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Bryozoans in transition: The depauperate and patchy Jurassic biota

机译:转型中的苔藓虫:侏儒生物区系绝灭和斑块状

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摘要

Bryozoans were profoundly affected by the end Permian and probably also by the end Triassic mass extinction events. Their recovery in terms of diversity and disparity during the Jurassic was slow and geographically patchy. Critical compilation of data from the published literature reveals only 172 valid species – 160 cyclostomes, 10 ctenostomes and 2 cheilostomes – some as yet not formally named. However, the rate of description of new Jurassic bryozoan species during the last two hundred years implies that many more species remain to be discovered and described. The Jurassic is the only geological period during which cyclostomes were the dominant order and is also important in having the oldest cheilostome bryozoan, the first representative of the order that dominates the modern bryozoan biota. Species diversity peaked in the Bathonian where local assemblages may contain up to 33 species. Encrusters account for 124 (73%) of the 172 Jurassic species, among which small sheet-like forms, especially those assigned to the form-genus 'Berenicea', are the most numerous. The overwhelming predominance in the Jurassic of ‘weeds’ with runner, ribbon or sheet colony-forms is striking. Unlike the Triassic and Cretaceous, large, tree-like or frondose erect colonies are uncommon, and species with fenestrate, articulated and free-living colonies are unknown. Of 92 geographically categorized entries for Jurassic bryozoans in the Zoological Record (1937–2003), 80 (87%) are European records. Outside Europe, diversity appears to have remained low throughout the Jurassic, and nonweedy species are particularly scarce. Compared with the Cretaceous, Jurassic bryozoans show no adaptations that can be interpreted as related to the increased predation pressure associated with the Mesozoic Marine Revolution. The Jurassic bryozoan biota shares characteristics with both the stenolaemate-dominated Palaeozoic–Triassic biota and the cheilostome-dominated Cretaceous–Recent biotas.
机译:苔藓虫受到二叠纪末期以及三叠纪末期生物灭绝事件的深刻影响。在侏罗纪时期,它们在多样性和悬殊性方面的恢复缓慢且地理分布不均。对已发表文献的数据进行的严格汇编显示,只有172个有效物种-160个气旋气孔,10个节肢动物和2个化学风孔-有些尚未正式命名。然而,在过去的200年中,侏罗纪新的苔藓虫新物种的描述速度意味着还有更多的物种有待发现和描述。侏罗纪是唯一一个以气旋成因为主导的地质时期,对拥有最古老的螯龙科巨噬动物也是重要的一环。物种多样性在巴吞尼亚人中达到顶峰,那里的地方组合可能包含多达33个物种。包壳动物占172个侏罗纪物种中的124个(73%),其中小片状形式,尤其是归类于“贝雷尼察”属的形式最多。在“杂草”的侏罗纪中,具有亚军,带状或片状集落形式的压倒性优势是惊人的。与三叠纪和白垩纪不同,大型,树状或弗朗西斯直立的殖民地并不常见,而有先兆,铰接和自由生活的殖民地的物种则是未知的。在《动物学记录》(1937–2003年)中,侏罗纪苔藓动物的92个地理分类条目中,有80个(87%)是欧洲记录。在欧洲以外,整个侏罗纪的生物多样性似乎仍然很低,非杂草物种尤其稀少。与白垩纪相比,侏罗纪的苔藓虫没有适应性变化,可以解释为与中生代海洋革命带来的掠食压力增加有关。侏罗纪的苔藓生物群与以乙二酸酯为主的古生代-三叠纪生物群和以化学吻合动物为主的白垩纪-近代生物群具有共同的特征。

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