Multiple sulfur isotopes discriminate organoclastic and methane-based sulfate reduction by sub-seafloor pyrite formation by Liu, Jiarui, Pellerin, André, Wang, Jiasheng, Rickard, David, Antler, Gilad, Zhao, Jie, Wang, Zhou, Jørgensen, Bo Barker, Ono, Shuhei

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Early diagenesis of sulfur in Bornholm Basin sediments: The role of upward diffusion of isotopically “heavy” sulfide by Liu, Jiarui, Pellerin, André, Antler, Gilad, Izon, Gareth, Findlay, Alyssa J., Røy, Hans, Ono, Shuhei, Kasten, Sabine, Turchyn, Alexandra V., Jørgensen, Bo Barker

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Early diagenesis of sulfur in Bornholm Basin sediments: The role of upward diffusion of isotopically “heavy” sulfide by Liu, Jiarui, Pellerin, André, Antler, Gilad, Izon, Gareth, Findlay, Alyssa J., Røy, Hans, Ono, Shuhei, Kasten, Sabine, Turchyn, Alexandra V., Jørgensen, Bo Barker

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Isotopically “heavy” pyrite in marine sediments due to high sedimentation rates and non-steady-state deposition by Liu, Jiarui, Antler, Gilad, Pellerin, André, Izon, Gareth, Dohrmann, Ingrid, Findlay, Alyssa J., Røy, Hans, Ono, Shuhei, Turchyn, Alexandra V., Kasten, Sabine, Jørgensen, Bo Barker

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