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本文引用的文献
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A composite reference section for terminal proterozoic strata of southern Namibia.
J Sediment Res A Sediment Petrol Process. 1998 Nov;68(6):1223-35. doi: 10.2110/jsr.68.1223.
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A Vendian-Cambrian boundary succession from the northwestern margin of the Siberian Platform: stratigraphy, palaeontology, chemostratigraphy and correlation.
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Anomalous carbonate precipitates: is the Precambrian the key to the Permian?
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Comparative Earth history and Late Permian mass extinction.
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Secular variation in carbon isotope ratios from Upper Proterozoic successions of Svalbard and East Greenland.
Nature. 1986 Jun 26;321(6073):832-8. doi: 10.1038/321832a0.
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Geochemistry of Precambrian carbonates: II. Archean greenstone belts and Archean sea water.
Geochim Cosmochim Acta. 1989;53:859-71. doi: 10.1016/0016-7037(89)90031-8.
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The post-Paleozoic chronology and mechanism of 13C depletion in primary marine organic matter.
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Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications.
Precambrian Res. 1995;73:27-49. doi: 10.1016/0301-9268(94)00070-8.
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Integrated chemostratigraphy and biostratigraphy of the Windermere Supergroup, northwestern Canada: implications for Neoproterozoic correlations and the early evolution of animals.
Geol Soc Am Bull. 1994 Oct;106(10):1281-92. doi: 10.1130/0016-7606(1994)106<1281:icabot>2.3.co;2.
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Tectonic control of the crustal organic carbon reservoir during the Precambrian.
Chem Geol. 1994;114:303-14. doi: 10.1016/0009-2541(94)90060-4.
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