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                <term xml:lang="en">Cenomaniane-Turonian Boundary Event</term>
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                <term xml:lang="en">Black shale</term>
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              <p>The CenomanianeTuronian Boundary Event (CTBE) event is not associated with a transgression on thesouthern margin of the Subalpine Basin, but with a steady shallowing-up trend beginning in the lowerhalf of the d13 C positive shift. The SWeNE Rouaine Fault had a complex role, first in isolating a black shalebasin to the west and a large, deep submarine plateau devoid of black shale to the east, then by a strike-slip movement that induced a forced progradation to the north of the southern platform in the easterncompartment. This compressive tectonic reactivation of the southern margin began around the depo-sition of the local equivalent of the Plenus bed of boreal basins, as shown by correlation supported byboth isotope and palaeontological data. Other local data are pieced together to suggest that the whole ofSE France underwent a short-lived transpressive tectonic pulse around the CenomanianeTuronianboundary, probably connected with the early compressive movement of Africa vs. Europe. On a largerscale, other published data suggest that this pulse could be a global one. It is coeval with renewed thrustloading, volcanism and transgression in the North-American Western Interior, local emergences duringthe event along the eastern Atlantic margin, suggesting a slight tendency to inversion of the margin, anda tilting to the east of the North-Africa plate that could explain the large transgression recorded fromMorocco to Tunisia on the Saharan Craton.New isotope and palaeontological (coiling ratio of Muricohedbergella delrioensis) data from SE Francesuggest that two coolings of suprabasinal importance occurred just before and during the build-up of thed13C shift, including the boreal “Plenus Marls“, especially its middle limestone bed and its SE Franceequivalent.Regarding the extinction of the genus Thalmaninella and Rotalipora and during the event, neitheranoxia nor climate changes can fully explain the palaeontological crisis, given that Rotalipora cushmanicrosses the first phase of anoxia without harm, as well as the two coolings, not only in SE France but on alarge scale, as shown by the correlation of the published data. This extinction needs alternative expla-nations as we challenge both anoxia and climate as major causes</p>
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