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• W3157739874 endingPage "103652" @default.
• W3157739874 startingPage "103652" @default.
• W3157739874 abstract "The present study reviews the main geochemical, sedimentological, and paleontological events associated with one of the largest perturbations in the Phanerozoic carbon cycle , the Mid-Ludfordian Carbon Isotope Excursion (MLCIE), which is globally documented in late Silurian marine successions. Climate changes associated with the MLCIE are not yet well documented in contrast to most other Silurian CIEs. We report seawater surface temperature changes across the entire MLCIE using δ 18 O apatite records of conodonts originating from different regions located in temperate as well as tropical paleolatitudes . Significant positive δ 18 O apatite excursions (up to 3.8‰) measured in temperate-water areas of the Prague Basin and Carnic Alps (peri-Gondwana) as well as in the tropical areas of Baltica (Laurussia) and Australia (Gondwana) provide evidence for significant global cooling during the MLCIE. The marked cooling of sea surface temperatures , coupled with a significant eustatic sea-level fall recorded on all corresponding paleocontinents, point to a major glaciation in polar and subpolar Gondwana which is denominated here as the “Mid-Ludfordian Glaciation”. The onset of rapid cooling in the Prague Basin (peri-Gondwana) is preceded by the deposition of shales enriched in redox-sensitive trace metals suggesting that anoxic/euxinic waters expanded on the deeper carbonate shelf just before the MLCIE. The coincidence of culmination of the anoxic event (named here as the Siluricus Ocean Anoxic Event) with the Lau/Kozlowskii extinction events is documented for the first time outside of the Laurussian epeiric basins. Widespread oxygen-deficient conditions are interpreted to have been stressful to shelfal ecosystems and may have been a major cause of the extinctions. The mid-Ludfordian glacio-eustatic sea-level fall caused a reduction of shelf habitats culminating in a lower faunal diversity and a change in the structure of faunal communities. The observed positive δ 18 O apatite excursion is tightly coupled to δ 13 C and δ 34 S anomalies documented from temperate (peri-Gondwana) as well as tropical (Laurussia) paleolatitudes. The δ 18 O apatite data complete the Silurian seawater temperature curve and show evidence that one of the largest positive carbon isotope anomalies (MLCIE) of the Phanerozoic was preceded by a widespread anoxic event and tightly linked with a climate cooling event as documented as well for most other Silurian CIEs." @default.
• W3157739874 created "2021-05-10" @default.
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• W3157739874 date "2021-09-01" @default.
• W3157739874 modified "2023-10-14" @default.
• W3157739874 title "The Mid-Ludfordian (late Silurian) Glaciation: A link with global changes in ocean chemistry and ecosystem overturns" @default.
• W3157739874 cites W1151321741 @default.
• W3157739874 cites W1512091300 @default.
• W3157739874 cites W1583491481 @default.
• W3157739874 cites W1648236804 @default.
• W3157739874 cites W1682777677 @default.
• W3157739874 cites W1753926244 @default.
• W3157739874 cites W1867832424 @default.
• W3157739874 cites W1902853003 @default.
• W3157739874 cites W1965338238 @default.
• W3157739874 cites W1965985769 @default.
• W3157739874 cites W1968838468 @default.
• W3157739874 cites W1969706231 @default.
• W3157739874 cites W1969706616 @default.
• W3157739874 cites W1971374523 @default.
• W3157739874 cites W1972987173 @default.
• W3157739874 cites W1973672156 @default.
• W3157739874 cites W1973900162 @default.
• W3157739874 cites W1980025807 @default.
• W3157739874 cites W1983037326 @default.
• W3157739874 cites W1983374490 @default.
• W3157739874 cites W1986916739 @default.
• W3157739874 cites W1991294214 @default.
• W3157739874 cites W1995386982 @default.
• W3157739874 cites W1996158379 @default.
• W3157739874 cites W1997022219 @default.
• W3157739874 cites W1998138507 @default.
• W3157739874 cites W1999285007 @default.
• W3157739874 cites W1999452572 @default.
• W3157739874 cites W2002533872 @default.
• W3157739874 cites W2003615542 @default.
• W3157739874 cites W2005428926 @default.
• W3157739874 cites W2006761122 @default.
• W3157739874 cites W2006933084 @default.
• W3157739874 cites W2008269318 @default.
• W3157739874 cites W2008443718 @default.
• W3157739874 cites W2018642934 @default.
• W3157739874 cites W2019629786 @default.
• W3157739874 cites W2019839279 @default.
• W3157739874 cites W2020299821 @default.
• W3157739874 cites W2022286459 @default.
• W3157739874 cites W2023606819 @default.
• W3157739874 cites W2024493806 @default.
• W3157739874 cites W2026173916 @default.
• W3157739874 cites W2027277459 @default.
• W3157739874 cites W2028496142 @default.
• W3157739874 cites W2030169181 @default.
• W3157739874 cites W2031053894 @default.
• W3157739874 cites W2035665736 @default.
• W3157739874 cites W2036392334 @default.
• W3157739874 cites W2036501693 @default.
• W3157739874 cites W2036789815 @default.
• W3157739874 cites W2036955212 @default.
• W3157739874 cites W2038281478 @default.
• W3157739874 cites W2038532363 @default.
• W3157739874 cites W2039191053 @default.
• W3157739874 cites W2039725359 @default.
• W3157739874 cites W2040059221 @default.
• W3157739874 cites W2040843921 @default.
• W3157739874 cites W2041835485 @default.
• W3157739874 cites W2042018343 @default.
• W3157739874 cites W2043768413 @default.
• W3157739874 cites W2044120187 @default.
• W3157739874 cites W2045375224 @default.
• W3157739874 cites W2045657700 @default.
• W3157739874 cites W2046895752 @default.
• W3157739874 cites W2047748419 @default.
• W3157739874 cites W2049606548 @default.
• W3157739874 cites W2051890883 @default.
• W3157739874 cites W2051982629 @default.
• W3157739874 cites W2052097214 @default.
• W3157739874 cites W2052895954 @default.
• W3157739874 cites W2054598905 @default.
• W3157739874 cites W2056474046 @default.
• W3157739874 cites W2057391595 @default.
• W3157739874 cites W2059055533 @default.
• W3157739874 cites W2059255716 @default.
• W3157739874 cites W2064299945 @default.
• W3157739874 cites W2064570291 @default.
• W3157739874 cites W2065756726 @default.
• W3157739874 cites W2066314486 @default.
• W3157739874 cites W2066452905 @default.
• W3157739874 cites W2067022994 @default.
• W3157739874 cites W2068227987 @default.
• W3157739874 cites W2068263661 @default.
• W3157739874 cites W2069112811 @default.

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