Description Robinson, E.; Cunningham, K. J. (2022). New larger benthic foraminifera from the subsurface Lower to Middle Eocene Oldsmar Formation of southeastern Florida (USA). Carnets de géologie (Notebooks on geology). 22(21): 857-865., available online athttps://doi.org/10.2110/carnets.2022.2221
page(s): figs. 5.1-5.12 (holotype fig. 5.6). Figure 5: 1-12, Globogypsinoides browardensis n.gen. n.sp. Random sections through twelve specimens. 1-3 are probable microspheric specimens and 4-12 are megalospheric specimens. Location and depths for 6, the holotype, and 3-4, 7 and 12, paratypes, are given in the text. 1-2, 5, 8 are from well G-3805 at a depth of 2,732.7 ft (832.9 m), well G-2994 at 2,930.3 ft (893.2 m), well G3805 at 2,737.8 ft (834.5 m) and from well G-3973 at a depth of 2,780.3ft (847.4 m) respectively. 9-12 are from well G2994 at depths of 2,930.3 ft (893.2 m), 2,938.9 ft (895.8 m), 2,934.2 ft (894.3 m) and 2,938.9 ft (895.8 m) respectively. The 0.5 mm scale is for 1; 1 mm scale for 3; and 0.2 mm scale for 2, 4-12.Author Le Coze, FrançoisJPG file - 293.98 kB - 1 000 x 800 pixelsadded on 2024-01-18109 viewsForaminifera taxaGlobogypsinoides browardensis Robinson & Cunningham, 2022 †checked Le Coze, François 2024-01-18 This work is licensed under a Creative Commons Attribution-Noncommercial-Share Alike 4.0 License