Longitudinal distribution of macroinvertebrates in snowmelt streams in northeast Greenland: understanding biophysical controls.

In a changing climate, Arctic streams are expected to show more influence from snowmelt, rainfall and groundwater, and less domination from glacial meltwater sources. Snowmelt streams are characteristic features of Arctic ecosystems, yet our current understanding of longitudinal patterns in benthic macroinvertebrate assemblages in these systems is limited when compared to glacier-fed systems. This study characterised longitudinal patterns of macroinvertebrate communities in snowmelt streams in northeast Greenland to provide novel insights into Arctic stream communities as dominant water sources shift with climate change. Benthic macroinvertebrates and environmental variables were sampled at three sites along five streams. Taxa diversity, evenness and abundance were expected to increase with distance from the stream source due to enhanced channel stability and warmer water temperature. This expectation for diversity and evenness was found in two streams, but abundance was up to ten times higher at the upstream sites compared to downstream, where biofilm biomass and ionic load were also highest. Here communities were largely dominated by the genus Eukiefferiella (Chironomidae). In the other three streams, no clear pattern in longitudinal macroinvertebrate community composition was evident due to low channel stability along the entire stream length. This study highlights the considerable variation in macroinvertebrate zonal distribution between snowmelt streams in northeast Greenland. A change towards more snowmelt-dominated streams in the Arctic could lead to shifts in the longitudinal organisation of macroinvertebrate community assemblages and the dominant species as a function of channel stability characteristics.

The use of invertebrates as indicators of environmental change in alpine rivers and lakes.

In alpine regions climatic change will alter the balance between water sources (rainfall, ice-melt, snowmelt, and groundwater) for aquatic systems, particularly modifying the relative contributions of meltwater, groundwater and rain to both rivers and lakes. While these changes are expected to have implications for alpine aquatic ecosystems, little is known about potential ecological tipping points and associated indicator taxa. We examined changes in biotic communities along a gradient of glacier influence for two study systems: (1) a stream network in the French Pyrénées; and (2) a network of lakes in the Italian Alps, with the aim of identifying potential indicator taxa (macroinvertebrates and zooplankton) of glacier retreat in these environments. To assess parallels in biotic responses across streams and lakes, both primary data and findings from other publications were synthesised. Using TITAN (Threshold Indicator Taxa ANalysis) changes in community composition of river taxa were identified at thresholds of <5.1% glacier cover and <66.6% meltwater contribution. Below these thresholds the loss of cold stenothermic benthic invertebrate taxa, Diamesa spp. and the Pyrenean endemic Rhyacophila angelieri was apparent. Some generalist taxa including Protonemura sp., Perla grandis, Baetis alpinus, Rhithrogena loyolaea and Microspectra sp. increased when glacier cover was <2.7% and <52% meltwater. Patterns were not as distinct for the alpine lakes, due to fewer sampling sites; however, Daphnia longispina grp. and the benthic invertebrate groups Plectopera and Planaria were identified as potential indicator taxa. While further work is required to assess potential indicator taxa for alpine lake systems, findings from alpine river systems were consistent between methods for assessing glacier influence (meltwater contribution/glacier cover). Hence, it is clear that TITAN could become a useful management tool, enabling: (i) the identification of taxa particularly sensitive to glacier retreat; and (ii) conservation efforts/resources to be better directed in alpine aquatic systems.

Interaction between ionizing radiation and supercoiled DNA within human tumor cells.

We have analyzed DNA supercoiling within histone-free nuclei (nucleoids) using four human squamous cell carcinoma cell lines that express varying degrees of radiosensitivity. The entire DNA, arranged as negative supercoiled loops attached to the nuclear matrix, was extracted from single cells, stained with ethidium bromide, and passed through a flow cytometer recording both light scatter and red (DNA) fluorescence. Supercoiled loops of DNA from all cells were unwound with a low concentration of ethidium bromide, as seen by increased light scatter. Nucleoids from radiosensitive but not radioresistant cells resisted the transition from zero to positive supercoiling at higher concentrations of ethidium bromide. The profile of red DNA fluorescence from ethidium bromide-stained nucleoids showed that the radiosensitive cells expressed a greater variation in the total amount of ethidium bromide bound. After 12 Gy of gamma-radiation, radiosensitive cell lines produced nucleoids that contained a greater proportion of relaxed supercoiled DNA, making them larger than those from radioresistant cell lines. We suggest these observations are secondary effects resulting from an altered affinity between supercoiled looped DNA and the nuclear matrix. Combined with radiation damage, these structural alterations may lead to a more complex type of damage to repair within the radiosensitive cell lines.

Analysis of free radical damage within single cells using flow cytometry.

The data presented here illustrates the additional information that can be gained on single cell biological effects by using a method of damage estimation based on single cells. The experiments involving primarily free radical damage carried out using H2O2 and the radioprotectors cysteamine and WR 1065, both revealed data that could not have been obtained from a macroscopic study of free radical-DNA chemistry and analysis of reaction products. This serves to emphasise the difficulty in extrapolating both free radical based and other chemical reactions to effects seen in living systems.

Effect of sodium fluoride, inorganic phosphate, and oxymetholone therapies in osteoporosis: a six-year progress report.

Elderly osteoporotic males treated with sodium fluoride or inorganic phosphate for 4 years plus 2 years of follow-up observations exhibited a mean but not significant decrease in the rate of bone mass loss in comparison with those receiving oxymetholone or a placebo. No hip fractures occurred in the patients who received fluoride, while 11 hip fractures occurred in the patients in the phosphate, oxymetholone, and control groups. Because the densitometric trends and fracture incidence are impressive, the progress of all subjects will be followed for an additional 4 years.