TY - JOUR A1 - Melnick, Daniel A1 - Moreno, Marcos A1 - Quinteros, Javier A1 - Carlos Baez, Juan A1 - Deng, Zhiguo A1 - Li, Shaoyang A1 - Oncken, Onno T1 - The super-interseismic phase of the megathrust earthquake cycle in Chile JF - Geophysical research letters N2 - Along a subduction zone, great megathrust earthquakes recur either after long seismic gaps lasting several decades to centuries or over much shorter periods lasting hours to a few years when cascading successions of earthquakes rupture nearby segments of the fault. We analyze a decade of continuous Global Positioning System observations along the South American continent to estimate changes in deformation rates between the 2010 Maule (M8.8) and 2015 Illapel (M8.3) Chilean earthquakes. We find that surface velocities increased after the 2010 earthquake, in response to continental-scale viscoelastic mantle relaxation and to regional-scale increased degree of interplate locking. We propose that increased locking occurs transiently during a super-interseismic phase in segments adjacent to a megathrust rupture, responding to bending of both plates caused by coseismic slip and subsequent afterslip. Enhanced strain rates during a super-interseismic phase may therefore bring a megathrust segment closer to failure and possibly triggered the 2015 event. KW - megathrust KW - earthquake KW - cycle KW - Chile Y1 - 2017 U6 - https://doi.org/10.1002/2016GL071845 SN - 0094-8276 SN - 1944-8007 VL - 44 IS - 2 SP - 784 EP - 791 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Mohr, Christian Heinrich A1 - Korup, Oliver A1 - Ulloa, Hector A1 - Iroume, Andres T1 - Pyroclastic Eruption Boosts Organic Carbon Fluxes Into Patagonian Fjords JF - Global biogeochemical cycles N2 - Fjords and old-growth forests store large amounts of organic carbon. Yet the role of episodic disturbances, particularly volcanic eruptions, in mobilizing organic carbon in fjord landscapes covered by temperate rainforests remains poorly quantified. To this end, we estimated how much wood and soils were flushed to nearby fjords following the 2008 eruption of Chaiten volcano in south-central Chile, where pyroclastic sediments covered >12km(2) of pristine temperate rainforest. Field-based surveys of forest biomass, soil organic content, and dead wood transport reveal that the reworking of pyroclastic sediments delivered similar to 66,500+14,600/-14,500tC of large wood to two rivers entering the nearby Patagonian fjords in less than a decade. A similar volume of wood remains in dead tree stands and buried beneath pyroclastic deposits (similar to 79,900+21,100/-16,900tC) or stored in active river channels (5,900-10,600tC). We estimate that bank erosion mobilized similar to 132,300(+21,700)/(-30,600)tC of floodplain forest soil. Eroded and reworked forest soils have been accreting on coastal river deltas at >5mmyr(-1) since the eruption. While much of the large wood is transported out of the fjord by long-shore drift, the finer fraction from eroded forest soils is likely to be buried in the fjords. We conclude that the organic carbon fluxes boosted by rivers adjusting to high pyroclastic sediment loads may remain elevated for up to a decade and that Patagonian temperate rainforests disturbed by excessive loads of pyroclastic debris can be episodic short-lived carbon sources. Plain Language Summary Fjords and old-growth forests are important sinks of organic carbon. However, the role of volcanic eruptions in flushing organic carbon in fjord landscapes remains unexplored. Here we estimated how much forest vegetation and soils were lost to fjords following the 2008 eruption ofunknownChaiten volcano in south-central Chile. Pyroclastic sediments obliterated near-pristine temperateunknownrainforest, and the subsequent reworking of these sediments delivered in less than a decade similar to 66,000 tC of large wood to the mountain rivers, draining into the nearby Patagonian fjords. A similar volume of wood remains in dead tree stands and buried beneath pyroclastic deposits or stored in active riverunknownchannels. We estimate that similar to 130,000 tC of organic carbon-rich soil was lost to erosion, thus adding to the carbon loads. While much of the wood enters the long-shore drift in the fjord heads, the finerunknownfraction from eroded forest soils is likely to be buried in the fjords at rates that exceed regional estimates by an order of magnitude. We anticipate that these eruption-driven fluxes will remain elevated forunknownthe coming years and that Patagonian temperate rainforests episodically switch from carbon sinks to hitherto undocumented carbon sources if disturbed by explosive volcanic eruptions. KW - Chile KW - Patagonia KW - rainforest KW - volcanic eruption KW - organic carbon KW - biomass Y1 - 2017 U6 - https://doi.org/10.1002/2017GB005647 SN - 0886-6236 SN - 1944-9224 VL - 31 SP - 1626 EP - 1638 PB - American Geophysical Union CY - Washington ER - TY - THES A1 - Schuster, Isabell T1 - Prevalence and Predictors of Sexual Aggression Victimization and Perpetration in Chile and Turkey T1 - Prävalenz und Prädiktoren sexueller Viktimisierung und Ausübung sexueller Aggression in Chile und der Türkei BT - A Cross-Cultural Analysis BT - Eine kulturübergreifende Analyse N2 - Background: Although sexual aggression is recognized as a serious issue worldwide, the current knowledge base is primarily built on evidence from Western countries, particularly the U.S. For the present doctoral research, Chile and Turkey were selected based on theoretical considerations to examine the prevalence as well as predictors of sexual aggression victimization and perpetration. The first aim of this research project was to systematically review the available evidence provided by past studies on this topic within each country. The second aim was to empirically study the prevalence of experiencing and engaging in sexual aggression since the age of consent among college students in Chile and Turkey. The third aim was to conduct cross-cultural analyses examining pathways to victimization and perpetration based on a two-wave longitudinal design. Methods: This research adopted a gender-inclusive approach by considering men and women in both victim and perpetrator roles. For the systematic reviews, multiple-stage literature searches were performed, and based on a predefined set of eligibility criteria, 28 studies in Chile and 56 studies in Turkey were identified for inclusion. A two-wave longitudinal study was conducted to examine the prevalence and predictors of sexual aggression among male and female college students in Chile and Turkey. Self-reports of victimization and perpetration were assessed with a Chilean Spanish or Turkish version of the Sexual Aggression and Victimization Scale. Two path models were conceptualized in which participants’ risky sexual scripts for consensual sex, risky sexual behavior, sexual self-esteem, sexual assertiveness, and religiosity were assessed at T1 and used as predictors of sexual aggression victimization and perpetration at T2 in the following 12 months, mediated through past victimization or perpetration, respectively. The models differed in that sexual assertiveness was expected to serve different functions for victimization (refusal assertiveness negatively linked to victimization) and perpetration (initiation assertiveness positively linked to perpetration). Results: Both systematic reviews revealed that victimization was addressed by all included studies, but data on perpetration was severely limited. A great heterogeneity not only in victimization rates but also in predictors was found, which may be attributed to a lack of conceptual and methodological consistency across studies. The empirical analysis of the prevalence of sexual aggression in Chile revealed a victimization rate of 51.9% for women and 48.0% for men, and a perpetration rate of 26.8% for men and 16.5% for women. In the Turkish original data, victimization was reported by 77.6% of women and 65.5% of men, whereas, again, lower rates were found for perpetration, with 28.9% of men and 14.2% of women reporting at least one incident. The cross-cultural analyses showed, as expected, that risky sexual scripts informed risky sexual behavior, and thereby indirectly increased the likelihood of victimization and perpetration at T2 in both samples. More risky sexual scripts were also linked to lower levels of refusal assertiveness in both samples, indirectly increasing the vulnerability to victimization at T2. High sexual self-esteem decreased the probability of victimization at T2 through higher refusal assertiveness as well as through less risky sexual behavior also in both samples, whereas it increased the odds of perpetration at T2 via higher initiation assertiveness in the Turkish sample only. Furthermore, high religiosity decreased the odds of perpetration and victimization at T2 through less risky sexual scripts and less risky sexual behavior in both samples. It reduced the vulnerability to victimization through less risky sexual scripts and higher refusal assertiveness in the Chilean sample only. In the Turkish sample only, it increased the odds of perpetration and victimization through lower sexual self-esteem. Conclusions: The findings showed that sexual aggression is a widespread problem in both Chile and Turkey, contributing cross-cultural evidence to the international knowledge base and indicating the clear need for implementing policy measures and prevention strategies in each country. Based on the results of the prospective analyses, concrete implications for intervention efforts are discussed. N2 - Hintergrund: Obwohl sexuelle Aggression als ein ernstzunehmendes Problem weltweit angesehen wird, stützt sich die gegenwärtige Datenlage in erster Linie auf Evidenz westlicher Staaten. Für die vorliegende Arbeit wurden die Länder Chile und Türkei anhand theoretischer Überlegungen ausgewählt, um sowohl die Prävalenz als auch Prädiktoren sexueller Aggression zu untersuchen. Das erste Ziel bestand darin, die Ergebnisse früherer Studien zu sexueller Aggression in jedem Land systematisch zu betrachten. Das zweite Ziel war, die Prävalenz von Viktimisierung und Ausübung sexueller Aggression seit dem Schutzalter unter Studierenden in Chile und der Türkei empirisch zu untersuchen. Das dritte Ziel war schließlich die Durchführung von interkulturellen Analysen, um Pfade zu Viktimisierung und Ausübung anhand eines längsschnittlichen Designs zu überprüfen. Methode: Es wurde ein geschlechterinklusiver Ansatz verfolgt, wobei Männer und Frauen sowohl als potentielle Opfer als auch Täter*innen betrachtet wurden. Für die systematischen Reviews wurden mehrstufige Literaturrecherchen durchgeführt. Basierend auf einem vordefinierten Satz an Auswahlkriterien wurden insgesamt 28 Studien für Chile und 56 Studien für die Türkei identifiziert. Weiterhin wurde eine Längsschnittstudie mit zwei Messzeitpunkten durchgeführt, um sowohl die Prävalenz als auch Prädiktoren sexueller Aggression unter Studierenden in Chile und der Türkei zu untersuchen. Selbstberichte über Viktimisierung und Ausübung sexueller Aggression wurden mittels einer spanischen bzw. türkischen Version der Sexual Aggression and Victimization Scale erhoben. Zwei Pfadmodelle wurden konzipiert, in denen riskante Skripts für konsensuelle Sexualkontakte, riskantes Sexualverhalten, sexuelles Selbstwertgefühl, sexuelle Assertivität und Religiosität zu T1 erfasst wurden und als Prädiktoren für Viktimisierung und Ausübung sexueller Aggression in den folgenden 12 Monaten (T2) verwendet wurden, jeweils mediiert durch vergangene Viktimisierung bzw. Ausübung sexueller Aggression. Die Modelle unterschieden sich darin, dass für sexuelle Assertivität unterschiedliche Funktionen für Viktimisierung (Ablehnungsassertivität negativ mit Viktimisierung assoziiert) und Ausübung sexueller Aggression (Initiierungsassertivität positiv mit Ausübung assoziiert) angenommen wurden. Ergebnisse: Die beiden Reviews zeigten, dass Viktimisierung von allen berücksichtigten Studien untersucht wurde, wohingegen kaum Daten zur Ausübung von sexueller Aggression vorlagen. Eine große Heterogenität wurde bei den Viktimisierungsraten, aber auch bei den Prädiktoren festgestellt, was vor allem auf mangelnde konzeptionelle und methodische Konsistenz zwischen den Studien zurückgeführt werden kann. In Bezug auf die Originaldaten zur Prävalenz in Chile zeigte sich, dass 51.9% der Frauen und 48.0% der Männer Viktimisierung angaben. Die Prävalenzraten zur Ausübung lagen bei 26.8% unter Männern und 16.5% unter Frauen. In den türkischen Originaldaten wurde Viktimisierung von 77.6% der Frauen und 65.5% der Männer berichtet. Niedigere Raten wurden erneut für die Ausübung gefunden: 28.9% der Männer und 14.2% der Frauen in der Türkei gaben mindestens einen sexuell aggressiven Übergriff an. Die interkulturellen Analysen zeigten, dass riskante sexuelle Skripts mit einem riskanteren Sexualverhalten assoziiert waren und dadurch indirekt die Wahrscheinlichkeit von Viktimisierung und Ausübung zu T2 in beiden Stichproben erhöhten. Riskantere sexuelle Skripts waren weiterhin mit einer geringeren Ablehnungsassertivität in beiden Stichproben assoziiert, was die Vulnerabilität für Viktimisierung zu T2 indirekt erhöhte. Höheres sexuelles Selbstwertgefühl verringerte die Wahrscheinlichkeit sexueller Viktimisierung zu T2 durch eine höhere Ablehnungsassertivität sowie durch weniger riskantes Sexualverhalten in beiden Stichproben, wohingegen die Wahrscheinlichkeit für Ausübung zu T2 durch eine höhere Initiierungsassertivität größer wurde, allerdings nur in der türkischen Stichprobe. Darüber hinaus verminderte höhere Religiosität die Wahrscheinlichkeit von Viktimisierung und Ausübung zu T2 über weniger riskante sexuelle Skripts und weniger riskantes Sexualverhalten in beiden Stichproben. In der chilenischen Stichprobe wurde die Vulnerabilität für Viktimisierung durch weniger riskante sexuelle Skripts und höhere Ablehnungsassertivität verringert. Hingegen erhöhte sich in der türkischen Stichprobe die Wahrscheinlichkeit für Viktimisierung und Ausübung durch ein niedrigeres sexuelles Selbstwertgefühl. Konklusion: Die Ergebnisse zeigen, dass sexuelle Aggression sowohl in Chile als auch in der Türkei ein weit verbreitetes Problem darstellt. Sie bereichern die internationale Wissensbasis mit interkultureller Evidenz und weisen auf die Notwendigkeit hin, politische Maßnahmen und Präventionsstrategien zu implementieren. Basierend auf den Ergebnissen der prospektiven Analysen werden konkrete Implikationen für Interventionsstrategien diskutiert. KW - Sexual Aggression KW - Prevalence KW - Risk and Vulnerability Factors KW - Chile KW - Turkey KW - Sexuelle Aggression KW - Prävalenz KW - Risiko- und Vulnerabilitätsfaktoren KW - Chile KW - Türkei Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-413897 ER - TY - JOUR A1 - Bernhardt, Anne A1 - Schwanghart, Wolfgang A1 - Hebbeln, Dierk A1 - Stuut, Jan-Berend W. A1 - Strecker, Manfred T1 - Immediate propagation of deglacial environmental change to deep-marine turbidite systems along the Chile convergent margin JF - Earth & planetary science letters N2 - Understanding how Earth-surface processes respond to past climatic perturbations is crucial for making informed predictions about future impacts of climate change on sediment "uxes. Sedimentary records provide the archives for inferring these processes, but their interpretation is compromised by our incomplete understanding of how sediment-routing systems respond to millennial-scale climate cycles. We analyzed seven sediment cores recovered from marine turbidite depositional sites along the Chile continental margin. The sites span a pronounced arid-to-humid gradient with variable relief and related sediment connectivity of terrestrial and marine environments. These sites allowed us to study event related depositional processes in different climatic and geomorphic settings from the Last Glacial Maximum to the present day. The three sites reveal a steep decline of turbidite deposition during deglaciation. High rates of sea-level rise postdate the decline in turbidite deposition. Comparison with paleoclimate proxies documents that the spatio-temporal sedimentary pattern rather mirrors the deglacial humidity decrease and concomitant warming with no resolvable lag times. Our results let us infer that declining deglacial humidity decreased "uvial sediment supply. This signal propagated rapidly through the highly connected systems into the marine sink in north-central Chile. In contrast, in south-central Chile, connectivity between the Andean erosional zone and the "uvial transfer zone probably decreased abruptly by sediment trapping in piedmont lakes related to deglaciation, resulting in a sudden decrease of sediment supply to the ocean. Additionally, reduced moisture supply may have contributed to the rapid decline of turbidite deposition. These different causes result in similar depositional patterns in the marine sinks. We conclude that turbiditic strata may constitute reliable recorders of climate change across a wide range of climatic zones and geomorphic conditions. However, the underlying causes for similar signal manifestations in the sinks may differ, ranging from maintained high system connectivity to abrupt connectivity loss. (C) 2017 Elsevier B.V. All rights reserved. KW - signal propagation KW - turbidity currents KW - Chile KW - sediment-routing system connectivity KW - Last Glacial Maximum Y1 - 2017 U6 - https://doi.org/10.1016/j.epsl.2017.05.017 SN - 0012-821X SN - 1385-013X VL - 473 SP - 190 EP - 204 PB - Elsevier CY - Amsterdam ER -