• Modern animal life could have origins in

    From ScienceDaily@1:317/3 to All on Wed Mar 23 22:30:44 2022
    Modern animal life could have origins in delta

    Date:
    March 23, 2022
    Source:
    University of Exeter
    Summary:
    The ancestors of many animal species alive today may have lived
    in a delta in what is now China, new research suggests.



    FULL STORY ==========================================================================
    The ancestors of many animal species alive today may have lived in a
    delta in what is now China, new research suggests.


    ==========================================================================
    The Cambrian Explosion, more than 500 million years ago, saw the rapid
    spread of bilaterian species -- symmetrical along a central line, like
    most of today's animals (including humans).

    The 518-million-year-old Chengjiang Biota -- in Yunnan, south-west
    China -- is one of the oldest groups of animal fossils currently known
    to science, and a key record of the Cambrian Explosion.

    Fossils of more than 250 species have been found there, including various worms, arthropods (ancestors of living shrimps, insects, spiders,
    scorpions) and even the earliest vertebrates (ancestors of fish,
    amphibians, reptiles, birds and mammals).

    The new study finds for the first time that this environment was a
    shallow- marine, nutrient-rich delta affected by storm-floods.

    The area is now on land in the mountainous Yunnan Province, but the team studied rock core samples that show evidence of marine currents in the
    past environment.



    ==========================================================================
    "The Cambrian Explosion is now universally accepted as a genuine rapid evolutionary event, but the causal factors for this event have been
    long debated, with hypotheses on environmental, genetic, or ecological triggers," said senior author Dr Xiaoya Ma, a palaeobiologist at the
    University of Exeter and Yunnan University.

    "The discovery of a deltaic environment shed new light on understanding
    the possible causal factors for the flourishing of these Cambrian
    bilaterian animal-dominated marine communities and their exceptional soft-tissue preservation.

    "The unstable environmental stressors might also contribute to the
    adaptive radiation of these early animals." Co-lead author Farid Saleh,
    a sedimentologist and taphonomist at Yunnan University, said: "We can see
    from the association of numerous sedimentary flows that the environment
    hosting the Chengjiang Biota was complex and certainly shallower than
    what has been previously suggested in the literature for similar animal communities." Changshi Qi, the other co-lead author and a geochemist
    at the Yunnan University, added: "Our research shows that the Chengjiang
    Biota mainly lived in a well-oxygenated shallow-water deltaic environment.



    ========================================================================== "Storm floods transported these organisms down to the adjacent deep
    oxygen- deficient settings, leading to the exceptional preservation we
    see today." Co-author Luis Buatois, a paleontologist and sedimentologist
    at the University of Saskatchewan, said: "The Chengjiang Biota, as
    is the case of similar faunas described elsewhere, is preserved in
    fine-grained deposits.

    "Our understanding of how these muddy sediments were deposited has
    changed dramatically during the last 15 years.

    "Application of this recently acquired knowledge to the study of
    fossiliferous deposits of exceptional preservation will change
    dramatically our understanding of how and where these sediments
    accumulated." The results of this study are important because they show
    that most early animals tolerated stressful conditions, such as salinity
    (salt) fluctuations, and high amounts of sediment deposition.

    This contrasts with earlier research suggesting that similar animals
    colonised deeper-water, more stable marine environments.

    "It is hard to believe that these animals were able to cope with
    such a stressful environmental setting," said M. Gabriela Ma'ngano,
    a palaeontologist at the University of Saskatchewan, who has studied
    other well-known sites of exceptional preservation in Canada, Morocco,
    and Greenland.

    Maximiliano Paz, a postdoctoral fellow at the University of Saskatchewan
    who specializes in fine-grained systems, added: "Access to sediment cores allowed us to see details in the rock which are commonly difficult to appreciate in the weathered outcrops of the Chengjiang area." This work
    is an international collaboration between Yunnan University, University of Exeter, the University of Saskatchewan, the Chinese Academy of Sciences,
    the University of Lausanne, and the University of Leicester.

    The research was funded by the Chinese Postdoctoral Science Foundation,
    the Natural Science Foundation of China, the State Key Laboratory of Palaeobiology and Stratigraphy, the Natural Sciences and Engineering
    Research Council of Canada, and by the George J. McLeod Enhancement
    Chair in Geology.


    ========================================================================== Story Source: Materials provided by University_of_Exeter. Note: Content
    may be edited for style and length.


    ========================================================================== Related Multimedia:
    * Arthropod_(Naroia)_fossil ========================================================================== Journal Reference:
    1. Farid Saleh, Changshi Qi, Luis A. Buatois, M. Gabriela Ma'ngano,
    Maximiliano Paz, Romain Vaucher, Quanfeng Zheng, Xian-Guang Hou,
    Sarah E.

    Gabbott, Xiaoya Ma. The Chengjiang Biota inhabited a deltaic
    environment.

    Nature Communications, 2022; 13 (1) DOI: 10.1038/s41467-022-29246-z ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2022/03/220323101241.htm

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