International Influences and Drag: Just a Case of Tucking or Binding?

Recently there has been an  internationalisation in the training of UK drag performers. Whilst papers exist focused on drag kings and queens related to their community, few explore how kings/queens train – and fewer still explore international aspects. There are formal courses for drag, but historically this training was informal, present within specific performance communities built around LGBTQ cultures. Tracing dominant figures in such training – the drag mother/father – in order to historicise and contextualise the current explosion in drag performance,the paper argues that the potential globalisation of drag is largely down to the diversification of sources of knowledge available via the internet. Traditionally, performers trained with an established practitioner, where regional variances of drag were passed on. However, current new performers often learn ‘tricks of the trade’ through internet videos posted by people on other continents. In these videos, practitioners pass on their knowledge from the perspective of their locality, as if universal. New kings/queens are not passive in this training and locally infuse their acts, yet historical and local erasures persist. The paper argues that to engage with drag as performance one must be aware of locality and the deep connects drag has with its communities

The topographic evolution of the Tibetan Region as revealed by palaeontology

The Tibetan Plateau was built through a succession of Gondwanan terranes colliding with Asia during the Mesozoic. These accretions produced a complex Paleogene topography of several predominantly east–west trending mountain ranges separated by deep valleys. Despite this piecemeal assembly and resultant complex relief, Tibet has traditionally been thought of as a coherent entity rising as one unit. This has led to the widely used phrase ‘the uplift of the Tibetan Plateau’, which is a false concept borne of simplistic modelling and confounds understanding the complex interactions between topography climate and biodiversity. Here, using the rich palaeontological record of the Tibetan region, we review what is known about the past topography of the Tibetan region using a combination of quantitative isotope and fossil palaeoaltimetric proxies, and present a new synthesis of the orography of Tibet throughout the Paleogene. We show why ‘the uplift of the Tibetan Plateau’ never occurred, and quantify a new pattern of topographic and landscape evolution that contributed to the development of today’s extraordinary Asian biodiversity