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35 results for “Kerguelen Plateau”
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.
Fig. 3 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)
Fig. 3. Large fraction (>150 µm) Globorotalia percentages in ODP Hole 747A between 15.0 and 12.2 Ma together with coiling ratios and percentages of encrusted individuals. Note 95% confidence intervals marked on the coiling ratio plots. Descriptions with arrows show stratigraphic position of foraminiferal specimens shown on Figs. 4 and 5. Note δ18O data and the five isotopic intervals (A–E) after Majewski and Bohaty (2010).
Fig. 11 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)
Fig. 11. Comparison of test−size variations in Globigerina bulloides at ODP 747A and sea surface temperature (SST) at ODP Site 1171 (Shevenell et al. 2004) between 15.0 and 12.2 Ma.
Fig. 8. Planktonic foraminifers from ODP Site 747, Kerguelen Plateau. A–F in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)
Fig. 8. Planktonic foraminifers from ODP Site 747, Kerguelen Plateau. A–F. Globoturborotalita woodi: 7H−5, 68–70 cm (A); 7H−5, 98–100 cm (B); 8H−1, 97.5–99.5 cm (C); 8H−4, 18–20 cm (D); 8H−6, 28–30 cm (E); 9H−2, 28–30 cm (F). G–O. Neogloboquadrina continuosa. G–J. Non−kummeform: 7H−5, 8–10 cm (G); 8H−1, 38–40 cm (H); 8H−2, 68–70 cm (I); 8H−4, 18–20 cm (J). K–O. Kummeform: 7H−5, 8–10 cm (K); 8H−1, 38–40 cm (L, M); 8H−3, 100–102 cm (N); 9H−4, 28–30 cm (O). P–T. Turborotalita quinqueloba: 7H−5, 8–10 cm (P); 7H−7, 8–10 cm (Q); 8H−5, 58–60 cm (R, S); 9H−2, 118–120 cm (T). All SEM images. Scale bars 100 µm. The stratigraphic position of pictured specimens is indicated on Fig. 7.
Fig. 9 in Planktonic foraminiferal response to Middle Miocene cooling in the Southern Ocean (ODP Site 747, Kerguelen Plateau)
Fig. 9. Microperforate planktonic foraminifera and small fraction (63–150 µm) juvenile Globorotalia percentages in ODP Hole 747 between 15.0 and 12.2 Ma. Descriptions with arrows show stratigraphic position of foraminiferal specimens shown on Fig. 10. Note δ18O data and the five isotopic Intervals (A–E) after Majewski and Bohaty (2010).
Figure 6 in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 6. – Length Frequency Distributions (LFD) of Muraenolepis marmorata fingerlings during early (January 2014, MYCTO 3 D) or late summer (March 1995, IPEKER) pelagic surveys. Photo: Muraenolepis marmorata, fingerling TL 35 mm (photo ©MYCTO 3D).
Figure 5 in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 5. – Depth range occurrence of Muraenolepis marmorata by-catch in the total bottom longlines deployed in the fishery (2006-2016) off the Kerguelen Islands (500-2000 m).
Figure 2 in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 2. – Geographical pelagic survey coverage off the Kerguelen Islands during the "IPEKER" (1995), "ICHTYOKER 1, 2 & 3" (1998-2000) and "MYCTO 3 D" (2014) cruises. Each station includes four depths hauls (subsurface, 50, 150, 300 m). Yellow circles are day stations, deep blue diamond- shaped are night stations.
Figure 4 in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 4. – Length Frequency Distributions (LFD) of Muraenolepis marmorata from POKER 1 (2006), POKER 2 (2010) Kerguelen Islands fish bottom biomass surveys and by-catch in the bottom longline fishery (2006-2016) off the Kerguelen Islands. Photo: Muraenolepis marmorata (photo ©POKER 2).
Figure 2 from: Guillaumot C, Martin A, Fabri-Ruiz S, Eléaume M, Saucède T (2016) Echinoids of the Kerguelen Plateau – occurrence data and environmental setting for past, present, and future species distribution modelling. ZooKeys 630: 1-17. https://doi.org/10.3897/zookeys.630.9856
Figure 2 - Distribution of the 12 echinoid species based on the specimens collected since 1872 on the Kerguelen Plateau.
Figure 1 from: Guillaumot C, Martin A, Fabri-Ruiz S, Eléaume M, Saucède T (2016) Echinoids of the Kerguelen Plateau – occurrence data and environmental setting for past, present, and future species distribution modelling. ZooKeys 630: 1-17. https://doi.org/10.3897/zookeys.630.9856
Figure 1 - Sampling effort. Red dots depict echinoid occurrences. Black squares correspond to visited sites at which no echinoid was sampled.
Figure 1. – Geographical coverage. A in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 1. – Geographical coverage. A: Bottom trawl stations conducted during the "POKER" 1 (2006 in white), POKER 2 (2010 in grey), and POKER 3 (2013 in black) surveys off the Kerguelen Islands; B: Bottom commercial longlines conducted from 2006 to 2016 off the Kerguelen Islands (source: PECHEKER database). Continuous line shows the boundary of the 200 Nautical Mille French Exclusive Eco- nomic Zone.
Figure 3 in The benthic and pelagic phases of Muraenolepis marmorata (Muraenolepididae) off the Kerguelen Plateau (Indian sector of the Southern Ocean)
Figure 3. – Densities (n/set) of Muraenolepis marmorata during the POKER surveys: POKER 1 2006 (top); POKER 2 2010 (bottom).
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