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Figure 2 in An alternative interpretation of Peltochelys duchastelii as a paracryptodire
Figure 2. The results of three separate phylogenetic hypotheses that include Peltochelys duchastelii. (a) The single most parsimonious tree with a length of 7.04066 resulting from the expanded analysis of Gaffney et al. (2007). (b) The strict consensus of the 27 most parsimonious solutions with a length of 13.43147 resulting from the updated analysis of Joyce (2007). (c) A time-calibrated extract of the single most parsimonious solution with a length of 9.22411 resulting from the expanded analysis of Lyson and Joyce (2011). The range of North American taxa is highlighted in blue and that of European taxa is highlighted in red.
Figure 1 in An alternative interpretation of Peltochelys duchastelii as a paracryptodire
Figure 1. IRSNB Ct.R.16, lectotype, Peltochelys duchastelii, Early Cretaceous (middle Barremian–early Aptian) Sainte-Barbe Formation of Bernissart, Hainault Province, Belgium. Photographs and line drawings in (a) dorsal and (b) ventral view. Arabic numerals denote the neural elements. Abbreviations: Ab, abdominal scute; An, anal scute; co, costal; EG, extragular; ent, entoplastron; epi, epiplastron; Fe, femoral scute; Gu, gular scute; Hu, humeral scute; hyo, hyoplastron; hyp, hypoplastron; IM, inframarginal scute; Ma, marginal scutes; nu, nuchal; Pe, pectoral scutes; per, peripheral; Pl, pleural scutes; py, pygal; sp, suprapygal; Ve, vertebral scute; xi, xiphiplastron.
Figure 12 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 12. Columnar section of the Cenomanian–Turonian boundary and the Lower and Middle Turonian part of the Wunstorf core Wu 2010/4 with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 4.
Figure 11 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 11. Columnar section of the Cenomanian part of the Baddeckenstedt quarry with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 3; log redrawn after Wilmsen (2003: Fig. 8).
Figure 6 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 6. Late Albian to Turonian agglutinated foraminifera from the Lower Saxonian Cretaceous; scale bars are 100 µm. (a) Saccammina grzybowski, Wunstorf Wu2010/1, 54.00 m. (b) Psammosphaera fusca, Wunstorf Wu2010/1, 59.05 m. (c) Tipeammina elliptica, Söhlde section, 31.00 m. (d–e) Tipeammina sp. 1, Wunstorf Wu2010/4, 43.30 m. (f) Hyperammina gaultina, Wunstorf Wu 2010/4, 48.20 m. (g–h) Ammolagena clavata, two specimens sticking together, Wunstorf Wu2010/3, 25.50 m. (i) Ammolagena contorta, possibly previously attached on an inoceramid prism, Wunstorf Wu2010/4, 38.20 m. (j) Caudammina ovula, Söhlde section, 31.00 m. (k) Subreophax scalaris, Wunstorf Wu2010/1, 69.10 m. (l) Ammodiscus cretaceus, Wunstorf Wu 2010/4, 48.20 m. (m) Ammodiscus glabratus, Wunstorf Wu2010/1, 54.65 m. (n) Ammodiscus peruvianus, Wunstorf Wu2010/1, 54.00 m. (o) Ammodiscus tenuissimus, Wunstorf Wu2010/4, 43.30 m. (p) Glomospira diffundens, Wunstorf Wu2010/1, 49.05 m. (q) Glomospira gordialis, Wunstorf Wu 2010/3, 66.05 m. (r) Repmanina charoides, Wunstorf Wu2010/4, 38.20 m. (s) Lituotuba lituiformis, Wunstorf Wu 2010/4, 48.95 m. (t) Rzehakina minima, Wunstorf Wu2010/1, 54.80 m.
Figure 8 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 8. Late Albian to Turonian agglutinated foraminifers from the Lower Saxonian Cretaceous; scale bars are 100 µm. (a) Tritaxia gaultina, Wunstorf Wu2010/1, 19.05 m. (b) Tritaxia tricarinata, Wunstorf Wu2010/1, 19.05 m. (c) Tritaxia macfadyeni, Wunstorf Wu2010/1, 34.10 m. (d–e) Eggerellina brevis, Baddeckenstedt section, 19.30 m. (f) Eggerellina mariae, Wunstorf Wu2010/3, 30.15 m. (g) Flourensina intermedia, Wunstorf Wu2010/1, 54.80 m. (h) Gaudryina sp. 1, Baddeckenstedt section, 39.00 m. (i) Verneuilinoides sp., Wunstorf Wu2010/4, 48.95 m. (j) Vialovella frankei, Wunstorf Wu2010/1, 15.20 m. (k) Arenobulimina bochumensis, Baddeckenstedt section, 9.00 m. (l) Arenobulimina preslii, Wunstorf Wu2010/4, 43.30 m. (m) Arenobulimina truncata, Wunstorf Wu2010/4, 43.30 m. (n–o) Ataxophragmium depressum, Wunstorf Wu2010/4, 58.60 m. (p) Hagenowella elevata, Wunstorf Wu2010/4, 58.60 m. (q) Voloshinoides advenus, Wunstorf Wu2010/1, 29.25 m. (r) Voloshinoides anglicus, Baddeckenstedt section, 7.00 m. (s) Pseudotextulariella cretosa, Wunstorf Wu2010/1, 19.05 m. (t) Kadriayina gradata, Wunstorf Wu2010/3, 66.05 m. (u) Marssonella ozawai, Wunstorf Wu2010/1, 15.20 m.
Figure 3 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 3. Schematic locality details of the study area of Wunstorf and position of the cores: green (Voigt et al., 2008b), blue (Erbacher et al., 2020), and red (this study). Modified from Seibertz (2013: Fig. 5).
Figure 9 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 9. Columnar section of the Albian to Cenomanian part of the Wunstorf core Wu 2010/1 with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 3.
Figure 1 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 1. Paleogeographical map of Europe and the study area. (A) Paleogeography of Europe during the Cenomanian, modified after Philip and Floquet (2000). (B) Paleogeography of southern Lower Saxony during the early Cenomanian, modified from Wilmsen et al. (2021), base map from Hiss (1995).
Figure 7 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 7. Late Albian to Turonian agglutinated foraminifers from the Lower Saxonian Cretaceous; scale bars are 100 µm. (a) Reophax subfusiformis, Wunstorf Wu2010/1, 54.00 m. (b) Pseudonodosinella nodulosa, Wunstorf Wu2010/4, 48.20 m. (c) Pseudonodosinella parvula, Wunstorf Wu2010/4, 48.20 m. (d) Pseudonodosinella troyeri, Baddeckenstedt section, 39.00 m. (e) Haplophragmoides suborbicularis, Wunstorf Wu2010/3, 70.50 m. (f) Haplophragmoides walteri, Wunstorf Wu2010/4, 48.95 m. (g) Ammobaculites agglutinans, Söhlde section, 31.00 m. (h) Ammobaculites wenonahae, Wunstorf Wu2010/1, 19.05 m. (i) Bulbobaculites problematicus, Wunstorf Wu2010/1, 24.75 m. (j) Spiroplectammina navarroana, Wunstorf Wu2010/4, 48.20 m. (k) Spiroplectinella cretosa, Baddeckenstedt section, 2.00 m. (l) Bicazammina lagenaria, Söhlde section, 24.00 m. (m) Parvigenerina sp. 3, Wunstorf Wu2010/4, 48.95 m. (n) Eobigenerina kuhnti, Söhlde section, 9.50 m. (o) Eobigenerina variabilis, Söhlde section, 1.50 m. (p) Rectogerochammina eugubina, Wunstorf Wu2010/4, 48.95 m. (q) Gerochammina stanislawi, Wunstorf Wu2010/4, 53.15 m. (r) Plectina cenomana, Wunstorf Wu2010/3, 45.00 m. (s) Plectina mariae, Wunstorf Wu2010/3, 84.00 m.
Figure 4 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 4. Correlated columnar sections of the Wunstorf cores Wu 2010/1 and Wu 2010/3 and their carbon isotope patterns. On the right correlation to the carbon isotopes of the Wunstorf Wu2011/8 core of Erbacher et al. (2020: Fig. 3) and to the Anderten-1 core of Bornemann et al. (2017: Fig. 3). Brown bar: correlation of a sequence boundary based on the isotopic pattern; green bar: correlation based on a bio-event; grey bar: correlation based on a lithoevent.
Figure 2 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 2. Chronostratigraphy, selected events, and depositional sequences as well as interpreted sea level curve of the Lower Saxony Cretaceous. Depositional sequences, associated sequence boundaries, and sea level curve are from Janetschke et al. (2015). Age of stage boundaries are from Gradstein et al. (2020).
Figure 13 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 13. Columnar section of the Cenomanian–Turonian boundary and the Lower to Upper Turonian part of the Söhlde–Loges quarry with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 4; log redrawn after Wiese (2009: Fig. 6).
Figure 10 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 10. Columnar section of the Lower Cenomanian part of the Wunstorf core Wu 2010/3 with agglutinated foraminiferal morphogroups, Fisher alpha index, species richness, and foraminiferal events (acmes) indicated by arrows. For log legend, see Fig. 3.
Figure 14 in Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation
Figure 14. Albian, Cenomanian, and Turonian FOs and LOs (first – and last occurrences) of selected agglutinated foraminifers from Lower Saxony (Wunstorf, Baddeckenstedt, Söhlde), the Münsterland (Frieg and Kemper, 1989) and the English Chalk (Hart et al., 1989), and the DWAF (deep-water agglutinated foraminifera) zonation of the western Tethys (Coccioni et al., 1995; Kaminski et al., 2011).
Fig. 2 in Phylogenetic placement of a new paleoendemic pill scarab from the Udzungwa Mountains, Tanzania, triggers biogeographic interpretations (Coleoptera: Hybosoridae, Ceratocanthinae)
Fig. 2 – Balleriodes sphaera gen. et sp. nov., paratypes (A-R, specimen 8969, S, specimen 8752), details. A-B, head, fronto-dorsal (A) and frontal (B); C, maxilla; D, labrum; E-F, mandibles; G, antenna; H: labium; I-J, elytron in ventral view showing phoretic mites (J, enlarged); K, prothorax, ventral view; L-N, fore, middle and hind left legs; O, pterothorax, ventral view; P-R, phallobase and parameres, right lateral (P), left lateral (Q) and dorsal (R) views; abdomen, with male genitalia in situ. Images are not to scale.
Fig. 4 in Phylogenetic placement of a new paleoendemic pill scarab from the Udzungwa Mountains, Tanzania, triggers biogeographic interpretations (Coleoptera: Hybosoridae, Ceratocanthinae)
Fig. 4 – Habitus of select ingroup and outgroup pill scarabs, left lateral view; images are to scale.
Fig. 5 in Phylogenetic placement of a new paleoendemic pill scarab from the Udzungwa Mountains, Tanzania, triggers biogeographic interpretations (Coleoptera: Hybosoridae, Ceratocanthinae)
Fig. 5 – Maximum likelihood tree of Ceratocanthinae pill scarabs (Coleoptera: Hybosoridae), as reconstructed by RAxML from the three-fragment concatenated matrix.Balleriodes sphaera gen. et sp. nov. is inside the monophyletic Synarmostes group. Branches with ML bootstrap support percentage ≥90 are marked by black circles; those with bootstrap <90 and ≥75 are marked by open rhombi. Colours of Ceratocanthinae taxa and branches indicate their biogeographical region. Habitus images are to scale; small black arrows indicate imaged specimens.
Fig. 1 – A in Phylogenetic placement of a new paleoendemic pill scarab from the Udzungwa Mountains, Tanzania, triggers biogeographic interpretations (Coleoptera: Hybosoridae, Ceratocanthinae)
Fig. 1 – A, Distribution of Balleriodes sphaera gen. et sp. nov. and potentially related and/or similar pill scarabs in Africa and Madagascar. B-F: Balleriodes sphaera gen. et sp. nov., holotype, habitus (B: left lateral, C: dorsal, D: ventral; E: anterior, F: posterior).
Fig. 1. A in Alternative interpretations of some earliest Ediacaran fossils from China
Fig. 1. A new Lantian fossil illustrated by Yuan et al. (2011: fig. 3E), ~632.5 6 0.5 Myr, southern Anhui, Province, South China. A. Specimen of Type A (NIGPAS−LT−295) showing corner crown consisting of a single ribbon. B. Line drawing B apical angle showing an alternative interpretation of this fossil as a conulariid or conulariid−like cnidarian.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.