Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis
Mercury (Hg) concentrations and isotopes from a deep-ocean Triassic–Jurassic (~201 Ma) boundary section provide evidence of large inputs from terrestrial organic-rich sources through combustion by magmatic sills and wildfires.
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Nature Portfolio
2022-03-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-022-28891-8 |
| _version_ | 1828487932773662720 |
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| author | Jun Shen Runsheng Yin Thomas J. Algeo Henrik H. Svensen Shane D. Schoepfer |
| author_facet | Jun Shen Runsheng Yin Thomas J. Algeo Henrik H. Svensen Shane D. Schoepfer |
| author_sort | Jun Shen |
| collection | DOAJ |
| description | Mercury (Hg) concentrations and isotopes from a deep-ocean Triassic–Jurassic (~201 Ma) boundary section provide evidence of large inputs from terrestrial organic-rich sources through combustion by magmatic sills and wildfires. |
| first_indexed | 2024-12-11T09:59:52Z |
| format | Article |
| id | doaj.art-ea40ada92a68479d94f9af505d78b7e1 |
| institution | Directory Open Access Journal |
| issn | 2041-1723 |
| language | English |
| last_indexed | 2024-12-11T09:59:52Z |
| publishDate | 2022-03-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Nature Communications |
| spelling | doaj.art-ea40ada92a68479d94f9af505d78b7e12022-12-22T01:12:09ZengNature PortfolioNature Communications2041-17232022-03-011311810.1038/s41467-022-28891-8Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisisJun Shen0Runsheng Yin1Thomas J. Algeo2Henrik H. Svensen3Shane D. Schoepfer4State Key Laboratory of Geological Processes and Mineral Resources, China University of GeosciencesState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of SciencesState Key Laboratory of Geological Processes and Mineral Resources, China University of GeosciencesCentre for Earth Evolution and Dynamics (CEED), University of OsloDepartment of Geoscience and Natural Resources, Western Carolina UniversityMercury (Hg) concentrations and isotopes from a deep-ocean Triassic–Jurassic (~201 Ma) boundary section provide evidence of large inputs from terrestrial organic-rich sources through combustion by magmatic sills and wildfires.https://doi.org/10.1038/s41467-022-28891-8 |
| spellingShingle | Jun Shen Runsheng Yin Thomas J. Algeo Henrik H. Svensen Shane D. Schoepfer Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis Nature Communications |
| title | Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis |
| title_full | Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis |
| title_fullStr | Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis |
| title_full_unstemmed | Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis |
| title_short | Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis |
| title_sort | mercury evidence for combustion of organic rich sediments during the end triassic crisis |
| url | https://doi.org/10.1038/s41467-022-28891-8 |
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