峡东寒武纪第二期三管缠绕形壳Anabarites cf. tripartitus的螺旋手性研究
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1.长安大学;2.西北大学

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国家自然科学(编号:42172016,41890844)、中国科学院战略性先导科技专项(B类)项目(编号:XDB26000000)、现代古生物学和地层学国家重点实验室(中国科学院南京地质古生物研究所)开放基金项目(编号:203106)共同资助。


Spiral chirality study of three-lobes helical tube Anabarites cf. tripartitus from the Cambrian Age 2 in Three Gorges
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1.Chang’an University;2.Chang'3.'4.an University;5.Northwest University

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    摘要:

    在现生生物和化石记录中螺旋手性十分常见,然而其发生机制一直悬而未决,尤其是寒武纪早期小壳化石。阿纳巴管类(anabaritids)是一类广布于寒武纪纽芬兰世地层中呈明显三辐射对称的管状化石,前人对该类化石中螺旋扭转属种的研究大多仅限于形态描述,其手性机制讨论甚少。本文依托湖北宜昌寒武系纽芬兰统岩家河组中111枚均为右手螺旋手性的Anabarites. cf. tripartitus,探讨其右手螺旋模式生长机制,认为其螺旋扭转原因并非外部环境所致(水流变化、埋藏作用、科里奥利力),而应从生物自身因素(功能形态学、分子发育生物学)出发探究其固定的右旋不对称性的机制。

    Abstract:

    Helical chirality is common in living organisms today and the fossil record, however this phenomenon has remained almost unstudied, especially in small shelly fossils from the early Cambrian. Anabaritids are a kind of tubular fossils with distinct triradial symmetry, which are known from the early Cambrian strata worldwide. Previous studies on some helical species of anabaritids were mostly limited to morphological descriptions, and the reasons for their helical chirality were poorly discussed. Based on 111 specimens of Anabarites cf. tripartitus from Member 5 of the Yanjiahe Formation (Cambrian Stage 2) in Three Gorges area of Hubei Province, China, the mechanism of their fixed right-handed (dextral) spiral chirality was investigated. The cause of right-handed helical chirality should be inferred from the biological factors (e.g. functional morphology, molecular developmental biology) perspective of molecular genetics, instead of external environmental factors (e.g. water change, taphonomy, Coriolis force).

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  • 收稿日期:2023-03-10
  • 最后修改日期:2023-05-18
  • 录用日期:2023-05-22
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