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• W2072401076 abstract "Significance The snowball Earth hypothesis predicts that the entire Earth was covered with ice. Snowball Earth events were suggested to have occurred several times during the Precambrian. Classic paleo-thermometers (e.g., 18 O/ 16 O in marine carbonates) are not available from snowball Earth episodes, and only a few reconstructions of 18 O/ 16 O in ancient meteoric water exist. Here we present a novel approach to reconstruct the 18 O/ 16 O composition of ancient meteoric waters using the triple oxygen isotopic composition ( 17 O/ 16 O and 18 O/ 16 O) of hydrothermally altered rocks. The inferred 18 O/ 16 O for waters that precipitated at (sub)tropical paleo-latitudes on a Paleoproterozoic (∼2.4 gigayears ago) snowball Earth are extremely low. Today, similar compositions are observed only in central Antarctica." @default.
• W2072401076 created "2016-06-24" @default.
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• W2072401076 date "2015-04-13" @default.
• W2072401076 modified "2023-10-10" @default.
• W2072401076 title "Revealing the climate of snowball Earth from Δ ¹⁷ O systematics of hydrothermal rocks" @default.
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• W2072401076 doi "https://doi.org/10.1073/pnas.1422887112" @default.
• W2072401076 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4418898" @default.
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