Fig. 9 in Late Silurian palynomorphs from the Precordillera of San Juan, Argentina: Diversity, palaeoenvironmental and palaeogeographic significance
Fig. 9. Palynomorphs from the studied sections of the Los Espejos Formation of Argentina, Cerro La Chilca, Homerian? (A, L), Cerro La Chilca, Gorstian?–Ludfordian? (B, I), Cerro La Chilca, Ludfordian (C, H, O, Q, T), Quebrada Ancha, Ludfordian (D–G, J, N, P, R, S), Quebrada Ancha, Přídolí (K, U), Quebrada Ancha, Gorstian?–Ludfordian? (M). A–F. cf. Melikeriopalla sp. A. MPLP 1-61065 (W30/3). B. MPLP 3-61058 (L33). C. MPLP 7-61062 (P43/3). D. MPLP 2-60704 (L26). E. MPLP 3-60659 (F38). F. MPLP 4-62521 (T40/4). G. Multiplicisphaeridium arbusculum forma A of Mullins (2001); MPLP 7-60736 (D30/1). H. Multiplicisphaeridium cladum (Downie, 1963) Eisenack, 1969; MPLP 4-61059 (E50/1). I. Multiplicisphaeridium mingusi Le Hérissé, 1989; MPLP 2-61057 (M31/1). J. Multiplicisphaeridium monki Le Hérissé, 1989; MPLP 3-60659 (O45/2). K. Multiplicisphaeridium rochesterensis Cramer and Diez, 1972; MPLP 9-60664 (U27). L. Nanocyclopia sp.; MPLP 1-61065 (U38/1). M. Neoveryhachium carminae (Cramer, 1964a) Cramer, 1970; MPLP 1-60667 (P45/2). N. Onondagella asymmetrica (Deunff, 1961) Playford, 1977; MPLP 7-60736 (X44). O. cf. Oppilatala frondis (Cramer and Díez, 1972) Dorning, 1981; MPLP 4-61059 (F45). P. Oppilatala grahni Le Hérissé, 1989; MPLP 7-60736 (E38/1). Q. Oppilatala insolita (Cramer and Díez, 1972) Dorning, 1981; MPLP 4-61059 (Q50). R. Oppilatala ramusculosa (Deflandre, 1945) Dorning, 1981; MPLP 7-60736 (N37/4). S. Ozotobrachion palidodigitatus (Cramer, 1966b) Playford, 1977; MPLP 7-60736 (P48/4). T. Percultisphaera incompta Richards and Mullins, 2003; MPLP 4-61059 (W47/4). U. Polyedrixium? cf. embudum Cramer, 1964a; MPLP 9-60664 (D39/1). Scale bars 20 μm.
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