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78 results for “BEAGLE”
Figure 9 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 9. Ventojassa beagle sp. nov. Holotype, ovigerous female: (A–C) peraeopods 5–7; (D) pleopod 1; (E) pleopod 1 locking spines; (F) epimera 1–3; (G) uropod 1. Scale bars: a: (A–D, F) 0.2 mm; b: (E) 0.025 mm; c: (G) 0.05 mm.
Figure 8 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 8. Ventojassa beagle sp. nov. Holotype, ovigerous female: (A) gnathopod 1; (B) gnathopod 1 propodus; (C) gnathopod 2; (D) gnathopod 2 propodus; (E, F) peraeopods 3, 4. Scale bars: a: (A, C, E, F) 0.2 mm; b: (B), c: (D) 0.1 mm.
Figure 15 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 15. Oradarea surera sp. nov. Holotype, ovigerous female: (A) peraeopod 7; (B) pleopod 3; (C) pleopod 3 locking spines; (D) peraeonite 7 and pleonites 1–3. Scale bars: a: (A), b: (B), d: (D) 0.2 mm; c: (C) 0.05 mm.
Figure 4 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 4. Aora parda sp. nov. Holotype, male: (A–C) uropods 1–3; (D) telson. Paratype, male 7 mm: (E, F) antennae 1, 2. Paratype, male 5.85 mm: (G) gnathopod 1; (H) gnathopod 1 dactylus. Scale bars: a: (A–C), c: (E–G) 0.2 mm; b: (D), d: (H) 0.05 mm.
Figure 2 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 2. Aora parda sp. nov. Holotype, male: (A) maxilliped; (B) gnathopod 1; (C, D) gnathopod 1 palm and dactylus; (E) gnathopod 2; (F) gnathopod 2 dactylus; (G, H) peraeopods 3, 4. Scale bars: a: (A) 0.1 mm; b: (B, E, G, H) 0.2 mm; c: (C, D, F) 0.05 mm.
Figure 14 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 14. Oradarea surera sp. nov. Holotype, ovigerous female: (A) gnathopod 2; (B) gnathopod 2 palm; (C–F) peraeopods 3–6. Scale bars: a: (A, C–F) 0.2 mm; b: (B) 0.1 mm.
Figure 20 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 20. Erikus lovrichi sp. nov. Holotype, ovigerous female: (A) pleopod 1; (B) pleopod 1 locking spines; (C) epimeron 3; (D–F) uropods 1–3; (G) uropod 3 article 2; (H) telson; (I) telson apex. Scale bars: a: (A, C) 0.5 mm; b: (B, G, I) 0.1 mm; c: (D, E, H), d: (F) 0.2 mm.
Figure 34 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 34. Heterophoxus despard sp. nov. Holotype, ovigerous female: (A–C) uropods 1–3; (D) telson. Paratype, ovigerous female 6.9 mm: (E) mandibular palp; (F) gnathopod 1. Scale bars: a: (A–E) 0.1 mm; b: (F) 0.2 mm.
Figure 31 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 31. Heterophoxus despard sp. nov. Holotype, ovigerous female: (A) lateral view; (B) head; (C, D) antennae 1, 2; (E) upper lip; (F, G) right and left mandibles; (H, I) maxillae 1, 2; (J) lower lip. Scale bars: a: (A) 1 mm; b: (B) 0.2 mm; c: (C, D), d: (E, H–J) 0.1 mm; e: (F, G) 0.025 mm.
Figure 27 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 27. Lysianopsis ona sp. nov. Holotype, ovigerous female: (A) lateral view; (B) head; (C, D) antennae 1, 2; (E) epistome and upper lip; (F, G) right and left mandibles; (H) mandibular palp. Scale bars: a: (A) 1 mm; b: (B) 0.2 mm; c: (C–E), d: (F–H) 0.1 mm.
Figure 12 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 12. Oradarea surera sp. nov. Holotype, ovigerous female: (A) lateral view; (B) head; (C, D) antennae 1, 2; (E) upper lip and epistome; (F, G) right and left mandibles; (H) left lacinia mobilis. Scale bars: a: (A) 3 mm; b: (B), c: (C, D) 0.2 mm; d: (E), e: (F, G) 0.1 mm; f: (H) 0.025 mm.
Figure 30 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 30. Lysianopsis ona sp. nov. Holotype, ovigerous female: (A) epimeron 3; (B–D) uropods 1–3; (E) telson. Paratype, ovigerous female 5.8 mm: (F) maxilla 1. Paratype, male 5.3 mm: (G) gnathopod 1 propodus. Scale bars: a: (A) 0.2 mm; b: (B–G) 0.1 mm.
Figure 11 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 11. Ventojassa beagle sp. nov. Paratype, male 3.95 mm: (A) gnathopod 2; (B) gnathopod 2 palm; (C) uropod 3; (D) uropod 3 outer ramus. Scale bars: a: (A) 0.2 mm; b: (B, C) 0.05 mm; c: (D) 0.025 mm.
Figure 29 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 29. Lysianopsis ona sp. nov. Holotype, ovigerous female: (A–E) peraeopods 3–7. Scale bar: 0.2 mm.
Figure 3 in Amphipod crustaceans (Corophiidea and Gammaridea) associated with holdfasts of Macrocystis pyrifera from the Beagle Channel (Argentina) and additional records from the Southwestern Atlantic
Figure 3. Aora parda sp. nov. Holotype, male: (A–C) peraeopods 5–7; (D) pleopod 1; (E) pleopod 1 locking spines; (F, G) epimera 2, 3. Scale bars: a: (A), b: (B), c: (C), d: (D, F, G) 0.2 mm; e: (E) 0.025 mm.
Data from: Identification of the Beagle 2 lander on Mars
Open the record for dataset details and reuse information.
Beagle kelp maps from: One of the least disturbed marine coastal ecosystems on Earth: Spatial and temporal persistence of Darwin's sub-Antarctic giant kelp forests
<p>Aim: Marine habitats and their dynamics are difficult to systematically monitor, particularly those in remote locations. This is the case with the sub-Antarctic ecosystem of the giant kelp <i>Macrocystis pyrifera</i>, which was already noted by Charles Darwin in his accounts on the <i>Voyage of the Beagle</i> and recorded on the nautical charts made during that expedition. We combined these and other nautical charts from the 19th and early 20th centuries with surveys conducted in the 1970s and 1980s and satellite detection algorithms from 1984 to 2019, to analyse kelp distribution through time and the factors that correlate with it.</p> <p>Location: Marine ecoregions of Channels and Fjords of Southern Chile, Falkland Islands (Malvinas), and the island of South Georgia.</p> <p>Taxon: <i>Macrocystis pyrifera</i>.</p> <p>Methods: We characterised 309 giant kelp forests by their coastal geospatial attributes. Statistically significant variables were included in a conditional inference tree to predict kelp forest size. Sea surface temperature (SST) records were analysed to confirm temperature ranges over the last four decades. Nautical charts, historical surveys, aerial photogrammetry, unmanned aerial vehicle (UAV) surveys and satellite imagery were overlaid to assess spatial distribution of kelp forest canopies, spanning the period 1829–2020.</p> <p>Results: Considering the extensive natural and human caused changes over the last two centuries, this diverse kelp ecosystem is remarkably persistent. We found that the ocean currents and wave exposure, combined with the geomorphological settings of the coastline are the most critical factors predicting the extent of the kelp forests.</p> <p>Main conclusions: We have described the long-term ecological persistence of the kelp forests in this vastly under-studied region that offers a conceptual biogeographical model supporting the global importance proposed by Charles Darwin 200 years ago (Darwin, 1845). In the current context of global change, the need for conservation of this persistent and well-preserved marine ecosystem has never been more important.</p>
Salinity, temperature and PAR data collected at Inner Bahía Brown, Beagle Channel, Argentina
<p>This is a series of environmental data collected at fixed moorings in Brown Bay in the Begale Channel, Tierra del Fuego, Argentina. The moorings were placed in 2021 and left in place for two years. Continuous data, collected at 3 or 4 depths (sub-surface, 6, 11 and 16 meters).</p>
Figure 10 from: Chatzimanolis S (2014) Darwin's legacy to rove beetles (Coleoptera, Staphylinidae): A new genus and a new species, including materials collected on the Beagle's voyage. ZooKeys 379: 29-41. https://doi.org/10.3897/zookeys.379.6624
Figure 10 - Original BMNH labels for the holotype of Darwinilus sedarisi Chatzimanolis, sp. n. Image Copyright Natural History Museum (London).
Figures 6-7 from: Chatzimanolis S (2014) Darwin's legacy to rove beetles (Coleoptera, Staphylinidae): A new genus and a new species, including materials collected on the Beagle's voyage. ZooKeys 379: 29-41. https://doi.org/10.3897/zookeys.379.6624
Figures 6-7 - Abdomen of the holotype of Darwinilus sedarisi Chatzimanolis, sp. n. 6 Dorsal view 7 Ventral view. Scale = 3 mm Image Copyright Natural History Museum (London).
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