272 resultados para Ornament


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Three closely allied shallow marine taxa, Neohornibrookella sorrentae (Chapman and Crespin), Neohornibrookella glyphica (Neil), and Neohornibrookella nepeani sp. nov. are recorded from latest early Miocene to late Pliocene strata in southeastern Australia. These taxa, together with Neohornibrookella quadranodosa (Holden) from the Miocene of Midway Island (Northwestern Hawaiian Islands), form a morphologically distinct group of relatively large species (the sorrentae-group) within the genus Neohornibrookella Jellinek. Latitudinal expansion of the subtropical and warm-temperate climatic belts together with the influence of warm western boundary surface currents associated with the North and South Pacific gyres, are likely to have played key roles in the Miocene dispersal of this species group. Species of the sorrentae-group first migrated south from equatorial west Pacific regions into southeastern Australia during the early Miocene, under the influence of the East Australian Current. During three time intervals (i) latest early Miocene, (ii) latest late Miocene and (iii) earliest late Pliocene, forceful pulses of the East Australian Current played a significant role in propelling the widespread distribution of thermophilic Neohornibrookella species across southeast Australian shallow marine realms. During intervening middle and late Miocene times, Neohornibrookella species are only sporadically present across the Bass Strait region of southeast Australia, indicating a weaker East Australian Current influence and the cooling influence of coastal upwelling. During the mid early Pliocene Neohornibrookella species disappeared from the western Bass Strait region, suggesting the complete exclusion of East Australian Current waters from this region. This was probably due to the counteracting influence of the eastward flowing Zeehan Current (extension of the Leeuwin Current) impinging on the western Bass Strait region. This mid early Pliocene palaeobiogeographical partition in Bass Strait, defined by the distribution of sorrentae-group species, is here termed the Bassian Gateway. The two species, N. sorrentae and N. glyphica, occur concurrently during the mid Miocene in southeast Australia, but are associated with different lithofacies. It is hypothesised that there is a heterochronic evolutionary relationship expressed in the ornament of these two species. The thaerocytherid genera Neohornibrookella Jellinek, Tenedocythere Sissingh and Bosasella Bonaduce are here included in the new ostracod subfamily Tenedocytherinae.

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‘The Influence of British Rule on Elite Indian Menswear: The Birth of the Sherwani’ is a study of the influence of politics on fashion and the resulting development of new garments. This research is designed to demonstrate the effect on elite Indian menswear of the two centuries of British rule in India. It is an effort to understand how the flowing garments worn by elite Indian men in the 18th century gradually became more tailored and fitted with the passage of time. The study uses multiple sources to bring to light lesser known facts about Indian menswear, the evolution of different garments and especially of the sherwani. The sherwani is a knee-length upper garment worn by South-Asian men, and is considered to be India’s traditional menswear. My study highlights the factors responsible for the birth of the sherwani and dispels the myth that it was a garment worn by the Mughals. Simultaneously, this study examines the concept and value of ‘tradition’ in cultures. It scrutinises the reasons for the sherwani being labelled as a traditional Indian garment associated with the Mughal era, when in fact it was born towards the end of the 19th century. The study also analyses the role of the sherwani as a garment of distinction in pre- and post-independence India.