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FIGURE 4 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 4. Mean relative abundance of planktic species preserved across the three units of the Walvis BayLüderitz cores.
FIGURE 3 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 3. Mean relative abundance, represented by column charts, of the major components within the complete sand fractions of core 1479.
FIGURE 2 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 2. Stratigraphy of the Conception and Meob Bay cores. The depositional ages and units are defined by Compton and Bergh (2016). Unit 6 = reworked foram layer; unit 5 = brown to olive-green mud unit; unit 4 = pelletal phosphorite sandy layer; unit 3 = slightly shelly layer; unit 2 = shelly sandy layer; unit 1 = shelly gravel layer (Compton and Bergh, 2016).
Plate 5 in A new record of larger benthic foraminifera from Jeju Island (South Korea)
Plate 5. Scanning electron microscope images of Sorites orbiculus (Forsskål in Niebuhr, 1775). A. peripheral, apertural view; B-G. closeup of apertural side. Scales = 100 μm; H-M. close-up of broken part, some diatoms (white arrowhead) are on the inner surface of chamberlet. Scales = 10 μm.
Fig. 2. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 2. a – age model and AMS radiocarbon ages for Cores FC WH and CADIAC WH; b – X-Ray photograph of Core CADIAC WH and grain-size parameters.
Fig. 3 in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 3. Benthic foraminiferal fauna characteristics of Core FC WH: a – densities of the main (> 5% in at least one sample) living benthic foraminifera (ind. 50 cm–3 of wet sediment); b – species richness of the living benthic fauna; c – densities of the main (> 5% in at least one sample) dead benthic foraminiferal species (ind. 50 cm–3 of wet sediment); d – species richness of the dead benthic fauna.
Fig. 11 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 11: 1-15 Abatomphalus sp.cf. A.intermedius, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12434; 16-21 Reugotruncana ellissi Brönnimann & Brown 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12426; 22-27 Gansseria gansseri (Bolli 1951), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12442 (All specimens x 90).
Fig. 1 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 1: 1-3 Rugoglobigerina subbotinae Maslakova 1978, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV. 12446; 4 Rugoglobigerina macrocephalla Brönnimann 1952, Maastrichtian, Tata Valley-Pietrositza, LPB.IV. 12413; 5-6 Rugoglobigerina rotundata Brönnimann, 1952, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12416; 7-15 Rugoglobigerina subbotinae Maslakova 1978, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12419; 16-27 Rugotruncana subrugosa (Gadolfi 1955), Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12420; 28-33 Globotruncanella subpetaloidea (Gandolfi 1955), Maastrichtian, Țâța Valley, LPB.IV. 12442; 34-36 Rugotruncana subcircumnodifer (Gandolfi 1955), Maastrichtian, Țâța Valley, LPB.IV. 12439 (All specimens x 90).
Fig. 8 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 8 Geographic distribution of occurrences of Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. 1: Organya, Pyrenees, Spain 2: Alpilles, Southern France 3: Provence, Southern France 4: Alpes occidentales and Jura, South- Eastern France and Switzerland 5: Northern Calcareous Alps, Austria 6: Pădurea Craiului, Apuseni Mountains, Romania 7: Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania 8: Vâlcan and Vânturariţa Mountains, Southern Carpathians, Romania 9: Dâmbovicioara zone, Southern Carpathians, Romania 10: Dobrogea, South-East Romania 11: Jerma River canyon, Eastern Serbia 12: Western Bulgaria.
Fig. 4 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 4: 1-9 Rugoglobigerina subbotinae Maslakova 1978, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12446; 10-15 Globotruncanella havanensis (Voorwjik 1937), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12429; 16-21 Globotruncanella pshadae (Keller 1946), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12427; 22-24, 31-36 Globotruncanella petaloidea (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12428; 25-30 Archaeoglobigerina blowi Pessagno 1967, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12449 (All specimens x 90).
Fig. 2 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 2 Schematic test reconstruction of Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. modified from Peybernès (2004, fig. 3, for Conicopfenderina? balkanica). Pseudo-kerioteka refers to the thin section 14731 Jerma river, Serbia (above), and RR4027 Kurilovo, Serbia (scale bar = 0.2 mm).
Fig. 17 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 17: Reproductions of different Globotruncanella taxa from the original papers. 1-6 Globigerina cretacea var. saratogensis Applin 1920 (modified from Applin, 1920); 7-9 Globotruncana havanensis Voorwjik 1937 (modified from Voorwjik, 1937); 10-15 Rugotruncana havanensis (Voorwjik 1937) emend. Brönnimann & Brown 1955, LPB.IV. 12429 (specimens x 90, Neagu Collection); 16-33 Globorotalia pshadae Keller 1946 (modified from Subbotina, 1953).
Fig. 6 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 6: 1-3 Rugoglobigerina ordinaria (Subbotina 1953), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12446; 4-6, 13-15 Rugotruncana subpennyi (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12426; 7-9 Rugotruncana subrugosa (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12420; 10-12 Rugoglobigerina beldingi Gandolfi 1955 Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12419; 16-21 Rugotruncana subloetterli (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12423; 22- 24 Rugoglobigerina kelleri (Subbotina 1953), Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12451 (All specimens x 90).
Fig. 13 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran
Fig. 13 Pseudcyclammina lituus Yokoyama (a–c) compared to Persiella pseudolituus n. gen., n. sp. (d–f). a, d Equatorial sections; b, e axial sections; c, f subaxial-tangential sections. From Hottinger (1967): a = pl. 10, fig. 11 (late Jurassic of Poland), b and c = pl. 10, fig. 12 and fig. 13 (topo-type from Tithonian-Berriasian Torinosu limestone, Japan).
Fig. 11 Persiella pseudolituus n. gen., n in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran
Fig. 11 Persiella pseudolituus n. gen., n. sp. from the upper Maastrichtian of the Tarbur Formation of the Naghan section, Zagros Zone, SW Iran. a-b, d, g-h, m Axial sections (partly slightly oblique); note initial streptospiral coiling in a. e–f Subaxial sections. i–j: Details from f and h showing pseudokeriotheka-like wall structure. k–l Oblique sections. Thinsections: 2NG 76 (a), 2NG 120-1 (b), 2NG 152 (c), 2NG 122 (d), 2NG 153 (e), 2NG 154 (f, i), 2NG 127 (g), 2 NG 186 (h, j), 2NG 152-1 (k–l), NG 3-1 (m).
Fig. 1 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 1 Location of the studied sections on the Romanian (A) and Serbian (B) territory showing the occurrence intervals (red lines) of Moulladella jourdanensis (Foury & Moullade) n. gen., nov. comb. A1 – location of the two studied sections in Romania; 1, Reşiţa-Moldova Nouă zone; 2, Dâmbovicioara zone, A2 – Succession of the Lower Cretaceous deposits from the Reşiţa- Moldova Nouă zone (modified from Bucur, 1997): 1, conglomerates and sandstones; 2, alternating sandstones and shales; 3, bedded bioclastic limestones; 4, massive bioclastic limestones; 5, chert-bearing limestones; 6, marly-limestones and marls; 7, micritic limestones; 8, micritic limestones with chert intercalations. A3 – Succession of the Lower Cretaceous deposits from Dâmbovicioara zone (modified from Bucur et al., 2011): 1, alternating marls and limestones; 2, marls with patch-reef limestone intercalations; 3, marly-limestones and marls; 4, glauconite-bearing limestones; 5, bedded limestones; CNM = Cetatea Neamţului Member. B1 – Location of the studied section in Serbia. JRA = Jerma River Area. B2 – Succession of the Lower Cretaceous deposits from the Jerma River Canyon (modified from Bucur et al., 1995): 1, conglomerates, sandstones and shales; 2, bedded limestones.
Fig. 6 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 6 Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. (a) Axial section of a megalospheric specimen. (b, f) Subaxial sections. (c–d, g, l) Oblique sections. (e, k, m–n, p) Slightly oblique transverse sections. (h, o) Tangential sections. (i–j) Tangential-oblique sections. Central zone highlighted in grey. b, beam; d,?deuteroconch; f, foramen; is, initial spire; p, proloculus; s, septum. Thin-sections: 14098-4 (a, c), 12568-4 (b), 12562-2 (d), 9-Mandrisag (e), 272-Ciclova (f), 4222- Ilidia (g), M10-Crivina (h), 14729 (i, l), 14734 (j–k), Lo 11 (m–n), 14733 (o). Location and age: (a-d) Dâmbovicioara area, Southern Carpathian, Romania (Early Valanginian); (e-h) Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania (Early Barremian); (i-l, o) Jerma River Canyon, Eastern Serbia (Early Valanginian); (m-n) Losenstein, Northern Calcareous Alps, Austria (Early Barremian, cobbles in Albian-Cenomanian conglomerates).
Fig. 12 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 12: 1-3 Gansserina gansseri (Bolli 1951), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12442; 4-6 Gansserina wiedenmayeri (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12431; 7-9 Rugotruncana subglaessneri (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12421; 10-16 Abatomphalus mayaroensis (Bolli 1951), Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12433; 17-19 Globotruncanella havanensis (VOORWJIK 1937) emend. Brönnimann & Brown 1955, Maastrichtian, Țâța Valley, PietroȘița, L.P.B. VI. 12429 (All specimens x 90).
Fig. 9 in Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera
Fig. 9: 1-6 Globotruncanella havanensis (Voorwjik 1937) emend. Brönnimann & Brown 1955, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12429; 7-9 Globotruncanella petaloidea (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12428; 10-12 Globotruncanella pshadae (Keller 1946), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12427; 13-21 Rugotruncana subpenny (Gandolfi, 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12426; 22-24 Rugotruncana subloetterli (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12423; 25-27 Rugotruncana subcircumnodifer (Gandolfi 1955), Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12439 (All specimens x 90).
Fig. 4 in Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran
Fig. 4 Vertical distribution of Persiella pseudolituus n. gen., n. sp. and some other larger benthic foraminifera in the Tarbur Formation of the Mandegan section.
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