Novel coprolitic records from the Silurian (Přídolí) Wallace Shale of New South Wales

R. Bicknell, Patrick M. Smith, J. Kimmig
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引用次数: 1

Abstract

Abstract Evidence of successful predation or scavenging in the fossil record represents important palaeobiological data to more thoroughly understanding extinct ecosystems. Shelly coprolites are particularly useful indications of durophagous predation in deposits, as they can have a higher preservational potential than their producers. Here we present a new shelly coprolite from the Silurian (Přídolí) Wallace Shale of New South Wales, Australia. This specimen contains abundant fragments of the trilobite Denckmannites rutherfordi Sherwin, 1968 that show limited disarticulation across exoskeletal sections. We propose that a pterygotid eurypterid was the most likely producer of this coprolite, although trilobites and fishes are not completely excluded as possible trace-makers. In documenting this specimen, we highlight that the Wallace Shale likely preserves a more complex palaeoecosystem than previously thought and renewed efforts to understand this deposit are needed in light of this new insight. R.D.C. Bicknell [rdcbicknell@gmail.com], Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, New South Wales, 2351, Australia; P.M. Smith [Patrick.Smith@austmus.gov.au], Palaeontology Department, Australian Museum Research Institute, Sydney, New South Wales, 2010, Australia; Department of Biological Sciences, Macquarie University, Sydney, New South Wales, 2109, Australia; J. Kimmig [julien.kimmig@smnk.de], Abteilung Geowissenschaften, Staatliches Museum für Naturkunde Karlsruhe, Karlsruhe, 76133, Germany.
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新南威尔士志留系(Přídolí)华莱士页岩中新的粪虫记录
化石记录中成功捕食或食腐的证据为更彻底地了解灭绝生态系统提供了重要的古生物学数据。Shelly粪化石是沉积物中硬食性捕食的特别有用的指示物,因为它们比它们的生产者具有更高的保存潜力。本文报道了澳大利亚新南威尔士州志留系(Přídolí)华莱士页岩中发现的一种新的shelly粪化石。该标本包含大量三叶虫denkmannites rutherfordi Sherwin, 1968年的碎片,显示在外骨骼部分有有限的脱臼。虽然三叶虫和鱼类也不完全排除它们可能是粪化石的制造者,但我们认为最有可能产生这种粪化石的是一种翼足类的泛翅类动物。在记录这个标本时,我们强调华莱士页岩可能比以前认为的保存了一个更复杂的古生态系统,并且根据这一新的见解,需要重新努力了解这个沉积物。R.D.C. Bicknell [rdcbicknell@gmail.com],新英格兰大学环境与农村科学学院古科学研究中心,新南威尔士州阿米代尔2351;下午史密斯[Patrick.Smith@austmus.gov.au],澳大利亚博物馆研究所古生物系,悉尼,新南威尔士,2010,澳大利亚;麦考瑞大学生物科学系,新南威尔士州悉尼2109;J. Kimmig [julien.kimmig@smnk.de],德国卡尔斯鲁厄国家博物馆,德国卡尔斯鲁厄,76133。
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