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Mulde event

The Mulde event was an anoxic event,[4] and marked the second of three1 relatively minor mass extinctions (the Ireviken, Mulde, and Lau events) during the Silurian period. It coincided with a global drop in sea level, and is closely followed by an excursion[clarification needed] in geochemical isotopes. Its onset is synchronous with the deposition of the Fröel Formation in Gotland.[4] Perceived extinction in the conodont fauna, however, likely represent a change in the depositional environment of sedimentary sequences rather than a genuine biological extinction.[5]

Higher resolution δ13C isotope analysis identifies differences in the organic and carbonate carbon isotope curves (Δ13C), allowing the inference of a sustained drop in CO2 levels coincident with the extinction once sedimentological data are taken into account.[6]

Notes Edit

^1 The Ireviken, Mulde, and Lau events were all closely followed by isotopic excursions.

References Edit

  1. ^ Jeppsson, L.; Calner, M. (2007). "The Silurian Mulde Event and a scenario for secundo—secundo events". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 93 (02): 135–154. doi:10.1017/S0263593300000377.
  2. ^ Munnecke, A.; Samtleben, C.; Bickert, T. (2003). "The Ireviken Event in the lower Silurian of Gotland, Sweden-relation to similar Palaeozoic and Proterozoic events". Palaeogeography, Palaeoclimatology, Palaeoecology. 195 (1): 99–124. doi:10.1016/S0031-0182(03)00304-3.
  3. ^ "Chart/Time Scale". www.stratigraphy.org. International Commission on Stratigraphy.
  4. ^ a b Samtleben, C.; Munnecke, A.; Bickert, T. (2000). "Development of facies and C/O-isotopes in transects through the Ludlow of Gotland: Evidence for global and local influences on a shallow-marine environment". Facies. 43 (1): 1–38. doi:10.1007/BF02536983. S2CID 130640332.
  5. ^ Jarochowska, Emilia; Ray, David C; Röstel, Philipp; Worton, Graham; Munnecke, Axel (2017). "Harnessing stratigraphic bias at the section scale: Conodont diversity in the Homerian (Silurian) of the Midland Platform, England". Palaeontology. 61: 57–76. doi:10.1111/pala.12326. S2CID 135200300.
  6. ^ Biebesheimer, Ellie J.; Cramer, Bradley D.; Calner, Mikael; Barnett, Bruce A.; Oborny, Stephan C.; Bancroft, Alyssa M. (2021). "Asynchronous δ13Ccarb and δ13Corg records during the onset of the Mulde (Silurian) positive carbon isotope excursion from the Altajme core, Gotland, Sweden". Chemical Geology. 576: 120256. Bibcode:2021ChGeo.576l0256B. doi:10.1016/j.chemgeo.2021.120256. ISSN 0009-2541. S2CID 234817512.

mulde, event, silurian, graphical, timelinethis, viewtalkedit, paleozoicordoviciansiluriandevonianllandoverywenlockludlowpřídolírhuddanianaeroniantelychiansheinwoodianhomeriangorstianludfordian, event, ireviken, event, subdivision, silurian, according, 2021, v. Silurian graphical timelineThis box viewtalkedit 444 442 440 438 436 434 432 430 428 426 424 422 420 418 PaleozoicOrdovicianSilurianDevonianLlandoveryWenlockLudlowPridoliRhuddanianAeronianTelychianSheinwoodianHomerianGorstianLudfordian Lau event Mulde event 1 Ireviken event 2 Subdivision of the Silurian according to the ICS as of 2021 3 Vertical axis scale millions of years ago The Mulde event was an anoxic event 4 and marked the second of three1 relatively minor mass extinctions the Ireviken Mulde and Lau events during the Silurian period It coincided with a global drop in sea level and is closely followed by an excursion clarification needed in geochemical isotopes Its onset is synchronous with the deposition of the Froel Formation in Gotland 4 Perceived extinction in the conodont fauna however likely represent a change in the depositional environment of sedimentary sequences rather than a genuine biological extinction 5 Higher resolution d13C isotope analysis identifies differences in the organic and carbonate carbon isotope curves D13C allowing the inference of a sustained drop in CO2 levels coincident with the extinction once sedimentological data are taken into account 6 Notes Edit 1 The Ireviken Mulde and Lau events were all closely followed by isotopic excursions References Edit Jeppsson L Calner M 2007 The Silurian Mulde Event and a scenario for secundo secundo events Earth and Environmental Science Transactions of the Royal Society of Edinburgh 93 02 135 154 doi 10 1017 S0263593300000377 Munnecke A Samtleben C Bickert T 2003 The Ireviken Event in the lower Silurian of Gotland Sweden relation to similar Palaeozoic and Proterozoic events Palaeogeography Palaeoclimatology Palaeoecology 195 1 99 124 doi 10 1016 S0031 0182 03 00304 3 Chart Time Scale www stratigraphy org International Commission on Stratigraphy a b Samtleben C Munnecke A Bickert T 2000 Development of facies and C O isotopes in transects through the Ludlow of Gotland Evidence for global and local influences on a shallow marine environment Facies 43 1 1 38 doi 10 1007 BF02536983 S2CID 130640332 Jarochowska Emilia Ray David C Rostel Philipp Worton Graham Munnecke Axel 2017 Harnessing stratigraphic bias at the section scale Conodont diversity in the Homerian Silurian of the Midland Platform England Palaeontology 61 57 76 doi 10 1111 pala 12326 S2CID 135200300 Biebesheimer Ellie J Cramer Bradley D Calner Mikael Barnett Bruce A Oborny Stephan C Bancroft Alyssa M 2021 Asynchronous d13Ccarb and d13Corg records during the onset of the Mulde Silurian positive carbon isotope excursion from the Altajme core Gotland Sweden Chemical Geology 576 120256 Bibcode 2021ChGeo 576l0256B doi 10 1016 j chemgeo 2021 120256 ISSN 0009 2541 S2CID 234817512 Retrieved from https en wikipedia org w index php title Mulde event amp oldid 1170325741, wikipedia, wiki, book, books, library,

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