Intracellular Development of Enterocytozoon, A Unique Microsporidian Found in the Intestine of AIDS Patients

Enterocytozoon was 1st described in 1985, in an AIDS patient with intestinal malabsorption and diarrhea. Since then, additional cases of infection with this organism have been observed, but only in individuals with AIDS and malabsorption. Intestinal tissue biopsies were obtained from a 45-year-old man prior to AIDS diagnosis, again nine months later and then at autopsy two months later. When the biopsies were examined electron microscopically, both sets contained the microsporidian parasite. However, the 2nd intestinal biopsy, when wasting was much more severe, contained infection in almost every small intestinal enterocyte examined. The parasite was actively developing, allowing us to detail its life cycle. The parasite is apansporoblastic, polysporous and has characteristics not previously reported in the Microsporida: (1) an electron lucent inclusion not usually seen in Microsporida is prominent and always present; (2) extremely elongated sausage-shaped nuclei occur in the proliferative phase of parasite development; (3) the polar tube development uniquely involves the production of electron dense discs, yet results in the formation of a typical spore; and (4) polar tube development occurs prior to the final division of the multi-nucleate sporont. On the basis of these characteristics, we are placing this genus in a new family, Enterocytozoonidae, n. fam.     

Changes in dissolved organic material determine exposure of stream benthic communities to UV-B radiation and heavy metals: implications for climate change

Changes in regional climate in the Rocky Mountains over the next 100 years are expected to have significant effects on biogeochemical cycles and hydrological processes. In particular, decreased discharge and lower stream depth during summer when ultraviolet radiation (UVR) is the highest combined with greater photo-oxidation of dissolved organic materials (DOM) will significantly increase exposure of benthic communities to UVR. Communities in many Rocky Mountain streams are simultaneously exposed to elevated metals from abandoned mines, the toxicity and bioavailability of which are also determined by DOM. We integrated field surveys of 19 streams (21 sites) along a gradient of metal contamination with microcosm and field experiments conducted in Colorado, USA, and New Zealand to investigate the influence of DOM on bioavailability of heavy metals and exposure of benthic communities to UVR. Spatial and seasonal variation in DOM were closely related to stream discharge and significantly influenced heavy metal uptake in benthic organisms. Qualitative and quantitative changes in DOM resulting from exposure to sunlight increased UV-B (290–320 nm) penetration and toxicity of heavy metals. Results of microcosm experiments showed that benthic communities from a metal-polluted stream were tolerant of metals, but were more sensitive to UV-B than communities from a reference stream. We speculate that the greater sensitivity of these communities to UV-B resulted from costs associated with metal tolerance. Exclusion of UVR from 12 separate Colorado streams and from outdoor stream microcosms in New Zealand increased the abundance of benthic organisms (mayflies, stoneflies, and caddisflies) by 18% and 54%, respectively. Our findings demonstrate the importance of considering changes in regional climate and UV-B exposure when assessing the effects of local anthropogenic stressors.     

Sex, Symbiosis and Coral Reef Communities

SYNOPSIS. Questions about how today's corals and coral reefswill fare in a future that holds not only increasing directanthropogenic impacts, but also global change, cannot be satisfactorilyanswered if we do not understand the relations of corals andreef systems to today's environmental conditions. This paperdiscusses four aspects of modern reef biology: coral reproduction,coral population biology, the coral-zooxanthella symbiosis,and reef community ecology. Conclusions of this survey of currentknowledge are that complexities of cnidarian reproductive biology,and our rudimentary knowledge of reproductive patterns in reefcnidarians, make forecasting based on current knowledge uncertainat best; new discoveries about the coral algal symbiotic systemsuggest a possible mode of adjustment to environmental changethat warrants a strong research effort; coral communities ofthe future may well be unlike what we are familiar with today;and these new assemblages will be shaped by the interactionof novel environmental conditions and the characteristics ofindividual reef species.     

Taphonomy and ichnology of cephalopod shells in a Maastrichtian chalk from Western Australia

The post-mortem history of a prolific Maastrichtian ammonite and nautiloid fauna preserved as phosphatic steinkerns in chalk of the upper Miria Formation of Western Australia is described. Sediment infilling of phragmocones, required for their fossilisation, was accomplished by means of perforations in the shell wall induced by the activity of abundant endoliths. These include borings ascribed to clionid sponges (Entobia), thallophytes, polychaete worms (including Caulostrepis and probable Maeandropolydora), phoronids (Talpina and Gnathichnus) and others of conjectural origin. Sediment infilling by this mechanism is considered to be more applicable to the taphonomy of phragmocones in general than sediment entry through the siphuncle and to be indicative of low sedimentation rates for the hosting strata. Nonheteromorph ammonites, and the nautiloid Cimomia, are preserved almost exclusively as phragmocones in the upper Miria Formation, and are numerically subordinate to the heteromorph Eubaculites which, together with Glyptoxoceras, is preserved predominantly as body chambers. This phragmocone/body chamber preservational contrast is attributed to the influence of shell shape on pre-burial mechanical abrasion. The apparent dominance of Eubaculites is considered to be largely a preservational artifact and ascribed to the ease with which body chambers were infilled, and thereby favoured for steinkern formation, relative to phragmocones. Phragmocones, or parts thereof. not filled with sediment were eliminated from the fossil record by diagenetic aragonite dissolution. Many ammonites with open umbilici have the early whorls missing. This we attribute to the trapping of sediment in the umbilicus prior to burial, preventing endolith attack whereby the early whorls avoided a sediment infilling. However, the protected inner whorls of involute ammonites and Cimomia, which have closed umbilici, and the inner whorls of evolute ammonites where a cemented umbilical plug supported the mouldic cavity left by shell dissolution, were preserved and were commonly infilled with calcite spar later in diagenesis. The dearth of cephalopod fossils in chalk underlying the upper Miria Formation is ascribed to diagenesis in which aragonite dissolution was not preceded by cementation.     

Fiber Ultrastructure and Contraction Kinetics in Insect Fast Muscles

SYNOPSIS. Isometric contraction kinetics were measured and fiberstructure was quantified in tymbal muscles from different cicadaspecies. Twitch duration is directly correlated with the sizeof the myofibrils and with the ratio of the fraction of fibervolume which is myofibril to that which is sarcoplasmic reticulum(SR) and T-tubules (fast muscles have small myofibrils and arelatively large volume of SR and T-tubules). Twitch durationis not significantly correlated with fiber size, with sarcomerelength, nor with the fractional volume of the fibers which ismitochondria, indicating that these structural features arenot strongly involved in the determination of isometric contractionkinetics. In the tettigoniid Neoconocephalus robustus, twitchesfrom forewing muscles of male animals become progressively shorterover the first five days following the adult molt. This changein contraction kinetics is associated with an increase in therelative volume of SR and T-tubules. Denervation blocks theacquisition of rapid kinetics, indicating that neural inputis necessary for this transformation.     

Genetic diversity and connectivity of deep‐sea hydrothermal vent metapopulations

Deep‐sea hydrothermal vents provide ephemeral habitats for animal communities that depend on chemosynthetic primary production. Sporadic volcanic and tectonic events destroy local vent fields and create new ones. Ongoing dispersal and cycles of extirpation and colonization affect the levels and distribution of genetic diversity in vent metapopulations. Several species exhibit evidence for stepping‐stone dispersal along relatively linear, oceanic, ridge axes. Other species exhibit very high rates of gene flow, although natural barriers associated with variation in depth, deep‐ocean currents, and lateral offsets of ridge axes often subdivide populations. Various degrees of impedance to dispersal across such boundaries are products of species‐specific life histories and behaviours. Though unrelated to the size of a species range, levels of genetic diversity appear to correspond with the number of active vent localities that a species occupies within its range. Pioneer species that rapidly colonize nascent vents tend to be less subdivided and more diverse genetically than species that are slow to establish colonies at vents. Understanding the diversity and connectivity of vent metapopulations provides essential information for designing deep‐sea preserves in regions that are under consideration for submarine mining of precious metals.     

Aboriginal Occupation at High Altitude: Alpine Villages in the White Mountains of Eastern California

Villages with well-built dwellings and extensive chipped- and ground-stone assemblages found between 3,130 m and 3,854 m in the White Mountains, California, and Toquima Range, Nevada, indicate intensive seasonal use of both ranges by groups engaged in alpine plant and animal procurement. Lichenometric measurements, radiocarbon assays, and time-sensitive artifacts show that the White Mountain alpine villages postdate A.D. 600, and are temporally distinct from older hunting blinds and sparse lithic scatters in that range that suggest a less-intensive form of alpine land use centered on hunting; a similar, and roughly contemporaneous, adaptive succession is indicated in the Toquima Range. These changes probably reflect adaptive responses to population growth and may be connected with the spread of Numic-speaking peoples.