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The Mulde event was an anoxic event, and marked the second of three 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 in geochemical isotopes. Its onset is synchronous with the deposition of the in Gotland. Perceived extinction in the conodont fauna, however, likely represent a change in the depositional environment of sedimentary sequences rather than a genuine biological extinction.

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  • حدث مولدي (ar)
  • Mulde event (en)
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  • حدث مولدي (بالإنجليزية: Mulde)‏، ثاني حدث من الثلاثة أحداث للانقراضات الطفيفة نسبيا (إيرفكن ومولدي ولاو) خلال العصر السيلوري. وهو قد تزامن مع الانخفاض العالمي في مستوى سطح البحر، وتبعه رحلة في النظائر الجيوكيميائية. وتتزامن بدايته مع ترسب تكوين فرول في غوتلاند. وتعتبر مخروطيات الأسنان أكثر ما لوحظ في هذا الانقراض، وعلى أية حال، من المحتمل أن تمثل تغييراً في البيئة الترسبية للتسلسلات الرسوبية بدلاً من الانقراض البيولوجي الحقيقي. (ar)
  • The Mulde event was an anoxic event, and marked the second of three 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 in geochemical isotopes. Its onset is synchronous with the deposition of the in Gotland. Perceived extinction in the conodont fauna, however, likely represent a change in the depositional environment of sedimentary sequences rather than a genuine biological extinction. (en)
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  • حدث مولدي (بالإنجليزية: Mulde)‏، ثاني حدث من الثلاثة أحداث للانقراضات الطفيفة نسبيا (إيرفكن ومولدي ولاو) خلال العصر السيلوري. وهو قد تزامن مع الانخفاض العالمي في مستوى سطح البحر، وتبعه رحلة في النظائر الجيوكيميائية. وتتزامن بدايته مع ترسب تكوين فرول في غوتلاند. وتعتبر مخروطيات الأسنان أكثر ما لوحظ في هذا الانقراض، وعلى أية حال، من المحتمل أن تمثل تغييراً في البيئة الترسبية للتسلسلات الرسوبية بدلاً من الانقراض البيولوجي الحقيقي. (ar)
  • The Mulde event was an anoxic event, and marked the second of three 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 in geochemical isotopes. Its onset is synchronous with the deposition of the in Gotland. Perceived extinction in the conodont fauna, however, likely represent a change in the depositional environment of sedimentary sequences rather than a genuine biological extinction. 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. (en)
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