During Saturday core drilling at Sose bugt continued slowly. Because the sedimentary succession is fairly unconsolidated we are drilling with a technique that encase the cored sediments in 1,5 m long pipes. This means that it is only possible to investigate the cored sediments at the top or bottom of each core section. Typical Early Jurassic whitish sands and grey clays had been cored during the first three days of drilling. On Saturday we were closing in on two prominent seismic horizons, one which we suspected could be the top of the Triassic redbeds. At 91 m there were still grey clays but also coal. But at 95 m the top of the core showed dark grey clays, while the bottom consisted of light green sand and clay typical for the Upper but not the uppermost Triassic. We had finally reached the Triassic! 🙂
Drilling will continue for a few more hours tomorrow until the geophysical logging equipment arrives. We are all very excited and can’t wait to get the cores back to GEUS so that we can study them. Almost 95 m of Lower Jurassic and hopefully also uppermost Triassic (Rhaetian) near coastal sedimentary strata which we think will provide us with additional information on the end-Triassic mass extinction and the biotic recovery that followed.