Chlorite-illite/muscovite interlayered and interstratified crystals: A TEM/STEM study

Phyllosilicates in rocks which are transitional from mudstone to slate from Lehigh Gap, Pa., have been studied by a variety of techniques, including high resolution Transmission Electron Microscopy and Analytical Electron Microscopy. The principal minerals are white mica which is transitional from illite in mudstone to ordered twolayer mica in slate, and chlorite. 7Å berthierine occurs more rarely. Dioctahedral and trioctahedral layers are shown to be interleaved in individual crystals at all scales between the following two end members: (1) both random and regular 11 interlayering at the scale of individual layers, as shown, in part, by lattice fringe images. (2) packets of trioctahedral and dioctahedral layers up to a few thousand Ångstroms or microns in thickness, detectable with ordinary optical techniques. The complete range of intermediate structures is represented in samples which are in transition to slate. Bulk analytical (EMPA), X-ray diffraction or other measurements are shown to result in averages over both kinds of layers when TEM techniques are not used.Contribution No. 400 from the Mineralogical Laboratory, Department of Geological Sciences, The University of Michigan     

The relationship between dissolved humic acids and soluble iron in estuaries

Dissolved humic acid and soluble iron appear to be chemically unassociated in estuaries despite their coincident removal. This conclusion is supported by differences in the aggregation kinetics of soluble iron and dissolved humic acid, the inability of extracted humic acid to stabilize laboratory preparations of ferric hydroxide, and decreasing ratios of humic acid carbon to soluble iron along the axes of some estuaries.     

Latitudinal patterns in seagrass epifauna: Do patterns exist,and can they be explained?

Seagrass-associated epifauna of several taxa constitute a major parallel element of seagrass communities over a range of latitudes. Hypotheses relating to latitudinal variation of several factors (e.g., predation, competition, primary production, habitat structure, stability and time) have been proposed to explain geographic variation in the structure of biological systems. We have summarized available information to firstly determine whether any latitudinal patterns exist for the seagrass-associated epifauna, and secondly to examine hypotheses which might explain observed patterns. Diversity and density of various seagrass epifaunal groups showed inconsistent latitudinal patterns. Diversity of decapod and amphipod crustaceans increased significantly with decreasing latitude, while diversity of isopods and fishes showed nonsignificant trends with latitude. Amphipod diversity was highly correlated with seagrass biomass over the range of latitudes. However, density of amphipods showed no pattern with either latitude or seagrass biomass; large within-site differences may have overwhelmed latitudinal patterns. For seagrass-associated amphipods, two parameters presumably related to predation intensity showed contradictory patterns. Size of individuals generally decreased toward the tropics, yet susceptibility to predators showed weak trends of increasing in the tropics. We found little support for the assumed gradients of those hypotheses proposed to explain latitudinal patterns in biota. Only a weak trend of increasing seagrass production toward the tropics was found; there was no relationship between latitude and seagrass biomass (=habitat complexity in part), epiphyte species richness (=habitat heterogeneity in part), or predator abundance. No data were available comparing actual intensity of predation on seagrass fauna or on proposed gradients of stability and competition. The patterns found were not consistent with the predictions of any single hypothesis. Contrary to evidence from other biological systems, it appears that latitude is, in general, an inconsistent predictor of differences in structure of the epifaunal component of seagrass communities. Although we did find some latitudinal patterns of increasing diversity and susceptibility to predators and decreasing size of individual amphipods toward the tropics, we were astonished by the lack of data supporting the assumptions of hypotheses concerning primary productivity, stability, time, competition, predation and habitat heterogeneity and complexity.     

The pitfalls of thresholding atmospheric dispersion data

Atmospheric dispersion data are invariably corrupted by random noise and perhaps baseline drift giving rise to unreal negative values. This paper shows that the indiscriminate use of thresholding can give rise to large errors in estimates of some key statistical parameters.     

Researching European 'alternative' food networks: some methodological considerations

Recent European literature on 'alternative' food networks (AFNs) draws heavily upon an apparently accessible and diverse body of non-conventional food networks in the agro-food sector and whilst researchers frequently refer to individual examples of farmers markets, box schemes, producer cooperatives and community-supported agriculture projects, less attention is given to the methodological processes that facilitate the identification and examination of these networks. From the preliminary stages of a research project focusing on examples of AFNs, ² this paper examines the process of operationalizing AFNs research and reviews the difficulties associated with identifying, comparing and characterizing AFNs.     

The Middle Pleistocene terraces of the central Waveney valley,Earsham, south Norfolk,UK

Although substantial work has been done on the pre-glacial terraces of East Anglia, very little systematic work has been done to understand the origin of river terraces in East Anglia that have formed since ice last covered the region. This paper records the results of studies of exposures and borehole records in ‘classical’ Quaternary terrace landforms that are considered to have formed since the Anglian (MIS 12) Glaciation, in the middle Waveney Valley. These features have been examined in terms of their morphological and sedimentological properties, in order to provide a detailed record of their form and composition, understand their processes of formation, and identify their stratigraphical status. The results show that the main body of the highest terrace (Homersfield Terrace, Terrace 3) is not composed of river sediments, but of shallow marine sediments, and is a remnant of early Middle Pleistocene Wroxham Crag. River sediments, in the form of Anglian age (MIS 12) glaciofluvial Aldeby Sands and Gravels also exist in the area as a channel fill, cut through the Wroxham Crag, and reflect outwash erosion and sedimentation from a relatively proximal ice margin to the west. The results mean that the interpretations previously presented for the terrace landforms of the middle Waveney valley are not applicable. The issue of why the terrace stratigraphy, hitherto identified in East Anglia cannot be related to that for the River Thames to the south and the rivers of Midland England to the west, still requires further research.     

Alternative framings of alternative food: A typology of practice

‘Alternative’ food initiatives (AFIs) are often interpreted as political movements, constructed as defiant alternatives to industrial agri‐food relations, and represented by a performance of singular alterity. This understanding of alternative collapses into a mere politics of identity, criticised in the literature for its oversimplification. In this paper, we utilise an established methodological framework that retains AFI diversity, to create a novel typology of AFIs by diverse and embodied practice rather than animating political project. In doing so, we point to the political potential for AFIs to ‘do’ food otherwise and make different worlds.