808 Cambridge Drive, Round Rock, Texas 78664 The La Ventana Tongue, the thickest (240 m) bench, and internally consists of eight genetically related, stacked J.J. PALMER sandstone subunits. Their net-sandstone and facies maps Exxon Exploration Company indicate distinctive sandstone geometries that suggest depo- and sition as wave-dominated deltas and associated strand A.J. SCOTT University of Texas plain-coastal barrier systems along with shelf sand-bar P.O. Box 7909, Austin, Texas 78712 systems. Previous outcrop studies verify these interpreta- tions. Inferred sedimentary facies and depositional pro- The Cliff House Sandstone, the uppermost unit of the cesses are believed to be similar to those of the modern Cretaceous Mesaverde Group in the San Juan Basin, was Nile delta. deposited as marginal marine facies along the western shore of the Western Interior seaway during marine transgression. Through examination of over 2000 electric logs in the western San Juan Basin, several units within the Cliff House Sandstone reveal various depositional responses to changes in eustatic sea level and in rates of basin subsidence and sediment supply. The Cliff House Sandstone consists of long, narrow (8 km), thick (maximum 61-240 m) sandstone 'benches' that trend N 50° W and are typically separated by broad (to 13 .

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Central San Juan Basin
Acta - ---- - - ---Palaeontologic- -- ---' ~ Polonica Vol. 28, No. 1-2 pp. 195-204 Warszawa, 1983 Second Symposium on Mesozoic Terrestiol. Ecosystems, Jadwisin 1981 SPENCER G. LUCAS and NIALL J. MATEER VERTEBRATE PALEOECOLOGY OF THE LATE CAMPANIAN (CRETACEOUS):FRUITLAND FORMATION, SAN JUAN BASIN, ~EW MEXICO (USA) LUCAS, s. G. and MATEER, N. J .: Vertebrate paleoecology of the late Campanian (Cretaceous) Fruitland Formation, San Juan Basin, New Mexico (USA). Acta Palaeontologica Polonica, 28, 1-2, 195-204, 1983. Sediments of the Fruitland Formation in northwestern New Mexico represent a delta plain that prograded northeastward over the retrating strandline of the. North American epeiric seaway during the late Campanian. Fruitland fossil · vertebrates are fishes, amphibians, lizards, a snake, turtles, crocodilians, dinosaurs (mostly h adrosaurs and ceratopsians) and mammals. Autochthonous fossils in the Fruitland ' Form ation represent organisms of the trophically-complex Para saurolophus community. Differences in diversity, physical stress and life-history strategies within the ParasaurolopllUS community . fit well the stablllty-time hypothesis. Thus, dinosaurs experienced relatively low physical stress whereas fishes, amphibians, small reptiles and mammals experienced greater physical stress. Because of this, dinosaurs were less likely to recover from an environment al catastrophe than were smaller contemporaneous vertebrates. The terminal Cretaceous extinctions selectively eliminated animals that lived in less physlcally -stressed situations, indicating that the extinctions resulted from an environmental catastrophe. Key w 0 r d s: Fruitland Formation, New Mexico, delta plain, stablllty-time hypothesis, Cretaceous extinctions. Spencer G. Lucas, Department ot Geology and Geophysics and Peabody Museum ot Natural History, Yale University, P.O. Box 6666, New Haven, Connecticut 06511 USA ; NlaU J .
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