The Infona portal uses cookies, i.e. strings of text saved by a browser on the user's device. The portal can access those files and use them to remember the user's data, such as their chosen settings (screen view, interface language, etc.), or their login data. By using the Infona portal the user accepts automatic saving and using this information for portal operation purposes. More information on the subject can be found in the Privacy Policy and Terms of Service. By closing this window the user confirms that they have read the information on cookie usage, and they accept the privacy policy and the way cookies are used by the portal. You can change the cookie settings in your browser.
Sedimentological, micropalaeontological and organic geochemical (Rock-Eval pyrolysis) criteria suggest that calving glaciers, probably from Antarctica, likely reached the sea and floated by New Zealand during the middle Paleocene, dropping angular coarse detritus into marine mud. The dropstone event coincides with marked shifts in organic geochemistry of the associated marine shale as well as changes...