Multiple phases of carbon cycle disturbance from large igneous province formation at the Triassic-Jurassic transition
The end-Triassic mass extinction (ca. 201.4 Ma) coincided with a major carbon cycle perturbation, based on an ~5%‰-6%‰ negative excursion in δ13CTOC (total organic carbon) records. Both events coincided directly with the onset of massive flood basalt volcanism in the Central Atlantic Magmatic Provin...
Những tác giả chính: | Ruhl, M, Kürschner, WM |
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Định dạng: | Journal article |
Ngôn ngữ: | English |
Được phát hành: |
2011
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