Ultrastructure,Behavior, and Algal Flagellate Affinities of the Helioflagellate Ciliophrys marina,and the Classification of the Helioflagellates (Protista,Actinopoda, Heliozoea)1

Ciliophrys marina is a small marine helioflagellate, with a central nucleus, which is capable of reversibly transforming from a rapidly swimming flagellate cell with no axopodia to the structure of a heliozoan with a flagellum that beats only a few times a minute. When in the flagellate form, the flagellum acts as a tractellum due to the tubular mastigonemes found along its length. When the rapidly swimming flagellate strikes a piece of debris, the flagellum goes through a very characteristic shock-induced avoidance reaction. Similarly, when a mechanical shock is delivered to the cell in its heliozoan form, the axopodia are contracted in less than 20 msec. Both reactions are inhibited in low calcium seawater. Transformation from the heliozoan to the flagellate form is accomplished by slow retraction and absorbance of the axopodia and activation of the flagellum. Ultrastructurally, each axopodium is found to contain three microtubules which attach to the outer nuclear membrane of the central nucleus at sites that this study characterizes by electron microscopy of thin sections and freeze fracture preparations. The mitochondria have tubular cristae, each containing an intracristal filament. Finally, a taxonomic review of the helioflagellates is presented, and it is suggested that C. marina is derived from the chrysomonads. An argument is also made for classifying C. marina with the heliozoan order Actinophryida, as a recently published classification of the protozoa does.     

The Irradiation of Dividing Cells: Changes in Sensitivity to X-Rays during Mitosis

Roots of Vicia faba were given combined X-ray and colchicinetreatments. Breaks were not visible immediately after irradiation,even at metaphase. Breaks and reunions were, therefore, scoredlater in 2x nuclei, and in the 4x nuclei derived from 2x nucleiafter colchicine treatment. It was shown that metaphase is themost sensitive stage of mitosis Breaks per chromosome are less frequent in 4x nuclei than in2x nuclei after irradiation of resting stage. This apparentphysiological difference between the two types of nuclei mayaffect either the frequency of breakage or of restitution. Afterthe irradiation of prophase, metaphase, or telophase cells,however, breaks per chromosome are more frequent in the 4x nucleithan they are in 2x nuclei in the same sample owing to the factthat the 2x, unlike the 4x nuclei, are not accurately timed.They must include cells irradiated during the less sensitiveresting stage. Chromosome reunion occurred, probably at telophase. Chromatidreunion and sister reunion did not occur frequently. Chromatidbreaks, like chromatid reunions, were infrequent except afterirradiation of resting stage cells. The evidence indicates thatthe chromosome, at metaphase just as at resting stage, reactsto X-rays as a single functional unit.     

Effects of experimental drought on soil respiration and radiocarbon efflux from a temperate forest soil

Soil moisture affects microbial decay of SOM and rhizosphere respiration (RR) in temperate forest soils, but isolating the response of soil respiration (SR) to summer drought and subsequent wetting is difficult because moisture changes are often confounded with temperature variation. We distinguished between temperature and moisture effects by simulation of prolonged soil droughts in a mixed deciduous forest at the Harvard Forest, Massachusetts. Roofs constructed over triplicate 5 × 5 m² plots excluded throughfall water during the summers of 2001 (168 mm) and 2002 (344 mm), while adjacent control plots received ambient throughfall and the same natural temperature regime. In 2003, throughfall was not excluded to assess the response of SR under natural weather conditions after two prolonged summer droughts. Throughfall exclusion significantly decreased mean SR rate by 53 mg C m^?2 h^?1 over 84 days in 2001, and by 68 mg C m^?2 h^?1 over 126 days in 2002, representing 10–30% of annual SR in this forest and 35–75% of annual net ecosystem exchange (NEE) of C. The differences in SR were best explained by differences in gravimetric water content in the Oi horizon (r²=0.69) and the Oe/Oa horizon (r²=0.60). Volumetric water content of the A horizon was not significantly affected by throughfall exclusion. The radiocarbon signature of soil CO₂ efflux and of CO₂ respired during incubations of O horizon, A horizon and living roots allowed partitioning of SR into contributions from young C substrate (including RR) and from decomposition of older SOM. RR (root respiration and microbial respiration of young substrates in the rhizosphere) made up 43–71% of the total C respired in the control plots and 41–80% in the exclusion plots, and tended to increase with drought. An exception to this trend was an interesting increase in CO₂ efflux of radiocarbon‐rich substrates during a period of abundant growth of mushrooms. Our results suggest that prolonged summer droughts decrease primarily heterotrophic respiration in the O horizon, which could cause increases in the storage of soil organic carbon in this forest. However, the C stored during two summers of simulated drought was only partly released as increased respiration during the following summer of natural throughfall. We do not know if this soil C sink during drought is transient or long lasting. In any case, differential decomposition of the O horizon caused by interannual variation of precipitation probably contributes significantly to observed interannual variation of NEE in temperate forests.