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Fig. 7 in On The Occurrence Of Salpingoporella Pasmanica Radoičić, 2002, (Dasycladales) From The Late Maastrichtian Of The Zagros Zone, Sw Iran

Fig. 7 Schematic distribution of larger benthic foraminifera in the Eocene Trentinara Formation of Italy (based on Vecchio and Hottinger, 2007, fig. 5), and the Maastrichtian Tarbur Formation (examples; without scale). 1 Rotaliids (e.g., Rotorbinella), 2 Siderolites, 3 Orbitoides, 4 Loftusia, 5-6 Orbitolinidae (5: Dictyoconella minima), 7 Gyroconulina, 8 Rhapydionidae, 9 Spirolina, 10 Pyrgo?, 11 Broeckina. 5-7: Agglutinated conical foraminifera, 8-11: Porcelaneous foraminifera. Note the basinal facies corresponds to the Gurpi Formation.

ShareScore

28/100

Overall dataset sharing score

Score breakdown

These five areas show where the dataset supports — or may limit — practical reuse.

Stewardship
8
Harmonization
4
Access
16
Reuse readiness
0
Engagement
0

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