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产自加拿大不列颠哥伦比亚省中寒武统布尔吉斯页岩的一种新型固着滤食生物。

A new stalked filter-feeder from the middle Cambrian Burgess Shale, British Columbia, Canada.

机构信息

Department of Ecology and Evolutionary Biology, University of Toronto, Toronto, Ontario, Canada.

出版信息

PLoS One. 2012;7(1):e29233. doi: 10.1371/journal.pone.0029233. Epub 2012 Jan 18.

DOI:10.1371/journal.pone.0029233
PMID:22279532
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3261148/
Abstract

Burgess Shale-type deposits provide invaluable insights into the early evolution of body plans and the ecological structure of Cambrian communities, but a number of species, continue to defy phylogenetic interpretations. Here we extend this list to include a new soft-bodied animal, Siphusauctum gregarium n. gen. and n. sp., from the Tulip Beds (Campsite Cliff Shale Member, Burgess Shale Formation) of Mount Stephen (Yoho National Park, British Columbia). With 1,133 specimens collected, S. gregarium is clearly the most abundant animal from this locality.This stalked animal (reaching at least 20 cm in length), has a large ovoid calyx connected to a narrow bilayered stem and a small flattened or bulb-like holdfast. The calyx is enclosed by a flexible sheath with six small openings at the base, and a central terminal anus near the top encircled by indistinct openings. A prominent organ, represented by six radially symmetrical segments with comb-like elements, surrounds an internal body cavity with a large stomach, conical median gut and straight intestine. Siphusauctum gregarium was probably an active filter-feeder, with water passing through the calyx openings, capturing food particles with its comb-like elements. It often occurs in large assemblages on single bedding planes suggesting a gregarious lifestyle, with the animal living in high tier clusters. These were probably buried en masse more or less in-situ by rapid mud flow events.Siphusauctum gregarium resembles Dinomischus, another Cambrian enigmatic stalked animal. Principal points of comparison include a long stem with a calyx containing a visceral mass and bract-like elements, and a similar lifestyle albeit occupying different tiering levels. The presence in both animals of a digestive tract with a potential stomach and anus suggest a grade of organization within bilaterians, but relationships with extant phyla are not straightforward. Thus, the broader affinities of S. gregarium remain largely unconstrained.

摘要

伯吉斯页岩型矿床为身体结构的早期进化和寒武纪群落的生态结构提供了宝贵的见解,但仍有许多物种继续挑战系统发育解释。在这里,我们将这个名单扩展到包括一种新的软体动物,Siphusauctum gregarium n. gen. and n. sp.,来自 Mount Stephen(Yoho 国家公园,不列颠哥伦比亚省)的郁金香床(Campsite Cliff Shale 成员,伯吉斯页岩组)。通过收集的 1133 个标本,S. gregarium 显然是该地点最丰富的动物。这个有柄动物(至少长 20 厘米),有一个大的卵形花萼连接到一个狭窄的双层茎和一个小的扁平或球根状固着器。花萼被一个灵活的鞘包围,底部有六个小开口,顶部附近有一个中央终端肛门,周围有不明显的开口。一个突出的器官,由六个具有梳状元件的放射状对称段组成,围绕着一个内部体腔,其中有一个大胃、圆锥形中肠和直肠。Siphusauctum gregarium 可能是一种活跃的滤食动物,水通过花萼开口流过,用梳状元件捕捉食物颗粒。它经常在单个层面上大量聚集,表明群居生活方式,动物生活在高层集群中。这些动物可能是通过快速的泥流事件被集体埋葬在原位。Siphusauctum gregarium 类似于 Dinomischus,另一种寒武纪神秘的有柄动物。主要的比较点包括一个带有包含内脏团和苞片样元件的花萼的长茎,以及类似的生活方式,尽管占据不同的分层水平。在这两种动物中,消化道具有潜在的胃和肛门,这表明在两侧动物中存在组织层次,但与现存门的关系并不简单。因此,S. gregarium 的更广泛亲缘关系在很大程度上仍然没有得到限制。

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1
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2
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Integr Comp Biol. 2007 Nov;47(5):693-700. doi: 10.1093/icb/icm041. Epub 2007 Jun 1.
3
Primitive soft-bodied cephalopods from the Cambrian.寒武纪原始软体头足类动物。
Sci Rep. 2021 Sep 24;11(1):19039. doi: 10.1038/s41598-021-98362-5.
4
A new species of the deuterostome Herpetogaster from the early Cambrian Chengjiang biota of South China.中国南方早寒武世澄江生物群中的一种新的后口动物海鞘纲(Herpetogaster)物种。
Naturwissenschaften. 2020 Aug 28;107(5):37. doi: 10.1007/s00114-020-01695-w.
5
Three Cambrian fossils assembled into an extinct body plan of cnidarian affinity.三个寒武纪化石组合成一个已灭绝的刺胞动物亲缘体计划。
Proc Natl Acad Sci U S A. 2017 Aug 15;114(33):8835-8840. doi: 10.1073/pnas.1701650114. Epub 2017 Jul 31.
6
Gut contents as direct indicators for trophic relationships in the Cambrian marine ecosystem.肠道内容物可作为寒武纪海洋生态系统中营养关系的直接指示物。
PLoS One. 2012;7(12):e52200. doi: 10.1371/journal.pone.0052200. Epub 2012 Dec 26.
7
Cambrian bivalved arthropod reveals origin of arthrodization.寒武纪瓣鳃类节肢动物揭示关节形成的起源。
Proc Biol Sci. 2012 Dec 7;279(1748):4699-704. doi: 10.1098/rspb.2012.1958. Epub 2012 Oct 10.
Nature. 2010 May 27;465(7297):469-72. doi: 10.1038/nature09068.
4
Tentaculate fossils from the Cambrian of Canada (British Columbia) and China (Yunnan) interpreted as primitive deuterostomes.来自加拿大(不列颠哥伦比亚省)和中国(云南)寒武纪的触手状化石被解释为原始的后口动物。
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5
The Burgess Shale anomalocaridid Hurdia and its significance for early euarthropod evolution.布尔吉斯页岩的奇虾类动物赫德虾及其在早期真节肢动物演化中的意义。
Science. 2009 Mar 20;323(5921):1597-600. doi: 10.1126/science.1169514.
6
New burgess shale fossil sites reveal middle cambrian faunal complex.新的布尔吉斯页岩化石遗址揭示了中寒武世动物群复合体。
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7
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8
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9
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10
Paleobiology. Decoding the Ediacaran enigma.古生物学。解读埃迪卡拉纪之谜。
Science. 2004 Aug 20;305(5687):1115-7. doi: 10.1126/science.1102673.