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The Earth’s magnetic field (EMF) is generated by convections in the electrically conducting liquid iron-rich outer core, modified by the Earth’s rotation. A drastic manifestation of the dynamics of this fluid body is the occurrence of geomagnetic field reversals in the Earth’s history but also geomagnetic excursions, which are more frequent features of otherwise stable polarity chrons, but often poorly constrained in the geological record. To better understand the origin of the field, we need to know how the field has varied on different geological timescales. This includes not only information about changes in the ancient field’s direction but also about the absolute intensity (palaeointensity) and the age. This palaeointensity record is needed for compiling a full-vector description of the field. A palaeomagnetic and palaeointensity study on lava flows allows gaining insights about the evolution of the EMF through time and space. However, constraining the EMF evolution over different geological timescales remains a difficult objective due to the paucity of available palaeointensity data. One new alternative approach in palaeointensity studies is the recently proposed multispecimen parallel differential pTRM (MS) method, which has potentially several advantages over the commonly used Thellier method, because it is in theory independent of magnetic domain state, less prone to biasing effects, such as thermal alteration and significantly faster to perform in the laboratory. A study of highly active volcanic regions, such as the Trans-Mexican Volcanic Belt, seems promising when attempting a full-vector reconstruction or when looking for field excursions. One aim of this thesis was to gain new information about the occurrence and global validity of geomagnetic excursions from the Brunhes- or Matuyama Chron. For this purpose some 75 lava flows from within the Trans-Mexican Volcanic Belt were sampled for palaeomagnetic analyses. The scatter of virtual geomagnetic poles from lavas younger than 1.7 Ma was used for estimating palaeosecular variation and was found to be consistent with latitude dependent Model G and other high quality palaeomagnetic data from Mexico. The palaeomagnetic mean-vectors of 56 lavas were correlated to the Geomagnetic Polarity Timescale supplemented with information on geomagnetic excursions. On the grounds of their associated radioisotopic ages, four lavas were tentatively correlated with known excursions from marine records. Two lava flows dating of Brunhes Chron were associated with the Big Lost and Delts/Stage 17 excursions, respectively. From further two flows dating of Matuyama Chron, one flow was associated with either the Santa Rosa- or Kamikatsura excursions, while the other could have been emplaced during the Gilsa excursion. The most significant outcome was the finding that both Brunhes excursional flows display nearly fully reversed directions that deviate almost 180°C from the expected normal polarity direction. This observation could indicate that in particular the Big Lost and Delta/Stage17 excursions may represent other short periods during which the field completed a full reversal for a short time, such as was previously found for other older cryptochrons or tiny wiggles. Another focus of this thesis was set on estimating the feasibility of the new MS method for routine palaeointensity determination. This was accomplished by applying the MS method to samples from 11 historical lava flows from Mexico and Iceland from which the actual field intensity was either known from contemporary observatory data, or deduced from magnetic field models. Comparing observed with expected intensity values allowed to test the accuracy of the MS method. It a was found that the majority of palaeointensity estimates after the MS method yielded results that were very close or indistinguishable within the range of uncertainty from the expected values. However, a general trend towards an overestimate in the palaeointensity was also observed, which, on the grounds of corroborating rock magnetic analyses, was associated with multidomain material. This observation was taken as first evidence that the MS method is not entirely independent of magnetic domain state, as was originally claimed. However, a second experiment in which a modification of the most widely used Thellier method was applied to sister samples from 5 Icelandic flows revealed that, in comparison to the MS method, the latter produced more accurate and statistically better defined palaeointensities. Thus, from these first results, the MS method appeared as a viable alternative for future palaeointensity studies. Subsequently it was attempted to corroborate the directional record from Mexican lavas with palaeointensity data. It was possible to acquire palaeointensity estimates for 32 out of 51 investigated lava flows. These new results revealed that the new MS palaeointensities for Mexico are, with a high degree of statistical significance, around 30% higher than expected. The generally high palaeointensities seem to corroborate the results obtained from historical lava flows in this study and other previous studies on synthetic samples where domain state effects were found to cause overestimates in the palaeointensity of up to 30 per cent in the MS method. The primary process that leads to this overestimate is assigned to an asymmetry in the demagnetisation and remagnetisation process. Yet, this overestimate is expected to be no larger than what might be expected from Thellier experiments performed on samples with a given degree of multidomain behaviour.
The military in Mexico started out as a revolutionary army that secured the regime of the governmental party PRI. The article discusses the change of this army into a national and hemispheric police force under the influence of the USA. Today, the functions of the Mexican army are a mix of fighting against drugs, organized delinquency, terrorism and counterinsurgency and cooperating with US as well as other Latin American forces.
We present varve chronologies for sediments from two maar lakes in the Valle de Santiago region (Central Mexico): Hoya La Alberca (AD 1852-1973) and Hoya Rincn de Parangueo (AD 1839-1943). These are the first varve chronologies for Mexican lakes. The varved sections were anchored with tephras from Colima (1913) and Paricutin (1943/1944) and (210)Pb ages. We compare the sequences using the thickness of seasonal laminae and element counts (Al, Si, S, Cl, K, Ti, Mn, Fe, and Sr) determined by micro X-ray fluorescence spectrometry. The formation of the varve sublaminae is attributed to the strongly seasonal climate regime. Limited rainfall and high evaporation rates in winter and spring induce precipitation of carbonates (high Ca, Sr) enriched in (13)C and (18)O, whereas rainfall in summer increases organic and clastic input (plagioclase, quartz) with high counts of lithogenic elements (K, Al, Ti, and Si). Eolian input of Ti occurs also in the dry season. Moving correlations (5-yr windows) of the Ca and Ti counts show similar development in both sequences until the 1930s. Positive correlations indicate mixing of allochthonous Ti and autochthonous Ca, while negative correlations indicate their separation in sublaminae. Negative excursions in the correlations correspond with historic and reconstructed droughts, El Nio events, and positive SST anomalies. Based on our data, droughts (3-7 year duration) were severe and centred around the following years: the early 1850s, 1865, 1880, 1895, 1905, 1915 and the late 1920s with continuation into the 1930s. The latter dry period brought both lake systems into a critical state making them susceptible to further drying. Groundwater overexploitation due to the expansion of irrigation agriculture in the region after 1940 induced the transition from calcite to aragonite precipitation in Alberca and halite infiltration in Rincn. The proxy data indicate a faster response to increased evaporation for Rincn, the lake with the larger maar dimensions, solar radiation receipt and higher conductivity, whereas the smaller, steeper Alberca maar responded rapidly to increased precipitation.
Inhalt:
Eberhard Knobloch: Der Briefwechsel zwischen Alexander von Humboldt und Charles Lyell: Ein Überblick
Alejandro Cheirif Wolosky: La recepción humboldtiana de Cristóbal Colón
Luiz Estevam O. Fernandes: Political Essay on the Kingdom of New Spain: Humboldt and the history of Mexico
Dominik Erdmann/Christian Thomas: „… zu den wunderlichsten Schlangen der Gelehrsasmkeit zusammengegliedert“. Neue Materialien zu den ‚Kosmos-Vorträgen‘ Alexander von Humboldts, nebst Vorüberlegungen zu deren digitaler Edition
Konstantin Treuber „Warum ich nicht Diorit-Trachyt sagen soll.“ – Ein geologischer Brief Gustav Roses an Alexander von Humboldt
Anja Werner: Alexander von Humboldt’s Footnotes: “Networks of Knowledge” in the Sources of the 1826 Essai politique sur l’île de Cuba
Peter Honigmann: Alexander von Humboldts Journale seiner russisch-sibirischen Reise 1829 [mit einer Einführung von Eberhard Knobloch]
-Ulrich Päßler, Ingo Schwarz: Ein Brief Alexander von Humboldts an Charles-Guillaume Étienne
-Ottmar Ette: Alexander von Humboldt im Archiv. Die Entstehung eines neuen Humboldt-Bildes aus dem mobilen Blick in vergangene Zukünfte
-Miguel Ángel Puig-Samper: Humboldt and his geographical album of New Spain
-Karin Reich: Die Beziehungen zwischen Alexander von Humboldt und Hans Christian Ørsted: Treffen, Briefwechsel
-Kurt-R. Biermann: Die Datierung der Briefe Alexander von Humboldts – dargestellt als Modellfall für die editorische Bearbeitung naturwissenschaftlicher Briefe und Dokumente
Inhalt:
Alexander von Humboldt-Forschungsstelle: Ingo Schwarz zum 65. Geburtstag
Ottmar Ette: Findung und Erfindung einer Leserschaft. Neuere Editionsprojekte zu Alexander von Humboldt als Grundlage und Herausforderung künftigen Forschens
Eberhard Knobloch: Alexandre de Humboldt et le Marquis de Laplace
Oliver Schwarz: Alexander von Humboldt als astronomischer Arbeiter, Diskussionspartner und Ideengeber
Petra Werner: Innenwelten und bleiche Gärten. Alexander von Humboldt untertage und in der Caripe-Höhle
Christian Suckow: Alexander von Humboldt in Ust’-Kamenogorsk
Anne Jobst: Neue Briefe Christian Gottfried Ehrenbergs an Alexander von Humboldt
Thomas Schmuck: Humboldt, Baer und die Evolution
Manfred Ringmacher: Zwei Briefe auf Guaraní in Alexander von Humboldts Handschrift
Ute Tintemann: Julius Klaproths Mithridates-Projekt, Alexander von Humboldt und das Verlagshaus Cotta
Ulrike Leitner: „Ja! Wenn Berlin Bonn wäre!“ Friedrich Rückerts Berufung nach Berlin
Frank Holl: „Zur Freiheit bestimmt“ – Alexander von Humboldts Blick auf die Kulturen der Welt
Sebastian Panwitz: Das Humboldt-Mendelssohn-Haus Jägerstraße 22. Ein Quellenfund
Laura Péaud: Du Mexique à l‘Oural : l‘expertise humboldtienne au service du politique
Bärbel Holtz: „Cicerone“ des Königs? Alexander von Humboldt und Friedrich Wilhelm III.
Menso Folkerts: Ein unerwartetes Zusammentreffen in Sanssouci. Alexander von Humboldt und Karl Ludwig Hencke an der Tafel Friedrich Wilhelms IV.
Ulrich Päßler: Preußens Mann in Washington. Fünf Briefe Friedrich von Gerolts an Alexander von Humboldt (1858/1859)
Bill Roba: German-Iowan Strategies in Celebrating the Centennial of Alexander von Humboldt’s Birth
Regina Mikosch: Ingo Schwarz‘ Veröffentlichungen zur Alexander von Humboldt
Über die Autoren
During his trip to New Spain in 1803, Alexander von Humboldt visited large tracts of New Spanish territory, which includes modern Mexico and part of the United States. This trip provided the data for his geographical Atlas of the region, as well as information about the ancient Mexican cultures that he would later include in the general Atlas and in other major works, such as Vues des Cordillères. Likewise, Humboldt’s Political Essay on the Kingdom of New Spain displayed a comprehensive physical, natural, economic, and social description of Mexico in the colonial period, which will also be analysed. With these works, Humboldt presented a new geographical and cultural image of New Spain to the European audiences. In addition to this, his work made important contributions to cartographic knowledge.
Migration ist ein weltweites Phänomen. Der Politikwissenschaftler Christian Kube betrachtet sie in „Immigration und Arbeitskämpfe in den USA“ am Beispiel mexikanischer Einwanderer in Kalifornien. Der Autor analysiert das Verhältnis zwischen Arbeitern aus Mexiko und der US-amerikanischen Arbeiterbewegung, insbesondere den Gewerkschaften. Er tut dies an zwei Fallbeispielen, in denen Gewerkschaften versuchten bzw. versuchen, in Kalifornien transnationale Arbeiter zu organisieren: Zum einen wird das Los Angeles Manufacturing Project (LAMAP) betrachtet, zum anderen der immer noch andauernde Arbeitskampf in der Mandelfabrik Blue Diamond Growers (BDG) in Sacramento/Kalifornien. Abschließend wird die Frage beantwortet, ob die traditionellen Gewerkschaften der USA für die Interessenvertretung und Integration von Menschen mit Migrationshintergrund im Niedriglohnsektor geeignet sind. Christian Kube ist der Ansicht, dass sie einen wesentlichen Beitrag zur Organisation transnationaler Arbeiter leisten müssen, da es derzeit keine annähernd so mitgliederstarken Institutionen wie die Gewerkschaften in den USA gibt.
Literaturbericht Rezensierte Literatur: Nikolaus Werz: Lateinamerika. Eine Einführung, Nomos Verlagsgesellschaft, Baden-Baden 2005, 400 S., ISBN 3-8329-1068-9 Klaus Bodemer/Detlef Nolte/Hartmut Sangmeister (Hrsg.): Lateinamerika Jahrbuch 2004, Vervuert, Frankfurt a.M. 2004, 385 S., ISBN 3-86527-123-5 Peter Imbusch/Dirk Messner/Detlef Nolte (Hrsg.): Chile heute. Politik, Wirtschaft, Kultur, Vervuert, Frankfurt a.M. 2004, 957 S., ISBN 3-89354-590-5 Walther L. Bernecker/Marianne Braig/Karl Hölz/Klaus Zimmermann (Hrsg.): Mexiko heute. Politik, Wirtschaft, Kultur, Vervuert, Frankfurt a.M. 2004, 3. vollständig neu bearbeitete Auflage, 826 S., ISBN 3-86527-140-5 Rafael Sevilla/Andreas Boeckh (Hrsg.): Venezuela – die Bolivarische Republik, Horlemann, Bad Honnef 2005, 322 S., ISBN 3-89502-197-0
Isabel Lake is a hypersaline crater-lake on Isabel Island, Mexico, situated in the eastern tropical Pacific, an area highly sensitive to hydrological changes. Today, annual rainfall mostly occurs during the wet season, from June to October, when the northern edge of the Intertropical Convergence Zone (ITCZ) extends over the island. In order to evaluate the potential of sedimentary lipid biomarker signatures as a proxy of past hydro-climatic variability we have performed a calibration analysis comparing changes in biomarker distribution in the upper 16 cm of the sediment core with a regional instrumental data set. Annual laminations present in the sediment sequence allow for precise chronological control (1942-2006), More than 80 different lipid compounds were identified in the sediment and could be assigned to three major groups of source organisms: (1) algal populations; (2) a mixed community of ciliates, bacteria and cyanobacteria; and (3) photosynthetic sulfur bacteria. We found that the observed changes in the. relative contribution of the different lipid biomarkers to the sediment record were determined by the regional rainfall variability over the last 65 years. The planktonic community of Isabel Lake was highly sensitive to salinity fluctuations related to rainfall variability; seasonal precipitation results in freshwater input into the lake, driving an annual algal bloom and a relative decrease in the abundance of the more halotolerant populations of (cyano) bacteria and ciliates. Consequently, the concentration ratio between the two most abundant biomarkers in the Isabel Lake sediments, n-alkyl diols and tetrahymanol (which we define as the DiTe index), representing algal and ciliate planktonic populations, respectively, was significantly correlated with the seasonal rainfall anomaly (r = 0.68, p < 0.01). We propose that the DiTe index is a proxy of changes in the aquatic ecosystem of Isabel Lake and, by extension, regional hydrological changes in a sensitive climatic area of the eastern tropical Pacific.
This article investigates the fictional narratives written by „Sub-commandante Marcos“ of the Zapatista movement EZLN. It is shown that Marcos uses three distinct frames of reference in his fictional account of the Zapatista guerrilla: an ethnic, a national and a post-national one. Contrary to other studies that emphasize the harmony between the three levels, it can be argued that there exists a fundamental tension between them. There is a tension between the ethnic discourse and the Mexican nationalist discourse which envisions a nation rather than a nation dominated by a single ethno-cultural group. Finally, it can be deduced from these tensions that the EZLN guerrilla is subject to divergent pressures.
Wahlen im Schatten des organisierten Verbrechens : Mexiko zwischen State Capture und Staatsversagen
(2012)
Kurz vor der Wahl am 1. Juli steht Mexiko vor großen Turbulenzen: Parteien beschuldigen sich gegenseitig, Mitglieder oder -läufer der organisierten Kriminalität zu sein. Der Krieg gegen die Drogen, der zuvor noch nationale Einheit heraufbeschwor, wird jetzt zum Instrument der Verleumdung des politischen Gegners. Wie kann angesichts brüchiger Staatlichkeit eine sichere Wahl gewährleistet werden?