<caption><image_28>The image is a slide from a presentation on the high productivity deposits in Israel. The slide is divided into three sections. 

The first section on the left side of the slide has a title that reads "The Late Cretaceous marine succession composed a variety of rock-types, that are an outcome of weakening regime." Below the title, there is a diagram that shows the different types of deposits in the region.

In the center of the image, there are three sections that explain the different deposits. The first section is titled "Sediments enriched in S-P-C. Great lateral and basal changes." The second section is labeled "Cherts, phosphates and organic rich carbonate (Oil shale) in Southern Israel." The third section is labelled "Organic rich carbonates in Central and Northern Israel."

There are also three smaller sections on the slide, each showing a different type of deposit. The top section has a color-coded representation of the deposits, with different shades of green, yellow, and pink representing the different levels of sedimentary deposits. There is also a legend that explains the meaning of each color in the diagram.</caption><transcript><audio_29>neurons that accompany this system are rich in silica carbon and phosphate in israel as i said this regime persists over 20 million years and and produced</transcript><transcript><audio_30>sediment enriched with organic matter with great lateral and basement changes and as you can see in this illustration in the in the south and</transcript> neurons that accompany this system are rich in silica carbon and phosphate in israel as i said this regime persists over 20 million years and and produced sediment enriched with organic matter with great lateral and basement changes and as you can see in this illustration in the in the south and
{"source": "grass-yt-cc-by.1Dw9X0V9KnM|shard_10058|create_multimodal_data.extract_yt_and_generate_transcripts.54|shard_10058|create_multimodal_data.generate_captions.54", "params": {"id": "1Dw9X0V9KnM", "channel_id": "UCJYhmN5PBsm9VRLWwnEqL5Q", "duration": 3255, "view_count": 62, "age_limit": 0, "chapters": [{"start_time": 0, "end_time": 613.0, "title": "<Untitled Chapter 1>"}, {"start_time": 613.0, "title": "Study section and Motivation", "end_time": 686.0}, {"start_time": 686.0, "title": "Planktic foraminifera extinction at the KPg boundary", "end_time": 714.0}, {"start_time": 714.0, "title": "What killed the dinosaurs?", "end_time": 750.0}, {"start_time": 750.0, "title": "The KPg Mass Extinction event - 66.04 Myr", "end_time": 801.0}, {"start_time": 801.0, "title": "The famous KPg boundary in Israel", "end_time": 950.0}, {"start_time": 950.0, "title": "Primary producers crash", "end_time": 1042.0}, {"start_time": 1042.0, "title": "Goals", "end_time": 1166.0}, {"start_time": 1166.0, "title": "Methods", "end_time": 1340.0}, {"start_time": 1340.0, "title": "Planktonic foraminifera biostratigraphy", "end_time": 1517.0}, {"start_time": 1517.0, "title": "Age model", "end_time": 1711.0}, {"start_time": 1711.0, "title": "Sedimentation rate", "end_time": 1755.0}, {"start_time": 1755.0, "title": "Comparison with other KPg section", "end_time": 1812.0}, {"start_time": 1812.0, "title": "The carbonatic components", "end_time": 2030.0}, {"start_time": 2030.0, "title": "Redox conditions and preservation", "end_time": 2111.0}, {"start_time": 2111.0, "title": "Rapid resurgence at the Southern Tethys upwelling belt", "end_time": 2320.0}, {"start_time": 2320.0, "title": "The Negative 8C excursion", "end_time": 3102.0}, {"start_time": 3102.0, "title": "Planktic foraminifera extinction at the Golan Heights core", "end_time": 3255}], "like_count": 0, "channel_follower_count": 90, "license": "Creative Commons Attribution license (reuse allowed)", "uploader_id": "@marinegeosciences7087", "yt_tar_file": "/leonardo_work/EUHPC_E03_068/audio/fixed_download/grass-yt-cc-by//shard_10058/1Dw9X0V9KnM.tar.gz"}}