The strongest support in the paper is temporal coupling: supracrustal deformation onset in both the Ross Orogen (Antarctica) and the Delamerian Orogen (southern Australia) is biostratigraphically tied to the Pararaia janeae trilobite Zone within Series 2 Stage 4, and the authors argue this interval overlaps the first/oldest Kalkarindji LIP activity they cite as beginning as early as ~514β513 Ma.
However, the causal chain remains inferential: the paper must bridge from (i) tectonic/reef drowning and (ii) ocean redox/climate proxies to (iii) extinction selectivity at global scale. Independent functional-diversity work on the Sinsk Event shows a decoupling where ecosystem functioning (functional richness) declines differently than taxonomic diversity, supporting major biotic restructuringβbut it does not directly validate the tectonic-trigger mechanism.
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