Baraminological Analysis of Devonian and Carboniferous Tetrapodomorphs

According to evolutionary theory, the origin of tetrapods (or limbed vertebrates) from a fish-like ancestor during the Devonian Period was one of the major events in the history of life. Devonian sediments have yielded several families of tetrapod-like fishes, including the elpistostegids which range from the Givetian to Frasnian of the Middle to Upper Devonian and are regarded as close to the evolutionary ancestry of tetrapods. Two of the best-known ‘early’ tetrapods are Ichthyostega and Acanthostega, first described from fossil material discovered in the Famennian (uppermost Upper Devonian) sediments of East Greenland. These taxa (and others subsequently described) display mosaic combinations of fish-like and tetrapod-like characters, along with some unique traits (such as polydactyly) not found in more ‘derived’ tetrapods. Creationists have claimed that these organisms are not evolutionary intermediates, but were rather the inhabitants of aquatic environments associated with a pre-Flood floating forest biome, with morphologically intermediate traits that equipped them for life in an environment that was itself intermediate between the sea and the land. This paper evaluates the baraminic status of a range of Devonian and Carboniferous fishes and tetrapods using the techniques of statistical baraminology. Baraminic distance correlation (BDC) and three-dimensional multidimensional scaling (MDS) are applied to six previously published character-taxon matrices. The results reveal little evidence of continuity, and significant evidence of discontinuity, between the elpistostegids and tetrapods such as Ichthyostega and Acanthostega, consistent with the creationist claim of separate ancestry. However, further work will be required to elucidate the baraminic relationships within these presumably apobaraminic groups

The Coconino Sandstone (Permian, Arizona, USA): Implications for the Origin of Ancient Cross-bedded Sandstones

The Permian Coconino Sandstone is one of the most prominent layers of rock in the Grand Canyon and is important to creationists because it has often been used by conventional scientists to discredit the Bible since it is a supposed wind-blown (eolian) deposit. Their argument is that deposits like this would be impossible to form in the midst of a global flood as described in Genesis. Over the past forty years, new data has been collected by us and others that we believe indisputably identifies the Coconino as a subaqueous sandstone--data that will be difficult for our critics to counter. These data include evidence from petrology, fossil footprint studies, sedimentology, regional stratigraphy and soft sediment deformation features. In our studies we found that there are many misconceptions or “urban myths” about the Coconino Sandstone including its grain roundness, grain sorting, grain frosting and angle of cross-bed dips. There are no modern analogs that match the precise sedimentology of the Coconino, but we believe that subaqueous sand waves may be a start in the right direction to understand how the Coconino was deposited. Instead of the Coconino being a problem for creationists, it can be one of our most powerful arguments in support of the biblical account of the Flood. There are many other similar cross-bedded sandstones around the world; the Coconino may be the key to unlocking their origin as well

Creative accounting three score years ago; Office management as a profession

Professor Garner brought the following human interest item to the attention of this editor. Emphasis (italics) was supplied throughout by Dr. Garner. From: Alpha Kappa Psi Diary, June, 1924 OFFICE MANAGEMENT AS A PROFESSION By A. W. T. Ogilvie, Gamma Chapter. There is also a note acknowledging Dr. Garner\u27s contribution to the Endowment Fund

Intraformational Parabolic Recumbent Folds in the Coconino Sandstone (Permian) and Two Other Formations in Sedona, Arizona (USA)

We report sedimentary structures that in all ways resemble parabolic recumbent folds (PRFs) in the cross-bedded portions of the Schnebly Hill Formation, the Coconino Sandstone and the Toroweap Formation (Arizona, USA). Field evidence suggests they are penecontemporaneous and intraformational. Intraformational refers to deformation that occurs between undeformed beds. Recumbent cross-bed sets occur over a wide area (\u3e375 km2 [144 mi2]) at many different locations and horizons in the Sedona area, especially within the Coconino Sandstone. Deformation resulting from slumping dunes (dry or damp) is ruled out because of the nature of the deformation along cross-bed dip, the size and length of the deformation along horizontal bedding planes (sometimes up to 170 m [557 ft] along dip) and the lack of small faults usually concurrent with such slumping known from modern dunes. Neither do the folds resemble deformation that has been caused by post-depositional groundwater movement or seismic activity which often produces convolute bedding. We do report some seismic features in the Schnebly Hill Formation, but these features have distinct characteristics that distinguish them from PRFs. Although the exact mechanism of PRF formation is still debated, it is generally agreed that strong water currents combined with liquefaction play major roles in overturning the top of a cross-bed set during the deposition of the cross-bed. Rare planar-beds, directly associated with the PRFs in the Coconino, suggest that the needed liquefaction may have occurred from changes in flow regime. Some workers have already suggested that parts of the Schnebly Hill and Coconino were deposited by marine sand waves on a shallow continental shelf; a hypothesis that is considerably strengthened in light of these new data along with additional petrographic data that we have collected

Baraminological Analysis of Jurassic and Cretaceous Avialae

The baraminic status of Jurassic and Cretaceous Avialae was evaluated using statistical baraminology. Baraminic distance correlation (BDC) and three dimensional multidimensional scaling (MDS) was applied to six previously published character matrices. The results reveal discontinuities between most Avialae and the Deinonychosauria (Troodontidae + Dromaeosauridae) and little evidence of continuity between modern birds and dinosaurs, suggesting that recent claims that statistical baraminology supports the evolution of birds from dinosaurs are misplaced. Nevertheless, we did find positive BDC and MDS clustering of some Avialae and deinonychosaurs in four of our analyses, suggesting that at least some Jurassic and Cretaceous Avialae may be clustered with dinosaurs. This observation raises the interesting philosophical question: what is a bird

Treatment of urinary schistosomiasis: methodological issues and research needs identified through a Cochrane systematic review

SUMMARY Guidelines recommend praziquantel (PZQ) for the treatment and control of schistosomiasis, with no real alternative. Metrifonate was still widely used against Schistosoma haematobium in the 1990s, and then withdrawn. Experimental studies and clinical trials suggest that artemisinin compounds are active against S. haematobium. In a Cochrane systematic review assessing the efficacy and safety of drugs for treating urinary schistosomiasis, 24 randomized controlled trials (n=6315 individuals) met our inclusion criteria. These trials compared a variety of single agent and combination regimens with PZQ, metrifonate or artemisinin derivatives. The review confirmed that both the standard recommended doses of PZQ (single 40 mg/kg oral dose) and metrifonate (3×7·5-10 mg/kg oral doses administered fortnightly) are efficacious and safe in treating urinary schistosomiasis, but there is no study comparing these two regimens head-to-head. There is currently not enough evidence to evaluate artemisinin compounds. Most of the studies included in the Cochrane systematic review were insufficiently powered, lacked standardization in assessing and reporting outcomes, and had a number of methodological limitations. In this paper we discuss the implications of these findings with respect to public health and research methodology and propose priority research needs

The impact of cognitive load on processing efficiency and performance effectiveness in anxiety: evidence from event-related potentials and pupillary responses

Anxiety has been associated with poor attentional control, as reflected in lowered performance on experimental measures of executive attention and inhibitory control. Recent conceptualisations of anxiety propose that individuals who report elevated anxiety symptoms worry about performance and will exert greater cognitive effort to complete tasks well, particularly when cognitive demands are high. Across two experiments, we examined the effect of anxiety on task performance and across two load conditions using (1) measures of inhibitory control (behavioural reaction times and eye-movement responses) and (2) task effort with pupillary and electrocortical markers of effort (CNV) and inhibitory control (N2). Experiment 1 used an oculomotor-delayed-response task that manipulated load by increasing delay duration to create a high load, relative to a low load, condition. Experiment 2 used a Go/No-Go task and load was manipulated by decreasing the No-Go probabilities (i.e., 20% No-Go in the high load condition and 50% No-Go in the low load condition). Experiment 1 showed individuals with high (vs. low) anxiety made more antisaccade errors across load conditions, and made more effort during the high load condition, as evidenced by greater frontal CNV and increased pupillary responses. In Experiment 2, individuals with high anxiety showed increased effort (irrespective of cognitive load), as characterised by larger pupillary responses. In addition, N2 amplitudes were sensitive to load only in individuals with low anxiety. Evidence of reduced performance effectiveness and efficiency across electrophysiological, pupillary, and oculomotor systems in anxiety provides some support for neurocognitive models of frontocortical attentional dysfunction in anxiety

Individual differences in search and monitoring for color targets in dynamic visual displays

Many jobs now involve the monitoring visual representations of data that change over time. Monitoring dynamically changing displays for the onset of targets can be done in two ways: detecting targets directly post their onset or predicting their onset from the prior state of distractors. In the present study, participants? eye movements were measured as they monitored arrays of 108 colored squares whose colors changed systematically over time. Across three experiments, the data show that participants detected the onset of targets both directly and predictively. Experiments 1 and 2 showed that predictive detection was only possible when supported by sequential color changes that followed a scale ordered in color space. Experiment 3 included measures of individual differences in working memory capacity (WMC) and anxious affect and a manipulation of target prevalence in the search task. It found that predictive monitoring for targets, and decisions about target onsets, were influenced by interactions between individual differences in verbal and spatial WMC and intolerance of uncertainty, a characteristic that reflects worry about uncertain future events. The results have implications for the selection of individuals tasked with monitoring dynamic visual displays for target onsets

Interleukin-8 levels and activity in delayed-healing human thermal wounds

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/72020/1/j.1524-475x.2000.00216.x.pd