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opennotspecifiedJul 2014View details →

Distribution. Restricted to the cooler waters of the N Atlantic Ocean, as far N as the Davis Strait, Jan Mayen, and Spitsbergen, and as far S as NE USA, Azores, and Canary Is; in E Atlantic Ocean, this species appears to be relatively rare S of Bay of Biscay. Although its occurrence seems to be relatively continuous in some parts of its distribution, such as in the E Atlantic Ocean, it appears to be more fragment ed in others, such as in the waters off E Canada. in Ziphiidae

Distribution. Restricted to the cooler waters of the N Atlantic Ocean, as far N as the Davis Strait, Jan Mayen, and Spitsbergen, and as far S as NE USA, Azores, and Canary Is; in E Atlantic Ocean, this species appears to be relatively rare S of Bay of Biscay. Although its occurrence seems to be relatively continuous in some parts of its distribution, such as in the E Atlantic Ocean, it appears to be more fragment ed in others, such as in the waters off E Canada.

opencc-by-4.0May 2024View details →

Results of water temperature measurements and observations of ice cover occurrence on the Ropa and Biala rivers

The dataset contains the results of water temperature measurements and ice cover occurrence on two rivers - the Ropa and the Biala. The measurements were carried out on December 29, 2021 under a research grant funded by the National Science Center of Poland (grant number: 2020/39/O/ST10/00652).

opencc-by-4.0Dec 2023View details →

Water slowing down drives the occurrence of the low temperature dynamical transition in microgels

Data presented in the article entitled Water slowing down drives the occurrence of the low temperature dynamical transition in microgels.

opennotspecifiedDec 2013View details →

FIGURES 26‑31 in Anatomy Of Phyllodina Persica (Bivalvia: Tellinidae), And Its First Occurrence In Southeastern Brazilian Waters

FIGURES 26‑31: Phyllodina persica anatomy. 26, Pericardial region sectioned and posterior loops of intestine visible by transparency, with right lobe of kidney withdrawn (asterisk); 27, detail of anterior region with foot protractor muscle withdrawn, right view; 28, posterior foot retractor muscles, posterior view (dotted line representing the rectum); 29, detail of base of siphons showing branches of right siphonal muscle; 30, right siphonal muscle; 31, cruciform muscle and ventral channel, dorsal view. Scales bar = 1.5 mm.

opennotspecifiedApr 2018View details →

FIGURE 1. Chaceon affinis. Zoea I. a in Morphology of the first zoea of Chaceon affinis (A. Milne-Edwards & Bouvier, 1894) and occurrence of Chaceon spp. larvae (Decapoda: Brachyura: Gerynonidae) in the Canary Islands waters, Northeastern Atlantic

FIGURE 1. Chaceon affinis. Zoea I. a, carapace frontal view; b, carapace ventral margin; c, antennule; d, antenna; e, maxillule; f, maxilla; g, maxilliped I; h, maxilliped II; i, dorsal and i' lateral view of pleon and telson. Scale bars: a = 0.5 mm; b–f = 0.2 mm.

opennotspecifiedAug 2008View details →

FIGURE 1 in Acartia (Odontacartia) ohtsukai Ueda and Bucklin, 2006 (Copepoda, Calanoida, Acartiidae): First Record of its Occurrence in Korean Waters and Habitat Segregation from its Sibling Species A. pacifica Steuer, 1915

FIGURE 1. Acartia ohtsukai (Ueda and Bucklin, 2006). Female (A) Habitus, dorsal view; (B) leg 5; Male (C) habitus, dorsal view; (D) leg 5. Scale bars A,C = 200, B,D = 50; r, right leg; l, left leg.

opennotspecifiedAug 2008View details →

FIGURE 2 in Acartia (Odontacartia) ohtsukai Ueda and Bucklin, 2006 (Copepoda, Calanoida, Acartiidae): First Record of its Occurrence in Korean Waters and Habitat Segregation from its Sibling Species A. pacifica Steuer, 1915

FIGURE 2. Temperature-salinity-abundance diagram for A. ohtsukai and A. pacifica. Abundance (ind./m3) of each species is estimated by multiplying numbers on scale by 102 for A. ohtsukai (black circle) and A. pacifica (white circle).

Figure 6 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 6. Total length frequency distribution for blue sharks (Prionace glauca) captured in the southeastern Mediterranean large pelagic fisheries during 1998–2005.

Figure 3 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 3. Map depicting capture locations of blue sharks (Prionace glauca) in the southeastern Mediterranean large pelagic fisheries during 1998–2005.

Figure 5 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 5. Map depicting capture locations of other large shark species in the southeastern Mediterranean large pelagic fisheries during 1998–2005.

Figure 2 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 2. (Top) Annual trend of large shark species richness as inferred from the slope of a linear regression of average number of species upon year on a series of randomly selected hauls in each year. Open circles depict number of species observed during a year. Dashed lines indicate centred 95% confidence intervals. (Bottom) Generalized additive model derived effects of the investigated parameters on the binomial probability of encountering large sharks. Dashed lines indicate two standard errors above and below the estimates.

Figure 7. A in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 7. A rare specimen of basking shark (Cetorhinus maximus) landed in the Athens auction fish market in March 2009.

Figure 4 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 4. Map depicting capture locations of mackerel shark species (Lamniformes) in the southeastern Mediterranean large pelagic fisheries during 1998–2005.

Figure 1 in Occurrences of large sharks in the open waters of the southeastern Mediterranean Sea

Figure 1. Map of the study area in the southeastern Mediterranean Sea. Fishing locations are indicated by crosses (1998–2001) and solid triangles (2003–2005). Shaded marine regions designate potential Exclusive Economic Zones (EEZ) as provided by Flanders Marine Institute (VLIZ), available at: http://www.vliz.be/vmdcdata/marbound/. To date, very few Mediterranean countries have claimed an EEZ.

Fig. 3 in Temporal occurrence of three blue whale populations in New Zealand waters from passive acoustic monitoring

Fig. 3.—Temporal occurrence pattern of New Zealand (dark blue), Antarctic (red), and Australian (yellow) blue whale song detections at each of the five hydrophones. The y-axis represents the number of hours per day that blue whale song was detected, and the x-axis represents the recording period. Grayed out sections represent gaps in recording due to hydrophone refurbishment.

Fig. 2 in Temporal occurrence of three blue whale populations in New Zealand waters from passive acoustic monitoring

Fig. 2.—Example spectrograms of the three song types recorded in New Zealand waters. (A) New Zealand song on 31 May 2016, (B) Antarctic song on 26 August 2017, and (C) Australian song on 22 January 2017. Spectrograms are configured with a 2048-point fast Fourier transform, Hann window, 50% overlap.

Fig. 4 in Temporal occurrence of three blue whale populations in New Zealand waters from passive acoustic monitoring

Fig. 4.—Conceptual map illustrating the current understanding of the approximate typical range of each blue whale population. Colors indicate the song type, and patterns represent inferred ecological use of each region. Distribution and occurrence patterns are synthesized from acoustic research published in the literature (e.g., Stafford et al. 2004; Balcazar et al. 2015, 2017; Tripovich et al. 2015; McCauley et al. 2018; Warren et al. 2021), and findings presented in this study.

Fig. 1 in Temporal occurrence of three blue whale populations in New Zealand waters from passive acoustic monitoring

Fig. 1.—Map of the study area in the South Taranaki Bight region, with hydrophone locations denoted by the stars. Gray lines show bathymetry contours at 50-m depth increments, from 0 to 500 m. Location of the study area within New Zealand is indicated by the inset map.