File:Phanerozoic mass extinctions with evidence of increased microbial abundances.png
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From the study "Lethal microbial blooms delayed freshwater ecosystem recovery following the end-Permian extinction"
Summary
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| Description |
English: "Inferred minor/local or moderate/regional microbial abundances may be in part due to inadequate data coverage. Extinction event types from ref. 59. Data sources: late early Cambrian (c. 509 Ma)63,85,86; end-Ordovician (c. 445 Ma)63,87; Lau Event (c. 424 Ma)64; Late Devonian (c. 372 Ma)62,63; Hangenberg Event (c. 359 Ma)62,63; end-Guadalupian (c. 260 Ma)19,88; end-Permian (c. 252 Ma)10,16,37,44,47,49,50,51,52,53,54,63,89; end-Triassic (c. 183 Ma)60,64,90,91,92; Toarcian oceanic anoxic event (c. 183 Ma)93,94,95; Cretaceous OAE 1a (c. 123 Ma)96; Cretaceous OAE 2 (c. 94 Ma)96,97,98,99,100,101,102; end-Cretaceous (c. 66 Ma)62,63,69,70,103,104,105; Paleocene-Eocene Thermal Maximum (c. 56 Ma)61,106,107,108,109; Holocene1,2,110,111. Ed. = Ediacaran, Ma = millions of years ago, Ne. = Neoproterozoic, Neog. = Neogene, OAE = oceanic anoxic event, PETM = Paleocene-Eocene thermal maximum, Q = Quaternary." |
| Date | |
| Source | https://www.nature.com/articles/s41467-021-25711-3 |
| Author | Authors of the study: Chris Mays, Stephen McLoughlin, Tracy D. Frank, Christopher R. Fielding, Sam M. Slater & Vivi Vajda |
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| current | 10:30, 10 June 2024 | | 2,060 × 519 (132 KB) | Prototyperspective (talk | contribs) | Uploaded a work by Authors of the study: Chris Mays, Stephen McLoughlin, Tracy D. Frank, Christopher R. Fielding, Sam M. Slater & Vivi Vajda from https://www.nature.com/articles/s41467-021-25711-3 with UploadWizard |
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