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Fig. 3 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 3: 1-9 Globotruncanella coarctata (Bolli 1957), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12427; 10-17 Globotruncanella pshadae (Keller 1946), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12427; 18-20 Globotruncanella petaloidea (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12428; 21-24 Globotruncanella havanensis (Voorwjik 1937), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12329; 25-27 Globotruncanella saratogensis (Applin 1920), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12441; 28-30 Rugotruncana subrugosa (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12420; 31 Schsckoina multispinata (Cush.Wick 1940), Maastrichtian, Țâța Valley, PietroȘița-Fieni (All specimens x 90).

Fig. 2 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 2: 1-3 Rugoglobigerina pennyi Brönnimann 1952, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV. 12417; 4-9 Rugoglobigerina subbotinae Maslakova 1978, Maastrichtian, Țâța Valley, LPB.IV. 12411; 10-12 Rugoglobigerina kingi Trujillo 1960 Maastrichtian, Țâța Valley, L.P.B.IV. 12450; 13- 15 Rugoglobigerina ordinaria (Subbotina 1953), Maastrictian, Țâța Valley, LPB.IV.12446; 16-21 Rugotruncana subglaessneri (Gandolfi 1955), Maatrichtian, Țâța Valley, PietroȘița, LPB.IV.12421, 22- 25 Rugotruncana subornata (Gandolfi 1955), Maatrichtian, Țâța Valley, LPB.IV.12440; 26-28 Rugotruncana subrugosa (Gandolfi 1955), Țâța Valley, LPB.IV. 12436; 29-31 Rugotruncana subhexacamerata (Gandolfi 1955), Maastrichtian, Țâța Valley, LPB.IV.12426; 32-34 Rugotruncana subcircumnodifer (Gandolfi 1955), Maastrichtian, Țâța Valley, LPB.IV.12431 (All specimens x 90).

Fig. 13 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 13: 1-3 Rugotruncana subpennyi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12426; 4-6 Rugotruncana subhexacamerata (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12422; 7-12 Archaeoglobigerina blowi Pessagno 1967, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12441; 13-15 Globotruncanella pshadae (KELLER 1946), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12427; 16-18 Rugoglobigerina kelleri (Subbotina 1953), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12451; 19-26 Globotruncanella sarmientoi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12448 (All specimens x 90).

Fig. 5 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 5: 1-3 Rugoglobigerina pennyi Brönnimann 1952, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12417; 4-6 Rugoglobigerina pustulata Brönnimann 1952, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12415; 7-9 Rugoglobigerins kelleri (Subbotina 1953), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12451; 10-12, 27-29 Rugoglobigerina macrocephala Brönnimann, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12413; 13-15, 19-24 Rugotruncana ellissi Brönnimann & Brown 1955, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV 12426; 16-18 Rugoglobigerina loetterli (Nauss 1947), Maestrichtian, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12443; 15-27 Globotruncanella sarmientoi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița LPB.12448 (All specimens x 90).

Fig. 16 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 16: 1-17 Abatomphalus pessagnoi (Longoria 1973), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12434; 18-20 Rugotruncana subbeldigi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12452; 21-26 Rugotruncana subloetterli (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12423 (All specimens x 90).

Fig. 15 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 15: 1-3 Globigerinella glaessneri (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12418; 4-12 Rugotruncana subcircumnodifer (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12439; 13-24 Globotruncanella sarmientoi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12448; 25-27 Rugoglobigerina kingi Trujillo 1960, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12450 (All specimens x 90).

Fig. 8 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera

Fig. 8: 1-3 Globotruncanella coarctata (Bolli 1957), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12437; 4-6 Globigerinella glaessneri (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12418; 7-9 Archaeoglobigerina blowi Pessagno 1967, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12449; 10-12 Rugotruncana subpenny (Gandolfi l955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12426; 13-18 Rugoglobigerina kelleri (Subbotina 1953), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12451; 19-21 Rugotruncana tilevi Brönnimannn & Brown 1955, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12436; 22-27 Abatomphalus pessagnoi (Longoria 1973), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12434 (All specimens x 90).

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Text-fig. 3. Filogranula cincta (GOLDFUSS), locality Chrtníky (Early Turonian), no. NM-O7620, a – general view of two specimens attached to a lychniscosan sponge Diplodictyon heteromorphum. Length of the sponge is 60 mm. b – detail of the tubes. Length of the left tube is 5.4 mm. The diameter of the aperture is 1.2 mm. Length of the right tube is 6 mm without the looped posterior portion. The diameter of the aperture is 1.4 mm. Scale bars are 5 mm. in Filogranula Cincta (G , 1831), A Serpulid Worm (Polychaeta, Sedentaria, Serpulidae) From The Bohemian Cretaceous Basin

Text-fig. 3. Filogranula cincta (GOLDFUSS), locality Chrtníky (Early Turonian), no. NM-O7620, a – general view of two specimens attached to a lychniscosan sponge Diplodictyon heteromorphum. Length of the sponge is 60 mm. b – detail of the tubes. Length of the left tube is 5.4 mm. The diameter of the aperture is 1.2 mm. Length of the right tube is 6 mm without the looped posterior portion. The diameter of the aperture is 1.4 mm. Scale bars are 5 mm.

Fig. 1 in A new mammal from the Turonian-Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania

Fig. 1. Digital surface reconstructions from μCT scans of the?gondwanatherian mammal Galulatherium jenkinsi sp. nov. (holotype, RRBP 02067) from the Turonian–Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania; left dentary in lateral (A1), medial (A2), anterior (A3), posterior (A4), dorsal (A5), and ventral (A6) views. Dashed line estimates the anterior margin of the masseteric fossa. Abbreviations: ch, lower cheek teeth; inc, lower incisor.

Fig. 5 in A new mammal from the Turonian-Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania

Fig. 5. Lower jaw reconstruction of the?gondwanatherian mammal Galulatherium jenkinsi sp. nov. (holotype, RRBP 02067, A) from the Turonian– Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania and gondwanatherian mammal Sudamerica ameghinoi Scillato-Yané and Pascual, 1984 (holotype, MPEFCH 534, B) from the Paleocene Salamanca Formation, Punta Peligro, Chubut Province, Argentina; in dorsal (A1, B1), left lateral (A2, B2), posterior (A3, B3), and anterior (A4, B4) views. The preserved left dentaries of both Galulatherium and Sudamerica have been digitally mirrored to approximate the conformation of the anatomy from the contralateral side. The displaced apical ends of ch2–ch4 in Galulatherium have been digitally repositioned (see SOM 4 for details regarding repositioning).

Fig. 3 in A new mammal from the Turonian-Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania

Fig. 3. Digital semi-transparent reconstructions from μCT scans of the ? gondwanatherian mammal Galulatherium jenkinsi sp. nov. (holotype, RRBP 02067) from the Turonian–Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania; lower left dental series in buccal (A3) and lingual (A4) views to illustrate the extent of the pulp cavity within individual teeth. Ghosted left dentary (medium gray) with teeth in-situ (light gray crowns, dark gray roots) to highlight hypselodonty and relative positions of teeth within the dentary (A1). Digital semi-transparent reconstruction of left dentary with teeth in-situ to highlight path of mandibular canal ( dark gray) (A2). Abbreviations: ch, lower cheek teeth; inc, lower incisor.

Fig. 2 in A new mammal from the Turonian-Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania

Fig. 2. Digital surface reconstructions from μCT scans of the?gondwanatherian mammal Galulatherium jenkinsi sp. nov. (holotype, RRBP 02067) from the Turonian–Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania; lower left dental series in buccal (A1), apical/occlusal (A2), abapical/ventral (A3), and lingual (A4) views. Abbreviations: ch, lower cheek teeth; d, distal edge of incisor; inc, lower incisor; ics1, incisor cross-section near alveolar margin; ics2, incisor cross-section near root tip; ln, lingual edge of incisor; dashed lines indicate the approximate locations from which incisor metrics were collected.

Fig. 4 in A new mammal from the Turonian-Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania

Fig. 4. Selected μCT slice images highlighting internal anatomy of the left dentary of the?gondwanatherian mammal Galulatherium jenkinsi sp. nov. (holotype, RRBP 02067) from the Turonian–Campanian (Upper Cretaceous) Galula Formation, southwestern Tanzania. Sagittal slices with top image corresponding to locations of slices through dataset. YZ150 (A1), YZ200 (A2), YZ225 (A3), YZ245 (A4), YZ253 (A5), YZ285 (A6). Abbreviations: ch, lower cheek teeth; inc, lower incisor.

Fig. 5 in Ammonoid biodiversity changes across the Cenomanian-Turonian boundary in the Yezo Group, Hokkaido, Japan

Fig. 5. Temporal changes in faunal components of ammonoid species richness in the Mikasa area. Abbreviations: CIUs, carbon isotopic units; e., early; m., middle.

Fig. 4 in Ammonoid biodiversity changes across the Cenomanian-Turonian boundary in the Yezo Group, Hokkaido, Japan

Fig. 4. Temporal changes in ammonoid species richness, extinction, and origination rates in the Mikasa, Obira, and Oyubari areas. Abbreviations: CIUs, carbon isotopic units; CTBE, Cenomanian–Turonian boundary event; e., early; m., middle.

Fig. 2 in Ammonoid biodiversity changes across the Cenomanian-Turonian boundary in the Yezo Group, Hokkaido, Japan

Fig. 2. Composite columnar sections in the Mikasa (A), Obira (B), and Oyubari (C) areas and the stratigraphical levels of macrofossil datum planes used in the present study. The shaded portion shows the Cenomanian–Turonian boundary event (CTBE). The molluscan fossil data are from Tanabe et al. (1977), Futakami (1986), Kurihara and Kawabe (2003), Funaki and Hirano (2004), Kurihara et al. (2007) and unpublished original data. The planktonic foraminiferal zonation and the CTBE are from Hasegawa (1997, 1999), Nishi et al. (2003), Kurihara (2006), and Uramoto et al. (2007, 2009). Abbreviations: Ka, Katsurazawa Formation; Hk, Hikagenosawa Formation; mdst, mudstone; sdst, sandstone; A. nipponicus, Actinoceramus nipponicus; Hel. helvetica, Helvetoglobotruncana helvetica; I. hobetsensis, Inoceramus hobetsensis nonsulcatus; I. kamuy, Inoceramus kamuy; W. arc., Whiteinella archaeocretacea.

Fig. 3 in Ammonoid biodiversity changes across the Cenomanian-Turonian boundary in the Yezo Group, Hokkaido, Japan

Fig. 3. Correlation of Upper Cretaceous δ13C stratigraphy of terrestrial organic materials in the Mikasa, Obira, and Oyubari areas, Japan and reference δ13C stratigraphy of carbonates in Europe (after Jarvis et al. 2006). Six carbon isotopic units (CIUs) were identified in the present study. Abbreviations: e., early; m., middle; PDB, Pee Dee Belemnite Standard; Aj, Acanthoceras jukesbrownei; An, Actinoceramus nipponicus; Ar, Acanthoceras rhotomagense; Ca, Calycoceras spp.; Cg, Calycoceras guerangeri; Ci, Cunningtoniceras inertme; Cu, Cunningtoniceras spp.; Cw, Collignoniceras woollgari; Fc, Fagesia catinus; Ih, Inoceramus hobetsensis; Ik, Inoceramus kamuy; Md, Mantelliceras dixoni; Mg, Metoicoceras geslinianum; Mn, Mammites nodosoides; Nj, Neocardioceras juddii; Wd, Watinoceras devonense.

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Fig. 5 in Lower Turonian record of belemnite Praeactinocamax from NW Siberia and its palaeogeographic significance

Fig. 5. Palaeogeographic map of the Northern hemisphere (North pole projection). A. Turonian. B. Maastrichtian. Asterisked is locality Lower Agapa River under this study; arrows indicate the position of Turgai Channel; grey are lands, white are seas and oceans.

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Fig. 3 in Lower Turonian record of belemnite Praeactinocamax from NW Siberia and its palaeogeographic significance

Fig. 3. The alveolar fracture (alveolar end) reconstruction of Praeactinocamax aff. plenus with the position of phragmocone. A. Morphotype A, specimen MSU 3025−3/1 with low cone−shaped fracture, in ventral (A1) and lateral (A2) views. B. Morphotype B, specimen MSU 3025−3/2 with a very shallow pseudoalveolus with a pit in the centre, in ventral (B1) and lateral (B2) views.