Dynamics of a stepped carbon-isotope excursion: Ultra high-resolution study of Early Toarcian environmental change
In the Toarcian (Early Jurassic; ~183Myr ago), the ocean-atmosphere system was subject to one of the largest perturbations of the carbon cycle in the last 250Myr known as the Toarcian Oceanic Anoxic Event (T-OAE). This event was accompanied by a -6‰ negative carbon-isotope excursion (CIE) caused by...
Những tác giả chính: | , , , , , |
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Định dạng: | Journal article |
Ngôn ngữ: | English |
Được phát hành: |
2012
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