...Frederick S. Rogers Abstract The Little Cedar and lower Coralville formations of the Cedar Valley Group (Middle Devonian) of Iowa were deposited on a cratonic, shallow-water, carbonate and evaporite shelf during the Taghanic onlap. Four conodont subzones, zones, or cratonic biofacies faunas can...

... of conspecific neighbors. Taxa that exhibit clustering greater than expected under the random model probably clustered in life, revealing features of the local spatial structure. An example of the method is presented, using bedding planes from the Rapid Member of the Little Cedar Formation at the Devonian Fossil...

...Figure 6 Structure maps: (A) on top of the Smackover deeper water, subtidal lime mudstone and (B) on top of the Smackover Formation in the Little Cedar Creek field area illustrating the absence of structural closure in the field. ...

...David Lawrence Dunn Abstract Two new occurrences of some relatively little known microfossils are reported. These microfossils, called chitinozoans, are believed to represent an extinct order of rhizopod protozoans. The fauna described is that of the Devonian Cedar Valley formation, and represents...

... of the Cedar Mesa Formation. Thin, laterally discontinuous and crossbedded, medium-grained sandstones are observed throughout the HF, though they compose little of the formation volumetrically. These beds were deposited by fluvial reworking of sediment likely sourced from the highlands of the Uncompagre...

... architecture of these intersections nor the duration of the martian fluvial activity they represent. Here, we analyze a fluvial ridge intersection in the Cretaceous Cedar Mountain Formation of eastern Utah, USA, that we interpret to reflect the evolution of a river channel avulsion node exposed in 3-D. Through...