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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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Figure 3 in Tintinnina (Ciliophora) and Foraminifera in plankton of hypersaline Lagoon Bardawil (Egypt): spatial and temporal variability

Figure 3. Dependence of number of found tintinnid species on number of analyzed samples in Lagoon Bardawil (a) and the Mediterranean Sea (b).

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Figure 2 in Tintinnina (Ciliophora) and Foraminifera in plankton of hypersaline Lagoon Bardawil (Egypt): spatial and temporal variability

Figure 2. Dependence of total tintinnid abundance on number of tintinnid species in Lagoon Bardawil during 2009 and 2010 (a- winter, b- all seasons).

Figure 6 in Comparison of microplankton heterotrophic-photoautotrophic balance based on the content of ATP and chlorophyll a in the plankton of the northern area of the Black Sea during the autumn and spring seasons

Figure 6. Distribution of microplankton HPI in the photic zone of the Crimean coastal waters and deep-water northern part of the Black Sea at April 2017.

Figure 4 in Comparison of microplankton heterotrophic-photoautotrophic balance based on the content of ATP and chlorophyll a in the plankton of the northern area of the Black Sea during the autumn and spring seasons

Figure 4. Distribution of microplankton HPI in the photic zone of the Crimean coastal waters and deep-water northern part of the Black Sea at October 2016.

Figure 3 in Comparison of microplankton heterotrophic-photoautotrophic balance based on the content of ATP and chlorophyll a in the plankton of the northern area of the Black Sea during the autumn and spring seasons

Figure 3. Distribution of microplankton HPI in the surface waters of the Crimean coastal waters and deep-water northern part of the Black Sea at October 2016.

Figure 1 in Comparison of microplankton heterotrophic-photoautotrophic balance based on the content of ATP and chlorophyll a in the plankton of the northern area of the Black Sea during the autumn and spring seasons

Figure 1. Distribution of microplankton chlorophyll a and ATP concentrations in the Crimean coastal waters and deepwaternorthern part of the Black Sea at October 2016.

Fig. 7 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 7. Percentages of some planktonic foraminifera in ODP Hole 747A between 15.0 and 12.2 Ma. Descriptions with arrows show the stratigraphic position of foraminiferal specimens shown on Fig. 8. Note δ18O data and the five isotopic intervals (A–E) after Majewski and Bohaty (2010).

Fig. 10. Middle Miocen microperforate planktonic foraminifera from ODP Site 747, Kerguelen Plateau. A–D in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 10. Middle Miocen microperforate planktonic foraminifera from ODP Site 747, Kerguelen Plateau. A–D. Globigerinita juvenilis: 7H−6, 38–40 cm (A); 8H−3, 40–42 cm (B); 9H−1, 4–6 cm (C); 9H−2, 118–120 cm (D). E, F. Globigerinita uvula: 7H−6, 98–100 cm (E); 9H−3, 118–120 cm (F). G–I. Globigerinita glutinata s.l.: 7H−7, 8–10 cm (G); 8H−4, 48–50 cm (H); 9H−4, 148–150 cm (I). J–S. Low trochospiral Tenuitella–Tenuitellinata: 7H−5, 8–10 cm (J); 7H−5, 68–70 cm (K); 8H−3, 100–102 cm (L, M); 9H−4, 118–120 cm (N, O); including Tenuitella jamesi: 8H−2, 68–70 cm (P); 8H−2, 128–130 cm (Q); 9H−2, 118–120 cm (R); 9H−4, 118–120 cm (S). All SEM images. Scale bars 50 µm. The stratigraphic position of pictured specimens is indicated on Fig. 9.

Fig. 5. Middle Miocene planktonic foraminifer Globorotalia preascitula plexus from ODP Site 747, Kerguelen Plateau. A–D in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 5. Middle Miocene planktonic foraminifer Globorotalia preascitula plexus from ODP Site 747, Kerguelen Plateau. A–D. Globorotalia praescitula: 7H−5, 8–10 cm (A); 7H−6, 98–100 cm (B); 8H−6, 88–90 cm (C); 9H−3, 148–150 cm (D). E–H. Globorotalia miozea: 8H−3, 40–42 cm (E); 8H−5 118–120 cm (F); 9H−3, 28–30 cm (G); 9H−4, 58–60 cm (H). I–L. Globorotalia sp.: 7H−5, 128–130 cm (I); 7H−6, 30–40 cm (J); 8H−3, 10–12 cm (K); 8H−6, 88–90 cm (L). In axial (A1–L1) and umbilical (A2–L2) views. All SEM images. Scale bars 100 µm. Stratigraphic position of pictures specimens is indicated on Fig. 3.

Fig. 4. Middle Miocene planktonic foraminifer Globorotalia zealandica plexus from ODP Site 747, Kerguelen Plateau. A–D in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 4. Middle Miocene planktonic foraminifer Globorotalia zealandica plexus from ODP Site 747, Kerguelen Plateau. A–D. Globorotalia amuria. Encrusted: 8H−1, 38–40 cm (A); 8H−6, 28–30 cm (C); 9H−3, 98–100 cm (D). Non−encrusted: 8H−3, 100–102 cm (B). E–H. Globorotalia cf. conica. Non−pustulose: 8H−2, 128–130 cm (E); 8H−6, 146.5–148.5 cm (F). Pustulose: 9H−1, 4–6 cm (G); 9H−4, 148–150 cm (H). A1–H1 axial view, A2–H2 umbilical view. All SEM images. Scale bars 100 µm. The stratigraphic position of pictured specimens is indicated on Fig. 3.

Fig. 2 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 2. Major foraminiferal and paleoenvironmental events at ODP Site 747A (15.0–12.2 Ma) discussed in this paper, related to age after Majewski and Bohaty (2010). Oxygen Mi3, Mi4 and carbon CM4, CM5, CM6 stable isotopic events as well as Middle Miocene 18O shift (MMS) are indicated on the stable isotopic plots. Dashed lines show limits of the five isotopic intervals (A–E) from Majewski and Bohaty (2010). The paleotemperature records from Shevenell et al. (2004) and Verducci et al. (2007).

Fig. 1 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 1. Location of ODP Sites 747, 744, and 1171 on a paleogeographic reconstruction for 15 Ma modified from Lawver et al. (1992).

Fig. 6 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)

Fig. 6. Planktonic foraminifers Globigerina bulloides and Globoturborotalita sp. percentages in ODP Hole 747A between 15.0 and 12.2 Ma. Note δ18O data and the five isotopic Intervals (A–E) after Majewski and Bohaty (2010). SEM foraminiferal images. A–D. G. bulloides: 7H−5, 128–130 cm (A); 8H−2, 68–70 cm (B); 8H−4, 48–50 cm (C); 9H−4, 58–60 cm (D). E–G. Globoturborotalita sp.: 8H−4, 136.5–138.5 cm (E); 9H−1, 4–6 cm (F); 9H−4, 118–120 cm (G). E1 umbilical view, E2 spiral view. Scale bars 100 µm.