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opencc-by-4.0Feb 2011View details →

Fig. 3 in Distribution Of Small Cetaceans In The Nearshore Waters Of Sarawak, East Malaysia

Fig. 3. Box and whisker plots showing the minimum and maximum values, median and upper and lower quartiles of the values for depth (a), distance to shore (b), and distance to nearest river mouth (c) for on-effort sightings of Irrawaddy dolphins (n=35), finless porpoises (n=24) and bottlenose dolphins (n=3).

opencc-by-4.0Feb 2011View details →

Fig. 4 in Distribution Of Small Cetaceans In The Nearshore Waters Of Sarawak, East Malaysia

Fig. 4. (a) Kuching and (b) Similajau survey areas with 2k m × 2 km grid cells shaded according to encounter rate (number of sightings/distance searched in each grid cell). Only grid cells with dolphin sightings are shaded – others are left blank to better display underlying survey effort.

opencc-by-4.0Mar 2024View details →

Data files for manuscript "Coral growth along a natural gradient of seawater temperature, pH, and oxygen in a nearshore seagrass bed on Dongsha Atoll, Taiwan"

Data files and README file for the manuscript "Coral growth along a natural gradient of seawater temperature, pH, and oxygen in a nearshore seagrass bed on Dongsha Atoll, Taiwan" by Ariel K. Pezner, Travis A. Courtney, Wen-Chen Chou, Hui-Chuan Chu, Benjamin W. Frable, Samuel A. H. Kekuewa, Keryea Soong, Yi Wei, and Andreas J. Andersson. Data files include carbonate chemistry data from discrete seawater samples taken over a shallow seagrass bed, Porites skeletal extension, density, and calcification rates from 15 coral cores collected in the seagrass bed (as well as collection locations), and data from an autonomous CTD sensor deployed in the shallow seagrass.

opencc-by-4.0Dec 2022View details →

Fig. 5 in Ostracodes (Crustacea, Ostracoda) In The Rocky Nearshore Water Area Of Zmiiniy Island (Black Sea)

Fig. 5. The non-metric multidimensional scaling (nMDS) analysis of ostracodes species abundance in the sample from different substrates in Zmiiniy Island.

opencc-by-4.0Dec 2022View details →

Fig. 2 in Ostracodes (Crustacea, Ostracoda) In The Rocky Nearshore Water Area Of Zmiiniy Island (Black Sea)

Fig. 2. The percentages of ostracodes in average density of meiobenthos at the different type of substrate from Zmiiniy Island.

opencc-by-4.0Dec 2022View details →

Fig. 6 in Ostracodes (Crustacea, Ostracoda) In The Rocky Nearshore Water Area Of Zmiiniy Island (Black Sea)

Fig. 6. The results of CLUSTER analysis with the SIMPROF test based on the biomass on different substrates in Zmiiniy Island.

opencc-by-4.0Jul 2024View details →

Dataset in "Near real-time in-situ monitoring of nearshore ocean currents using Distributed Acoustic Sensing on submarine fiber-optic cable"

Dataset in "Near real-time in-situ monitoring of nearshore ocean currents using Distributed Acoustic Sensing on submarine fiber-optic cable"  <a href="../api/records/13133835/draft/files/tmdcm.txt/content" target="_blank" rel="noopener noreferrer">tmdcm.txt</a>: current meter data  <a href="../api/records/13133835/draft/files/tide.txt/content" target="_blank" rel="noopener noreferrer">tide.txt</a>: tidal gauge data  <a href="../api/records/13133835/draft/files/windspeed.txt/content" target="_blank" rel="noopener noreferrer">windspeed.txt</a>: windspeed data  Figure 2: Figure2.npy Figure 3: Figure 3 abc .npy Figure16:  <a href="../api/records/13133835/draft/files/spatial_Vc.npy/content" target="_blank" rel="noopener noreferrer">spatial_Vc.npy</a> & <a href="13133835" target="_blank" rel="noopener noreferrer">spatial_h.npy</a>  Figure 17: <a href="../api/records/13133835/draft/files/streching_ncf.npy/content" target="_blank" rel="noopener noreferrer">streching_ncf.npy</a>

opencc-by-4.0Oct 2017View details →

COMMENTS.— Although not breeding in the Mediterranean, the species forages in Libyan waters (van Dijk et al. 2014). In addition to the single beached record, an individual was pulled from nearshore waters of the Tajura coast in 1996 and died in the rehabilitation facility of the Marine Biology Research Centre (MBRC) at Tajura, where it was subsequently taxidermied at the MBRC Museum (Hamza 2010). Capra's (1949) records were based on a report in "L'Idea Coloniale" for 2 May 1927 (Mongàr) and an unspecified specimen in the Museo Civico di Storia Naturale di Trieste (Sella). IUCN THREAT STATUS.— Vulnerable A2bd. MAP 3. Distribution of Dermochelys coriacea in Libya showing stranding site records. in Atlas of the Reptiles of Libya

COMMENTS.— Although not breeding in the Mediterranean, the species forages in Libyan waters (van Dijk et al. 2014). In addition to the single beached record, an individual was pulled from nearshore waters of the Tajura coast in 1996 and died in the rehabilitation facility of the Marine Biology Research Centre (MBRC) at Tajura, where it was subsequently taxidermied at the MBRC Museum (Hamza 2010). Capra's (1949) records were based on a report in "L'Idea Coloniale" for 2 May 1927 (Mongàr) and an unspecified specimen in the Museo Civico di Storia Naturale di Trieste (Sella). IUCN THREAT STATUS.— Vulnerable A2bd. MAP 3. Distribution of Dermochelys coriacea in Libya showing stranding site records.

opencc-by-4.0Nov 2009View details →

Text-fig. 3. Distribution of main types of volcanoes in the NearShore Volcanic Belt of Eastern Sikhote-Alin' (Eocene–Neogene). 1 – Central volcanoes (partly preserved); 2 – Central volcanoes (destructed); 3 – Shield and gentle sloping volcanoes with a dolerite or trachy-basaltic neck on the top; 4 – Lava and scoria cones; 5 – Pyroclastic, tuffaceous coarse- and fine-grained terrigenous sedimentary rocks, partly with plant-bearing levels; 6 – Eruption centers of plateau-basalts and the direction of lava flows; 7 – Main Late Cenozoic basaltic plateaus; 8 – Fumarol fields; 9 – Hot springs. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)

Text-fig. 3. Distribution of main types of volcanoes in the NearShore Volcanic Belt of Eastern Sikhote-Alin' (Eocene–Neogene). 1 – Central volcanoes (partly preserved); 2 – Central volcanoes (destructed); 3 – Shield and gentle sloping volcanoes with a dolerite or trachy-basaltic neck on the top; 4 – Lava and scoria cones; 5 – Pyroclastic, tuffaceous coarse- and fine-grained terrigenous sedimentary rocks, partly with plant-bearing levels; 6 – Eruption centers of plateau-basalts and the direction of lava flows; 7 – Main Late Cenozoic basaltic plateaus; 8 – Fumarol fields; 9 – Hot springs.

FIGURE 1 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 1 | A. Map of the study area, nearshore waters in front of the Huizache-Caimanero estuarine system, located in the southeast Gulf of California, Sinaloa, Mexico. Sampling sites are indicated by black circles. B. Detail of the study area and sampling sites located in front of the Presidio River inlet.

FIGURE 4 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 4 | Boxplots for diversity and evenness for the sampled months from September 1994 to June 1995. A. Diversity, B. Evennes. Line: median; box: 25th to 75th percentiles; whiskers: minimum to maximum value range. Differences in GLM p-values are shown by lowercase letters, different letters mean significant differences for the indexes (p-value <0.05).

FIGURE 7 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 7 | Vertical distribution of the abundance of the species found in the study. Bars indicate the mean value (individuals m-3) and error bars the Standard Error.

FIGURE 3 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 3 | Water temperature and salinity profiles at each sampling site, for each sampled month from September 1994 to June 1995.

FIGURE 5 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 5 | Correlation triplot of the db-RDA showing the relationship between explanatory (temperature and salinity) and response variables (species). Black labels indicate the position of species in the ordination; their size increase according to the abundance of the species to achieve a better visualization. Samples are coded by depths and months. The angles between species and explanatory variables reflect their correlations; a small angle implies a positive correlation, a large one suggests a negative correlation, and a 90° angle indicates no correlation between two variables.

FIGURE 2 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 2 | A. Box plots showing temporal variations in temperature and salinity during the sampling period (1994–1995). Line: median; box: 25th to 75th percentiles; whiskers: minimum to maximum value range. Months with the same letters do not significantly differ using Dunn's test. B. Monthly variability of salinity from October 2011 to August 2014, dots indicate the mean value and error bars the Standard Deviation.

FIGURE 6 in Larval fish assemblages in nearshore waters of southeast Gulf of California: vertical and temporal patterns

FIGURE 6 | Temporal and vertical variations of the abundance of the most abundant species found in the study. Dots indicate the mean value and error bars the Standard Error. SEP: September, DEC: December, Apr: April, JUN: June.

Fig. 7 in Mollusc biodiversity in late Holocene nearshore environments of the Caspian Sea: A baseline for the current biodiversity crisis

Fig. 7. Late Holocene Novocaspian gastropod species from Turali, with indication of sample and collection number. A Clathrocaspia gmelinii: M0203, RGM.1309848 B Clessiniola variabilis: M0204, RGM.1309864 C Ecrobia grimmi: M0202, RGM.1309863 D Laevicaspia sieversii: M0204, RGM.1309849 E Laevicaspia kolesnikoviana: M0221, RGM.1309850 F Laevicaspia conus: M0204, RGM.1309851 G Turricaspia spica: M0202, RGM.1309858 H Turricaspia sp. indet. M0222, RGM.962401. I Abeskunus brusinianus: low morph, M0204, RGM.962355 J Abeskunus brusinianus: high morph, M0204, RGM.962355 K Theodoxus pallasi: M0204, RGM.130985, L. Theodoxus pallasi: M0220, RGM.1309862, M Abeskunus exiguus, M0204, RGM.962357. Scale bars 1 mm.

Fig. 6 in Mollusc biodiversity in late Holocene nearshore environments of the Caspian Sea: A baseline for the current biodiversity crisis

Fig. 6. Late Holocene Novocaspian bivalve species from Turali, with indication of sample and collection number. LV displayed on the left, RV on the right. A–B Adacna laeviuscula (Eichwald, 1829). A M0222, RGM.962359 B M0222, RGM.962358 C–D Adacna vitrea (Eichwald, 1829) C M0221, RGM.962360 D M0221, RGM.962361 E–F Hypanis plicata (Eichwald, 1829) E M0221, RGM.962362 F M0221, RGM.962363 G–H Monodacna albida (Logvinenko & Starobogatov, 1967) G M0202, RGM.962364 H M0202, RGM.962365 I–J Monodacna caspia (Eichwald, 1829) I M0204, RGM.962367 J M0205, RGM.962368 K–L Monodacna semipellucida (Logvinenko & Starobogatov, 1967) K M0222, RGM.962369 L M0222, RGM.962370 M–N Dreissena caspia (Eichwald, 1855) M M0222, RGM.962371 N M0202, RGM.962372 O–P Dreissena elata (Andrusov, 1897) O M0203, RGM.962375 P M0221, RGM.962376 Q–R Dreissena grimmi (Andrusov, 1890) Q M0203, RGM.962374 R M0202, RGM.962373. Scale bars 5 mm.

Fig. 2 in Mollusc biodiversity in late Holocene nearshore environments of the Caspian Sea: A baseline for the current biodiversity crisis

Fig. 2. Schematic representation of sections Turali 1-3. Asterisks (*) denote calibrated 14C ages BP. Small case letters refer to sedimentary units: a. eastwards-dipping bay fill, b. eastwards-dipping bay fill, c. sand with shells along eastward-dipping foresets, d. deformed laminated silts and sands, e. massive gravel beds, f. coarsegrained pebble lag, g. slightly dipping sand layers with shells, h. low-angle clinoforms with pebbles and shells, i. stratified silt stone, lagoonal, j. silt layer with shells, k. Aeolian interval, l. stratified silt stone, lagoonal.

Fig. 3 in Mollusc biodiversity in late Holocene nearshore environments of the Caspian Sea: A baseline for the current biodiversity crisis

Fig. 3. Paired Didacna eichwaldi (Turali-2, sample M0205) exposed just below the water table of the Great Turali Lake. Width of the shells approximately 2 cm. Photograph SBK, 2002.