Warum trauert das Vaterland? : eine Predigt, gehalten bei dem Trauergottesdienste am 14. August 1859 wegen Ablebens Sr. Maj. des hochseligen Königs Oscar I. gesegneten Andenkens

von Dr. L. Lewysohn

Negative regulation of Drosophila Transformer2 by SR splicing factors

The Drosophila Transformer-2 (Tra2) protein activates the splicing of doublesex and fruitless pre-mRNA and represses M1 intron splicing in its own RNA in male germline. The M1 retention is part of negative feedback mechanism that controls Tra2 protein synthesis. However it is not known how the M1 intron is repressed or why Tra2 activates splicing of some RNAs while repressing splicing in others. Here we show that Tra2 and SR protein Rbp1 function together to specifically repress M1 splicing in vitro through the same intronic silencer by binding independently to distinct sites. The role of Rbp1 in M1 repression in vivo was validated by the finding that increased expression of Rbp1 in S2 cells promotes M1 retention. Furthermore, Tra2 blocks prespliceosomal A complex formation, a step corresponding to U2 snRNP recruitment to the branchpoint. High levels of Tra2 repression require an upstream enhancer. Together, we propose that the complex formed by Tra2 and Rbp1 on the silencer achieves splicing repression by blocking the recognition of the branchpoint or antagonizing enhancer function. ^ In addition, both splicing regulatory activities of Tra2 are essential developmental events, doublesex splicing is the key for Drosophila sex determination in the soma, while M1 retention occurs in the male germline and is necessary for spermatogenesis. However, active Tra2 is expressed ubiquitously. So another issue we have studied is how Tra2 accomplishes negative and positive splicing regulation in a tissue-specific fashion. Surprisingly, we found that nuclear extract from somatically-derived S2 cells support M1 repression in vitro. This led us to hypothesize that no germline specific factor is required and that high levels of Tra2 expression in the male germline is sufficient to trigger M1 retention. To test it, I examined whether increased expression of Tra2 could promote M1 retention in cells outside male germline. My results show that increased Tra2 expression promotes M1 retention in somatically-derived S2 cells as well as in the somatic tissues of living flies. These results show that somatic tissues are capable of supporting M1 repression but do not normally do so because the low levels of Tra2 do not trigger negative feedback regulation. ^

87Sr/86Sr ratios, Sr and Rb concentrations and stable oxygen isotope values for some basalts from ODP Hole 504B (Table 1)

Seventeen whole-rock samples, generally taken at 25-50 m intervals from 5 to 560 m sub-basement in Hole 504B, drilled in 6.2 m.y. old crust, were analysed for 87Sr/86Sr ratios, Sr and Rb concentrations, and 18O/16O ratios. Sr isotope ratios for 8 samples from the upper 260 m of the hole range from 0.70287 to 0.70377, with a mean of 0.70320. In the 330-560 m interval, 5 samples have a restricted range of 0.70255-0.70279, with a mean of 0.70266, the average value for fresh mid-ocean ridge basalts (MORB). In the 260-330 m interval, approximately intermediate Sr isotopic ratios are found. Delta18O values (?) range from 6.4 to 7.8 in the upper 260 m, 6.2-6.4 in the 270-320 m interval, and 5.8-6.2 in the 320-560 m interval. The values in the upper 260 m are typical for basalts which have undergone low-temperature seawater alteration, whereas the values for the 320-560 m interval correspond to MORB which have experienced essentially no oxygen isotopic alteration. The higher 87Sr/86Sr and 18O/16O ratios in the upper part of the hole can be interpreted as the result of a greater overall water/rock ratio in the upper part of the Hole 504B crust than in the lower part. Interaction of basalt with seawater (87Sr/86Sr = 0.7091) increased basalt 87Sr/86Sr ratios and produced smectitic alteration products which raised whole-rock delta18O values. Seawater circulation in the lower basalts may have been partly restricted by the greater number of relatively impermeable massive lava flows below about 230 m sub-basement. These flows may have helped to seal off lower basalts from through-flowing seawater.

(Table 1) Nd and Sr isotopic analyses of ODP Leg 127 basalts

Sr and Nd isotopic compositions are reported for basaltic rocks collected during ODP Leg 127 from the Yamato Basin, a rifted backarc basin in the Japan Sea. The basalts are classified into two groups in terms of Nd isotopic composition: the upper sills at Site 797 are characterized by higher 143Nd/144Nd ratios (0.513083-0.513158, epsilon-Nd = 8.68-10.14) and the basalts from Site 794 and the lower sills at Site 797 have lower 143Nd/144Nd ratios (0.512684-0.512862, epsilon-Nd = 0.90-4.37). All of the basalts show higher Sr isotopic compositions than those of the mantle array, which is attributed to seawater alteration. The basalts with lower Nd isotopic values ranging in age from 20.6 to 17.3 Ma have tapped an enriched subcontinental upper mantle (SCUM) with the minor involvement of a depleted asthenospheric mantle (AM). Subsequent change in composition through the physical replacement of SCUM by AM yielded the basalts of the upper sills of higher Nd isotopic compositions. This event within the upper mantle was associated with the breakup of the overlying lithosphere during the rifting of the Japan Sea backarc basin.