subject predicate object context
6248 Creator b0e9eb49c58c5a8568d7ca6193664618
6248 Creator cacb76ae818ff026f97828ea97a0481b
6248 Date 2002-03
6248 Is Part Of p00917613
6248 Is Part Of repository
6248 abstract The Late Triassic–Early Jurassic was a time of major global change; however, the fundamental processes driving these changes are less than clear. We have determined the Re and Os abundances, and Os isotope compositions, of marine mudrock samples that span the Triassic-Jurassic boundary in the UK and have established that major isotopic and geochemical shifts in the composition of seawater took place in the latest Triassic. We argue that these shifts were caused by the sudden initiation of widespread igneous activity within the Central Atlantic magmatic province, associated with rifting of the supercontinent Pangea. The Os isotope composition of seawater responded rapidly to these events, demonstrating that the seawater Os isotope system has great potential in identifying the nature and precise timing of major environmental change.
6248 authorList authors
6248 issue 3
6248 status peerReviewed
6248 volume 30
6248 type AcademicArticle
6248 type Article
6248 label Cohen, Anthony S. and Coe, Angela L. (2002). New geochemical evidence for the onset of volcanism in the Central Atlantic magmatic province and environmental change at the Triassic-Jurassic boundary. Geology, 30(3) pp. 267–270.
6248 label Cohen, Anthony S. and Coe, Angela L. (2002). New geochemical evidence for the onset of volcanism in the Central Atlantic magmatic province and environmental change at the Triassic-Jurassic boundary. Geology, 30(3) pp. 267–270.
6248 Title New geochemical evidence for the onset of volcanism in the Central Atlantic magmatic province and environmental change at the Triassic-Jurassic boundary
6248 in dataset oro