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Appendix 1 in Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths
<p><b>Appendix 1</b> (continued) Number of non-otolith taxa identified to lowest taxonomic ranking within each Claiborne Group unit. Shaded areas represent the stratigraphic range of taxa within Claiborne Group units in Alabama, USA.</p><table><thead><tr><th><b>Taxon</b></th><th colspan="2"><b>Meridian lower upper Tallahatta “lower” “upper” Lisbon/ lower Tallahatta Sand Tallahatta Tallahatta /Lisbon Lisbon Lisbon Gosport Gosport Fm. Member Fm. Fm. contact Fm. Fm. contact Sand</b></th><th><b>Gosport Sand</b></th><th><b>Total</b></th></tr></thead><tbody><tr><th><i>Myliobatis</i> sp. 1</th><td>5</td><td>307</td><td></td><td><b>312</b></td></tr><tr><th><i>Myliobatis</i> sp. 2</th><td></td><td>18 207 1 48</td><td colspan="2">13 <b>287</b></td></tr><tr><th><i>Pseudaetobatus belli</i></th><td>15</td><td>210</td><td></td><td><b>225</b></td></tr><tr><th><i>Rhinoptera</i> sp. <i>Meridiania</i> cf. <i>M. convexa</i></th><td>16</td><td>14 18 181 1 5 1525 1 1</td><td colspan="2">131 <b>1891</b> 2 <b>4</b></td></tr><tr><th><i>Leidybatus jugosus</i></th><td></td><td>2 28 41</td><td></td><td><b>71</b></td></tr><tr><th><i>Burnhamia daviesi</i></th><td></td><td>6 1 1</td><td>4</td><td><b>12</b></td></tr><tr><th><i>Eoplinthicus yazooensis</i></th><td></td><td></td><td colspan="2">1 <b>1</b></td></tr><tr><th>Batomorphii indet.</th><td></td><td>4</td><td>3</td><td><b>7</b></td></tr><tr><th>Myliobatidae indet.</th><td></td><td>750 4 74 776 1 7 762</td><td>212</td><td><b>2586</b></td></tr><tr><th><i>Cylindracanthus ornatus</i></th><td></td><td>2 1</td><td></td><td><b>3</b></td></tr><tr><th><i>Cylindracanthus rectus</i></th><td></td><td>24 16 4 2</td><td></td><td><b>46</b></td></tr><tr><th><i>Cylindracanthus</i> sp.</th><td></td><td>4 4 13 45 6</td><td></td><td><b>72</b></td></tr><tr><th><i>Pycnodus</i> sp.</th><td></td><td>8 2 10</td><td></td><td><b>20</b></td></tr><tr><th>Lepisostidae indet.</th><td></td><td>1 2 10</td><td>23</td><td><b>36</b></td></tr><tr><th><i>Egertonia isodonta</i></th><td></td><td>35 12 7 37</td><td colspan="2">37 <b>128</b></td></tr><tr><th><i>Paralbula</i> aff. <i>P. marylandica</i></th><td></td><td>17 52</td><td></td><td><b>69</b></td></tr><tr><th><i>Phyllodus toliapicus Albula eppsi Albula oweni</i></th><td></td><td>8 15 3 23 2 1 6 1 15 3 1 6</td><td colspan="2"><b>26 33 25</b></td></tr><tr><th><i>Albula</i> sp.</th><td></td><td>3 1</td><td></td><td>4</td></tr></tbody></table>
Appendix 1 in Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths
<p><b>Appendix 1</b> (continued) Number of non-otolith taxa identified to lowest taxonomic ranking within each Claiborne Group unit. Shaded areas represent the stratigraphic range of taxa within Claiborne Group units in Alabama, USA.</p><table><thead><tr><th><b>Taxon</b></th><th colspan="5"><b>Meridian lower upper Tallahatta “lower” “upper” Tallahatta Sand Tallahatta Tallahatta /Lisbon Lisbon Lisbon Fm. Member Fm. Fm. contact Fm. Fm.</b></th><th><b>Lisbon/ Gosport contact</b></th><th><b>lower Gosport Sand</b></th><th><b>Gosport Sand</b></th><th><b>Total</b></th></tr></thead><tbody><tr><th><i>Physogaleus alabamensis</i> comb. nov. <i>Physogaleus secundus</i></th><td></td><td>31 131</td><td>1 1</td><td></td><td>185 232 1 53 555 1</td><td></td><td>15 38</td><td colspan="2">17 <b>507</b> 27 <b>786</b></td></tr><tr><th><i>Physogaleus</i> sp.</th><td></td><td></td><td></td><td></td><td>1 1</td><td></td><td></td><td></td><td><b>2</b></td></tr><tr><th><i>Galeocerdo eaglesomei</i></th><td></td><td></td><td></td><td></td><td>4 13</td><td>1</td><td>2</td><td>18</td><td><b>38</b></td></tr><tr><th><i>Galeocerdo clarkensis</i></th><td></td><td></td><td></td><td></td><td></td><td></td><td>83</td><td colspan="2">3 <b>86</b></td></tr><tr><th><i>Galeocerdo</i> sp.</th><td></td><td></td><td></td><td></td><td></td><td></td><td>16</td><td></td><td><b>16</b></td></tr><tr><th>Galeomorphii indet.</th><td></td><td></td><td></td><td></td><td>1</td><td></td><td></td><td></td><td><b>1</b></td></tr><tr><th>Pristidae indet.</th><td></td><td></td><td></td><td></td><td>4</td><td></td><td>2</td><td colspan="2">7 <b>13</b></td></tr><tr><th><i>Anoxypristis</i> sp. <i>Pristis</i> sp.</th><td></td><td>1 27</td><td></td><td></td><td>11 4 91 27</td><td></td><td>2 36</td><td>66</td><td><b>18 247</b></td></tr><tr><th><i>Propristis schweinfurthi</i></th><td></td><td></td><td></td><td></td><td></td><td></td><td>2</td><td colspan="2">8 <b>10</b></td></tr><tr><th>Myliobatiformes indet.</th><td></td><td></td><td></td><td></td><td>1 288 3</td><td></td><td></td><td>60</td><td><b>352</b></td></tr><tr><th>“ <i>Dasyatis</i> ” aff. <i>D. charlisae</i></th><td></td><td></td><td></td><td></td><td>4 4</td><td></td><td></td><td></td><td><b>8</b></td></tr><tr><th>“ <i>Dasyatis</i> ” <i>jaekeli</i></th><td></td><td>3</td><td></td><td></td><td>13</td><td></td><td></td><td></td><td><b>16</b></td></tr><tr><th>“ <i>Dasyatis</i> ” sp.</th><td></td><td></td><td></td><td></td><td>6</td><td></td><td>2</td><td></td><td><b>8</b></td></tr><tr><th><i>Aturobatis</i> aff. <i>A. aquensis</i></th><td></td><td></td><td></td><td></td><td>2</td><td></td><td></td><td></td><td><b>2</b></td></tr><tr><th><i>Coupatezia</i> sp.</th><td></td><td>1</td><td></td><td></td><td>17</td><td></td><td></td><td></td><td><b>18</b></td></tr><tr><th><i>Hypolophodon sylvestris</i></th><td></td><td>7</td><td></td><td></td><td></td><td></td><td></td><td></td><td><b>7</b></td></tr><tr><th><i>Jacquhermania duponti</i></th><td></td><td></td><td></td><td></td><td>11</td><td></td><td>16</td><td colspan="2">1 <b>28</b></td></tr><tr><th><i>Aetobatis</i> sp.</th><td></td><td></td><td></td><td></td><td>12 103</td><td>1</td><td></td><td>11</td><td><b>127</b></td></tr><tr><th><i>Aetomylaeus</i> sp.</th><td>11</td><td>80</td><td></td><td></td><td>12 123 4</td><td></td><td>153</td><td>9</td><td>392</td></tr></tbody></table>
FIG. 3 in Nouvelles faunes de rongeurs (Mammalia, Rodentia) d'âge miocène moyen en Languedoc-Roussillon (Sud de la France) ; biostratigraphie et corrélations
FIG. 3. — Biochronologie des gisements du Miocène moyen en Languedoc-Roussillon et corrélations avec les sites de la région lyonnaise. B.K.S.A., Berggren, Kent, Swisher, Aubry.
FIG. 5 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 5. Paleogene outcrops on the Houldjin escarpment and Wulanhuxiu (= Chimney Butte, 8 mi north of the Tukhum Lamasery): A, the yellow and gray, pebbly gravels of the Houldjin Formation on the Houldjin escarpment near the Erenhot Railway Station; B, the outcrops at Wulanhuxiu, showing a steep, upper "red member" and a gradual, lower "white member."
FIG. 4 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 4. Stratigraphic distributions of perissodactyl fossils and taxa in the Tukhum, Shara Murun, Ulan Gochu, and Baron Sog formations at Baron Sog Mesa. The profile of the section is based on the sketch at Xilin Nor North (= 4 mi north of Baron Sog Mesa) (Granger, 1925, see also Wang et al., 2012, fig. 2A). The superscripts in front of taxon names indicate the localities of the holotypes: numbers 1, and 2 refer to Ula Usu and 4 mi north of Baron Sog Mesa, respectively. Abbreviations: BS, Baron Sog Formation; Hyra., Hyracodontidae; P., Paraceratheriidae; T, Tukhum Formation; and UG, Ulan Gochu Formation.
FIG. 2 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 2. Cranial and mandibular reconstructions of typical Eocene perissodactyls from the Erlian Basin of Inner Mongolia, China. tapiroid A, Lophialetes expeditus; B, Paracolodon fissus; paraceratheriid C, Pappaceras meiomenus; D, Juxia sharamurenensis; amynodontid E, Rostriamynodon grangeri; F, Sharamynodon mongoliensis; brontotheriid G, Protitan grangeri; H, Embolotherium andrewsi. Scale bar equals 10 cm.
FIG. 1 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 1. Paleogene fossil localities in the Erlian Basin of Inner Mongolia, China, and the related routes of Central Asiatic Expeditions during 1920s (modified from Jiang, 1983; Mao and Wang, 2012; Wang et al., 2012). 1, Houldjin; 2, Arshanto; 3, Irdin Manha; 4, Daoteyin Obo (= Overnight Camp, 5 mi east of Camp Margetts); 5, Duheminboerhe (= Camp Margettes); 6, Nuhetingboerhe (= 6 mi west of Camp Margetts); 7, Wulanboerhe; 8, Huheboerhe (= 7 mi west and southwest [235°] of Camp Margetts); 9, Chaganboerhe (= 10 mi southwest of Camp Margetts); 10, Bayan Ulan; 11, Nom Khong (= Holy Mesa); 12, Wulantaolegai (= Viper Camp, 4 mi north of Tukhum Lamasery); 13, Wulanhuxiu (= Chimney Buttes, 8 mi north of Tukhum Lamasery); 14, Erden Obo (= Urtyn Obo); 15, Ganggan Obo (= Ulan Shireh Obo); 16, Heretu (= Spring Camp); 17, Bayan Obo (= Twin Obos); 18, Jhama Obo; 19, Xilin Nor North (= 4 mi north of Baron Sog Lamasery); 20, Ulan Gochu (= 8 mi north of Baron Sog Lamasery); 21, Ula Usu. The black-and-white dashed line represents railway.
FIG. 7 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 7. Paleogene outcrops in the Shara Murun region: A, the outcrops at Ula Usu, where the Shara Murun Formation was named, showing an upper member dominated by white sandstones and a lower member dominated by sandy clays with varied colors; B, the outcrops at Xilin Nor North (= 4 mi north of Baron Sog Lamasery), showing the red clays of the Ulan Gochu Formation overlying the grayish white sandstones of the upper part of the Shara Murun Formation.
FIG. 6 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 6. Sketch profile from Wulanhuxiu (= Chimney Butte, 8 mi north of Tukhum Lamasery) at North Mesa (Granger, 1928: 6). The layers 3–5 are grouped into an upper "red member", and the layers 6–14 are grouped into a lower "white member."
FIG. 9 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 9. Paleogene outcrops at Erden Obo: A, the outcrops of the "Lower Red," "Lower White," and "Middle Red." The lower-right part of the photo is mainly the "Lower White," which overlies the "Lower Red" and is overlain by the "Middle Red" as shown by the hill, far left; B, the outcrops of the "Middle Red," "Middle White," "Upper Red," and "Upper White." The lower-right part of the photo is mainly the basal part of the "Upper Red," which overlies the "Middle White" and is overlain by the "Upper White (or yellow)." The top of the "Upper White" forms the Gobi surface.
FIG. 10 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
FIG. 10. Stratigraphic distributions of perissodactyl fossils and taxa from Erden Obo. The profile of section is based on the sketch by Granger (1928) and modified from Li (2017). The asterisks in front of taxa indicate where the holotype occurred in the section. Abbreviations: Amyno., Amynodontidae; BR, Basal Red; BW, Basal White; Chali., Chalicotherioidea; LR, Lower Red; MW, Middle White; and UW, Upper White.
Figure 17. A–G in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 17. A–G, Operculinoides soldadensis Vaughan & Cole; A, Loma El Santo, CA-215-871; B, Loma Candelaria, 98LC-1-669; C– F, Norona; C, NOR-UN 24; D–F, NOR-UN 15/14; G, holotype, Trinidad. H, I, Palaeonummulites trinitatensis (Nutall); H, Loma Candelaria, 98LC-1ICT3; I, holotype of Operculinoides kugleri Vaughan & Cole, Trinidad. J, Operculinoides ocalanus (Cushman), Loma Jabaco, CA-4-724. A–D, G–J, A forms in equatorial section; E, A form in axial section; F, external view.
Figure 18. A, B, D–H in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 18. A, B, D–H, Heterostegina ocalana Cushman; A, Loma Viǵıa, CA-216-D1a; B, Norona, NOR-UN 15/14; D, Loma Viǵıa, CA-216-79; E, F, Loma Jabaco; E, LM-52-756; F, LM-52-752; G, H, Norona, NOR-UN 24. C, Heterostegina cubana Cizancourt, Loma candelaria, 98LC-1H-809. I, Heterostegina sp. indet., Loma Candelaria, 98LC-1H-808. A, B, A forms in axial section; C–G, I, A forms in equatorial section; H, external view.
Figure 14 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 14. Distribution of larger benthic foraminifera (LBF) in the Loma Viǵıa section, central Cuba.
Figure 12 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 12. Distribution of larger benthic foraminifera (LBF) in the Loma El Santo section, central Cuba.
Figure 11 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 11. Distribution of larger benthic foraminifera (LBF) in the Loma Candelaria section, western Cuba (modified from Torres-Silva et al. 2017).
Figure 15. Nummulites striatoreticulatus Rutten. A–C in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 15. Nummulites striatoreticulatus Rutten. A–C, Entronque de Herradura; A, 98LC-2-686; B, 98LC-2-687; C, 98LC-2-1a. D–F, Loma Candelaria; D, 98LC-1-660; E, 98LC-1-630; F, 98LC-1-806. G–K, La Esperanza; G, E-126-474; H, E-126-466; I, E-126-458; J, E-126-470, gaps in the septa between adjacent alar prolongations of the chambers; K, E-126-459; L, M, Loma El Santo; L, CA-215- 865; M, CA-215- 65. A, B, E, F, H, I, L and M are A forms in equatorial section; C, D, G and J are A forms in axial section.
Figure 13 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 13. Distribution of larger benthic foraminifera (LBF) in the Norona section, western Cuba (modified from Torres-Silva et al. 2017).
Figure 10 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 10. Distribution of larger benthic foraminifera (LBF) in the Entronque de Herradura section, western Cuba.
Figure 8 in Morphometric analysis of Eocene nummulitids in western and central Cuba: taxonomy, biostratigraphy and evolutionary trends
Figure 8. Palaeogeographical distribution of the Eocene nummulitid species found at the Cuban localities. Map adapted from Pindell (2009).
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