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112 results for “Kerguelen”
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).
FIG. 4 in Terrestrial macro-arthropods of the sub-Antarctic islands of Possession (Crozet Archipelago) and Kerguelen: inventory of native and non-native species
FIG. 4. — Some indigeneous arthropod species: Diptera: A, Telmatogeton amphibius (Eaton, 1875); B, Amalopteryx maritima Eaton, 1875; Hymenoptera: C, Kleidotoma icarus (Quinlan, 1964); Coleoptera: D, Antarctotachinus crozetensis Enderlein, 1909; Hemiptera: E, Phthirocoris antarcticus Enderlein, 1904; Lepidoptera: F, Pringleophaga kerguelensis Enderlein, 1905. Photos: Bernard Chaubet.
FIG. 1 in Terrestrial macro-arthropods of the sub-Antarctic islands of Possession (Crozet Archipelago) and Kerguelen: inventory of native and non-native species
FIG. 1. — The South Indian Ocean sub-Antarctic islands, with details of Kerguelen Island (A) and Possession Island (B, in Crozet archipelago). Modified from D. Fourcy, Inrae, 2020.
FIG. 3 in Terrestrial macro-arthropods of the sub-Antarctic islands of Possession (Crozet Archipelago) and Kerguelen: inventory of native and non-native species
FIG. 3. — Some indigeneous arthropod species: Arachnida: A, Hahnia crozetensis Hickman, 1939; B, Myro paucispinosus Berland, 1947; Coleptera: C, Ectemnorhinus viridis G. R. Waterhouse, 1853; D, Palirhoeus eatoni (C. O. Waterhouse, 1876); E, Amblystogenium pacificum (Putzeys, 1869); F, Meropathus chuni Enderlein, 1901; Diptera: G, Calycopteryx moseleyi Eaton, 1875; H, Anatalanta aptera Eaton, 1875. Photos: Bernard Chaubet.
FIG. 2 in Terrestrial macro-arthropods of the sub-Antarctic islands of Possession (Crozet Archipelago) and Kerguelen: inventory of native and non-native species
FIG. 2. — Some typical habitats of sub-Antarctic islands: A, wide open valley; B, wet coastal cliffs; C, slopes covered with Acaena magellanica; D, fell field; E, native vegetation; F, introduced vegetation; G, coastal slopes and foreshore; H, marine animal colonies. Photos: Maurice Hullé.
FIG. 5 in The marine vegetation of the Kerguelen Islands: history of scientific campaigns, inventory of the flora and first analysis of its biogeographical affinities
FIG. 5. — Graph of the similarity network between regions (coloured nodes) based on the Kerguelen macroalgae (black nodes) co-occurrence dataset (using ForceAtlas2 layout algorithm). Colour codes are the same as in Figure 1. Nodes size is relative to the number of species co-occurring in the Kerguelen Islands. 51 species of doubtful taxonomic status were not considered. Sites: AMS, Amsterdam I.; SPA, Saint-Paul I.; MAR, Marion I.; PED, Prince Edwards Is.; CRO, Crozet Is.; HEA, Heard and McDonald Is.; MAQ, Macquarie I.; AUK, Auckland Is.; CAM, Campbell Is.; FUE, Fuegia; FAL, Falkland Is.; SGI, South Georgia Is.; SSI, South Shetland Is.; SOI, South Orkney Is.; APE, Antarctic Peninsula; END, Enderby L.; McR, MacRobertson L.; QMA, Queen Mary L.; WIL, Wilkes L.; ADE, Adelie L.; VIC, Victoria L.
FIG. 4 in The marine vegetation of the Kerguelen Islands: history of scientific campaigns, inventory of the flora and first analysis of its biogeographical affinities
FIG. 4. — Number of marine macroalgae species reported in the Kerguelen Islands since the Ross expedition (1840), in each phylum (Delépine 1996 is a personnal communication to J.-P. Féral).
FIG. 3. — A in The marine vegetation of the Kerguelen Islands: history of scientific campaigns, inventory of the flora and first analysis of its biogeographical affinities
FIG. 3. — A, Number of nominal species per family of marine macroalgae of the Kerguelen Islands; B, taxonomic status (accepted, uncertain, co-occurrence in the Northern Hemisphere) of the species for the three considered phyla (Chlorophyta, Ochrophyta-Phaeophycae and Rhodophyta).
FIG. 2 in The marine vegetation of the Kerguelen Islands: history of scientific campaigns, inventory of the flora and first analysis of its biogeographical affinities
FIG. 2. — Location of historical collections of macroalgae in the Kerguelen Islands. Precise locations are not given by all reports and should be partly inferred. The map shows the sites visited during 1, the Ross expedition (Hooker 1844-1847); 2, the Challenger expedition (Dickie 1876a, b, c, e); 3, the US (Farlow 1876); 4, English (Dickie 1876d, f); and 5, German (Askenasy 1889); 6, Venus transit expeditions, as well as the German south polar expedition (Foslie 1908, Reinbold 1908). 7, The Hopeful Bay (Zinova 1973) was added.
FIG. 1 in The marine vegetation of the Kerguelen Islands: history of scientific campaigns, inventory of the flora and first analysis of its biogeographical affinities
FIG. 1. — Sub-Antarctic and Antarctic regions considered in the biogeographical analysis of the Kerguelen Islands marine macroalgae also occurring elsewhere in the Southern Ocean. Colours: orange, temperate Southern Africa; blue, sub-Antarctic Islands; light blue, sub-Antarctic New Zealand; light green, Magellanic region; green, Scotia Sea; violet, continental High Antarctic (after Spalding et al. 2007). Geographical coordinates are given in the inset.
Catalog of seismicity for the Kerguelen Islands (1999-2020)
<p>This catalog of the seismicity of the Kerguelen Islands is related to the article: 'Recent seismicity on the Kerguelen Islands' by O. Lengliné, J. Rimpôt, A. Maggi and D. Zigone, Seismica, 2023.<br> </p>
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).
Southern Ocean kelp particle trajectories from Kerguelen, Macquarie Island and South Georgia
<p>Trajectory files from particle tracking simulations to model kelp drift pathways from three sub-Antarctic islands. More than 3.8 million virtual particles were released from a 2° latitude by 4° longitude box surrounding each of three sub-Antarctic source locations: Kerguelen Island, Macquarie Island and South Georgia. Particles were released daily throughout 2013 to sample seasonality and storm variability. Virtual particles were advected offline for three years from the time of release using the Connectivity Modelling System (Paris et al. 2013, <a href="https://github.com/beatrixparis/connectivity-modeling-system">https://github.com/beatrixparis/connectivity-modeling-system</a>). Particles were advected with the sum of daily snapshots of two-dimensional surface velocity data from an eddying ocean model (HYCOM; Bleck 2002) and wave-driven Stokes drift velocities from WAVEWATCH III (Rascle and Ardhuin 2013) over the period 2013-2016, as described in further detail in Fraser et al. 2018.</p> <p>Netcdf files contain particle trajectory latitude and longitude, and release date. Output has a temporal frequency of 1 day. Each release site has multiple zip files (e.g. Kerguelen_1.zip) which each contain multiple trajectory files. Each trajectory file contains a subset of the full ~ 4 million particles released at the site.</p> <p> </p> <p>Citation of associated paper: Fraser, C. I, Dutoit, L., Morrison, A. K., Miguel Pardo, L., Smith, S., Pearman, W., Parvizi, E., Waters, J., Macaya Horta, E. (2022). Southern Hemisphere coastal ecosystems are biologically connected by frequent, long-distance rafting events, submitted to <em>Current Biology</em>.</p> <p> </p> <p>References:</p> <p>Bleck, R. (2002). An oceanic general circulation model framed in hybrid isopycnic-Cartesian coordinates. <em>Ocean Modelling,</em> <strong>4</strong>, 55-88.</p> <p>Fraser, C. I. , A. K. Morrison, A. McC Hogg, E. C. Macaya, E. van Sebille, P. G. Ryan, A. Padovan, C. Jack, N. Valdivia, J. M. Waters (2018), Antarctica’s ecological isolation will be broken by storm-driven dispersal and warming, <em>Nat. Clim. Change</em>, <strong>8</strong>, 704-708.</p> <p>Paris, C. B., Helgers, J., van Sebille, E., & Srinivasan, A. (2013). Connectivity Modeling System: A probabilistic modeling tool for the multi-scale tracking of biotic and abiotic variability in the ocean. <em>Environmental Modelling and Software</em>, <strong>42</strong>, 47-54.</p> <p>Rascle, N., and Ardhuin, F. (2013). A global wave parameter database for geophysical applications. Part 2: Model validation with improved source term parameterization. <em>Ocean Modelling,</em> <strong>70</strong>, 174-188.</p>
Stress resistance as a component of dispersal syndromes in the non-native Merizodus soledadinus on Kerguelen islands
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FIGURES 11–16 in Studies on the Canacidae (Diptera), subfamily Apetaeninae. I. Apetaenus enderleini, nomen novum for Listriomastax litorea Enderlein, 1909, with remarks on the chaetotaxy, morphology, and habitats of the Apetaeninae from the Kerguelen Biogeographical Province
FIGURES 11–16. Specimens from the Crozet archipelago (figures 11–14). 11. Apetaenus enderleini, habitus of macropterous male; 12. Apetaenus litoralis, habitus of male; 13. Apetaenus enderleini, female abdomen showing the deep, median split on syntergite 1+2 (specimen photographed in alcohol); 14. Apetaenus litoralis, female abdomen dorsally; 15. Apetaenus litoralis, habitus of female; 16. ditto, head lateral view. (Figures 15–16, after Séguy, 1940, © Publications Scientifiques du MNHN, Paris).
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