%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Moulin, M.
%A Fluteau, F.
%A Courtillot, V.
%A Marsh, J.
%A Delpech, G.
%A Quidelleur, X.
%A Gérard, Martine
%T Eruptive history of the Karoo lava flows and their impact on early Jurassic environmental change
%D 2017
%L fdi:010069297
%G ENG
%J Journal of Geophysical Research : Solid Earth
%@ 2169-9313
%K AFRIQUE DU SUD
%M ISI:000396132200001
%N 2
%P 738-772
%R 10.1002/2016jb013354
%U https://www.documentation.ird.fr/hor/fdi:010069297
%> https://www.documentation.ird.fr/intranet/publi/2017/03/010069297.pdf
%V 122
%W Horizon (IRD)
%X This paper reports new paleomagnetic and geochronologic data from a similar to 1500m thick composite section belonging to the Drakensberg group, the thickest remnant of the Karoo lavas in Northern Lesotho. Flow-by-flow analysis of paleomagnetic directions reveals 21 magnetic directional groups, corresponding to single eruptive events, and 16 individual lava flows. The new age determinations of lava flows range from 180.1 +/- 1.4 to 182.8 +/- 2.6 Ma. These data, combined with previous results, allow us to propose that the main part of the Drakensberg group and the Karoo intrusive complex dated around 181-183 Ma may have been erupted over a period as short as 250 kyr and may have coincided with the two main phases of extinction in the Early Toarcian. This scenario agrees well with the discontinuous rhythm of environmental and biotic perturbations in the Late Pliensbachian-Toarcian interval.
%$ 066 ; 064