Lithium isotope constraints on the plumeworld hypothesis for the Marinoan Snowball Earth
Tian Gan,
Meng Tian,
Xi-Kai Wang
et al.
Abstract:The Snowball Earth hypothesis predicts that continental chemical weathering was curtailed substantially during but rebounded strongly after the Marinoan ice age some 635 million years ago. Defrosting the planet would result in a plume of fresh glacial meltwater with a different chemical composition than underlying hypersaline seawater, generating an onshore-offshore geochemical gradient. Here we test the plumeworld hypothesis using lithium isotope abundances in the basal Ediacaran Doushantuo cap dolostone that… Show more
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