Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning

<table>Relationship among astronomically forced lithological cycles, abundances of selected planktonic foraminifera, warm/cold ratio, and inferred insolation cycles in different Mediterranean successions (Sicily; Gavdos Basin—Greece; Sorbas Basin—Spain). (Modified after [<a href="/journals/paleontology/2013/947839/#B15">73</a>, <a href="/journals/paleontology/2013/947839/#B92">74</a>].)</table>

Paleontology Journal

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Figure 3: Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning 

Figure 3 | Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning 