<transcript><audio_99>insight into our working hypothesis and this includes a course by stratigraphy and paleontology or foreign including the isotope signature biostratigraphy and</transcript><transcript><audio_100>paleo ecology of calcareous nanoplankton isotopic profile of carbon oxygen sulfur and a nitrogen of organic and inorganic phases</transcript><transcript><audio_101>in trace metal analysis and biomarker analysis so of course um well okay so one can say that if the eye productivity regime didn't crash so</transcript><caption><image_102>The image is a graph that shows the plankistic foraminifera extinction at the Golan Heights core. The graph is divided into three sections, each representing a different type of extinction.

The first section is a bar graph with different colors representing the different types of plankistic structures. The colors are red, orange, yellow, green, and blue. The bars are arranged in a vertical line, with the highest bar at the top and the lowest at the bottom. The highest bar is labeled "Plankistic foramenifera Extinction" and is colored in red, indicating that it is the highest level of extinction in the Golian Heights core, while the lowest level is labeled as "Golan Heights Core."

In the bottom right corner of the image, there is a small image of a person standing in front of a computer screen. The person is wearing a blue shirt and appears to be giving a presentation.</caption> insight into our working hypothesis and this includes a course by stratigraphy and paleontology or foreign including the isotope signature biostratigraphy and paleo ecology of calcareous nanoplankton isotopic profile of carbon oxygen sulfur and a nitrogen of organic and inorganic phases in trace metal analysis and biomarker analysis so of course um well okay so one can say that if the eye productivity regime didn't crash so
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