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206 results for “sub-Antarctic”

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zenodo48/100

Raw multibeam bathymetry data collected around the sub-Antarctic Prince Edward Islands on board the R/V Akademik Tryoshnikov during the austral summer of 2016/2017 as part of the Antarctic Circumnavigation Expedition (ACE).

<p><strong>Dataset abstract</strong></p> <p>An ELAC Nautik 3020 multibeam echo sounder with a 20 kHz transducer mounted on the hull of the R/V Akademik Tryoshnikov, was used to collect multibeam bathymetry data during the Antarctic Circumnavigation Expedition (ACE). This particular dataset was collected around the sub-Antarctic Prince Edward Islands in the austral summer of 2016/2017.</p> <p>Bathymetry data were used live during the cruise to look for suitable locations where benthic trawling and remotely-operated vehicle deployments could take place, rather than to undertake specific bathymetric surveys.</p> <p>This raw dataset is provided without calibration information for the surface sound velocity or instrumentation itself and should be used with due caution.</p> <p><strong>Dataset contents</strong></p> <ul> <li>lineYYYYDDmonHHMMSS.xse, data file, proprietary format</li> <li>*.txt, ancillary file, ASCII</li> <li>location.hydrostar, ancillary file, ASCII</li> <li>data_file_header.txt, metadata, text</li> <li>README.txt, metadata, text</li> </ul> <p><strong>Dataset license</strong></p> <p>This raw multibeam bathymetry dataset is made available under the Creative Commons Attribution 4.0 International License (CC BY 4.0) whose full text can be found at https://creativecommons.org/licenses/by/4.0/</p>

opencc-by-4.0Oct 2019View details →
zenodo44/100

Diverse baleen whale acoustic occurrence around two sub-Antarctic Islands: A tale of residents and visitors

<p>This dataset contains the acoustic .wav file of all exemplar calls illustrated by the spectrograms in the manuscript figure, MS Excel Spreadsheet file with baleen whale call occurrence and environmental data, and the R code used for fitting the RF models. R codes must be run in the following manner:</p> <p>1. 01_tune_occ_enviro_rf_model_balance_baleen_whales</p> <p>2. 02_process_occ_enviro_rf_model_balance_baleen_whales</p> <p>The codes are self-explanatory given the comments contained therein, and the source code for fitting the codes is provided as 000_source_all.</p>

opencc-by-4.0Mar 2024View details →
zenodo40/100

Figs 44–66 in Revision of the non-marine centric diatom flora (Bacillariophyta) of the sub-Antarctic Campbell Island (southern Pacific Ocean) with the descriptions of five new species

Figs 44–66. Ferocia houkiana Goeyers &amp; Van de Vijver sp. nov. LM and SEM. Campbell Island holotype population, sample BAS284 (BR-4578). LM. 44–49. Several frustules in girdle view, often connected to each other. 50–51. Internal valves. 52–62. Several valves in valve face view clearly showing the central ring of spines. SEM. 63. Frustule in girdle view with the narrow copulae. 64. Frustule in girdle view with the narrow copulae on one side and one the side showing the broad mantle with one indicated rimoportula. 65. External view of a valve face and the girdle. Note the central ring of partly hollow spines. 66. External view of two valves connected via their linking spines. The arrow indicates the Müller step. Scale bars = 10 μm.

opencc-by-4.0Jul 2020View details →
zenodo40/100

Figs 20–27 in Revision of the non-marine centric diatom flora (Bacillariophyta) of the sub-Antarctic Campbell Island (southern Pacific Ocean) with the descriptions of five new species

Figs 20–27. Angusticopula chilensis (Grunow) Houk et al. SEM. Campbell Island epitype population, sample BAS286. 20–22. SEM view of several valves in girdle view showing the ligulate, open, narrow girdle bands. The arrows indicate the ligulae in Fig. 20, the rimmed mantle edge in Fig. 21 and the fimbriate pars interior of the copulae in Fig. 22. 23. External view of a valve face. 24. External detail of the very fine striae and the small, rounded areolae. 25. Internal view of an entire valve showing the rimoportulae and the thick mantle. 26. External view of the mantle/valve face junction with several openings of the rimoportulae (arrows). 27. Internal detail of the valve mantle with some rimoportulae. Scale bars: 20–23, 25–26 = 10 μm; 24, 27 = 1 μm.

opencc-by-4.0Jul 2020View details →
zenodo40/100

Figs 28–36 in Revision of the non-marine centric diatom flora (Bacillariophyta) of the sub-Antarctic Campbell Island (southern Pacific Ocean) with the descriptions of five new species

Figs 28–36. Angusticopula cosmica Goeyers &amp; Van de Vijver sp. nov. LM. Campbell Island holotype population, sample BAS303 (BR-4577). 28. Frustule in girdle view showing the discoid chloroplasts. 29. Frustule in valve face view showing the discoid chloroplasts. 30–36. Several valves in valve face view showing clearly the submarginal ring of rimoportulae (arrows) and the striated valve face margin. Scale bar = 10 μm.

opencc-by-4.0Jul 2020View details →
zenodo40/100

Figs 1–19 in Revision of the non-marine centric diatom flora (Bacillariophyta) of the sub-Antarctic Campbell Island (southern Pacific Ocean) with the descriptions of five new species

Figs 1–19. Angusticopula chilensis (Grunow) Houk et al. LM. Campbell Island epitype population, sample BAS286. 1–6, 12–13. Several frustules in girdle view. 5, 12. Internal valves. 7–11, 14–19. Several valves in valve face view clearly showing the marginal rimoportulae. Scale bar = 10 μm.

opencc-by-4.0Jul 2020View details →
zenodo40/100

Data used in "The Complex Role of Storms in Modulating Air-Sea CO2 Fluxes in the sub-Antarctic Southern Ocean"

<p>The data included in this repository were used to generate the figures for the paper "The Complex Role of Storms in Modulating Air-Sea CO2 Fluxes in the sub-Antarctic Southern Ocean" in Geophysical Research Letter.</p> <p>Abstract:</p> <p>"The intra-seasonal CO<sub>2</sub> flux (FCO<sub>2</sub>) variability across the Southern Ocean is poorly understood due to sparse observations at the required temporal and spatial scales. Twinned Waveglider-Seaglider experiments were used to investigate how storms influence FCO<sub>2</sub> through both the gas transfer velocity (k<sub>w</sub>) and the air-sea gradient in partial pressure of CO<sub>2</sub> (&Delta;pCO<sub>2</sub>) in the sub-Antarctic zone. Winter-spring storms caused &Delta;pCO<sub>2</sub> to weaken (by 15-55 &mu;atm) due to mixing/entrainment and weaker stratification. This response in &Delta;pCO<sub>2</sub> was in phase with k<sub>w</sub> resulting in a counteractive weakening in FCO<sub>2</sub> (by 6.6 - 26.5% per storm), despite the wind-driven increase in k<sub>w</sub>. Stronger stratification during summer explained the weaker sensitivity of &Delta;pCO<sub>2</sub> to storms, instead its thermal drivers dominated the &Delta;pCO<sub>2 </sub>variability. These results highlight the importance of observing synoptic-scale variability in &Delta;pCO<sub>2</sub>, the absence of which may propagate significant biases to the mean annual FCO<sub>2</sub> estimates from large-scale observing programmes and reconstructions."</p> <p>The data collected from the Wave Glider, such as the concentration of CO<sub>2</sub> in the atmosphere (xCO<sub>2air</sub>) and in the ocean (xCO<sub>2sea</sub>), surface temperature and salinity were used to calculate the different parameters of the bulk CO<sub>2</sub> flux formula (FCO<sub>2</sub> = k<sub>w</sub> x ko x &Delta;pCO<sub>2</sub>). Note that the meteorological weather station of one of the Wave Gliders was faulty and the wind speed, wind direction and wind stress data was replaced by hourly ERA5 data provided by ECMWF available at&nbsp;<a href="https://doi.org/10.24381/cds.bd0915c6">https://doi.org/10.24381/cds.bd0915c6</a>.&nbsp;</p> <p>The temperature, pressure and salinity data collected by the Seaglider were used to calculate the Mixed Layer Depth and the Brunt Vaisala Frequency of the first 300m of the ocean.</p>

opencc-by-4.0Dec 2023View details →
zenodo40/100

Fig. 4 in Africanacetus from the sub-Antarctic region: The southernmost record of fossil beaked whales

Fig. 4. The beaked whale Africanacetus sp., skull (YugNIRO 409) in posterior view. A. Photograph. B. Explanatory drawing.

opencc-by-4.0Dec 2011View details →
zenodo40/100

Fig. 6 in Africanacetus from the sub-Antarctic region: The southernmost record of fossil beaked whales

Fig. 6. Geographical range of the beaked whale Africanacetus. 1, type area; 2, Banzare Bank (from where the present material was recovered).

opencc-by-4.0Dec 2011View details →
zenodo40/100

Fig. 2 in Africanacetus from the sub-Antarctic region: The southernmost record of fossil beaked whales

Fig. 2. The beaked whale Africanacetus sp., skull (YugNIRO 409) in ventral view. A. Photograph. B. Explanatory drawing.

opencc-by-4.0Dec 2011View details →
zenodo40/100

Fig. 1 in Africanacetus from the sub-Antarctic region: The southernmost record of fossil beaked whales

Fig. 1. The beaked whale Africanacetus sp., skull in dorsal view. A. YugNIRO 409, photograph (A1) and explanatory drawing (A2). B. YugNIRO 408.

opencc-by-4.0Dec 2011View details →
zenodo40/100

Fig. 5 in Africanacetus from the sub-Antarctic region: The southernmost record of fossil beaked whales

Fig. 5. The beaked whale Africanacetus sp. (YugNIRO 408), narial region of the skull in ventral view.

opencc-by-4.0Dec 2011View details →
zenodo40/100

Linked collectors and determiners for: Records of Parochlus steinenii in the Maritime Antarctic and sub-Antarctic regions.

Natural history specimen data linked to collectors and determiners held within, "Records of Parochlus steinenii in the Maritime Antarctic and sub-Antarctic regions". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/30c49fbf-4e2e-482e-bb49-4d294bc332cb">https://bionomia.net/dataset/30c49fbf-4e2e-482e-bb49-4d294bc332cb</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/30c49fbf-4e2e-482e-bb49-4d294bc332cb">https://gbif.org/dataset/30c49fbf-4e2e-482e-bb49-4d294bc332cb</a>. Formatted as a Frictionless Data package.

opencc-zeroJan 2024View details →
zenodo40/100

Figure 1 in Distribution of microarthropods across altitude and aspect in the sub-Antarctic: climate change implications for an isolated oceanic island

Figure 1 Interaction plots of mite and springtail species richness (S) and abundance (N) at low, middle and high altitudes on the eastern and western aspect of Marion Island (weighted means ± 95 % confidence intervals). Groups not sharing letters differ significantly (p &lt;0.05). Model results provided in Table 2 and Appendix 2.

opencc-by-4.0Sep 2018View details →
zenodo40/100

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.

opencc-zeroSep 2021View details →
zenodo40/100

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.

opencc-zeroSep 2021View details →
zenodo40/100

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.

opencc-zeroSep 2021View details →
zenodo40/100

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.

opencc-zeroSep 2021View details →
zenodo40/100

FIG. 4 in Populations of a new morphotype of corrugate Lessonia Bory in the Beagle Channel, sub-Antarctic Magellanic ecoregion: a possible case of on-going speciation

FIG. 4. — Phylogenetic tree based on concatenated ITS1 and atp8-trnS partial sequences (418 bp). Note that corrugated Lessonia Bory specimens are grouped with Lessonia flavicans Bory specimens which have smooth blade surface. First number on the branches refers to the bootstrap value determined from the ML phylogeny and the second is the posterior probability from the BI analysis. Scale bar: 0.05 substitution per site.

opencc-zeroOct 2020View details →
zenodo40/100

FIG. 5 in Populations of a new morphotype of corrugate Lessonia Bory in the Beagle Channel, sub-Antarctic Magellanic ecoregion: a possible case of on-going speciation

FIG. 5. — Phylogenetic tree based on concatenated cox1 and cox3 partial sequences (1176 bp). Note that corrugated Lessonia Bory specimens are grouped with Lessonia flavicans Bory specimens which have smooth blade surface. First number on the branches refers to the bootstrap value determined from the ML phylogeny and the second is the posterior probability from the BI analysis. Scale bar: 0.01 substitution per site.

opencc-zeroOct 2020View details →

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