Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction. [PDF]
Sci Adv, 2022 Kozik NP +8 more
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Az alsó-toarci feketepala Réka-völgyi szelvényének ásványtani jellemzése (Óbányai Aleurolit Formáció, Mecsek-hegység): őséghajlattani következtetések | Mineralogy of the Lower Toarcian black shale section from the Réka Valley (Óbánya Siltstone Formation, Mecsek Mountains, Hungary): implications for palaeoclimate [PDF]
, 2008 Munkánkban az alsó-toarci feketepala (Óbányai Aleurolit Formáció, Réka-völgy, Mecsek) nagyfelbontású ásványtani vizsgálati eredményeit mutatjuk be.
Raucsik, Béla +1 more
core
Chemostratigraphy Across the Triassic–Jurassic Boundary
, 2019 The Triassic‐Jurassic transition (~201.5 Ma) is marked by one of the largest mass extinctions in Earth’s history. This was accompanied by significant perturbations in ocean and atmosphere geochemistry, including the global carbon cycle, as expressed by major fluctuations in carbon isotope ratios. Central Atlantic Magmatic
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A transient peak in marine sulfate after the 635-Ma snowball Earth. [PDF]
Proc Natl Acad Sci U S A, 2022 Peng Y +7 more
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Chemostratigraphy of Carbonate-Evaporite Successions from the Southern Arabian Gulf :ABSTRACT
, 1997 Ross Peebles
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Mercury abundance and isotopic composition indicate subaerial volcanism prior to the end-Archean "whiff" of oxygen. [PDF]
Proc Natl Acad Sci U S A, 2021 Meixnerová J +6 more
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Chemostratigraphy of Madeira Abyssal Plain Miocene-Pleistocene turbidites, Site 950
, 1998 Ian Jarvis, J. Moreton, M. Gérard
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