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

<table>ODP Hole 953C abundance curves of selected planktonic foraminiferal (as a percentage of the total planktonic foraminiferal fauna) and position of most significant biohorizons. Grey color in <i>Globorotalia menardii </i>gr., <i>Neogloboquadrina acostaensis, </i>and <i>N</i>. <i>pachyderma</i> distributions indicates the percentage of sinistral forms. The red dotted line designates the hiatus. The following acronyms indicate bioevents: LO (Last Occurrence), FO (First Occurrence), LRO (Last Regular Occurrence), and S/D (sinistral/dextral coiling change).</table>

Paleontology Journal

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Figure 2: Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning 

Figure 2 | Revision of the Messinian-Early Zanclean Sediments from ODP Hole 953C (Canary Island Archipelago, North-Eastern Atlantic): Biostratigraphy, Cyclostratigraphy, and Astronomical Tuning 