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Fig. 3 in A new evidence of passing the Maastichtian-Paleocene boundary by larger benthic foraminifers: The case of Elazigina from the Maastrichtian Tarbur Formation of Iran
Fig. 3. Stratigraphic columns from Mandegan (A) and Rod-Abad (B) sections with position of the studied samples and distribution of Elazigina siderea sp. nov.
ShareScore
40/100
Overall dataset sharing score
Score breakdown
These five areas show where the dataset supports — or may limit — practical reuse.
- Stewardship
- 8
- Harmonization
- 4
- Access
- 20
- Reuse readiness
- 8
- Engagement
- 0