Covert or Overt Intervention? The Reagan Administration in Latin America

In my thesis I looked at Cold War interventionism by America. In the Post WWII period, many countries were searching for freedom from colonial rule, and many were attracted to the idea of communism or socialism. In this context of a destabilized world and power struggle between the U.S.A and the U.S.S.R., revolutions often became points of interests and parts of this larger power play. Any type of revolution was a destabilization, in a system that was unstable at best, and peace between the powers rested precariously on the idea of “Mutually Assured Destruction.” I would like to look more specifically, at the Latin American Region, which seemed full of upheaval, and was an area of much intervention, especially during the Reagan Administration. This administration had varying goals and conflicts about the region. The large amount of interventionism in the 1980s was in part a response to the Vietnam War, which was seen as an American failure, since prevention of communism did not occur. Following this, American strength needed to be shown again in the international stage, especially in Latin America, due to its close proximity to America. I would like to explore the intervention in Grenada and see if it followed a pattern of intervention in the region. This will be contrasted with the case of Nicaragua, which seemed more typical of interventions in the region. The causes of intervention in the region as well as the reasons these interventions took such different courses will be explored and investigated.

The in vivo and in vitro formation of sticky DNA and the GAA.TTC trinucleotide repeat associated with Friedreich's ataxia

Friedreich's ataxia is caused by the expansion of the GAA•TTC trinucleotide repeat sequence located in intron 1 of the frataxin gene. The long GAA•TTC repeats are known to form several non-B DNA structures including hairpins, triplexes, parallel DNA and sticky DNA. Therefore it is believed that alternative DNA structures play a role in the loss of mRNA transcript and functional frataxin protein in FRDA patients. We wanted to further elucidate the characteristics for formation and stability of sticky DNA by evaluating the structure in a plasmid based system in vitro and in vivo in Escherichia coli. The negative supercoil density of plasmids harboring different lengths of GAA•TTC repeats, as well as either one or two repeat tracts were studied in E. coli to determine if plasmids containing two long tracts (≥60 repeats) in a direct repeat orientation would have a different topological effect in vivo compared to plasmids that harbored only one GAA•TTC tract or two tracts of < 60 repeats. The experiments revealed that, in fact, sticky DNA forming plasmids had a lower average negative supercoil density (-σ) compared to all other control plasmids used that had the potential to form other non-B DNA structures such as triplexes or Z-DNA. Also, the requirements for in vitro dissociation and reconstitution of the DNA•DNA associated region of sticky DNA were evaluated. Results conclude that the two repeat tracts associate in the presence of negative supercoiling and MgCl 2 or MnCl2 in a time and concentration-dependent manner. Interaction of the repeat sequences was not observed in the absence of negative supercoiling and/or MgCl2 or in the presence of other monovalent or divalent cations, indicating that supercoiling and quite specific cations are needed for the association of sticky DNA. These are the first experiments studying a more specific role of supercoiling and cation influence on this DNA conformation. To support our model of the topological effects of sticky DNA in plasmids, changes in sticky DNA band migration was measured with reference to the linear DNA after treatment with increasing concentrations of ethidium bromide (EtBr). The presence of independent negative supercoil domains was confirmed by this method and found to be segregated by the DNA-DNA associated region. Sequence-specific polyamide molecules were used to test the effect of binding of the ligands to the GAA•TTC repeats on the inhibition of sticky DNA. The destabilization of the sticky DNA conformation in vitro through this binding of the polyamides demonstrated the first conceptual therapeutic approach for the treatment of FRDA at the DNA molecular level. ^ Thus, examining the properties of sticky DNA formed by these long repeat tracts is important in the elucidation of the possible role of sticky DNA in Friedreich's ataxia. ^

Roles of IkappaB kinase alpha in centrosome duplication and skin carcinogenesis

IκB kinase α (IKKα) is one kinase subunit of the IKK complex that is responsible for NF-κB activation. Previous studies have shown that IKKα determines mouse keratinocyte terminal differentiation independent of the NF-κB pathway. Accumulating evidence suggests that IKKα functions as a tumor suppressor in skin carcinogenesis; however, the downstream pathways mediating this function are largely unknown. By using primary cultured keratinocytes, we found that Ikkα-/- cells developed aneuploidy and underwent spontaneous immortalization and transformation while wild type cells underwent terminal differentiation in the same culture condition. Using proteomic analysis we identified nucleophosmin (NPM), a centrosome duplication regulator, as an IKKα substrate. We further demonstrated that IKKα interacted with NPM and colocalized with NPM on the centrosome, suggesting that NPM is a physiological substrate of IKKα. Loss of IKKα reduced centrosome-bound NPM and promoted abnormal centrosome amplification, which contributed to aneuploidy development. Detailed analysis revealed that ablation of IKKα target site serine-125 of NPM induced destabilization of NPM hexamers, disrupted NPM association with centrosomes, and resulted in abnormal centrosome amplification. Re-introduction of IKKα rescued the defect in Ikkα-/- keratinocytes. Thus, IKKα is required for maintaining proper centrosome duplication by phosphorylating NPM. ^ UV is the major etiological agent for human skin cancer and UV-induced mouse skin carcinogenesis is one of the most relevant experimental models for human skin carcinogenesis. Thus, we further evaluated IKKα function in UV-induced skin carcinogenesis in Ikkα+/- mice. We demonstrated that IKKα is also critical in UV skin carcinogenesis, as evidenced by increased tumor multiplicity and reduced tumor latency in Ikkα+/- mice after chronic UVB treatment. Reduced expression of IKKα decreased UV-induced apoptosis and promoted accumulation of P53 mutations in the epidermis. This indicates that IKKα is critical for UV-induced apoptosis in vivo and thus prevents mutation accumulation that is important for tumor development. ^ Together, these findings uncover previously unknown in vivo functions of IKKα in centrosome duplication and apoptosis, thus providing a possible mechanism of how loss of IKKα may contribute to skin carcinogenesis. ^

ARD1 stabilization of TSC2 suppresses tumorigenesis via the mTOR signaling pathway

Mammalian target of rapamycin (mTOR) plays an important role in regulating various cellular functions, and the tuberous sclerosis 1 (TSC1)/TSC2 complex serves as a major repressor of the mTOR pathway. Here we demonstrated that arrest-defective protein 1 (ARD1) physically interacts with, acetylates, and stabilizes TSC2, thereby reducing mTOR activity. The inhibition of mTOR by ARD1 suppresses cell proliferation and increases autophagy, which further impairs tumorigenicity. Correlation between the levels of ARD1 and TSC2 was found in multiple tumor types, suggesting the physiological importance of ARD1 in stabilizing TSC2. Moreover, evaluation of loss of heterozygosity (LOH) at Xq28 revealed allelic loss in 31% of tested breast cancer cell lines and tumor samples. Together, our findings suggest that ARD1 functions as a negative regulator of the mTOR pathway and that dysregulation of the ARD1/TSC2/mTOR axis may contribute to cancer development. To further explore the signaling pathway of ARD1, we provided evidence showing the phosphorylation of ARD1 by IKKβ, which mediated the destabilization of ARD1. Future work may be needed to study the biological effect of this post-translational modification. ^

Stability and potential application of spliced nuclear pre -mRNA introns

A major portion of this thesis work was dedicated to study the nature and significance of spliced introns. The initial work was focused on studying the IVS1$\sb{\rm C\beta 1}$ intron from a T-cell receptor (TCR)-$\beta$ gene. Compared to an intron lariat control from adenovirus pre-mRNA that was spliced in vitro, IVS1$\sb{\rm C\beta 1}$ was debranched less efficiently by HeLa S100 extracts, although IVS1$\sb{\rm C\beta 1}$ also used the consensus branchpoint in vivo. Subcellular-fractionation analysis showed that most IVS1$\sb{\rm C\beta 1}$ lariats cofractionated with pre-mRNA in the nucleus, consistent with the possibility that intron degradation releases splicing factors which will be available for further rounds of splicing. The half-life of IVS1$\sb{\rm C\beta 1}$ from the endogenous TCR-$\beta$ gene was measured using the general transcription inhibitor actinomycin D to be about $\sim$15 min, which was similar to that of unstable mRNAs such as c-myc mRNA.^ The general transcription inhibitor DRB was also used for intron stability analysis. Unexpectedly, DRB decreased intron and pre-mRNA levels only initially, it later increased the levels of intron-containing RNAs. Inhibition of transcription initiation appeared to be the major early effect (the reduction phase); whereas enhanced premature transcription termination was dominant later (the induction phase).^ Having established the procedures for studying in vivo spliced introns, this approach was applied to study the mechanism of nonsense-mediated downregulation (NMD), a phenomena in which premature termination codons (PTCs) decrease the levels of mRNAs. In this study, the novel intron-oriented approach was applied to study the mechanism of NMD. The levels of spliced introns immediately upstream and downstream of a PTC-bearing exon in a TCR-$\beta$ gene were identified and analyzed along with their pre-mRNA. Although PTC reduced the mRNA levels by 4 to 9 fold, the steady-state levels of spliced introns and the pre-mRNA-to-intron ratios were not significantly altered, indicating that the PTC did not significantly inhibit TCR-$\beta$ RNA splicing. Consistent with this conclusion, the half-lives of the PTC$\sp+$ and PTC$\sp-$ pre-mRNA were similar. The protein synthesis inhibitor cyclohexmide (CHX) upregulated the levels of the PTC$\sp+$ mRNA over 10 fold without affecting the levels of the spliced introns, suggesting that the reversal effect of CHX was through stabilization, not production. These results indicated that inhibition of splicing could not be the major mechanism for the NMD pathway of the TCR-$\beta$ gene, instead, suggesting that mRNA destabilization may be more important. (Abstract shortened by UMI.) ^

Mechanism of translationally coupled mRNA turnover mediated by c-fos protein-coding-region determinant

Proto-oncogene c-fos is a member of the class of early-response genes whose transient expression plays a crucial role in cell proliferation, differentiation, and apoptosis. Degradation of c- fos mRNA is an important mechanism for controlling c-fos expression. Rapid mRNA turnover mediated by the protein-coding-region determinant (mCRD) of the c-fos transcript illustrates a functional interplay between mRNA turnover and translation that coordinately influences the fate of cytoplasmic mRNA. It is suggested that mCRD communicates with the 3′ poly(A) tail via an mRNP complex comprising mCRD-associated proteins, which prevents deadenylation in the absence of translation. Ribosome transit as a result of translation is required to alter the conformation of the mRNP complex, thereby eliciting accelerated deadenylation and mRNA decay. To gain further insight into the mechanism of mCRD-mediated mRNA turnover, Unr was identified as an mCRD-binding protein, and its binding site within mCRD was characterized. Moreover, the functional role for Unr in mRNA decay was demonstrated. The result showed that elevation of Unr protein level in the cytoplasm led to inhibition of mRNA destabilization by mCRD. In addition, GST pull-down assay and immuno-precipitation analysis revealed that Unr interacted with PABP in an RNA-independent manner, which identified Unr as a novel PABP-interacting protein. Furthermore, the Unr interacting domain in PABP was characterized. In vivo mRNA decay experiments demonstrated a role for Unr-PABP interaction in mCRD-mediated mRNA decay. In conclusion, the findings of this study provide the first evidence that Unr plays a key role in mCRD-mediated mRNA decay. It is proposed that Unr is recruited by mCRD to initiate the formation of a dynamic mRNP complex for communicating with poly(A) tail through PABP. This unique mRNP complex may couple translation to mRNA decay, and perhaps to recruit the responsible nuclease for deadenylation. ^

Methane concentration and delta deuterium of methane from the NGRIP ice core

The causes of past changes in the global methane cycle and especially the role of marine methane hydrate (clathrate) destabilization events are a matter of debate. Here we present evidence from the North Greenland Ice Core Project ice core based on the hydrogen isotopic composition of methane [dD(CH4)] that clathrates did not cause atmospheric methane concentration to rise at the onset of Dansgaard-Oeschger (DO) events 7 and 8. Box modeling supports boreal wetland emissions as the most likely explanation for the interstadial increase. Moreover, our data show that dD(CH4) dropped 500 years before the onset of DO 8, with CH4 concentration rising only slightly. This can be explained by an early climate response of boreal wetlands, which carry the strongly depleted isotopic signature of high-latitude precipitation at that time.

Stable isotope and geochemical record of sediments from the Bering Sea

here is controversy over the role of marine methane hydrates in atmospheric methane concentrations and climate change during the last glacial period. In this study of two sediment cores from the southeast Bering Sea (700 m and 1467 m water depth), we identify multiple episodes during the last glacial period of intense methane flux reaching the seafloor. Within the uncertainty of the radiocarbon age model, the episodes are contemporaneous in the two cores and have similar timing and duration as Dansgaard-Oeschger events. The episodes are marked by horizons of sediment containing 13C-depleted authigenic carbonate minerals; 13C-depleted archaeal and bacterial lipids, which resemble those found in ANME-1 type anaerobic methane oxidizing microbial consortia; and changes in the abundance and species distribution of benthic foraminifera. The similar timing and isotopic composition of the authigenic carbonates in the two cores is consistent with a region-wide increase in the upward flux of methane bearing fluids. This study is the first observation outside Santa Barbara Basin of pervasive, repeated methane flux in glacial sediments. However, contrary to the "Clathrate Gun Hypothesis" (Kennett et al., 2003), these coring sites are too deep for methane hydrate destabilization to be the cause, implying that a much larger part of the ocean's sedimentary methane may participate in climate or carbon cycle feedback at millennial timescales. We speculate that pulses of methane in these opal-rich sediments could be caused by the sudden release of overpressure in pore fluids that builds up gradually with silica diagenesis. The release could be triggered by seismic shaking on the Aleutian subduction zone caused by hydrostatic pressure increase associated with sea level rise at the start of interstadials.

Geochemistry and stable isotopes of peridotites of ODP Hole 103-637A

A ridge of strongly serpentinized, plagioclase-bearing peridotite crops out at the boundary between the Atlantic oceanic crust and the Galicia continental margin (western Spain). These peridotites, cored at Hole 637A (ODP Leg 103) have been mylonitized at high-temperature, low-pressure conditions and under large deviatoric stress during their uplift (Girardeau et al., 1988, doi:10.2973/odp.proc.sr.103.135.1988). After this main ductile deformation event, the peridotite underwent a polyphase metamorphic static episode in the presence of water, with the crystallization of Ti- and Cr-rich pargasites at high-temperature (800°-900°C) interaction with a metasomatic fluid or alkaline magma. Introduction of water produced destabilization of the pyroxenes and the subsequent development of hornblendes and tremolite at temperatures decreasing from 750° to 350°C. The main serpentinization of the peridotite occurred at a temperature below 300°C, and possibly around 50°C, as a consequence of the introduction of a large amount of seawater, which is suggested by stable isotope (d18O and SD) data. Finally, calcite derived from seawater precipitated in late-formed fractures or locally pervasively impregnated the peridotite at low temperature (~10°C).

Tensiones y heterogeneidades temporales en la desocupación

La privación del trabajo remunerado tiene profundas consecuencias sobre el tiempo vivido de las personas. El trabajo es consumidor de tiempo, estructura el desarrollo de la jornada, impone limitaciones a otras actividades y ejerce una fuerte impronta en la vida cotidiana. El desempleo no solo conduce a liberar tiempo sino que, fundamentalmente, da lugar a una desestabilización del tiempo de referencia. Sin embargo, el tiempo de los desempleados es también objeto de encuadres y prescripciones que tienden a imponer una forma específica a la experiencia del desempleo. A partir de ello, es posible considerar que la desocupación no puede ser disociada de una perspectiva temporal. En este sentido, este artículo explora el ordenamiento temporal de las actividades instrumentales en un grupo de desocupados asistidos por el Estado en la Ciudad de Rosario. Así, se considera actividades instrumentales a aquellas que, teniendo por contenido y función la producción y reproducción de las condiciones materiales que hacen posible la supervivencia de la especie, se caracterizan por ser socialmente heterónomas, producto de una división social del trabajo que se explica en líneas complejas de diferenciación y desigualdad. Dentro de ellas se analizan dos conjuntos: el primero constituido por el trabajo remunerado, las actividades de contraprestación y los estudios; y el segundo integrado por el trabajo doméstico y familiar, y el trabajo voluntario

Stable isotope record of foraminifera from ODP Hole 114-704A

Isotopic and sedimentologic data from Ocean Drilling Program hole 704A suggest that isotopic stages 7, 9, and 11 were marked by unusually strong interglacial conditions in surface waters of the southern ocean. During interglacial stages 9 and 11, warm surface waters penetrated far poleward and may have led to destabilization of the West Antarctic Ice Sheet. In contrast, the strongest glacial conditions in surface waters of the subantarctic South Atlantic occurred during oxygen isotopic stage 12. Comparisons of benthic carbon isotopic gradients between sites located in the North Atlantic, southern ocean, and Pacific indicate that the production of upper North Atlantic Deep Water (uNADW) was strongest during stages 7,9, and 11 and weakest during stage 12, These results suggest a possible link between the flux of uNADW and paleoceanographic change in the southern ocean and support the traditional NADW-Antarctic connection whereby increased NADW leads to warming of the southern ocean.

Tensiones y heterogeneidades temporales en la desocupación

La privación del trabajo remunerado tiene profundas consecuencias sobre el tiempo vivido de las personas. El trabajo es consumidor de tiempo, estructura el desarrollo de la jornada, impone limitaciones a otras actividades y ejerce una fuerte impronta en la vida cotidiana. El desempleo no solo conduce a liberar tiempo sino que, fundamentalmente, da lugar a una desestabilización del tiempo de referencia. Sin embargo, el tiempo de los desempleados es también objeto de encuadres y prescripciones que tienden a imponer una forma específica a la experiencia del desempleo. A partir de ello, es posible considerar que la desocupación no puede ser disociada de una perspectiva temporal. En este sentido, este artículo explora el ordenamiento temporal de las actividades instrumentales en un grupo de desocupados asistidos por el Estado en la Ciudad de Rosario. Así, se considera actividades instrumentales a aquellas que, teniendo por contenido y función la producción y reproducción de las condiciones materiales que hacen posible la supervivencia de la especie, se caracterizan por ser socialmente heterónomas, producto de una división social del trabajo que se explica en líneas complejas de diferenciación y desigualdad. Dentro de ellas se analizan dos conjuntos: el primero constituido por el trabajo remunerado, las actividades de contraprestación y los estudios; y el segundo integrado por el trabajo doméstico y familiar, y el trabajo voluntario

Tensiones y heterogeneidades temporales en la desocupación

La privación del trabajo remunerado tiene profundas consecuencias sobre el tiempo vivido de las personas. El trabajo es consumidor de tiempo, estructura el desarrollo de la jornada, impone limitaciones a otras actividades y ejerce una fuerte impronta en la vida cotidiana. El desempleo no solo conduce a liberar tiempo sino que, fundamentalmente, da lugar a una desestabilización del tiempo de referencia. Sin embargo, el tiempo de los desempleados es también objeto de encuadres y prescripciones que tienden a imponer una forma específica a la experiencia del desempleo. A partir de ello, es posible considerar que la desocupación no puede ser disociada de una perspectiva temporal. En este sentido, este artículo explora el ordenamiento temporal de las actividades instrumentales en un grupo de desocupados asistidos por el Estado en la Ciudad de Rosario. Así, se considera actividades instrumentales a aquellas que, teniendo por contenido y función la producción y reproducción de las condiciones materiales que hacen posible la supervivencia de la especie, se caracterizan por ser socialmente heterónomas, producto de una división social del trabajo que se explica en líneas complejas de diferenciación y desigualdad. Dentro de ellas se analizan dos conjuntos: el primero constituido por el trabajo remunerado, las actividades de contraprestación y los estudios; y el segundo integrado por el trabajo doméstico y familiar, y el trabajo voluntario

Stable carbon isotopes, Methane Index, and distributions of different GDGTs

Gas hydrates represent one of the largest pools of readily exchangeable carbon on Earth's surface. Releases of the greenhouse gas methane from hydrates are proposed to be responsible for climate change at numerous events in geological history. Many of these inferred events, however, were based on carbonate carbon isotopes which are susceptible to diagenetic alterations. Here we propose a molecular fossil proxy, i.e., the "Methane Index (MI)", to detect and document the destabilization and dissociation of marine gas hydrates. MI consists of the relative distribution of glycerol dibiphytanyl glycerol tetraethers (GDGTs), the core membrane lipids of archaea. The rational behind MI is that in hydrate-impacted environments, the pool of archaeal tetraether lipids is dominated by GDGT-1, -2 and -3 due to the large contribution of signals from the methanotrophic archaeal community. Our study in the Gulf of Mexico cold-seep sediments demonstrates a correlation between MI and the compound-specific carbon isotope of GDGTs, which is strong evidence supporting the MI-methane consumption relationship. Preliminary applications of MI in a number of hydrate-impacted and/or methane-rich environments show diagnostic MI values, corroborating the idea that MI may serve as a robust indicator for hydrate dissociation that is useful for studies of global carbon cycling and paleoclimate change.

Physical properties and geochemical pore-water analysis of sediment core GeoB16423-1

Several studies indicate that the 2011 Tohoku-Oki earthquake (Mw 9.0) off the Pacific coast of Japan has induced slip to the trench and triggered landslides in the Japan Trench. In order to better understand these processes, detailed mapping and shallow-coring landslides at the trench as well as Integrated Ocean Drilling Program (IODP) deep drilling to recover the plate boundary décollement (Japan Trench Fast Earthquake Drilling Project, JFAST) have been conducted. In this study we report sediment core data from the rapid response R/V SONNE cruise (SO219A) to the Japan Trench, evidencing a Mass Transport Deposit (MTD) in the uppermost section later drilled at this JFAST-site during IODP Expedition 343. A 8.7 m long gravity core (GeoB16423-1) recovered from ~7,000 m water depth reveals a 8 m sequence of semi-consolidated mud clast breccias embedded in a distorted chaotic sediment matrix. The MTD is covered by a thin veneer of 50 cm hemipelagic, bioturbated diatomaceous mud. This stratigraphic boundary can be clearly distinguished by using physical properties data from Multi Sensor Core Logging and from fall-cone penetrometer shear strength measurements. The geochemical analysis of the pore-water shows undisturbed linear profiles measured from the seafloor downcore across the stratigraphic contact between overlying younger background-sediment and MTD below. This indicates that the investigated section has not been affected by a recent sediment destabilization in the course of the giant Tohoku-Oki earthquake event. Instead, we report an older landslide which occurred between 700 and 10,000 years ago, implying that submarine mass movements are dominant processes along the Japan Trench. However, they occur on local sites and not during each megathrust earthquake.