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The marginalization of the hijra identity in postcolonial Pakistan perpetuates the inequalities that have dogged the transgender community since the colonial era. Although Pakistan has since ratified all concerned UN treaties aimed at protecting transgender people and preventing human rights violations against them, the country’s gender-variant population nevertheless remains vulnerable to these transgressions. As such, this study aims to explore the following inquiry: “What are the lifeways of the hijra community and how do hijra people face human rights violations in their daily life activities?”
The identity construction of the hijra is a complex process. Pakistan is a patriarchal society that determines gender based on biological sex. While a genitally ambiguous child is generally recognized as intersexed, the family usually obscures this circumstance or tries to enforce a predominantly male identity onto the child. To some degree, an intersexed child is allowed to perform feminine roles, particularly when compared to a biologically male individual who is inclined toward femininity. They may partake in “girls’ games” or in “women’s chores” like cooking; they may opt to don feminine clothing and jewelry or practice walking and talking “like a girl.” Many family members and relatives consider such actions a threat to family honor and/or an indication of weakness, which in turn renders the child vulnerable to sexual or physical assault. Abuse also causes some gender-variant children to drop out of school. As adults, many hijras do not see childhood sexual encounters as assault, particularly because they considered themselves to be feminine even from a young age. Nevertheless, experiences of isolation, abuse, and exclusion often compel a gender-variant child to seek company outside of his/her family of orientation.
Many transgender individuals see redemption in joining the hijra community: there, a new identity is defined and shaped. New members mirror themselves after more senior hijras. In the community, relationships are solidified through similar childhood experiences and interests as well as a shared freedom to express the outer reflection of an “inner feminine soul.” Here, they accept the childhood label affixed to them by heteronormative society: hijra. In fact, the identity now becomes the key to economic viability and socialization.
The predominant livelihood strategies within the hijra community are dancing and prostitution. New members must adhere to stringent norms and rules; they risk (sometimes severe) punishment if they do not. For example, a new hijra must adopt a very strict feminine appearance; if she does not appear feminine enough she may be socially isolated or physically punished. Similarly, a hijra is required to remain passive during sex. In fact, because hijras are stereotyped as passive and vulnerable, many clients physically exploit or even rape them. If she tries to resist, a hijra may face physical violence and, in extreme circumstances, death. Reporting abuse to law enforcement authorities often leads to further exploitation. As such, whether dancing or performing sexually, hijras are encouraged to do whatever is asked of them.
In the last decade, the Supreme Court of Pakistan has taken significant steps to ensure the rights of transgender people. The Court has similarly compelled local governments to amend existing legislation in order to protect the transgender community. Nevertheless, discrepancies exist in legislative and judicial interpretations of the transgender identity, which continues to impede the struggle for basic rights. Indeed, there is a long way to go in the effort to incorporate transgender people into the folds of mainstream Pakistani society.
Die Dissertation stellt das Machtgeflecht in der Islamischen Stadt Marawi City (Mindanao, Philippinen) dar, in die die dortigen Gender-Debatten involviert sind. In einer Umgebung, die als Konsequenz des Mindanao Konfliktes als “no war, no peace”-Umgebung definiert werden kann, gibt es drei Hauptdarsteller: die nationale Regierung des mehrheitlich christlichen Staates der Philippinen (GRP), die Autonome Regierung im Muslimischen Mindanao (ARMM), zu der auch Marawi City zählt, und die islamische Rebellengruppe Moro Islamic Liberation Front (MILF), die einen islamischen (unter-)Staat fordert. Die GRP unterstützt Re-Islamisierungs- und Re-Traditionalisierungsbewegungen in der ARMM, um die Opposition zur MILF zu stärken. Die Konsequenz ist jedoch keine Kollaboration zwischen der GRP und der ARMM. Stattdessen nutzen Politiker ihre Privilegien aus, um ihren eigenen Absichten zu folgen. Sei dies, um politische Gegner auszuspielen oder das traditionelle Sultanatssystem zu fördern. Für Gender-Debatten gibt es in diesem Kontext der ungelösten nationalen Frage kaum Spielraum außerhalb einer Islamischen Narrative; dies bedeutet jedoch nicht, dass Gender nicht debattiert wird, sondern, dass die Debatten inner-Islamisch sind, hauptsächlich zwischen Repräsentanten des traditionell synkretistischen Islam und Vertretern Islamischer Revitalisierungsbewegungen. Speziell erstere erscheinen sehr einflussreich bezüglich Gender Strategien in der Region. Dies ist nur teilweise auf die Unterstützung der nationalen Regierung zurückzuführen, sondern ist vor allem eine Frage von Identität. Diese wiederum wird nicht vorranging über Religion, sondern nach ethnischen Maßstäben und im Speziellen im Rahmen von Clanstrukturen definiert.
The geodynamic processes and the chemical and thermal evolution of the mantle beneath the Kaapvaal craton (South Africa) was investigated with further regard to diamond formation. For this, 31 coarse-grained peridotites and 21 individual subcalcic garnets from heavy mineral concentrates (HMC) from the Finsch mine were studied for their major and trace element compositions, Lu-Hf and Sm-Nd isotope composition. Furthermore, processes in the Earth’s mantle that follow kimberlite sampling and propagation were studied in polymict peridotite breccia from Kimberley mines. Inter mineral equilibrium of the peridotites was tested by comparing the results from different, independent thermometers. These, well equilibrated peridotites stem from a restricted pressure of 5 to 6.5 GPa (depth ~160-200 km) and a temperature range of 1050-1250°C, following the 40 mW/m2 conductive geotherm. The majority of the samples display a well developed anti-correlation of oxygen fugacity with pressure, which is in contrast to the sheared and oxidised, younger kimberlite erupted peridotites from Kimberley. All analysed samples have homogeneous trace element mineral chemistry. Variations in trace elements among Finsch peridotites reflect their complex nature and the intricate development of the subcratonic mantle. The 3.6 Ga is the oldest crustal age recorded in the Kaapvaal craton, and is confirmed by the Lu-Hf model age of a highly radiogenic subcalcic garnet in this study. Therefore, this age probably represents the oldest depletion (partial melting event) of the subcratonic mantle beneath the Kaapvaal craton. Both, subcalcic garnets and Finsch peridotites yield Lu-Hf isochron ages of around 2.5 Ga, which probably represent the last depletion event of the Kaapvaal craton. Several older (than 2.5 Ga) depletions were also necessary to explain higher isochron initials of the both isochrones. The Cr# and HREE concentrations and ratios of the Finsch subcalcic garnets and peridotites indicate that partial melting of the Kaapvaal craton happened at different depths. One group of subcalcic garnets (group-1) experienced depletion at high pressure in the garnet stability field and another one (group-2) at low pressures in the spinel or plagioclase stability field. Major and trace elements indicate that up to 50%, of the melt was remover from the primitive (primer) mantle in at least two melting events. Thus, first continental crust was created early (> 2.5 Ga) from high degrees of partial melting of the lithospheric mantle. According to the Sm-Nd isotope signatures at least two metasomatic events took place significantly after 2.5 Ga. As monitored by group-1 subcalcic garnets, the first enrichment was produced by a fluid and occurred at around 1.3 Ga. The second metasomatic event was much later at 500-300 Ma ago and has changed both Nd and Hf isotopic compositions of group-2 subcalcic garnet as well as some Finsch peridotites. During partial melting any carbon species will be dissolved in the melt and removed from the residue. Therefore, any diamond growth before the last depletion (~2.5 Ga) would have been probably completely removed from the lithospheric mantle. Consequently, carbon was apparently reintroduced into the system, i.e. during Metasomatism, and triggered the growth of diamonds. The Sm-Nd isotope systematics of the subcalcic garnets of this study indicates that enrichment occurred at ~1.3 Ga or later, which implies non-Archean, late diamond growth in Finsch. Fertilisation of the subcontinental craton associated with the percolation of group-2 (~120 Ma) or even younger (~90 Ma) group-1 kimberlites and their precursors are not observed in Finsch peridotites, but are well presented in mantle xenoliths from Kimberley. Therefore, these younger events were studied on specific mantle xenoliths, polymict breccia from Kimberley. A polymict peridotite found at the Boshof road dump, Kimberley, represents a mechanical mixture of upper mantle clasts and minerals (opx, cpx, garnet and olivine) of different lithologies, cemented by fine-grained olivine and minute amounts of interstitial ilmenite, phlogopite and sulphide. According to Ni in garnet thermometry, single porphyroclastic garnets were sampled and mixed during ascent in a 100 km stratigraphic column, starting from ~250 km until ~120 km. During this ascent, melt has reacted with the porphyroclasts and at theirrims neoblastic minerals were formed, i.e. neoblastic opx around opx porphyroclast, neoblastic garnet around garnet porphyroclast, and neoblastic opx around cpx porphyroclast. Analyses of those neoblastic minerals indicate that volatile-rich, kimberlite-like melt was the agent that collected the mantle minerals and amalgamated this xenolith. Several complex processes were responsible for the formation of the polymict breccia. They comprise melt degassing at high pressures that probably created “explosive” Brecciation of the cratonic roots (~250 km), propagation of the melt that collected different porphyroclasts on a way and amalgamation at around 120 km. The whole process of “explosive” brecciation, turbulent transport and mixing of mantle porphyroclasts and melt, porphyroclast dissolution and neoblast precipitation happened very fast and was part of the kimberlite formation. Therefore, the here studied sample probably represents one frozen part (with variable mantle clasts) of the kimberlitic magma precursor, with kimberlite eruption at ~90 Ma years ago in Kimberley.
The Way of the Beer analyses how Mafa re-enact their history in the ritual transfer of sorghum beer from junior to senior members of their society. Beer is the ‘Eucharist’ of Mafa religion, standing for the linkage between God, the ancestors, the fertility of the living and the agricultural land. The ritual sequences in which beer is exchanged and offered at family and community shrines are an encoding of settlement history. The CD-ROM version of the "Way of the Beer" not only contains everything found in the printed version of this work, but also a digital map (figure 8) whichis too large to be printed. The key to the digital map (figure 9) is electronically linked to the map. Please note that figure 9 is displayed when the option "key", found under each ward name (in the bookmark section of figure 8), is activated. If this is done for the first time, figure 8 needs to be brought up again in order to be tiled next to figure 9. However, the best option for exploring the map is to print out the key. Please refer to "The Way of the Beer"(pages 142-144) for further information on how the large digital map needs to be read. The text, maps and images can be viewed in Word (please install the linguistic fonts before using the Word version) or Acrobat Reader (version 4.0 has beencopied on to the CD-ROM). The CD-ROM also contains version 1.03 of the Northern Mandaras Homepage which must be viewed with Microsoft Explorer. The CD-ROM is organised in five main folders which are labelled "Text", "Figures", "Tables", "Plates" and "Homepage". Each folder contains a Word 97 as well as an Adobe Acrobat version of "The Way of the Beer". It is only the large digital map which does not exist as a Word but only as an Adobe Acrobat version. The page numbering apart from figure 8) continues through the sections, beginning with the text and ending with the plates.