Lunar sample analysis

The surface composition of two samples from the highly shocked, glass-coated lunar basalt (12054) and from four glass-coated fragments from the 1-2 mm (14161) fines were examined by X-ray photoemission spectroscopy to determine whether the agglutination process itself is responsible for the difference between their surface and bulk compositions. Auger electron spectroscopy of glass balls from the 15425 and 74001 fines were analyzed to understand the nature, extent, and behavior of volatile phases associated with lunar volcanism. Initial results indicate that (1) volatiles, in the outer few atomic layers sampled, vary considerably from ball to ball; (2) variability over the surface of individual balls is smaller; (3) the dominant volatiles on the balls are S and Zn; and (4) other volatiles commonly observed are P, Cl, and K

Lunar sample analysis

Results are presented from an extensive series of new high resolution scanning electron microscope studies of the very primative group of meteorites known as unequilibrated chondrites. These include quantitative analyses of micrometer sized phases and interpretation in terms of relevant phase equilibria. Several new meteorite minerals including high chromium metal, have been discovered

Fe-rich pentlandite in Allende bulk samples and separates: Mössbauer spectroscopy analysis.

Published versio

Type II spiral ganglion afferent neurons drive medial olivocochlear reflex suppression of the cochlear amplifier.

The dynamic adjustment of hearing sensitivity and frequency selectivity is mediated by the medial olivocochlear efferent reflex, which suppresses the gain of the 'cochlear amplifier' in each ear. Such efferent feedback is important for promoting discrimination of sounds in background noise, sound localization and protecting the cochleae from acoustic overstimulation. However, the sensory driver for the olivocochlear reflex is unknown. Here, we resolve this longstanding question using a mouse model null for the gene encoding the type III intermediate filament peripherin (Prph). Prph((-/-)) mice lacked type II spiral ganglion neuron innervation of the outer hair cells, whereas innervation of the inner hair cells by type I spiral ganglion neurons was normal. Compared with Prph((+/+)) controls, both contralateral and ipsilateral olivocochlear efferent-mediated suppression of the cochlear amplifier were absent in Prph((-/-)) mice, demonstrating that outer hair cells and their type II afferents constitute the sensory drive for the olivocochlear efferent reflex

The Lowland Maya "Protoclassic"

The term "Protoclassic," employed regularly but inexplicitly in the literature of lowland Maya archaeology, has become increasingly nebulous and ambiguous in both meaning and usage. This paper reviews the history and use of the term and presents a formal redefinition of the Protoclassic as a ceramic stage based explicitly and exclusively on ceramic criteria. Some suggestions regarding future use of the term also are offered. The paper further addresses and resolves a number of persisting questions regarding Protoclassic orange wares, including problems concerning the actual existence of the "Aguacate ceramic group." and the relationships of Aguacate-group pottery to other emergent orange wares of the terminal Late Preclassic and initial Early Classic periods. The nature and significance of the "Holmul I Style," the "Floral Park Ceramic Sphere." and the relationships of the two to each other and the larger, redefined "protoclassic" ceramic stage also are examined. A spatial distribution for protoclassic ceramics considerably expanded over what has ever been reported previously is described, and chronometric data are presented to support a revised chronology for the protoclassic ceramic stage. Finally, ceramic data are offered that suggest a real subdivision of the protoclassic ceramic stage into an early, emergent facet originating entirely within Late Preclassic lowland traditions, and a later, fully "Classic" facet corresponding to the early Tzakol (Tzakol 1) ceramic horizon

Design factors that influence PCR amplification success of cross-species primers among 1147 mammalian primer pairs

BACKGROUND: Cross-species primers have been used with moderate success to address a variety of questions concerning genome structure, evolution, and gene function. However, the factors affecting their success have never been adequately addressed, particularly with respect to producing a consistent method to achieve high throughput. Using 1,147 mammalian cross-species primer pairs (1089 not previously reported), we tested several factors to determine their influence on the probability that a given target will amplify in a given species under a single amplification condition. These factors included: number of mismatches between the two species (the index species) used to identify conserved regions to which the primers were designed, GC-content of the gene and amplified region, CpG dinucleotides in the primer region, degree of encoded protein conservation, length of the primers, and the degree of evolutionary distance between the target species and the two index species. RESULTS: The amplification success rate for the cross-species primers was significantly influenced by the number of mismatches between the two index species (6–8% decrease per mismatch in a primer pair), the GC-content within the amplified region (for the dog, GC ≥ 50%, 56.9% amplified; GC<50%, 74.2% amplified), the degree of protein conservation (R(2 )= 0.14) and the relatedness of the target species to the index species. For the dog, 598 products of 930 primer pairs (64.3%) (excluding primers in which dog was an index species) were sequenced and shown to be the expected product, with an additional three percent producing the incorrect sequence. When hamster DNA was used with the single amplification condition in a microtiter plate-based format, 510 of 1087 primer pairs (46.9%) produced amplified products. The primer pairs are spaced at an average distance of 2.3 Mb in the human genome and may be used to produce up to several hundred thousand bp of species-specific sequence. CONCLUSION: The most important factors influencing the proportion of successful amplifications are the number of index species mismatches, GC-richness of the target amplimer, and the relatedness of the target species to the index species, at least under the single PCR condition used. The 1147 cross-species primer pairs can be used in a high throughput manner to generate data for studies on the genetics and genomics of non-sequenced mammalian genomes

Late-holocene channel meander migration and mudflat accumulation rates, Lagoon of Venice, Italy

Coring in the Lagoon of Venice mudflats along previously collected high-resolution subbottom seismic-reflection survey profile lines has enabled the collection of interlayered radiocarbon-datable terrestrial plant material. Along present and former meander bends, dipping laminated sandy channel-bank deposits rest in sharp lithostratigraphic and chronologic contrast to the adjacent and overlying mudflat deposits. Horizontal channel migration rates of roughly 10 to 20 meters per century are orders of magnitude faster than the minimum estimates of vertical mudflat silt accumulation, which range from 5 to 25 centimeters per century. Given the nearly 6000-year history since the late-Holocene marine transgression that produced the initial lagoon environments of deposition, it is no surprise that channel meander migration has left a prevalence of channel-bank deposits in the subsurface lithostratigraphy. Furthermore, regional subsidence and rising relative sea level continue to enhance the net accumulation of mudflat and salt marsh deposition on top of the older deposits. Tapered variations of tidal-channel width, depth, and flow velocity, as well as wind-driven waves with associated intensities of turbulence along the meandering paths, lead to recognizable sediment grain size trends and lagoon deposit stratigraphy. Human interventions, such as dredging, spoil disposal, and powerboat wakes, introduce other contrasting processes and depositional features. For complete understanding of the depositional environments in the lagoon, the full set of dynamic processes and depositional consequences often need to be considered. Patterns and processes revealed in this case study probably have broad applicability to other coastal lagoon environments experiencing significant tidal flow and sea-level change

New information on the Havelte Group site Ahrenshöft LA 58 D (Nordfriesland, Germany) - Preliminary results of the 2008 fieldwork

Late Glacial processes of human colonisation, adaptation and development represent a large field of study with a wide range of approaches. With respect to the archaeological succession from the classic Hamburgian to the Havelte Group, studies on the latter are still rare in Northern Germany. This paper aims to contribute to the chronological and archaeological characterization of the Havelte Group by presenting some new results from the Ahrenshöft LA 58 D site. Located in a micro-region rich in Late Glacial occupations, especially of the Hamburgian, the site was the subject of excavation in 1995. Questions regarding the homogeneity and chronological attribution of the site had been raised, leading to further fieldwork in 2008. This included palynological, micro-tephra and soil micromorphology analyses, which were partly supplemented by samples collected in 2009. The preliminary results presented here confirm the absence of indications of archaeological heterogeneity and, despite taphonomic difficulties, seem to confirm a recent age for the occupation, after the early Late Glacial Interstadial and within the Havelte Group

A Blended Basic Course Examination of Communication Apprehension and Self-Efficacy: A Comparative Analysis

Students desire rich subject-matter and relevant pedagogy despite rising tuition costs, greater demands for flexibility, and unique learning preferences (Allen & Seaman, 2014; Donnelly, Rizvi, & Summers, 2013; Reed & Sork, 2009; Moore, 2007). As higher education modalities have evolved a careful examination of these newer approaches is necessary. This study is a comparative assessment of communication apprehension and self-efficacy of students in traditional (face-to-face) and blended (face-to-face and online instructional components) basic course modalities. Parallel sections of a basic communication course are assessed and results indicated no significant differences between the two groups with minor exceptions

Calibration commentary

Radiocarbon is by far and away the most widely used dating tool in the Late Quaternary. Hundreds of key papers rely on the method to provide absolute and relative chronological information on important topics, including the late evolution of our own species (e.g. Higham et al. 2006a) and the timing and nature of abrupt climatic changes during the last glaciation (Lowe et al. 2001). Calibration of 14C determinations is an essential part of the dating process, and the implications of calibration can lead to significant differences in the interpretation of important processes (Blockley et al. 2006). Any development that enhances the accuracy, precision, or time coverage of the calibration curves is therefore to be welcomed. Since the early 1980s, there has been periodic publication of carefully vetted data in the form of internationally recognized consensus calibration curves that have allowed 14C users to convert their raw 14C determinations into calendar ages (Klein et al. 1982; Stuiver and Reimer 1986, 1993; Stuiver et al. 1998; Reimer et al. 2004). In the beginning, the basis on which this was done was easy to understand, 14C measurements were made on tree rings and the absolute calendar age came from counting annual growth rings. Although not without its complexities, the terrestrial tree-ring approach remains the most certain method and is at the heart of calibration process in the period 0-12.4 cal kyr. However, for periods beyond the limit of the tree-ring sequences the situation was significantly more problematic, and at times, even controversial.The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact [email protected] for further information.Migrated from OJS platform February 202