Protozoic Stock Photos and Images
Jelly fish at Cape Town Waterfront's Two Ocean's Aquarium is a popular drawcard for both South African and international tourists visiting the city. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/jelly-fish-at-cape-town-waterfronts-two-oceans-aquarium-is-a-popular-drawcard-for-both-south-african-and-international-tourists-visiting-the-city-image439087085.htmlRF2GEA41H–Jelly fish at Cape Town Waterfront's Two Ocean's Aquarium is a popular drawcard for both South African and international tourists visiting the city.
A manual of the Infusoria : including a description of all known flagellate, ciliate, and tentaculiferous protozoa, British and foreign, and an account of the organization and the affinities of the sponges . c and comparatively amorphous protoplasmicbodies into mullicellular aggregates or Metazoa. Nay more, numberless examplesof the Ciliata are multinucleate, and therefore potentially multicellular, and furnish,by reason of such differentiation, the most perfect possible links of connectionbetween the Protozoic and Metazoic series. Where, consequently, as in the severalcases here submitted, th Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-manual-of-the-infusoria-including-a-description-of-all-known-flagellate-ciliate-and-tentaculiferous-protozoa-british-and-foreign-and-an-account-of-the-organization-and-the-affinities-of-the-sponges-c-and-comparatively-amorphous-protoplasmicbodies-into-mullicellular-aggregates-or-metazoa-nay-more-numberless-examplesof-the-ciliata-are-multinucleate-and-therefore-potentially-multicellular-and-furnishby-reason-of-such-differentiation-the-most-perfect-possible-links-of-connectionbetween-the-protozoic-and-metazoic-series-where-consequently-as-in-the-severalcases-here-submitted-th-image339938380.htmlRM2AN1ETC–A manual of the Infusoria : including a description of all known flagellate, ciliate, and tentaculiferous protozoa, British and foreign, and an account of the organization and the affinities of the sponges . c and comparatively amorphous protoplasmicbodies into mullicellular aggregates or Metazoa. Nay more, numberless examplesof the Ciliata are multinucleate, and therefore potentially multicellular, and furnish,by reason of such differentiation, the most perfect possible links of connectionbetween the Protozoic and Metazoic series. Where, consequently, as in the severalcases here submitted, th
. Report of a geological survey of Wisconsin, Iowa, and Minnesota : and incidentally of a portion of Nebraska Territory : made under instructions from the United States Treasury Department . OUTLET OF LAKE PEPIN.. CAP DES SIOUX 46 PROTOZOIC EOCKS A little below the Red Wing Village, near the northern extremity of LakePepin, is a remarkable headland, which has all the appearance of a hill splitdown the middle, as shown in the subjoined cut. Here the Lower Magnesian Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/report-of-a-geological-survey-of-wisconsin-iowa-and-minnesota-and-incidentally-of-a-portion-of-nebraska-territory-made-under-instructions-from-the-united-states-treasury-department-outlet-of-lake-pepin-cap-des-sioux-46-protozoic-eocks-a-little-below-the-red-wing-village-near-the-northern-extremity-of-lakepepin-is-a-remarkable-headland-which-has-all-the-appearance-of-a-hill-splitdown-the-middle-as-shown-in-the-subjoined-cut-here-the-lower-magnesian-image374987815.htmlRM2CP24NY–. Report of a geological survey of Wisconsin, Iowa, and Minnesota : and incidentally of a portion of Nebraska Territory : made under instructions from the United States Treasury Department . OUTLET OF LAKE PEPIN.. CAP DES SIOUX 46 PROTOZOIC EOCKS A little below the Red Wing Village, near the northern extremity of LakePepin, is a remarkable headland, which has all the appearance of a hill splitdown the middle, as shown in the subjoined cut. Here the Lower Magnesian
. Report of a geological survey of Wisconsin, Iowa, and Minnesota : and incidentally of a portion of Nebraska Territory : made under instructions from the United States Treasury Department . CAP DES SIOUX 46 PROTOZOIC EOCKS A little below the Red Wing Village, near the northern extremity of LakePepin, is a remarkable headland, which has all the appearance of a hill splitdown the middle, as shown in the subjoined cut. Here the Lower Magnesian. LA GRANGE MOUNTAIN. Limestone forms about one hundred and fifty feet of the upper portion of the hill.The base, for one hundred and eighty feet, is chief Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/report-of-a-geological-survey-of-wisconsin-iowa-and-minnesota-and-incidentally-of-a-portion-of-nebraska-territory-made-under-instructions-from-the-united-states-treasury-department-cap-des-sioux-46-protozoic-eocks-a-little-below-the-red-wing-village-near-the-northern-extremity-of-lakepepin-is-a-remarkable-headland-which-has-all-the-appearance-of-a-hill-splitdown-the-middle-as-shown-in-the-subjoined-cut-here-the-lower-magnesian-la-grange-mountain-limestone-forms-about-one-hundred-and-fifty-feet-of-the-upper-portion-of-the-hillthe-base-for-one-hundred-and-eighty-feet-is-chief-image374987878.htmlRM2CP24T6–. Report of a geological survey of Wisconsin, Iowa, and Minnesota : and incidentally of a portion of Nebraska Territory : made under instructions from the United States Treasury Department . CAP DES SIOUX 46 PROTOZOIC EOCKS A little below the Red Wing Village, near the northern extremity of LakePepin, is a remarkable headland, which has all the appearance of a hill splitdown the middle, as shown in the subjoined cut. Here the Lower Magnesian. LA GRANGE MOUNTAIN. Limestone forms about one hundred and fifty feet of the upper portion of the hill.The base, for one hundred and eighty feet, is chief
![. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Fig. 46.—Owen's geological sections. the Ohio, a portion of them being contemporaneous with the Calcif- erous group and Potsdam sandstone of New York. He noted also that the Fulls of St, Anthony are receding and were probably at one time at a point near Fort Snelling.. Please note that these Stock Photo](https://c8.alamy.com/comp/RM3BJC/annual-report-of-the-board-of-regents-of-the-smithsonian-institution-smithsonian-institution-smithsonian-institution-archives-discoveries-in-science-unstratified-rocks-primary-fosailif-crous-s-protozoic-rocks-fis4-gt-ftltrs-r-r-quot-s-coal-mtasures-samp5t-fig-46owens-geological-sections-the-ohio-a-portion-of-them-being-contemporaneous-with-the-calcif-erous-group-and-potsdam-sandstone-of-new-york-he-noted-also-that-the-fulls-of-st-anthony-are-receding-and-were-probably-at-one-time-at-a-point-near-fort-snelling-please-note-that-these-RM3BJC.jpg ". Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Fig. 46.—Owen's geological sections. the Ohio, a portion of them being contemporaneous with the Calcif- erous group and Potsdam sandstone of New York. He noted also that the Fulls of St, Anthony are receding and were probably at one time at a point near Fort Snelling.. Please note that these Stock Photo")
. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Fig. 46.—Owen's geological sections. the Ohio, a portion of them being contemporaneous with the Calcif- erous group and Potsdam sandstone of New York. He noted also that the Fulls of St, Anthony are receding and were probably at one time at a point near Fort Snelling.. Please note that these Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-board-of-regents-of-the-smithsonian-institution-smithsonian-institution-smithsonian-institution-archives-discoveries-in-science-unstratified-rocks-primary-fosailif-crous-s-protozoic-rocks-fis4-gt-ftltrs-r-r-quot-s-coal-mtasures-samp5t-fig-46owens-geological-sections-the-ohio-a-portion-of-them-being-contemporaneous-with-the-calcif-erous-group-and-potsdam-sandstone-of-new-york-he-noted-also-that-the-fulls-of-st-anthony-are-receding-and-were-probably-at-one-time-at-a-point-near-fort-snelling-please-note-that-these-image236102900.htmlRMRM3BJC–. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Fig. 46.—Owen's geological sections. the Ohio, a portion of them being contemporaneous with the Calcif- erous group and Potsdam sandstone of New York. He noted also that the Fulls of St, Anthony are receding and were probably at one time at a point near Fort Snelling.. Please note that these
![. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. %. /. Ten, a ar> Jo^itiferous Strata "-yfi-^s ZatT -fossiiifcrous, unstratificd rrx-ks. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly rese Stock Photo](https://c8.alamy.com/comp/RM3BK1/annual-report-of-the-board-of-regents-of-the-smithsonian-institution-smithsonian-institution-smithsonian-institution-archives-discoveries-in-science-ten-a-argt-joitiferous-strata-quot-yfi-s-zatt-fossiiifcrous-unstratificd-rrx-ks-unstratified-rocks-primary-fosailif-crous-s-protozoic-rocks-fis4-gt-ftltrs-r-r-quot-s-coal-mtasures-samp5t-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-rese-RM3BK1.jpg ". Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. %. /. Ten, a ar> Jo^itiferous Strata "-yfi-^s ZatT -fossiiifcrous, unstratificd rrx-ks. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly rese Stock Photo")
. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. %. /. Ten, a ar> Jo^itiferous Strata "-yfi-^s ZatT -fossiiifcrous, unstratificd rrx-ks. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly rese Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-board-of-regents-of-the-smithsonian-institution-smithsonian-institution-smithsonian-institution-archives-discoveries-in-science-ten-a-argt-joitiferous-strata-quot-yfi-s-zatt-fossiiifcrous-unstratificd-rrx-ks-unstratified-rocks-primary-fosailif-crous-s-protozoic-rocks-fis4-gt-ftltrs-r-r-quot-s-coal-mtasures-samp5t-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-rese-image236102917.htmlRMRM3BK1–. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. %. /. Ten, a ar> Jo^itiferous Strata "-yfi-^s ZatT -fossiiifcrous, unstratificd rrx-ks. Unstratified rocks Primary fosailif crous S -Protozoic Rocks Fis.4. '•> f*$T^<'rS***^— — ——r- r ' " s Coal MtasureS ^^^^S&5^^^t. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly rese
. Bergens Museums aarbok. 14 Oscar Sund. [Nr. 6 shrimps of the Atlantic, for instance, Acanthephyra, living in depths below 500 metres, owing to the greater intensity of light in the lipper water-layers compared with that in more northern seas.1). Fig. 8. Pasiphæa tarda, Krøyer, from the Skagerrack. C = 32 Telson, scapho- cerite, mandible, Ist and 2nd maxillae and Ist maxilliped. The numhers denote the enlargement of the original camera drawings. The hlock is rednced in the ratio 6r/ns- On the edge of the Ist max.p. is seen a duster of protozoic para- sites, which are very comnionly met with i Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bergens-museums-aarbok-14-oscar-sund-nr-6-shrimps-of-the-atlantic-for-instance-acanthephyra-living-in-depths-below-500-metres-owing-to-the-greater-intensity-of-light-in-the-lipper-water-layers-compared-with-that-in-more-northern-seas1-fig-8-pasipha-tarda-kryer-from-the-skagerrack-c-=-32-telson-scapho-cerite-mandible-ist-and-2nd-maxillae-and-ist-maxilliped-the-numhers-denote-the-enlargement-of-the-original-camera-drawings-the-hlock-is-rednced-in-the-ratio-6rns-on-the-edge-of-the-ist-maxp-is-seen-a-duster-of-protozoic-para-sites-which-are-very-comnionly-met-with-i-image234741939.htmlRMRHWBMK–. Bergens Museums aarbok. 14 Oscar Sund. [Nr. 6 shrimps of the Atlantic, for instance, Acanthephyra, living in depths below 500 metres, owing to the greater intensity of light in the lipper water-layers compared with that in more northern seas.1). Fig. 8. Pasiphæa tarda, Krøyer, from the Skagerrack. C = 32 Telson, scapho- cerite, mandible, Ist and 2nd maxillae and Ist maxilliped. The numhers denote the enlargement of the original camera drawings. The hlock is rednced in the ratio 6r/ns- On the edge of the Ist max.p. is seen a duster of protozoic para- sites, which are very comnionly met with i
