Mitochondrial dysfunction leads to NOX activation: A novel mechanism to maintain high glycolysis in cancer cells

Increased glycolysis and oxidative stress are common features of cancer cells. These metabolic alterations are associated with mitochondrial dysfunction and can be caused by mitochondrial DNA (mtDNA) mutations, oncogenic signals, loss of tumor suppressor, and tumor tissue hypoxia. It is well established that mitochondria play central roles in energy metabolism, maintenance of redox balance, and regulation of apoptosis. However, the biochemical and molecular mechanisms that maintain high glycolysis in cancer cells (the Warburg effect) with mitochondrial dysfunction and oxidative stress remain to be determined. The major goals of this study were to establish a unique experimental system in which the mitochondrial respiratory function can be regulated as desired, and to use this system to investigate the mechanistic link between mitochondrial dysfunction and the Warburg effect along with oxidative stress in cancer cells. To achieve these goals, I have established a tetracycline-inducible system in which a dominant negative form of mitochondrial DNA polymerase y (POLGdn) expression could be regulated by tetracycline; thus controlling mitochondrial respiratory function. Using this cell system, I demonstrated that POLGdn expression resulted in mitochondrial dysfunction through decreasing mtDNA content, depletion of mtDNA encoded mRNA and protein expression. This process was mediated by TFAM proteasome degradation. Mitochondrial dysfunction mediated by POLGdn expression led to a significant increase in cellular glycolysis and oxidative stress. Surprisingly, mitochondrial dysfunction also resulted in increased NAD(P)H oxidase (NOX) enzyme activity, which was shown to be essential for maintaining high glycolysis. Chemical Inhibition of NOX activity by diphenyliodonium (DPI) preferentially impacted the survival of mitochondrial defective cells. The colon cancer HCT116-/- cells that have lost transcriptional regulation of the mitochondrial assembling enzyme SCO2, leading to compromised mitochondrial respiratory function, were found to have increased NOX activity and were highly sensitive to DPI treatment. Ovarian epithelial cells with Ras transformation also exhibited an increase in NOX gene expression and NOX enzyme activity, rendering the cells sensitive to DPI inhibition especially under hypoxic condition. These data together suggest that NOX plays a novel role in maintaining high glycolysis in cancer cells with mitochondrial defects, and that NOX may be a potential target for cancer therapy. ^

Impact of COP9 signalosome subunit 6 (CSN6) on MDM2-p53 axis in DNA damage-mediated apoptosis and tumorigenesis

Mammalian COP9 signalosome, which connects signaling with the ubiquitin-mediated proteasome degradation pathway, is implicated in cell cycle regulation and DNA damage response. However, whether COP9 is dysregulated in cancers has not been well established. Here, we showed that COP9 subunit 6 (CSN6) was upregulated in malignant breast and thyroid tumors and positively correlated with MDM2 expression. Investigation of the underlying mechanism suggested that CSN6 stabilized MDM2, thereby accelerating the degradation of p53. We generated mice carrying a targeted disruption of the Csn6 gene, and found that the mice with both alleles disrupted (Csn6-/- ) died in early embryogenesis (E7.5). Csn6+/- mice were sensitized to undergo γ-radiation-induced p53-dependent apoptosis in both thymus and developing central nervous system. Consequently. Csn6 +/- mice were more susceptible to the lethal effects of high-dose γ-radiation than wild-type mice. Notably, Csn6+/- mice were less susceptible to γ-radiation-induced tumorigenesis and had better long-term survival after low-dose γ-radiation exposure compared with wild-type animals, indicating that loss of CSN6 enhanced p53-mediated tumor suppression in vivo. In summary, the regulation of MDM2-p53 signaling by CSN6 plays a significant role in DNA damage-mediated apoptosis and tumorigenesis, which suggests that CSN6 may potentially be a valuable diagnostic marker for cancers with a dysregulated MDM2-p53 axis. ^

Regulation of Protein Degradation in the Heart by AMP-Activated Protein Kinase

The degradation of proteins by the ubiquitin proteasome system is essential for cellular homeostasis in the heart. An important regulator of metabolic homeostasis is AMP-activated protein kinase (AMPK). During nutrient deprivation, AMPK is activated and intracellular proteolysis is enhanced through the ubiquitin proteasome system (UPS). Whether AMPK plays a role in protein degradation through the UPS in the heart is not known. Here I present data in support of the hypothesis that AMPK transcriptionally regulates key players in the UPS, which, under extreme conditions can be detrimental to the heart. The ubiquitin ligases MAFbx /Atrogin-1 and MuRF1, key regulators of protein degradation, and AMPK activity are increased during nutrient deprivation. Pharmacologic and genetic activation of AMPK is sufficient for the induction of MAFbx/Atrogin-1 and MuRF1 in cardiomyocytes and in the heart in vivo. Comprehensive experiments demonstrate that the molecular mechanism by which AMPK regulates MuRF1 expression is through the transcription factor myocyte enhancer factor 2 (MEF2), which is involved in stress response and cardiomyocyte remodeling. MuRF1 is required for AMPK-mediated protein degradation through the UPS in cardiomyocytes. Consequently, the absence of MuRF1 during chronic fasting preserves cardiac function, possibly by limiting degradation of critical metabolic enzymes. Furthermore, during cardiac hypertrophy, chronic activation of AMPK also leads to cardiac dysfunction, possibly through enhanced protein degradation and metabolic dysregulation. Collectively, my findings demonstrate that AMPK regulates expression of ubiquitin ligases which are required for UPS-mediated protein degradation in the heart. Based on these results, I propose that specific metabolic signals may serve as modulators of intracellular protein degradation in the heart.

Regulation of Protein Degradation in the Heart by AMP-Activated Protein Kinase

The degradation of proteins by the ubiquitin proteasome system is essential for cellular homeostasis in the heart. An important regulator of metabolic homeostasis is AMP-activated protein kinase (AMPK). During nutrient deprivation, AMPK is activated and intracellular proteolysis is enhanced through the ubiquitin proteasome system (UPS). Whether AMPK plays a role in protein degradation through the UPS in the heart is not known. Here I present data in support of the hypothesis that AMPK transcriptionally regulates key players in the UPS, which, under extreme conditions can be detrimental to the heart. The ubiquitin ligases MAFbx /Atrogin-1 and MuRF1, key regulators of protein degradation, and AMPK activity are increased during nutrient deprivation. Pharmacologic and genetic activation of AMPK is sufficient for the induction of MAFbx/Atrogin-1 and MuRF1 in cardiomyocytes and in the heart in vivo. Comprehensive experiments demonstrate that the molecular mechanism by which AMPK regulates MuRF1 expression is through the transcription factor myocyte enhancer factor 2 (MEF2), which is involved in stress response and cardiomyocyte remodeling. MuRF1 is required for AMPK-mediated protein degradation through the UPS in cardiomyocytes. Consequently, the absence of MuRF1 during chronic fasting preserves cardiac function, possibly by limiting degradation of critical metabolic enzymes. Furthermore, during cardiac hypertrophy, chronic activation of AMPK also leads to cardiac dysfunction, possibly through enhanced protein degradation and metabolic dysregulation. Collectively, my findings demonstrate that AMPK regulates expression of ubiquitin ligases which are required for UPS-mediated protein degradation in the heart. Based on these results, I propose that specific metabolic signals may serve as modulators of intracellular protein degradation in the heart.

Regulation of the heat shock response by thiol-reactive compounds in the yeast Saccharomyces cerevisiae

Cells govern their activities and modulate their interactions with the environment to achieve homeostasis. The heat shock response (HSR) is one of the most well studied fundamental cellular responses to environmental and physiological challenges, resulting in rapid synthesis of heat shock proteins (HSPs), which serve to protect cellular constituents from the deleterious effects of stress. In addition to its role in cytoprotection, the HSR also influences lifespan and is associated with a variety of human diseases including cancer, aging and neurodegenerative disorders. In most eukaryotes, the HSR is primarily mediated by the highly conserved transcription factor HSF1, which recognizes target hsp genes by binding to heat shock elements (HSEs) in their promoters. In recent years, significant efforts have been made to identify small molecules as potential pharmacological activators of HSF1 that could be used for therapeutic benefit in the treatment of human diseases relevant to protein conformation. However, the detailed mechanisms through which these molecules drive HSR activation remain unclear. In this work, I utilized the baker's yeast Saccharomyces cerevisiae as a model system to identify a group of thiol-reactive molecules including oxidants, transition metals and metalloids, and electrophiles, as potent activators of yeast Hsf1. Using an artificial HSE-lacZ reporter and the glucocorticoid receptor system (GR), these diverse thiol-reactive compounds are shown to activate Hsf1 and inhibit Hsp90 chaperone complex activity in a reciprocal, dose-dependent manner. To further understand whether cells sense these reactive compounds through accumulation of unfolded proteins, the proline analog azetidine-2-carboxylic acid (AZC) and protein cross-linker dithiobis(succinimidyl propionate) (DSP) were used to force misfolding of nascent polypeptides and existing cytosolic proteins, respectively. Both unfolding reagents display kinetic HSP induction profiles dissimilar to those generated by thiol-reactive compounds. Moreover, AZC treatment leads to significant cytotoxicity, which is not observed in the presence of the thiol-reactive compounds at the concentrations sufficient to induce Hsf1. Additionally, DSP treatment has little to no effect on Hsp90 functions. Together with the ultracentrifugation analysis of cell lysates that detected no insoluble protein aggregates, my data suggest that at concentrations sufficient to induce Hsf1, thiol-reactive compounds do not induce the HSR via a mechanism based on accumulation of unfolded cytosolic proteins. Another possibility is that thiol-reactive compounds may influence aspects of the protein quality control system such as the ubiquitin-proteasome system (UPS). To address this hypothesis, β-galactosidase reporter fusions were used as model substrates to demonstrate that thiol-reactive compounds do not inhibit ubiquitin activating enzymes (E1) or proteasome activity. Therefore, thiol-reactive compounds do not activate the HSR by inhibiting UPS-dependent protein degradation. I therefore hypothesized that these molecules may directly inactivate protein chaperones, known as repressors of Hsf1. To address this possibility, a thiol-reactive biotin probe was used to demonstrate in vitro that the yeast cytosolic Hsp70 Ssa1, which partners with Hsp90 to repress Hsf1, is specifically modified. Strikingly, mutation of conserved cysteine residues in Ssa1 renders cells insensitive to Hsf1 activation by cadmium and celastrol but not by heat shock. Conversely, substitution with the sulfinic acid and steric bulk mimic aspartic acid led to constitutive activation of Hsf1. Cysteine 303, located in the nucleotide-binding/ATPase domain of Ssa1, was shown to be modified in vivo by a model organic electrophile using Click chemistry technology, verifying that Ssa1 is a direct target for thiol-reactive compounds through adduct formation. Consistently, cadmium pretreatment promoted cells thermotolerance, which is abolished in cells carrying SSA1 cysteine mutant alleles. Taken together, these findings demonstrate that Hsp70 acts as a sensor to induce the cytoprotective heat shock response in response to environmental or endogenously produced thiol-reactive molecules and can discriminate between two distinct environmental stressors.

Requirement of the Jak2 tyrosine kinase in Bcr -Abl oncogenic transformation

Philadelphia chromosome (Ph)-positive chronic myeloid leukemia is caused by a clonal myeloproliferative expansion of malignant primitive hematopoietic progenitor cells. The Ph results from the reciprocal translocation of the ends of chromosome 9 and 22, which generate Bcr-Abl fusion proteins. The Bcr-Abl proteins possess a constitutively activated Abl tyrosine kinase, which is the driving force responsible for causing leukemia. The activated Bcr-Abl tyrosine kinase stimulates multiple signal transduction pathway affecting growth, differentiation and survival of cells. It is known that the Bcr-Abl tyrosine kinase activates several signaling proteins including Stat5, which is a member of the Jak/Stat pathway that is activated by cytokines that control the growth and differentiation of normal hematopoietic cells. Our laboratory was the first one to report that Jak2 tyrosine kinase is activated in a human Bcr-Abl positive hematopoietic cell line. In this thesis, we further investigated the activation of Jak2 by Bcr-Abl. We found that Jak2 is activated not only in cultured Bcr-abl positive cell lines but also in blood cells from CML blast crisis patients. We also demonstrated that SH2 domain of Bcr-Abl is required for efficient activation Jak2. We further showed that Jak2 binds to the C-terminal domain of Bcr-Abl; tyrosine residue 1007, which is critical for Jak2 activation, is phosphorylated by Bcr-Abl. We searched downstream targets of Jak2 in Bcr-Abl positive cells. We treated Bcr-Abl positive cells with a Jak2 kinase inhibitor AG490 and found that c-Myc protein expression is inhibited by AG490. We further demonstrated that Jak2 inhibitor AG490 not only inhibit C-MYC transcription but also protect c-Myc protein from proteasome-dependent degradation. We also showed that AG490 did not affect Bcr-Abl kinase activity and Stat5 activation and its downstream target Bcl-xL expression. AG490 also induced apoptosis of Bcr-Abl positive cells, similar to Bcr-Abl kinase inhibitor STI571 (also termed Gliveec, a very effective drug for CML), but unlike STI571 the apoptosis effects induced by AG490 can not be rescued by IL-3 containing WEHI conditioned medium. We further established several Bcr-Abl positive clones that express a kinase-inactive Jak2 and found that these clones had reduced tumor formation in nude mice assays. Taken together, these results establish that Jak2 is activated in Bcr-Abl positive CML cells and it is required for c-Myc induction and the oncogenic effects of Bcr-Abl. Furthermore, Jak2 and Stat5 are two independent targets of Bcr-Abl. ^

Model - data comparison of western African rainfall evolutions during the Last Interglacial (130-115 ka)

This dataset characterizes the evolution of western African precipitation indicated by marine sediment geochemical records in comparison to transient simulations using CCSM3 global climate model throughout the Last Interglacial (130-115 ka). It contains (1) defined tie-points (age models), newly published stable isotopes of benthic foraminifera and Al/Si log-ratios of eight marine sediment cores from the western African margin and (2) annual and seasonal rainfall anomalies (relative to pre-industrial values) for six characteristic latitudinal bands in western Africa simulated by CCSM3 (two transient simulations: one non-accelerated and one accelerated experiment).

Great Barrier Reef coral element/Ca and stable isotope data and U-Th ages from IODP Expedition 325

Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.

Chemical analysis with regard to global and local climatic forcing measured on sediment core GeoB3711-1, GeoB3711-3 and GeoB4917-8

Global and local climatic forcing, e.g. concentration of atmospheric CO2 or insolation, influence the distribution of C3 and C4 plants in southwest Africa. C4 plants dominate in more arid and warmer areas and are favoured by lower pCO2 levels. Several studies have assessed past and present continental vegetation by the analysis of terrestrial n-alkanes in near-coastal deep sea sediments using single samples or a small number of samples from a given climatic stage. The objectives of this study were to evaluate vegetation changes in southwest Africa with regard to climatic changes during the Late Pleistocene and the Holocene and to elucidate the potential of single sample simplifications. We analysed two sediment cores at high resolution, altogether ca. 240 samples, from the Southeast Atlantic Ocean (20°S and 12°S) covering the time spans of 18 to 1 ka and 56 to 2 ka, respectively. Our results for 20°S showed marginally decreasing C4 plant domination (of ca. 5%) during deglaciation based on average chain length (ACL27-33 values) and carbon isotopic composition of the C31 and C33 n-alkanes. Values for single samples from 18 ka and the Holocene overlap and, thus, are not significantly representative of the climatic stages they derive from. In contrast, at 12°S the n-alkane parameters show a clear difference of plant type for the Late Pleistocene (C4 plant domination, 66% C4 on average) and the Holocene (C3 plant domination, 40% C4 on average). During deglaciation vegetation change highly correlates with the increase in pCO2 (r² = 0.91). Short-term climatic events such as Heinrich Stadials or Antarctic warming periods are not reflected by vegetation changes in the catchment area. Instead, smaller vegetation fluctuations during the Late Pleistocene occur in accordance with local variations of insolation.

Recuerdos de infancia y adolescencia en la literatura argentina

Se amplía en este estudio el corpus de memorias de infancia y adolescencia descripto por Raúl Castagnino en su artículo “Evocaciones de infancia y adolescencia en la literatura argentina" de 1982. Los libros que se agregan y analizan son: Descubrimiento del mundo (1987) de Alicia Jurado, Cuando el tiempo era otro; una historia de infancia en la pampa gringa (1999) de Gladys Onega y El país de la ilusión (2005) de María Duprat. En este análisis se aportan nuevos puntos de vista en orden a destacar la reconstrucción epocal que implica cada evocación, las distintas tonalidades presentes en cada texto, la pervivencia del niño en el adulto, de qué manera y para qué fines se observan los memorialistas a sí mismos, de qué índole es la actividad introspectiva, cómo los intereses del adulto seleccionan o recortan los recuerdos, entre otros aspectos. Las tres obras, todas con valor estético, configuran literariamente la etapa fundante de la vida y son interesantes frisos de época, desde los años 20 a los 40 del siglo XX. Son también textos que ponen a prueba las teorizaciones sobre el género, con los aportes de sus propios matices.

(Table 1) Composition of clay minerals in DSDP Hole 75-532

An investigation of the quantitative composition of the coarse (> 40 µm) and clay (< 2 µm) fraction of HPC 532, DSDP Leg 75, in 1300 m water depth on the eastern Walvis Ridge off Southwest Africa yielded the following results: (1) The sediments reflect a complete Latest Miocene to Recent depositional history. Sedimentation rates vary between 2.3 and 7.8 cm/ka. (2) Preservation of calcium carbonate is subject to strong variations: short-term (< 100,000 years) and long-term (about 1 m.y.) cycles in carbonate dissolution have been observed, with strongest dissolution occurring during periods of lowered sea level. (3) Upwelling influence from the near-coastal upwelling centre has been detected by means of the opal content: interglacial periods show high opal contents, because the Benguela Current turned westward at about 20°S and carried opal-laden upwelled water to the west. Sediments from glacial periods, however, show opal minima. Besides these short-term cyclic variations in opal content, long-term cycles have been found, with maximum upwelling influence in the latest Pliocene/early Quaternary. (4) Each CaCO3 dissolution minimum (maximum) is correlated with an opal maximum (minimum) throughout the sediment sequence. (5) The oceanographic system off southwest Africa remained essentially unchanged since the latest Miocene: sea level rose and fell periodically on a small and on a large scale, and the Benguela Current flowed southeast-northwest and turned to the west at the latitude of Site 532 during interglacial periods, when sea level was high. (6) The climate in the near-coastal area of southwest Africa in the latitude of Site 532 has probably been arid throughout the investigated period.

Los detectives salvajes y el ocaso de las vanguardias

Este artículo estudia cómo Bolaño asoció en esta novela la poesía mexicana de las vanguardias históricas del 20, con las neovanguardias de los 60 y los 70 en México. La obsesión de los personajes de esta novela con la poesía se vuelve la razón última de su búsqueda, que es también la búsqueda por el alma de la poesía como modo último de trascendencia en el mundo de la literatura.

Geochemistry of ODP Sites 123-765 and 123-766

The sediments of the Argo and Gascoyne abyssal plains are generally lean in organic matter, are immature, and contain hydrocarbons trapped during sediment deposition rather than those generated during sediment catagenesis. TOC concentrations in the Argo Abyssal Plain Cenozoic sediments are 0.5 wt%, and organic matter appears to be from mixed marine and reworked, degraded, organic matter sources, with the latter being contributed by turbidity flows from the nearby continental margin. TOC concentrations within the Cenozoic sediments of the Gascoyne Abyssal Plain are mostly undetectable (<0.1 wt%). Biomarker distributions determined by gas chromatography (GC) and gas chromatography-mass spectrometry (GCMS) indicate that organic matter extracted from the Lower Cretaceous sediments from both sites is predominantly marine with varying contributions from terrestrial organic matter. The specific marine biomarker, 24-n-propylcholestane is in relatively high abundance in all samples. In addition, the relatively high abundance of the 4-methylsteranes with the 23,24-dimethyl side chain (in all samples) indicates significant dinoflagellate contributions and marine organic matter. The ratios of n-C27/n-C17 reflect relative contributions of marine vs. terrestrial organic matter. TOC, while generally low at Argo, is relatively high near the Barremian/Aptian boundary (one sample has a TOC of 5.1 wt%) and the Aptian/Albian boundary (up to 1.3 wt% TOC), and two samples from the Barremian and Aptian sections contain relatively high proportions of terrestrial organic carbon. TOC values in the Lower Cretaceous sediments from Gascoyne Abyssal Plain are low (<0.1 wt%) near the Aptian/Barremian boundary. TOC values are higher in older sediments, with maxima in the upper Barremian (1.02 wt%), the Barremian/Hauterivian (0.6 wt%), and Valanginian (1.8 wt%). Sediments from the upper Barremian contain higher amounts of terrestrial organic carbon than older sediments.

Sea-surface reconstruction of the east-equatorial South Atlantic

In order to reconstruct Late Quatemary variations of surface oceanography in the eastequatorial South Atlantic, time series of sea-surface temperatures (SST) and paleoproductivity were established from cores recovered in the Guinea and Angola Basins, and at the Walvis Ridge. These records, based on sedimentary alkenone and organic carbon concentrations, reveal that during the last 350,000 years surface circulation and productivity changes in the east-equatorial South Atlantic were highiy sensitive to climate forcing at 23- and 100-kyr periodicities. Covarying SST and paleoproductivity changes at the equator and at the Walvis Ridge appear to be driven by variations in zonal trade-wind intensity, which forces intensification or reduction of coastal and equatorial upwelling, as well as enhanced Benguela cold water advection from the South. Phase relationships of precessional variations in the paleoproductivity and SST records from the distinct sites were evaluated with respect to boreal summer insolation over Africa, movements of southem ocean thermal fronts, and changes in global ice volume. The 23-kyr phasing implies a sensitivity of eastem South Atlantic surface water advection and upwelling to West African monsoon intensity and to changes in the position ofthe subtropical high pressure cell over the South Atlantic, both phenomena which modulate zonal strength of southeasterly trades. SST and productivity changes north of 20°S lack significant variance at the 41-kyr periodicity; and at the Walvis Ridge and the equator lead changes in ice volume. This may indicate that obliquity-driven clirnate change, characteristic for northem high latitudes, e.g fluctuations in continental ice masses, did not substantially influence subtropical and tropical surface circulation in the South Atlantic. At the 23-kyr cycle SST and productivity changes in the eastern Angola Basin lag those in the equatorial Atlantic and at the Walvis Ridge by about 3500 years. This lag is explained by variations in cross-equatorial surface water transport and west-east countercurrent retum flow modifying precessional variations of SST and productivity in the eastem Angola Basin relative to those in the mid South Atlantic area under the central field of zonal trade winds. Sea level-related shifts of upwelling cells in phase with global clirnate change may be also recorded in SST and productivity variability along the continental margin off Southwest Africa. They may account for the delay of the paleoceanogreaphic signal from continental margin sites with respect to that from the pelagic sites at the equator and the Walvis Ridge.

Las huelgas de los estibadores portuarios en el sur santafesino en 1928

El 2 de mayo de 1928 se inicia una huelga de estibadores portuarios en Rosario después de años de tibia actividad sindical. Días más tarde, varios hechos de sangre provocaron la solidaridad obrera con dos paros generales que conmovieron a la ciudad por su agitación y violencia. Los portuarios villenses también se solidarizaron y, un mes más tarde, encabezaron un violento reclamo laboral. El motivo inicial de las huelgas fue el salarial, pero la cuestión de fondo que hilvana a ambas experiencias es la puja social por el deterioro de las condiciones laborales y las imposiciones empresarias en el control y selección de la fuerza de trabajo.En principio la espontaneidad de la protesta tomó por sorpresa a las organizaciones sindicales de izquierda que durante la década del 20 habían mostraban varias fracturas, no obstante será la oportunidad que explica la reorganización y difusión del movimiento obrero con posterioridad. En otro sentido, los conflictos en Rosario y Villa Constitución reflejan la compleja trama de la política santafesina y su conexión con el ámbito laboral. Asimismo, creemos que los sucesos de 1928 tienen una repercusión mayor que la estrictamente local engarzándose en un ciclo de conflictividad que involucra a buena parte de la economía agroexportadora