Regulation of mRNA splicing in Moloney murine sarcoma virus mutants

Cells infected with the conditionally defective MuSVts110 mutant of Moloney murine sarcoma virus are transformed at 33$\sp\circ$C but appear morphologically normal at 39$\sp\circ$C. The molecular basis for this phenotype is as follows: MuSVts110 contains a 1487 nucleotide central deletion that has truncated the 3$\sp\prime$ end to the gag gene and the 5$\sp\prime$ end of the mos gene. The resulting gag-mos junction is out-of-frame and the v-mos protein is not expressed. At 33$\sp\circ$C or lower, a splicing event is activated such that a 431 base intron is removed to realign the gag and mos gene in-frame, allowing the expression of a transforming protein P85$\sp{gag-mos}$. Temperature-dependent splicing appeared to be an intrinsic property of MuSVts110 transcripts and not a general feature of pre-mRNA splicing in 6m2 cells since splicing activity of a heterologous transcript in the same cells did not vary with temperature. The possibility that the splice event was not temperature-sensitive, but that the accumulation of spliced transcript at the lower growth temperatures was due to its selective thermolability was ruled out as stability studies revealed that the relative turnover rates of the unspliced and spliced MuSVts110 transcripts were not affected by temperature.^ The consensus sequences containing the splice sites activated in the MuSVts110 mutant (5$\sp\prime$ gag and 3$\sp\prime$ mos) are present, but not utilized, in wild-type MuSV-124. To test the hypothesis that it was the reduction of the 1919 base intervening sequence in MuSV-124 to 431 bases in MuSVts110 which activated splicing, the identical 1487 base deletion was introduced into cloned wild-type MuSV-124 DNA to create the MuSVts110 equivalent, ts32.^ To examine conditions permissive for splicing, we assayed splice site activation in a series of MuSV-124 "intron-modification" mutants. Data suggest that splicing in wild-type MuSV-124 may be blocked due to the lack of a proximal branchpoint sequence, but can be activated by those intron mutations which reposition a branch site closer to the 3$\sp\prime$ splice site. (Abstract shortened with permission of author.) ^

{\it cis\/} -acting determinants in the control of MuSVts110 RNA splicing

Like other simple retroviruses the murine sarcoma virus ts110 (MuSVts110) displays an inefficient mode of genome splicing. But, unlike the splicing phenotypic of other retroviruses, the splicing event effected upon the transcript of MuSVts110 is temperature sensitive. Previous work in this laboratory has established that the conditionally defective nature of MuSVts110 RNA splicing is mediated in cis by features in the viral transcript. Here we show that the 5$\sp\prime$ splice site of the MuSVts110 transcript acts as a point of control of the overall splicing efficiency at both permissive and nonpermissive temperatures for splicing. We strengthened and simultaneously weakened the nucleotide structure of the 5$\sp\prime$ splice site in an attempt to elucidate the differential effects each of the two known critical splicing components which interact with the 5$\sp\prime$ splice site have on the overall efficiency of intron excision. We found that a transversion of the sixth nucleotide, resulting in the formation of a near-consensus 5$\sp\prime$ splice site, dramatically increased the overall efficiency of MuSVts110 RNA splicing and abrogated the thermosensitive nature of this splicing event. Various secondary mutations within this original transversion mutant, designed to selectively decrease specific splicing component interactions, lead to recovery of inefficient and thermosensitive splicing. We have further shown that a sequence of 415 nucleotides lying in the downstream exon of the viral RNA and hypothesized to act as an element in the temperature-dependent inhibition of splicing displays a functional redundancy throughout its length; loss and/or replacement of any one sequence of 100 nucleotides within this sequence does not, with one exception detailed below, diminish the degree to which MuSVts110 RNA is inhibited to splice at the restrictive temperature. One specific deletion, though, fortuitously juxtaposed and activated cryptic consensus splicing signals for the excision of a cryptic intron within the downstream exon and markedly potentiated--across a newly defined cryptic exon--the splicing event effected upon the upstream, native intron. We have exploited this mutant of MuSVts110 to further an understanding of the process of exon definition and intron definition and show that the polypyrimidine tract and consensus 3$\sp\prime$ splice site, as well as the 5$\sp\prime$ splice site, within the intron at the 3$\sp\prime$ flank of the defined exon are required for the exon's definition; implying that definition of the downstream intron is required for the in vivo definition of the proximal, upstream exon. Finally; we have shown, through the construction of heterologous mutants of MuSVts110 employing a foreign 3$\sp\prime$ end-forming sequence, that efficiency of transcript splicing can be increased--to a degree which abrogates its thermosensitive nature--in direct proportion to increasing proximity of the 3$\sp\prime$ end-forming signal to the terminal 3$\sp\prime$ splice site. ^

Autoregulation of TRA-2 pre -mRNA splicing

One of the most elegant and tightly regulated mechanisms for control of gene expression is alternative pre-mRNA splicing. Despite the importance of regulated splicing in a variety of biological processes relatively little is understood about the mechanisms by which specific alternative splice choices are made and regulated. The transformer-2 (tra-2) gene encodes a splicing regulator that controls the use of alternative splicing pathways in the sex determination cascade of D. melanogaster and is particularly interesting because it directs the splicing of several distinct pre-mRNAs in different manners. The tra-2 protein positively regulates the splicing of both doublesex (dsx) and fruitless (fru) pre-mRNAs. Additionally tra-2 controls exuperantia (exu) by directing the choices between splicing and cleavage/polyadenylation and autoregulates the tra-2 pre-mRNA processing by repressing the removal of a specific intron (called M1). The goal of this study is to identify the molecular mechanisms by which TRA-2 protein affects the alternative splicing of pre-mRNA deriving from the tra-2 gene itself.^ The autoregulation of M1 splicing plays a key role in regulation of the relative levels of two functionally distinct TRA-2 protein isoforms expressed in the male germline. We have examined whether the structure, function, and regulation of tra-2 are conserved in Drosophila virilis, a species diverged from D. melanogaster by over 60 million years. We find that the D. virilis homolog of tra-2 produces alternatively spliced RNAs encoding a set of protein isoforms analogous to those found in D. melanogaster. When introduced into the genome of D. melanogaster, this homolog can functionally replace the endogenous tra-2 gene for both normal female sexual differentiation and spermatogenesis. Examination of alternative pre-mRNAs produced in D. virilis testes suggests that the germline-specific autoregulation of tra-2 function is accomplished by a strategy similar to that used in D. melanogaster.^ To identify elements necessary for regulation of tra-2 M1 splicing, we mutagenized evolutionarily conserved sequences within the tra-2 M1 intron and flanking exons. Constructs containing these mutations were used to generate transgenic fly lines that have been tested for their ability to carry out autoregulation. These transgenic fly experiments elucidated several elements that are necessary for setting up a context under which tissue-specific regulation of M1 splicing can occur. These elements include a suboptimal 3$\sp\prime$ splice site, an element that has been conserved between D. virilis and D. melanogaster, and an element that resembles the 3$\sp\prime$ portion of a dsx repeat and other splicing enhancers.^ Although important contextual features of the tra-2 M1 intron have been delineated in the transgenic fly experiments, the specific RNA sequences that interact directly with the TRA-2 protein were not identified. Using Drosophila nuclear extracts from Schneider cells, we have shown that recombinant TRA-2 protein represses M1 splicing in vitro. UV crosslinking analysis suggests that the TRA-2 protein binds to several different sites within and near the M1 intron. ^

Late Cenozoic silicoflagellate biostratigraphy, relative paleotemperature, and distribution of various genera and morphologic subgroups with remarks on noteworthy occurrences at DSDP Leg 86 Holes

A quantitative study of late Cenozoic silicoflagellates from the northwestern Pacific sites of Deep Sea Drilling Project Leg 86 shows a relative paleotemperature (Ts) gradient with lowest values (Ts = 30) in the north. Some new ecostratigraphic relations for the region are indicated, such as the last common occurrence of Dictyocha brevispina at 2.6 - 3.0 m.y. ago during a cool interval. Elements of North Pacific and low-latitude biostratigraphic zonations can be identified, but the mixing of cool- and warm-indicator taxa prompted the definition of the new Miocene Mesocena hexalitha Subzone and Pliocene Distephanus jimlingii Subzone. Scanning-electron microscope study of Leg 86 silicoflagellates was done to determine whether various types of skeletal surface texture are temperature dependent. To conduct the study we organized a new surface-texture descriptive code, which characterizes the apical structure/basal ring/spine sequence using new definitions of the terms crenulate (C), linear (L), nodular (N), reticulate (R), and smooth (S). One new silicoflagellate genus, Caryocha Bukry et Monechi, n. gen., is described and several new combinations are made.

Pollen and diatom analysis on varved sediments in Lake Jues (Harz Mountains, Germany)

Studies combining sedimentological and biological evidence to reconstruct Holocene climate beyond the major changes, and especially seasonality, are rare in Europe, and are nearly completely absent in Germany. The present study tries to reconstruct changes of seasonality from evidence of annual algal successions within the framework of well-established pollen zonation and 14C-AMS dates from terrestrial plants. Laminated Holocene sediments in Lake Jues (10°20.70' E, 51°39.30' N, 241 m a.s.l.), located at the SW margin of the Harz Mountains, central Germany, were studied for sediment characteristics, pollen, diatoms and coccal green algae. An age model is based on 21 calibrated AMS radiocarbon dates from terrestrial plants. The sedimentary record covers the entire Holocene period. Trophic status and circulation/stagnation patterns of the lake were inferred from algal assemblages, the subannual structure of varves and the physico-chemical properties of the sediment. During the Holocene, mixing conditions alternated between di-, oligo- and meromictic depending on length and variability of spring and fall periods, and the stability of winter and summer weather. The trophic state was controlled by nutrient input, circulation patterns and the temperature-dependent rates of organic production and mineralization. Climate shifts, mainly in phase with those recorded from other European regions, are inferred from changing limnological conditions and terrestrial vegetation. Significant changes occurred at 11,600 cal. yr. BP (Preboreal warming), between 10,600 and 10,100 cal. yr. BP (Boreal cooling), and between 8,400 and 4,550 cal. yr. BP (warm and dry interval of the Atlantic). Since 4,550 cal. yr. BP the climate became gradually cooler, wetter and more oceanic. This trend was interrupted by warmer and dryer phases between 3,440 and 2,850 cal. yr. BP and, likely, between 2,500 and 2,250 cal. yr. BP.

Seawater carbonate chemistry and zooxanthellate coral Cladocora caespitosa boron isotopic and elemental systematics during experiments, 2011

Boron isotopic and elemental systematics are used to define the vital effects for the temperate shallow water Mediterranean coral Cladocora caespitosa. The corals are from a range of seawater pH conditions (pHT ~ 7.6 to ~ 8.1) and environmental settings: (1) naturally living colonies harvested from normal pH waters offshore Levanto, (2) colonies transplanted nearby a subsea volcanic vent system, and (3) corals cultured in aquaria exposed to high (700 µatm) and near present day (400 µatm) pCO2 levels. B/Ca compositions measured using laser ablation inductively coupled mass spectrometry (LA-ICPMS) show that boron uptake by C. caespitosa cultured at different pCO2 levels is independent of ambient seawater pH being mainly controlled by temperature-dependent calcification. In contrast, the boron isotope compositions (delta11Bcarb) of the full suite of corals determined by positive thermal ionisation mass spectrometry (PTIMS) shows a clear trend of decreasing delta11Bcarb (from 26.7 to 22.2 %o) with decreasing seawater pH, reflecting the strong pH dependence of the boron isotope system. The delta11Bcarb compositions together with measurements of ambient seawater parameters enable calibration of the boron pH proxy for C. caespitosa, by using a new approach that defines the relationship between ambient seawater pH (pHsw) and the internally controlled pH at the site of calcification (pHbiol). C. caespitosa exhibits a linear relationship between pHsw and the shift in pH due to physiological processes (deltapH = pHbiol - pHsw) giving the regression deltapHClad = 4.80 - 0.52* pHsw for this species. We further apply this method ("deltapH-pHsw") to calibrate tropical species of Porites, Acropora, and Stylophora reported in the literature. The temperate and tropical species calibrations are all linearly correlated (r2 > 0.9) and the biological fractionation component (deltapH) between species varies within ~ 0.2 pH units. Our "deltapH-pHsw" approach provides a robust and accurate tool to reconstruct palaeoseawater pHsw for both temperate and tropical corals, further validating the boron fractionation factor (alphaB3-B4 = 1.0272) determined experimentally by Klochko et al. (2006) and the boron isotope pH proxy, both of which have been the foci of considerable debate.

Geochemistry of sediments beneath the Tonga-Kermadec arc

The fate of subducted sediment and the extent to which it is dehydrated and/or melted before incorporation into arc lavas has profound implications for the thermo-mechanical nature of the mantle wedge and models for crustal evolution. In order to address these issues, we have undertaken the first measurements of 10Be and light elements in lavas from the Tonga-Kermadec arc and the sediment profile at DSDP site 204 outboard of the trench. The 10Be/9Be ratios in the Tonga lavas are lower than predicted from flux models but can be explained if (a) previously estimated sediment contributions are too high by a factor of 2-10, (b) the top 1-22 m of the incoming sediment is accreted, (c) large amounts of sediment erosion are proposed, or (d) the sediment component takes several Myr longer than the subducting plate to reach the magma source region beneath Tonga. The lavas form negative Th/Be-Li/Be arrays that extend from a depleted mantle source composition to lower Th/Be and Li/Be ratios than that of the bulk sediment. Thus, these arrays are not easily explained by bulk sediment addition and, using partition coefficients derived from experiments on the in-coming sediment, we show that they are also unlikely to result from fluid released during dehydration of the sediment (or altered oceanic crust). However, partial melts of the dehydrated sediment residue formed at ~800 °C during the breakdown of amphibole +/- plagioclase and in the absence of cordierite have significantly lowered Th/Be ratios. The lava arrays can be successfully modelled as 10-15% partial melts of depleted mantle after it has been enriched by the addition of 0.2-2% of these partial melts. Phase relations suggest that this requires that the top of the subducting crust reaches temperatures of ~800 °C by the time it attains ~ 80 km depth which is in excellent agreement with the results of recent numerical models incorporating a temperature-dependent mantle viscosity. Under these conditions the wet basalt solidus is also crossed yet there is no recognisable eclogitic signal in the lavas suggesting that on-going dehydration or strong thermal gradients in the upper part of the subducting plate inhibit partialmelting of the altered oceanic crust.