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Sinsk Event

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Huayuan soft-bodied Cambrian biota reveals a diverse deep-sea ecosystem after the first Phanerozoic mass extinction
science2 months ago

Huayuan soft-bodied Cambrian biota reveals a diverse deep-sea ecosystem after the first Phanerozoic mass extinction

The Huayuan biota, a lower Cambrian Burgess Shale–type Lagerstätte from the Yangtze Block in South China, preserves 153 animal species across 16 phyla—51% or more new—mostly soft-bodied with preserved cellular tissues, including radiodonts and pelagic tunicates. This high-diversity, deep-water assemblage, dated shortly after the Sinsk event, links to Burgess Shale faunas via transoceanic dispersal and illuminates Cambrian ecosystem transitions between Ages 3 and 4 and the differential impacts of the first Phanerozoic mass extinction in shallow versus deep settings.

Tectonic Plate Shifts Linked to Ancient Mass Die-Off
science2 years ago

Tectonic Plate Shifts Linked to Ancient Mass Die-Off

New research suggests that a major extinction event 513 million years ago, known as the Sinsk event, was triggered by tectonic activity around the supercontinent Gondwana, causing the drowning of ancient reefs and altering the oceans. The study, led by sedimentologist Paul Myrow, found links between rock layers in Antarctica and Australia, indicating similar geological dynamics at the time of the extinction. The uplift of mountains and the release of greenhouse gases from large igneous provinces led to a decrease in ocean circulation, resulting in the death of many organisms. This sheds light on the role of tectonics in driving mass die-offs and provides insights into potential parallels with modern climate change.