<transcript><audio_139>so if we look at the sedimentation rates and get calculated along this sequence we see there is no change in sedimentation rates between the cretaceous and the pallogene you see here the sedimentation rate</transcript><transcript><audio_140>is pretty much the same there is not a reduction in the toc contents and in the tic is pretty much the same high sedimentation rates</transcript><transcript><audio_141>and high toc a level and no significant differences acro across the boundary and if we compare this profile to other profile in the textus so</transcript><caption><image_142>The image is a map of the Tethys at Late Maastrichtian showing the location of the Golden site within the uplifting region, as well as other Tethyyan sites crossing the KPG area. The map is color-coded, with different shades of orange, yellow, and red representing different elevations and elevations. The topography of the map is labeled with the names of the cities and towns, and the bottom of the image has a title that reads "Comparison with other KPG sections". There is also a small image of a person on the right side of the screen.</caption><transcript><audio_143>this is the golan profile here and the blue one is the delta c 13 a excursion and a isotope a data and the black one is the calcite</transcript><transcript><audio_144>concentration and here in color is the sedimentation rates and compared to carcava and gubeo and you see the differences between</transcript> so if we look at the sedimentation rates and get calculated along this sequence we see there is no change in sedimentation rates between the cretaceous and the pallogene you see here the sedimentation rate is pretty much the same there is not a reduction in the toc contents and in the tic is pretty much the same high sedimentation rates and high toc a level and no significant differences acro across the boundary and if we compare this profile to other profile in the textus so this is the golan profile here and the blue one is the delta c 13 a excursion and a isotope a data and the black one is the calcite concentration and here in color is the sedimentation rates and compared to carcava and gubeo and you see the differences between
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