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Bathyal zone Stock Photos and Images
RM2FKDJ2P–Dragonfish. Stomiidae. Deep-sea organisms in dark water. Black dragonfish bioluminescent photophores. Idiacanthus atlanticus Fish Of The Deep Sea
RMRHKNHN–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. COLD-WATER SPONGE REPRODUCTION STRATEGIES 85. Figure 11. Life-history scheme of My.wlUi incruxtan.i in the White Sea. the Sea of Japan and the California bathyal zone; in the Atlantic Ocean it extends south to the western Mediterra- nean and Cape Cod (Ereskovsky, 1994a). Thus, M. incntstans is apparently a eurythermic (— 1.9°- 16.2°C) and euryhaline (25^-35.59tr) species (Ereskovsky, 1994b). The area of the Pacific highboreal-Arctic species loplwn piceus is not so broad. I piceus is circumarctic; in the Pacific Ocean it is f
RMG1567D–Cross-sectional diagram showing zones of the ocean. From top to bottom: Epipelagic, Mesopelagic, Bathypelagic, Abyssopelagic, and Hadalpelagic.
RMRMGTYK–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. DEEP-WATER QUATERNARY OSTRACODA 315 boundary, there are large fluctuations in its abundance. Similarly, on approaching the Upper/Lower Bathyal Zone boundary (i.e. the shear zone between the AAIW and NADW masses), there is a large fall in abundance, that continues through the Lower Bathyal Zone (mean 39%, range 28-71%) into the Abyssal Zone (mean 20%, range 6-34%). Clearly, this species has a wide toler- ance of temperature and salinity, but it is relatively less successful in unstable, or mixed zones
RMG1567B–Cross-sectional diagram showing zones of the ocean. From top to bottom: Epipelagic, Mesopelagic, Bathypelagic, Abyssopelagic, and Hadalpelagic.
![. Bulletins of American paleontology. FORAMINIFERA-MIOCENE-PUOCENE CALIFORNIA: InGLE 287 <))»»»» ^m^' '"'''^^mjii.iA^spmmi^mm^. â SHELF ZONE- 500 â¢BATHYAL ZONE 1000 rMETRY IN METERS ^GLOBOROTALIA HIRSUTA ^GLOBIGERINITA GLUTINATA ^GLOBIGERINELLA SIPHONIFERAâ ^GLOBOROTALIA TRUNCATULINOIDES â â ORBULINA CHAMBERS -GLOBIGERINITA HUMILUS- -GLOBOROTALIA INFLATA- GLOBOROTALOIDES HEXAGONUS GLOBOROTALIA SCITULA ^^ââ Text-figure 28.âCumulative frequency of planktonic Foraminifera within a series of progressively deeper samples off southern California (Appendix Table 6). ments at the shelf ed Stock Photo](https://c8.alamy.com/comp/RG9EN5/bulletins-of-american-paleontology-foraminifera-miocene-puocene-california-ingle-287-lt-m-quotmjiiiaspmmimm-shelf-zone-500-bathyal-zone-1000-rmetry-in-meters-globorotalia-hirsuta-globigerinita-glutinata-globigerinella-siphonifera-globorotalia-truncatulinoides-orbulina-chambers-globigerinita-humilus-globorotalia-inflata-globorotaloides-hexagonus-globorotalia-scitula-text-figure-28cumulative-frequency-of-planktonic-foraminifera-within-a-series-of-progressively-deeper-samples-off-southern-california-appendix-table-6-ments-at-the-shelf-ed-RG9EN5.jpg ". Bulletins of American paleontology. FORAMINIFERA-MIOCENE-PUOCENE CALIFORNIA: InGLE 287 <))»»»» ^m^' '"'''^^mjii.iA^spmmi^mm^. â SHELF ZONE- 500 â¢BATHYAL ZONE 1000 rMETRY IN METERS ^GLOBOROTALIA HIRSUTA ^GLOBIGERINITA GLUTINATA ^GLOBIGERINELLA SIPHONIFERAâ ^GLOBOROTALIA TRUNCATULINOIDES â â ORBULINA CHAMBERS -GLOBIGERINITA HUMILUS- -GLOBOROTALIA INFLATA- GLOBOROTALOIDES HEXAGONUS GLOBOROTALIA SCITULA ^^ââ Text-figure 28.âCumulative frequency of planktonic Foraminifera within a series of progressively deeper samples off southern California (Appendix Table 6). ments at the shelf ed Stock Photo")
RMRG9EN5–. Bulletins of American paleontology. FORAMINIFERA-MIOCENE-PUOCENE CALIFORNIA: InGLE 287 <))»»»» ^m^' '"'''^^mjii.iA^spmmi^mm^. â SHELF ZONE- 500 â¢BATHYAL ZONE 1000 rMETRY IN METERS ^GLOBOROTALIA HIRSUTA ^GLOBIGERINITA GLUTINATA ^GLOBIGERINELLA SIPHONIFERAâ ^GLOBOROTALIA TRUNCATULINOIDES â â ORBULINA CHAMBERS -GLOBIGERINITA HUMILUS- -GLOBOROTALIA INFLATA- GLOBOROTALOIDES HEXAGONUS GLOBOROTALIA SCITULA ^^ââ Text-figure 28.âCumulative frequency of planktonic Foraminifera within a series of progressively deeper samples off southern California (Appendix Table 6). ments at the shelf ed
![. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Fig. 3. Latitude and water depth of samples bearing Cytherella species. There are two species in each of the Neritic and Bathyal zones: C. dromedaria Brady and Cytherella sp. nov., and C. serratula Brady and Cytherella sp. 3027, respectively. NERITIC. ABYSSAL C. sp.3027^ "i r water depth, km Fig. 4. Cytherella species as percentage of total ostracod fauna plotted against water depth. Note concentrations of samples on the continental shelf (<300 m), and at the Upper/Lower Bathyal Zone boundary Stock Photo](https://c8.alamy.com/comp/RMGXBE/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-fig-3-latitude-and-water-depth-of-samples-bearing-cytherella-species-there-are-two-species-in-each-of-the-neritic-and-bathyal-zones-c-dromedaria-brady-and-cytherella-sp-nov-and-c-serratula-brady-and-cytherella-sp-3027-respectively-neritic-abyssal-c-sp3027-quoti-r-water-depth-km-fig-4-cytherella-species-as-percentage-of-total-ostracod-fauna-plotted-against-water-depth-note-concentrations-of-samples-on-the-continental-shelf-lt300-m-and-at-the-upperlower-bathyal-zone-boundary-RMGXBE.jpg ". Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Fig. 3. Latitude and water depth of samples bearing Cytherella species. There are two species in each of the Neritic and Bathyal zones: C. dromedaria Brady and Cytherella sp. nov., and C. serratula Brady and Cytherella sp. 3027, respectively. NERITIC. ABYSSAL C. sp.3027^ "i r water depth, km Fig. 4. Cytherella species as percentage of total ostracod fauna plotted against water depth. Note concentrations of samples on the continental shelf (<300 m), and at the Upper/Lower Bathyal Zone boundary Stock Photo")
RMRMGXBE–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Fig. 3. Latitude and water depth of samples bearing Cytherella species. There are two species in each of the Neritic and Bathyal zones: C. dromedaria Brady and Cytherella sp. nov., and C. serratula Brady and Cytherella sp. 3027, respectively. NERITIC. ABYSSAL C. sp.3027^ "i r water depth, km Fig. 4. Cytherella species as percentage of total ostracod fauna plotted against water depth. Note concentrations of samples on the continental shelf (<300 m), and at the Upper/Lower Bathyal Zone boundary
RMRMGX8F–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. DEEP-WATER QUATERNARY OSTRACODA 259. water depth, km Fig. 8. Cytheropteron species as percentage of total ostracod fauna plotted against water depth. Values are five point running means. Depth ranges of species are shown by bars. N.B. Neritic species, Cytheropteron species 1-9, are not further discussed herein. occur with extensively overlapping depth ranges in the outer shelf/upper slope region, whereas in the Bathyal Zone only one species has an extensive depth range (C. cronini sp. nov., 990-2 070
RMRMGX5A–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 264 ANNALS OF THE SOUTH AFRICAN MUSEUM Cytheropteron (57 species), Krithe (54 species) is the most diverse genus in the Quaternary ostracod faunas of the bathyal and abyssal regions of the south- western Pacific. Similarly, Krithe (together with one species of Parakrithe) and Cytheropte- ron are the two most diverse genera in the deep-water faunas off south-western Africa (12 species each), whereas in the Abyssal Zone the genus Krithe is the most abundant taxon. It occurs across the entire latitudina
![. Bulletins of American paleontology. 240 Bulletin 236. PLANKTONIC INDEXES °f'-*'ONTUN- UPPER MOHNIAN T LOWER LIMIT V SINISTRAL ZONE GLOBIGERINA PACHYDERMA Text-figure 14.—Planktonic correlation of bathyal upper Tertiary sequences within the Capistrano embayment, Orange County, California, after Ingle (1962, 1963a). Alignment of sections on presumably isochronous surfaces illustrates that the traditional Miocene-Pliocene boundary between Delmontian and Repettian stages is time-transgressive in this embayment. "Lower Pliocene" Repettian benthic faunas appeared earlier in the Capistran Stock Photo](https://c8.alamy.com/comp/RG9F4W/bulletins-of-american-paleontology-240-bulletin-236-planktonic-indexes-f-ontun-upper-mohnian-t-lower-limit-v-sinistral-zone-globigerina-pachyderma-text-figure-14planktonic-correlation-of-bathyal-upper-tertiary-sequences-within-the-capistrano-embayment-orange-county-california-after-ingle-1962-1963a-alignment-of-sections-on-presumably-isochronous-surfaces-illustrates-that-the-traditional-miocene-pliocene-boundary-between-delmontian-and-repettian-stages-is-time-transgressive-in-this-embayment-quotlower-pliocenequot-repettian-benthic-faunas-appeared-earlier-in-the-capistran-RG9F4W.jpg ". Bulletins of American paleontology. 240 Bulletin 236. PLANKTONIC INDEXES °f'-*'ONTUN- UPPER MOHNIAN T LOWER LIMIT V SINISTRAL ZONE GLOBIGERINA PACHYDERMA Text-figure 14.—Planktonic correlation of bathyal upper Tertiary sequences within the Capistrano embayment, Orange County, California, after Ingle (1962, 1963a). Alignment of sections on presumably isochronous surfaces illustrates that the traditional Miocene-Pliocene boundary between Delmontian and Repettian stages is time-transgressive in this embayment. "Lower Pliocene" Repettian benthic faunas appeared earlier in the Capistran Stock Photo")
RMRG9F4W–. Bulletins of American paleontology. 240 Bulletin 236. PLANKTONIC INDEXES °f'-*'ONTUN- UPPER MOHNIAN T LOWER LIMIT V SINISTRAL ZONE GLOBIGERINA PACHYDERMA Text-figure 14.—Planktonic correlation of bathyal upper Tertiary sequences within the Capistrano embayment, Orange County, California, after Ingle (1962, 1963a). Alignment of sections on presumably isochronous surfaces illustrates that the traditional Miocene-Pliocene boundary between Delmontian and Repettian stages is time-transgressive in this embayment. "Lower Pliocene" Repettian benthic faunas appeared earlier in the Capistran
RMRMHK0Y–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. DEEP-WATER QUATERNARY OSTRACODA 301. Fig. 33. Distribution of modern species of Abyssocythere. Re-plotted from data in Benson (1971—dots), with sample site TBD 6851 off south-western Africa shown as an open circle. Genus Ambocy'there van den Bold, 19586 A listing of Recent species of this genus that have previously been described from relatively deep water, shows that the genus Ambocythere has a depth range from the inner continental shelf to the Abyssal Zone: Bathyal/Abyssal A. ramosa—Iceland, c. 1
RMRHJRR3–. Biology of the seas of the U.S.S.R. Marine biology -- Soviet Union; Hydrology -- Soviet Union. 806 BIOLOGY OF THE SEAS OF THE U.S.S.R, P. Ushakov (1953) divides the bathyal into two parts: an upper (200 to 750 m), and a lower (750 to 2,000 m), giving a colourful description of the peculiar fauna of the upper zone of the Sea of Okhotsk bathyal (Fig. 406,. Fig. 400. Quantitative distribution (in g/m2) of sessile sestonophages of hard soils of Sea of Okhotsk (Savilov). 1-5). 'The great Balanus evermanni forms large colonies on the steep rocky slopes . . many Octocorallia, and in particular the
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