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FIGURE 4 in Depth related brachiopod faunas from the lower Cambrian Forteau Formation of southern Labrador and western Newfoundland, Canada

FIGURE 4. Geology map of central part of the Great Northern Peninsula showing faunally productive localities studied at Mount St. Margaret, along Route 432 north of the Long Range Proterozoic massif, and along the Big East River resource road at the south end of Highlands of St. John. MSM - Mount St. Margaret, ECP - East Castor Pond road, R432-5 etc - Route 432; BER-5 etc - Big East River resource road.

FIGURE 3 in Depth related brachiopod faunas from the lower Cambrian Forteau Formation of southern Labrador and western Newfoundland, Canada

FIGURE 3. Sections measured in the Forteau Formation of south Labrador coast. FC1 (open shelf facies of James and Kobluk, 1978) and FC2a (Patch reef facies of James and Kobluk, 1978; bioherm of Debrenne and James, 1981) are adjacent to each other on the foreshore east of Fox Cove; FC2 is divided into a lower (FC2a) and upper part (FC2b) separated by a vertical fault that cuts out most of the Middle shale; FC3 is measured to the southwest of FC2 and is a composite of three short sections that are correlated over more than 50 m on the base of the Upper limestone (upper biostrome of Debrenne and James, 1981). Legend is applicable to all stratigraphic figures (Figures 5-6, 8-9).

FIGURE 7 in Depth related brachiopod faunas from the lower Cambrian Forteau Formation of southern Labrador and western Newfoundland, Canada

FIGURE 7. Geology map of the Gros Morne area showing location of sections in the Forteau Formation (based on Knight, 2013, figure 3). Samples GM07 -1 etc. were collected randomly in 2007 and are linked to localities GM11-1 etc. that were mapped, sectioned, and sampled in 2011 (see Figures 8-9).

FIGURE 10 in Depth related brachiopod faunas from the lower Cambrian Forteau Formation of southern Labrador and western Newfoundland, Canada

FIGURE 10. Distribution of brachiopod taxa recovered from sections measured in the Forteau Formation of the south Labrador coast. Shaded area indicates known stratigraphic range of individual taxa. Correlation of adjacent sections is approximate only. For more exact correlation of sections and samples see Figure 3.

opencc-by-4.0Dec 2016View details →

Figure 2 in Duvalius bozidari, a new cave-dwelling species of trechine ground beetles (Coleoptera: Carabidae: Trechinae) from western Serbia

Figure 2. The distribution of Duvalius (Neoduvalius) bozidari sp. n. (black circles) and D. (N.) guidononveilleri Janák & Moravec, 2008 (black star) in Serbia.

opencc-by-4.0Dec 2016View details →

Figure 1 in Duvalius bozidari, a new cave-dwelling species of trechine ground beetles (Coleoptera: Carabidae: Trechinae) from western Serbia

Figure 1. Duvalius (Neoduvalius) bozidari sp. n. from the Jovanjska Pećina Cave, village of Jovanje, near Valjevo, western Serbia: a - holotype male, habitus (dorsal view); b - holotype male, aedeagus (lateral view); c - holotype male, aedeagus (dorsal view); d - holotype male, abdominal sternite IX (urite); e - paratype female, genitalia. Scales = 2.00 mm (a) and 0.20 mm (b–e).

opencc-by-nc-4.0Nov 2023View details →

D-PLACE dataset derived from Jorgensen 1980 'Western Indians'

Cite the source of the dataset as: <blockquote> Jorgensen, JG. 1980. Western Indians: Comparative Environments, Languages, and Cultures of 172 Western American Indian Tribes. San Francisco: W.H. Freeman and Company. </blockquote>

FIGURE 3 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 3 | Lower mesophotic (below 90 m depth) ecosystems explored through technical rebreather diving around the Fernando de Noronha Archipelago. A. The insular shelf edge; and B. The steep wall.

FIGURE 7 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 7 | Evidence of human impacts (arrows) by fishing debris, plastics and other trash found in the ecosystems explored around the Fernando de Noronha Archipelago. A. and B. Mesophotic (> 30 m deep); C. Intertidal; and D. Shallow ecosystems (≤ 30 m deep). Photos A and B by L. A. Rocha and photos C and D by J. L. Gasparini.

FIGURE 1 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 1 | Location of the Fernando de Noronha Archipelago, Brazil (South-western Atlantic). Blue line indicates the area of the Marine National Park of Fernando de Noronha (no-take MPA). Dashed lines indicate the 30, 60, 90 and 150 m isobaths. Black triangles, red stars, golden squares and green dots indicate the position of stereo-BRUVS deployments, rebreather dives, SCUBA dives and ROV footages, respectively.

FIGURE 5 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 5 | New records of fishes from the mesophotic ecosystems collected and photographed in aquarium. A. Aulotrachichthys argyrophanus (~ 6.5 cm total length; CIUFES 3909); B. Corniger spinosus (~ 15 cm total length; CIUFES 3922); C. Decodon puellaris (~ 7.5 cm total length; CIUFES 3914); and D. Pronotogrammus martinicensis (~ 20 cm total length; CIUFES 3939 / 3960). Photos by J. L. Gasparini.

FIGURE 4 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 4 | New records of fishes at the mesophotic ecosystems. A. Chromis enchrysura (~ 10 cm total length); B. Balistes capriscus (~ 30 cm total length); C. Chromis scotti (~ 7.5 cm total length); D. Prognathodes guyanensis (~ 15 cm total length); E. Synodus sp. (~ 15 cm total length); F. Scorpaena sp. (~ 7.5 cm total length); G. Psilotris sp. (~ 5 cm total length); and H. Cosmocampus profundus (white arrow; ~ 15 cm total; I. Lutjanus buccanella (~ 50 cm total length). Photos by L. A. Rocha (A, C-G) and stereo-BRUVS (B, H and I). Tosanoides sp. is under description and its picture is not shown.

FIGURE 2 in Mesophotic ecosystems at Fernando de Noronha Archipelago, Brazil (South-western Atlantic), reveal unique ichthyofauna and need for conservation

FIGURE 2 | Middle mesophotic (61 to 90 m depth) mosaic of habitats sampled with stereo-BRUVS around the Fernando de Noronha Archipelago. A. Patch reefs; B. Sand bottoms; and C. Rhodoliths beds.

opencc-by-4.0Mar 2016View details →

Fig. 2 in Depletion of trophy large-sized sharks populations of the Argentinean coast, south-western Atlantic: insights from fishers' knowledge

Fig. 2. Variation in abundance reported by fishermen between the beginning of their fishing activity and the last part. (a) With all reports considered and (b) with no abundance variation excluded.

opencc-by-4.0Mar 2016View details →

Fig. 1 in Depletion of trophy large-sized sharks populations of the Argentinean coast, south-western Atlantic: insights from fishers' knowledge

Fig. 1. Location of coastal localities and distribution range of study species in the south west Atlantic. Continuous line: Notorynchus cepedianus; dotted line: Galeorhinus galeus; dashed line: Carcharhinus brachyurus and Carcharias taurus.

opencc-by-4.0Aug 2024View details →

manuscript (atmosphere-3145955) titled: The Black Sea Upwelling System: Analysis on the Western Shallow Waters Authored by: Maria Emanuela Mihailov was accepted in Atmosphere (ISSN 2073-4433) on 15 August 2024

Datasets represents the modelling results for: - Coastal Upwelling Transport Index (CUTI) of the National Oceanic and Administrative Administration’s Environmental Research Division (NOAA-ERD) was used to derive the time series of the coastal upwelling index in four locations on the north-western Black Sea coast. The coastal upwelling index time series was calculated using monthly average wind fields from the European Centre for Medium-Range Weather Forecasts (ECMWFs) reanalysis and MATLAB software to compute the CUTI   - The upwelling index (UI) is computed using the CUTI Formula (Bakun Index ), defined as CUTI (m3·s−1·100 m−1), representing the volume transport per distance unit of an alongshore section. The sign of Ekman transport is changed to define positive or negative values of UI as a response to upwelling or downwelling favourable winds. To compute the BEUTI, Copernicus Marine Service [1] data are used for dedicated locations. [1] Grégoire, M.; Vandenbulcke, L.; Capet, A. Black Sea Biogeochemical Reanalysis (CMEMS BS-Biogeochemistry) (Version 1) set. Copernicus Monitoring Environment Marine Service (CMEMS). 2020. Available online: https://marine.copernicus.eu/ (accessed on 10 November 2023).

FIGURE 11 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation

FIGURE 11. Body mass of caballine Equidae (Equus ferus and E. mosbachensis) in Middle and Late Pleistocene localities from Britain and Germany. For explanation of graph, see Figure 6.

FIGURE 10 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation

FIGURE 10. Body mass of bovine Bovidae (Bison priscus and Bos primigenius) from Middle and Late Pleistocene localities of Britain and Germany. For explanation of graph, see Figure 6.

FIGURE 8 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation

FIGURE 8. Body mass of Rhinocerotidae from Pleistocene localities of Britain and Germany. For explanation of graph, see Figure 6.

FIGURE 9 in Patterns of diet and body mass of large ungulates from the Pleistocene of Western Europe, and their relation to vegetation

FIGURE 9. Linear regressions of body mass (kg) of Bovidae and Equus ferus/mosbachensis from localities with pollen records, and minimum, maximum and mean NAP % in the pollen records of the localities. Each point represents an individual specimen. Numbers of specimens per each locality are given in brackets after the locality names.