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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. 5 in The hyaenodonts (Mammalia) from the French locality of Aumelas (Hérault), with possible new representatives from the late Ypresian
FIG. 5. — Values of the Ln (body mass) of mesonychids, oxyaenids, and hyaenodonts ("Proviverrinae" sensu Solé (2013), "Sinopinae", "Arfiinae", Hyaenodontinae, and Hyainailourinae) from MP7 to MP19 with particular attention on hyaenodonts from Aumelas. Aumelas is here represented to be close to the MP11 referencelevel. Abbreviations: ELMA, European Land Mammal Ages; EMP, Mammal Palaeogene. Values are available at Appendix 6.
Text-fig. 6. Correlation of the Cheringoma and Mazamba formations on the basis of benthic foraminiferans and mammals respectively. Identifications of foraminiferans are from Newton (1924) and Abrard (1928), and the ranges of foraminiferans are from Sella-Kiel et al. (1998). The time scale is from Gradstein et al. (2020). The distribution of Nummulites atacicus is included, but it is not known whether it is reworked from older deposits. If the identification is valid, it would support the thesis that there was a period of Ypresian deposition in the vicinity during which remains of the species were fossilised. in Stratigraphy, Chronology And Palaeontology Of The Tertiary Rocks Of The Cheringoma Plateau, Mozambique
Text-fig. 6. Correlation of the Cheringoma and Mazamba formations on the basis of benthic foraminiferans and mammals respectively. Identifications of foraminiferans are from Newton (1924) and Abrard (1928), and the ranges of foraminiferans are from Sella-Kiel et al. (1998). The time scale is from Gradstein et al. (2020). The distribution of Nummulites atacicus is included, but it is not known whether it is reworked from older deposits. If the identification is valid, it would support the thesis that there was a period of Ypresian deposition in the vicinity during which remains of the species were fossilised.
Figure 1 in A new species of the genus Cephalallus Sharp, 1905 (Coleoptera: Cerambycidae) from the Ypresian of Denmark
Figure 1. Cephalallus vitalii sp. n., no. MGUH 34320, body. a – part of impression, b – counterpart of impression, c – part of impression, with alcohol, d – counterpart of impression, with alcohol, e – outline, part of impression, f – outline, counterpart of impression. Scale bars = 2.0 mm.
Fig. 2 in A new pentatomoid bug from the Ypresian of Patagonia, Argentina
Fig. 2. Ventral habitus of female of pentatomoid bug Chinchekoala qunita gen. et sp. nov., holotype MPEF-PI 944b from Laguna del Hunco (Chubut, Argentina); Ypresian, lower Eocene. Photograph (A), camera lucida drawing (B).
Fig. 3 in A new pentatomoid bug from the Ypresian of Patagonia, Argentina
Fig. 3. Details of dorsal habitus of female of pentatomoid bug Chinchekoala qunita gen. et sp. nov., holotype MPEF-PI 944a from Laguna del Hunco (Chubut, Argentina); Ypresian, lower Eocene. Head (A), eye (B), last tergites (C).
Fig. 1 in A new pentatomoid bug from the Ypresian of Patagonia, Argentina
Fig. 1. Dorsal habitus of female of pentatomoid bug Chinchekoala qunita gen. et sp. nov., holotype MPEF-PI 944a from Laguna del Hunco (Chubut, Argentina); Ypresian, lower Eocene. Photograph (A), camera lucida drawing (B).
Fig. 4 in A new pentatomoid bug from the Ypresian of Patagonia, Argentina
Fig. 4. Details of ventral habitus of female of pentatomoid bug Chinchekoala qunita gen. et sp. nov., holotype MPEF-PI 944b from Laguna del Hunco (Chubut, Argentina); Ypresian, lower Eocene. Head (A), thoracic scent efferent system (B), genitalia (C).
Fig. 12 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 12. Character matrix of Daouitherium and other primitive lophodont proboscideans (see text: features 1–19) and most parsimonious cladogram resulting from parsimony analysis with Hennig86 program, with distribution of the derived features. Length = 56; CI = 85; RI = 82. This cladogram is unrooted. The significance of Daouitherium for the ancestral morphotype of proboscideans and the basal relationships of lophodont proboscidean taxa with respect to other proboscideans (e.g., Moeritherium, deinotheres) and tethytherians will be investigated separately with the study of the new material of Phosphatherium (work in preparation). Analysed features are additive and are weighted according to their relative importance (see matrix);howeverananalysisofthismatrixwithoutweightingthefeaturesdoes not change the resulting topology. Several reversions that are possible according to the algorithm have been discounted as being anatomically unlikely (features 1, 3, 4). Asterisk indicates convergent feature.
Fig. 9 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 9. Log transformed plot comparing the relative size (length × width) of the jugal teeth of Daouitherium and Numidotherium. After Court (1995: fig. 1). Note the slightly smaller size of Daouitherium and the strong size difference between m1 and m2. N. koholense is probably specialized in its large p2 with respect to p3 (feature 7).
Fig. 10 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 10. Comparison of the lower jugal dentition of Daouitherium rebouli gen. et sp. nov. and Numidotherium koholense. Occlusal sketches of the teeth. A. Daouitherium rebouli,CPSGMMA4,leftp2–4,m1–3,andalveoli for i1 or i2, i2 or i3, i3 or c1, c1 or p1. B. Numidotherium koholense, cast of unumbered specimen with left i1–2, diastema, p2–4, and m1–3. Drawings not to scale; scale bars 5 mm.
Fig. 11 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 11. Comparison of the upper premolar referred to Daouitherium rebouli gen. et sp. nov. with those of Phosphatherium and Numidotherium A. Phosphatherium escuilliei, holotype, P3–4. B. Phosphatherium escuilliei, PM18, P4. C. Daouitherium rebouli, CPSGM MA6, P4?. D. Numidotherium koholense, P3–4, unumbered cast. Occlusal sketches of the teeth. Drawings not proportional; scale bars 5 mm. CPSGM MA6 belongs to a noticeably small individual with respect to the hypodigm of Daouitherium rebouli.
Fig. 8 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 8. Daouitherium rebouli gen. et sp. nov. CPSGM MA6, left p4 in occlusal stereo−view. Anterior is up.
Fig. 7. Daouitherium rebouli gen. etsp.nov.MNHNPM3 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 7. Daouitherium rebouli gen. etsp.nov.MNHNPM3,rightdentary with with ascending ramus and m1–3, p3. in labial (A) and lingual (B) views.
Fig. 5 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 5. Daouitherium rebouli gen. et sp. nov. Drawing of m1–3, p2–4 preservedintheholotype,CPSGMMA4inlingual(A),labial(B),andocclusal (C) views. Scale bars 10 mm.
Fig. 6 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 6. Daouitherium rebouli gen. et sp. nov. MNHN PM3, right dentary with m1–3 and p3 in occlusal view.
Fig. 2 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 2. Daouitherium rebouli gen. et sp. nov. Holotype, CPSGM MA4, left dentary with m1–3, p2–4, and anterior alveoli in labial stereo−view (A) and lingual stereo−view (B).
Fig. 4 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 4. Daouitherium rebouli gen. et sp. nov. Holotype, CPSGM MA4. Detail of the anterior part showing the p2 and anterior alveoli (arrows) in sub−occlusal view.
Fig. 3 in A new large mammal from the Ypresian of Morocco: Evidence of surprising diversity of early proboscideans
Fig. 3. Daouitherium rebouli gen. et sp. nov. Holotype, CPSGM MA4. Detailed occlusal stereo−view of p2–4 (A), m1–2 (B), and m3 (C).
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