Supplemental Material for: Millennial-scale observations of microbially driving sulfur cycling: New model for microbialite formation after end-Permian extinction

Supplemental Material for: Millennial-scale observations of microbially driving sulfur cycling: New model for microbialite formation after end-Permian extinction. The Supplementary Material provides the results for δ13Ccarb, δ18Ocarb, δ34SCAS, [CAS], δ34SFPY (in situ), and content of trace elements from the P-Tr succession of the Yudongzi section.

《千年尺度微生物驱动硫循环观测：二叠纪末大灭绝后微生物岩形成新模型》配套补充材料。本补充材料提供了鱼洞子剖面（Yudongzi section）二叠纪-三叠纪（Permian-Triassic, P-Tr）界线地层序列中的碳酸盐碳同位素组成（δ¹³Ccarb）、碳酸盐氧同位素组成（δ¹⁸Ocarb）、碳酸盐伴生硫酸盐（Carbonate-associated sulfate, CAS）硫同位素组成（δ³⁴SCAS）、CAS含量、原位黄铁矿硫同位素组成（δ³⁴SFPY，in situ）以及微量元素含量的测试结果。