来自冈瓦纳志留纪和泥盆纪的新翼手目海蝎

IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Russell D.C. Bicknell , Patrick M. Smith , Aaron Goodman , Izak Schoon , Yong Yi Zhen
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引用次数: 0

摘要

海蝎(eurypterids)是一类已灭绝的水生螯足类动物,其化石记录跨越奥陶纪到二叠纪末期。由于其体型和保存潜力,欧洲和北美的沉积物中都有关于海龙类的详细记录,而冈瓦纳的证据则较少。澳大利亚化石记录中关于该类群的证据尤其有限。为了纠正这种情况,我们报告了来自新南威尔士州 Mulga Downs 组晚期志留纪华莱士页岩和早期泥盆纪 Merrimerriwa 地层的翼龙类新实例。这些标本被归入 sp.(华莱士页岩)和 c.f.(Merrimerriwa地层,Mulga Downs 组)。我们利用这些材料探讨了这些大型浮游食蚁兽的广泛分布和扩散情况,并考虑了这些动物在其各自的古生态系统中的位置。我们的结论是,这些新记录证明了澳大利亚沉积物中大型节肢动物的多样性,需要对这些稀有化石进行持续记录,以进一步了解澳大利亚的古生代。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Novel pterygotid sea scorpions from the Silurian and Devonian of Gondwana

Novel pterygotid sea scorpions from the Silurian and Devonian of Gondwana

Sea scorpions (eurypterids) are a group of extinct aquatic chelicerates that have a fossil record spanning the Ordovician through to the end Permian extinction. Due to their size and preservational potential, eurypterids have been well-documented in European and North American deposits, with less evidence from Gondwana. There is particularly limited evidence of the group from the Australian fossil record. To rectify this, we report new examples of pterygotid eurypterids from the late Silurian Wallace Shale and Early Devonian Merrimerriwa Formation, Mulga Downs Group in New South Wales. These specimens are assigned to Pterygotus sp. (Wallace Shale) and Jaekelopterus c.f. rhenaniae (Merrimerriwa Formation, Mulga Downs Group). The material is used to explore the extensive distribution and dispersal of these large, pelagic eurypterids and consider the position of the animals in their respective paleoecosystems. We conclude that these new records evidence the diversity of larger arthropods in Australian deposits and that ongoing documentation of these rare fossils is required to further understand the Paleozoic of Australia.

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来源期刊
Gondwana Research
Gondwana Research 地学-地球科学综合
CiteScore
12.90
自引率
6.60%
发文量
298
审稿时长
65 days
期刊介绍: Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.
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