Scarcity of chert in upper Lower Triassic Panthalassic deep-sea successions of Japan records elevated clastic inputs rather than depressed biogenic silica burial flux following the end-Permian extinction
Lower Triassic sedimentary rocks deposited in pelagic regions of Panthalassa show anomalously clay-rich and silica-poor lithologies compared with the deep marine chert-dominated successions that characterise older and younger strata. The end-Permian mass extinction, which impacted radiolarians, has...
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| Published in | Global and planetary change Vol. 195; p. 103330 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.12.2020
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| Subjects | |
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| Abstract | Lower Triassic sedimentary rocks deposited in pelagic regions of Panthalassa show anomalously clay-rich and silica-poor lithologies compared with the deep marine chert-dominated successions that characterise older and younger strata. The end-Permian mass extinction, which impacted radiolarians, has been proposed as an explanation for this so-called “chert gap” through its inferred impact on biogenic silica production. To test this hypothesis, we evaluated linear sedimentation rates (LSRs) for an upper Olenekian (upper Lower Triassic) siliceous claystone succession in Tsukumi, Oita Prefecture, Southwest Japan. Correlation of conodont biohorizons allows extrapolation of absolute ages obtained by previous studies in South China onto our studied sections. Results show that LSR is higher in the Lower Triassic claystone than in typical Mesozoic radiolarian bedded chert. This implies that increased burial flux of clastic material, not decreased biogenic silica burial flux, drove deposition of clay-rich sediments in pelagic Panthalassa during the late Olenekian.
•Lithostratigraphy of upper Lower Triassic pelagic Panthalassic deep-sea claystone.•Most detailed conodont biostratigraphy from Olenekian Panthalassic deep-sea strata.•Much of the Lower Triassic claystone was formed by high inputs of clastic material.•Collapse in radiolarian deposition during the Early Triassic needs reconsideration. |
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| AbstractList | Lower Triassic sedimentary rocks deposited in pelagic regions of Panthalassa show anomalously clay-rich and silica-poor lithologies compared with the deep marine chert-dominated successions that characterise older and younger strata. The end-Permian mass extinction, which impacted radiolarians, has been proposed as an explanation for this so-called “chert gap” through its inferred impact on biogenic silica production. To test this hypothesis, we evaluated linear sedimentation rates (LSRs) for an upper Olenekian (upper Lower Triassic) siliceous claystone succession in Tsukumi, Oita Prefecture, Southwest Japan. Correlation of conodont biohorizons allows extrapolation of absolute ages obtained by previous studies in South China onto our studied sections. Results show that LSR is higher in the Lower Triassic claystone than in typical Mesozoic radiolarian bedded chert. This implies that increased burial flux of clastic material, not decreased biogenic silica burial flux, drove deposition of clay-rich sediments in pelagic Panthalassa during the late Olenekian.
•Lithostratigraphy of upper Lower Triassic pelagic Panthalassic deep-sea claystone.•Most detailed conodont biostratigraphy from Olenekian Panthalassic deep-sea strata.•Much of the Lower Triassic claystone was formed by high inputs of clastic material.•Collapse in radiolarian deposition during the Early Triassic needs reconsideration. |
| ArticleNumber | 103330 |
| Author | Yamakita, Satoshi Takahashi, Satoshi Onoue, Tetsuji Muto, Shun |
| Author_xml | – sequence: 1 givenname: Shun surname: Muto fullname: Muto, Shun email: s-muto@aist.go.jp organization: The Geological Survey of Japan, National Institute of Advanced Science and Technology, Central 7, Higashi 1-1-1, Tsukuba, Ibaraki, Japan – sequence: 2 givenname: Satoshi surname: Takahashi fullname: Takahashi, Satoshi organization: Department of Earth and Planetary Science, The University of Tokyo, Hongo 7-3-1, Tokyo, Japan – sequence: 3 givenname: Satoshi surname: Yamakita fullname: Yamakita, Satoshi organization: Faculty of Education, University of Miyazaki, Gakuen Kibanadainishi 1-1, Miyazaki, Japan – sequence: 4 givenname: Tetsuji surname: Onoue fullname: Onoue, Tetsuji organization: Department of Earth and Planetary Sciences, Kyushu University, 744 Moto-oka, Nishi-ku, Fukuoka, Japan |
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| CitedBy_id | crossref_primary_10_9795_bullgsj_72_201 crossref_primary_10_2110_palo_2021_045 crossref_primary_10_9795_bullgsj_72_325 crossref_primary_10_1002_gj_4815 crossref_primary_10_1016_j_marmicro_2021_102084 crossref_primary_10_1016_j_gloplacha_2021_103650 crossref_primary_10_1016_j_earscirev_2023_104629 crossref_primary_10_1002_gdj3_244 crossref_primary_10_1111_let_12432 crossref_primary_10_9795_bullgsj_73_4_143 crossref_primary_10_1111_iar_12485 crossref_primary_10_3389_feart_2023_1162023 crossref_primary_10_35463_j_apr_2022_02_01 |
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