Tea Party imitators? The campaign against the carbon tax,the media and a new uncivil politics

The Gillard government's decision to reverse an election promise to not introduce a carbon tax prompted protest rallies around Australia during 2011–12. Beneath the hyperbole of critics who dismissed these protests as imitating US Tea Party extremism lies an intriguing possibility: that these are each examples of a new form of right-wing political expression enabled by structural changes in the media. This article considers the nature of the anti-carbon tax ‘people's revolt’ and its resemblance to the Tea Party. Both are a hybrid mix of top-down control and bottom-up grassroots populism whose emergence ‘outrage media’ facilitated. In a manner that echoes the support Fox News gave Tea Partiers, talkback radio in Sydney appears to have played a particular role shaping the identity, agenda and uncivil tone of the campaign against the carbon tax.

吉拉德政府决定背弃不征碳税的竞选承诺,在2011-12年引发了全澳大利亚的抗议示威。批评者将示威斥为对美国茶党极端主义的模仿。批评者夸张言辞的背后却是一种有趣的可能：此乃媒体结构变化所造成的、右翼政治表达的新形式。本文思考了反碳税“人民反叛”的性质,以及它与茶党的相似性。二者都是自上而下控制与自下而上草根民粹的混合,“愤怒的媒体”有利于它们的出现。就像狐狸新闻声援茶党那样,悉尼的对讲电台似乎在塑造反碳税运动的身份、议题以及粗暴的口吻方面发挥了特殊的作用。     

A short note on starch and xylem of Ipomoea batatas (sweet potato) in archaeological deposits from northern New Zealand

This study examines preservation of microfossils identified as introduced Ipomoea batatas in soils from northern New Zealand. Starch grains and xylem cells showed highly variable preservation, from good to extremely poor. For starch grains, the latter included brown-staining, expansion and distortion of the grain and vacuole, loss of the Maltese cross, pitting, cracking, fragmentation and disintegration. Degraded xylem showed similar brown-staining, occasional cracking, cross-wise fragmentation, with wall pits becoming progressively less visible or showing distortion, expansion and coalescence.     

Book reviews

Regions in Europe. Patrick Le Galès and Christian Lequesne (Eds). London, Routledge, 1998, 305. pp., ISBN 0 415 16483 4

Unemployment and Social Exclusion: Landscapes of Labour Inequality. Paul Lawless, Ron Martin and Sally Hardy (Eds). London, Jessica Kingsley 1998, 280 pp., £17.95 pb, ISBN 1 85302 341 8

Cities Back from the Edge. Roberta Brandes Gratz (with Norman Mintz). Chichester, John Wiley, 1998, £24.95, ISBN 0 471 14417 7     

Conodonts and tabulate corals from the Upper Ordovician Angullong Formation of central New South Wales,Australia

Zhen, Y.Y., Wang, G.X. &; Percival, I.G., August 2016. Conodonts and tabulate corals from the Upper Ordovician Angullong Formation of central New South Wales, Australia. Alcheringa 41, xxx–xxx. ISSN 0311-5518.

The Angullong Formation is the youngest Ordovician unit exposed in the Cliefden Caves area of central New South Wales. Its maximum age is constrained by a Styracograptus uncinatus graptolite Biozone fauna at the very top of the underlying Malongulli Formation, but the few fossils previously reported from higher in the Angullong Formation are either long-ranging or poorly known. From allochthonous limestone clasts in the middle part of the formation, we document a conodont fauna comprising Aphelognathus grandis, A. solidum, Aphelognathus sp., Aphelognathus? sp., Belodina confluens, Drepanoistodus suberectus, Panderodus gracilis, Panderodus sp., Phragmodus undatus, Pseudobelodina inclinata and Pseudobelodina? sp. aff. P. obtusa, which supports correlation with the Aphelognathus grandis Biozone (late Katian) of the North American Midcontinent succession. The species concepts of Aphelognathus and Pseudobelodina are reviewed in detail. Associated corals are exclusively tabulates, dominated by agetolitids, including Agetolites angullongensis sp. nov., Heliolites orientalis, Hemiagetolites breviseptatus, Hemiagetolites sp. cf. H. spinimarginatus, Navoites sp. cf. N. circumflexa, Plasmoporella bacilliforma, P. marginata, Quepora sp. cf. Q. calamus and Sarcinula sp. Affinities of the coral fauna from the Angullong Formation are closer to faunas from northern NSW and northern Queensland than to the locally recognized Fauna III of late Eastonian age in central NSW. We propose a subdivision of Fauna III to account for this difference, with the late Katian Fauna IIIB characterized by the incoming of agetolitid corals. The currently known distribution of representatives of this group with adequate age constraints suggests that agetolitids possibly originated in North China, subsequently migrating to Tarim, South China and adjacent peri-Gondwanan terranes while also spreading eastward to northern Gondwana, where they progressively moved through eastern Australia to reach the central NSW region by the early Bolindian.

Yong Yi Zhen* (yong-yi.zhen@industry.nsw.gov.au) and Ian G. Percival (ian.percival@industry.nsw.gov.au), Geological Survey of New South Wales, W.B. Clarke Geoscience Centre, 947–953 Londonderry Road, Londonderry, NSW 2753, Australia; Guangxu Wang (gxwang@nigpas.ac.cn), State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road Nanjing 210008 PR China.