Age trends in human chiasma frequencies and recombination fractions. I. Chiasma frequencies.

Chiasma frequency data on 183 males were subjected to an analysis of covariance. There appeared to be little or no linear trend in chiasma frequency with age. This conclusion was supported by a detailed analysis of chiasma frequencies for each autosome from 21 males. There were, however, significant differences among investigators in reported mean chiasma frequencies.     

Osmotic regulation of the uniflagellate phycomycete spore

In spores of the Blastocladiales there is a strict temporal correlation between the breakdown of the matrix of the gamma body and the swelling of the gamma body with the duration of the spore's motility. The swelling of the gamma body upon decay is interpreted as being due to water uptake. The swollen gamma bodies fuse with the plasmalemma and expel their content. We suggest that the swelling of the gamma body and its subsequent fusion with the plasmalemma of the spore are the means by which the spores of the Blastocladiales maintain osmotic balance with the medium in which they swim. The decay of the gamma body during the motile period of the spore is a separate and distinct process, not related to the mobilization of the remaining gamma bodies during encystment and cell wall formation.     

The saturated repair kinetics of Chinese hamster V79 cells suggests a damage accumulation--interaction model of cell killing

The aim of this study is to determine whether the repair process in log-phase Chinese hamster V79 cells exposed to X rays is unsaturated, saturable, or saturated. The kinetics of recovery from damage induced by 2 to 14 Gy of 250 kVp X rays was studied by treating cells with 0.5 M hypertonic saline for 20 min at different postirradiation repair intervals. From the kinetic data, the repair half-time (t1/2), the repair time (time needed to attain maximal survival), and the recovery ratio were calculated. The results show that the t1/2 (1.42 min/Gy) and the repair time (6.04 min/Gy) increase linearly with dose, the logarithm of the recovery ratio increases linear-quadratically with dose, and the D0 increases linearly with repair interval at a rate of 2.4 cGy/min. From these results we suggest a model: the repair of damage (undefined lesions) necessary for cell survival is effected by a repair process (t 1/2 of 1.42 min/Gy) which is saturated at doses as low as 2.4 cGy; repair saturation leads to a dose-dependent accumulation of repairable lesions; and interaction among accumulated repairable lesions results in the induction of irreparable (lethal) lesions. We call this the accumulation-interaction model of cell killing by low-LET radiation.     

A visit to the zoos and aquariums in Northern Japan

For their trip to the National Parks in Hokkaido the authors also included in their schedule visits to the zoos and aquariums in Northern Japan. Their tight scheduled tour started at the Aquamarine Fukushima, which was after the large tsunami rebuilt and re-opened in July 2011. They continued with a visit to the Kamo Aquarium, which is famous for its unique and large jellyfish exhibition. On Hokkaido Island they visited the smaller zoos in Kushiro and Obihiro with a good collection of native Hokkaido animal species. Included was also the Asahiyama Zoo, which is at the moment one of the most popular zoos in Japan. It is well-known for its innovative enclosures for seals and penguins. The Sapporo Maruyama Zoo and the Chitose Salmon Aquarium were the last highlights of this tour. The themes and animal collections of these different zoos and aquariums are described. The general situation for the northern zoos and aquariums is quite different compared to the institutions in the southern parts of the country and entirely to the zoos in the large city areas like Tokyo, Osaka and Nagoya. Here in the northern zoos and aquariums many native animal species and subspecies are kept and often successfully bred.     

Multiple Stressors in Agricultural Streams: A Mesocosm Study of Interactions among Raised Water Temperature,Sediment Addition and Nutrient Enrichment

Changes to land use affect streams through nutrient enrichment, increased inputs of sediment and, where riparian vegetation has been removed, raised water temperature. We manipulated all three stressors in experimental streamside channels for 30 days and determined the individual and pair-wise combined effects on benthic invertebrate and algal communities and on leaf decay, a measure of ecosystem functioning. We added nutrients (phosphorus+nitrogen; high, intermediate, natural) and/or sediment (grain size 0.2 mm; high, intermediate, natural) to 18 channels supplied with water from a nearby stream. Temperature was increased by 1.4°C in half the channels, simulating the loss of upstream and adjacent riparian shade. Sediment affected 93% of all biological response variables (either as an individual effect or via an interaction with another stressor) generally in a negative manner, while nutrient enrichment affected 59% (mostly positive) and raised temperature 59% (mostly positive). More of the algal components of the community responded to stressors acting individually than did invertebrate components, whereas pair-wise stressor interactions were more common in the invertebrate community. Stressors interacted often and in a complex manner, with interactions between sediment and temperature most common. Thus, the negative impact of high sediment on taxon richness of both algae and invertebrates was stronger at raised temperature, further reducing biodiversity. In addition, the decay rate of leaf material (strength loss) accelerated with nutrient enrichment at ambient but not at raised temperature. A key implication of our findings for resource managers is that the removal of riparian shading from streams already subjected to high sediment inputs, or land-use changes that increase erosion or nutrient runoff in a landscape without riparian buffers, may have unexpected effects on stream health. We highlight the likely importance of intact or restored buffer strips, both in reducing sediment input and in maintaining cooler water temperatures.