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Plate tectonic influences on Neoproterozoic-early Paleozoic climate and animal evolution

机译:板块构造对新元古代早古生代气候和动物演化的影响

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The initial diversifi cation of animals paralleled some of the most dramatic episodes of climate and environmental change in Earth history. We compiled global Neoproterozoic-early Paleozoic detrital zircon age data to track spatiotemporal variations in continental arc systems to explore the influence of tectonic outgassing of CO_2 on these climatic shifts. These data indicate that global continental arc systems were spatially reduced at the onset of the Cryogenian glacial interval, widespread during the Cambrian greenhouse, and reduced during Ordovician cooling. The Cambrian greenhouse was coincident with ecologically stressed conditions, whereas Ordovician global cooling was accompanied by a major biodiversifi cation event. Thus, variation in the continental arc CO_2 flux likely played a critical role in major climatic fluctuations, which profoundly influenced early animal evolution.
机译:动物最初的多样化与地球历史上最剧烈的气候和环境变化同时发生。我们收集了全球新元古代-早古生代碎屑锆石年龄数据,以追踪大陆弧系统的时空变化,以探索CO_2构造放气对这些气候变化的影响。这些数据表明,全球低温弧系统在低温冰期开始时在空间上减少,在寒武纪温室中广泛分布,在奥陶纪降温期间减少。寒武纪温室与生态胁迫条件相吻合,而奥陶纪全球降温伴随着重大的生物多样性事件。因此,大陆弧CO_2通量的变化可能在主要的气候波动中起着关键作用,这极大地影响了动物的早期进化。

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