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  • Blackwell Publishing Ltd  (1,571)
  • Annual Reviews
  • PANGAEA
  • 2005-2009
  • 1990-1994
  • 1980-1984
  • 1965-1969  (1,988)
  • 1966  (1,988)
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  • 2005-2009
  • 1990-1994
  • 1980-1984
  • 1965-1969  (1,988)
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  • 1
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    PANGAEA
    In:  EPIC3Kwartalnik geologiczny Wydawn, Geologiczne Warszawa, Bremerhaven, PANGAEA, 10(2), pp. 453-461
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 2
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 5
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 6
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    PANGAEA
    In:  EPIC3Deutsches Hydrographisches Institut, Hamburg, Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 7
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    PANGAEA
    In:  EPIC3Kwartalnik geologiczny Wydawn, Geologiczne Warszawa, Bremerhaven, PANGAEA, 10(2), pp. 442-452
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 8
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    PANGAEA
    In:  Supplement to: Sigal, Jacques; Truillet, René (1966): Étude micropaléontologique et illustration des filons-couches granoclassés du Capo Sant'Andrea (Sicile). Bulletin de la Societe Geologique de France, 7, 986-993, hdl:10013/epic.46163.d001
    Publication Date: 2023-08-28
    Description: In the region near Taormina, Sicily, the Mesozoic sedimentary veins which contain fillings have various ages ranging from Dogger-Malm until Paleocene-Ypresian. One can observe the development of graded sills parallel to the dip of the banking, formed by the superposition of limestone sequences with Globigerina, Gümbelines and Globotruncana. This study describes and illustrates these graded sills and the embedded fossil manganese nodules they contain.
    Keywords: Aluminium; Calcium; Capo Sant'Andrea, Sicilia; DEPTH, sediment/rock; HAM; Hammer; Iron; Magnesium; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Sample ID; SIGT01; Titanium; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 9
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1966): ZETES Expedition, March - August 1966, List of cores and dredge hauls copied from shipboard logs. Scripps Institution of Oceanography, UC San Diego, unpublished, 9 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/zetes/zetes_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described are taken during the R/V Argo ZETES Expedition from March until August 1966 by the Scripps Institute of Oceanography. A total of 53 cores and dredges were recovered and are available at Scripps Institute of Oceanography for sampling and study.
    Keywords: Argo; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image; ZETES; ZTES03AR; ZTES03AR-001D; ZTES03AR-002D; ZTES03AR-003D; ZTES04AR; ZTES04AR-005D; ZTES04AR-008D; ZTES05AR; ZTES06AR; ZTES06AR-027G-A; ZTES07AR; ZTES-10G; ZTES-11G; ZTES-12G; ZTES-13G; ZTES-15G; ZTES-16G; ZTES-18G; ZTES-1D; ZTES-21G; ZTES-23G; ZTES-27G-A; ZTES-28G; ZTES-2D; ZTES-31G; ZTES-38G; ZTES-3D; ZTES-5D; ZTES-5G; ZTES-6G; ZTES-8D
    Type: Dataset
    Format: text/tab-separated-values, 292 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Heezen, Bruce C; Glass, Bill; Menard, H William (1966): The Manihiki Plateau. Deep Sea Research and Oceanographic Abstracts, 13(3), 445-458, https://doi.org/10.1016/0011-7471(66)91079-5
    Publication Date: 2023-08-28
    Description: The Manihiki Plateau, a 600,000 km2 smooth and nearly flat-topped feature, lies in the west equatorial Pacific. Danger, Nassau, Suvorov and Manihiki Islands rise from the southern part of the plateau. Oceanic depths of about 5500 m surround the 2400-3000 m summit area. The top of the plateau is capped by approximately one kilometer of sediment. The sediment cores to the east and west of the plateau contain red clay but the top of the plateau is covered with foraminiferal ooze. Mineral grains and rock fragments in cores and dredge hauls from the east escarpment indicate that basic igneous rocks underlie a ridge that forms the eastern edge of the plateau north of 13°S. Bottom photographs and dredge hauls below 3000 m on the east scarp of the plateau and in the abyssal hills to the east reveal abundant manganese nodules. Most of the botton photographs show evidence of deep-sea currents. The plateau's shape is apparently controlled by faulting although much evidence of basic vulcanism is present in the cores. The occurrence of Cretaceous fossils on the eastern ridge of the plateau indicates that the bevelling of the plateau must have occurred during or before Cretaceous time. Twenty cores, two dredge hauls, four bottom trawls and fifteen camera stations from the Vema cruise 18.
    Keywords: CAME; Camera; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; File name; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; V18; V18-024RD; V18-025RD; V18-115SBT; V18-116SBT; V18-197C; V18-199C; V18-200C; V18-201C; V18-202C; V18-204C; V18-205C; V18-206C; V18-207C; V18-209C; V18-258; V18-263; V18-266; V18-267; V18-268; V18-269; V18-270; V18-273; V18-274; V18-275; V18-276; V18-277; V18-278; V18-279; V18-280; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 728 data points
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  • 11
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    PANGAEA
    In:  Supplement to: Feden, Robert H (1966): Volcanic rock from Caryn Seamount. Journal of Geophysical Research, 71(6), 1761-1763, https://doi.org/10.1029/JZ071i006p01761
    Publication Date: 2023-08-28
    Description: Caryn seamount (36° 42'N, 68° 02'W) was discovered in 1948 during Caryn cruise 1. During the summer of 1963 the Chain (cruise 36) occupied a dredge station on Caryn seamount. Caryn seamount (36° 42'N, 68° 02'W) was discovered in 1948 during Caryn cruise 1. During the summer of 1963 the Chain (cruise 36) occupied a dredge station on Caryn seamount. Manganese nodules, semiconsolidated mud, altered vesicular volcanics, and several glacial erratics were obtained from the western slope of the seamount between depths of about 3950 and 4300 m. The 1963 dredge haul by Chain, the first to obtain volcanic rocks, confirms the volcanic origin of the seamount. Previously, only manganese nodules had been dredged from Caryn, during cruise 21 of Chain.
    Keywords: Atlantic Ocean; CH03601; CH36-11PG; CH36-1PG; CH36-2PC; CH36-6RD; CH36-9PG; Chain; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 12
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    PANGAEA
    In:  Supplement to: Sackett, William M (1966): Manganese Nodules: Thorium-230: Protactinium-231 Ratios. Science, 154(3749), 646-647, https://doi.org/10.1126/science.154.3749.646
    Publication Date: 2023-08-28
    Description: The Th230/Pa231 activity ratio in 7 of 11 manganese nodules is less than 10.8, the theoretical production ratio of activities in the ocean. This finding indicates difierential accumulation of these nuclides in authigenic deposits of manganese-iron oxide.
    Keywords: A-266/D-40; Alpha spectrometry; AT26601; AT266-40; Atlantic Ocean; Atlantis (1931); Blake Plateau, Atlantic Ocean; CH03601; CH36-6RD; Chain; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWBD1; DWBD4; DWHD47; Event label; FANB01BD; FANBD-20D; FANFARE-B; GOS74; GOS74-2340; Gosnold; Horizon; Identification; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MIDPAC; MPC-25F-2; MPC-26A-3; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Protactinium-231; Protactinium-231, standard deviation; RC05; RC05-1RD; Robert Conrad; Sample code/label; Spencer F. Baird; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation; V18; V18-32RD; Vema
    Type: Dataset
    Format: text/tab-separated-values, 124 data points
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  • 13
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    PANGAEA
    In:  Supplement to: Jones, E J W; Laughton, Anthony S; Hill, M N; Davies, D (1976): A geophysical study of part of the western boundary of the Madeira-Cape Verde Abyssal plain. Deep Sea Research and Oceanographic Abstracts, 13(5), 889-907, https://doi.org/10.1016/0011-7471(76)90909-8
    Publication Date: 2023-08-28
    Description: The results are discussed of a geophysical survey undertaken by R.R.S. Discovery II early in 1962 in an area centred on 29° 15'N, 25° 5'W at the western extremity of the Madeira-Cape Verde Abyssal Plain. Seismic investigations show that the sediments are underlain by an intermediate layer about 2 km in thickness of velocity 4.1-5.4 km/sec which overlies a deep layer 5.2-km thick of velocity 6.3-6.8 km/sec. Refracted arrivals on the longest seismic line give a depth of 13.2 km to the M discontinuity. Magnetic results indicate that the topography of the abyssal hills in the western part of the area is probably continued eastwards as sub-bottom relief beneath the sediments of the abyssal plain. They also support the hypothesis that the intermediate seismic layer (layer 2) is composed predominantly of volcanic rocks. Examination of a well-defined magnetic anomaly over one topographic feature ("The Madcap Volcano") shows it to be composed of magnetized rocks (I = 8.4 × 10**-3 e.m.u./cm**3) having a direction of magnetization which points upwards at 25° with an azimuth of 305°. Measurements at ten heat flow stations show that the average geothermal flux in this region is 1.20 (±0.11) µcal/cm**2/sec.
    Keywords: Atlantic Ocean; D4810; D4814; Deposit type; DEPTH, sediment/rock; Description; Discovery II (1929); Event label; File name; Identification; MADCAP_62; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 14
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    PANGAEA
    In:  Supplement to: Hill, M N; Laughton, Anthony S (1966): RRS DISCOVERY Cruise 4 Report, Feb.-March 1965, Geology and geophysics in the N.E. Atlantic. Cruise Report Series, CR-11, 31 pp, https://store.pangaea.de/Projects/NOAA-MMS/RRSDiscovery_Cruise4_1965.pdf
    Publication Date: 2023-08-28
    Description: A total of 36 coring stations were worked during the cruise of which twenty-five were successful. Both piston and free-fall gravity coring techniques were employed and the cores were extruded and rough logged on board ship as soon as they had been taken. Twelve dredge stations were occupied on the cruise, all of them lying in the Peake Deep area, and nine were successful.
    Keywords: Atlantic Ocean; D4; D5607; D5608; D5619; D5627; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 15
    Publication Date: 2023-08-28
    Description: Manganese nodules recovered in the Pacific Ocean by the U. S. Bureau of Mines and by DeepSea Ventures Ltd. are studied for their chemical composition using X microprobe and X-ray fluorescence methods.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 16
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Date/Time of event; DEPTH, sediment/rock; Description; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Loss on ignition; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Organic matter; Phosphorus pentoxide; Sample ID; Water in rock; Wet chemistry; WNT-A7; WNT-CIII; WNT-S3
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 17
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Core; CORE; Date/Time of event; DEPTH, sediment/rock; Description; DIVER; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Insoluble residue; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Sampling by diver; Wet chemistry; WNT-11A; WNT-12A; WNT-15A; WNT-24; WNT-28B; WNT-2A; WNT-3; WNT-36; WNT-4; WNT-5; WNT-6; WNT-A11; WNT-A18; WNT-A19; WNT-A23; WNT-A3; WNT-A31; WNT-A7; WNT-CIII; WNT-CIV-A; WNT-CIV-B; WNT-F12A; WNT-F23-C; WNT-F58A; WNT-N1; WNT-N2; WNT-N3; WNT-N4; WNT-P20; WNT-P7A; WNT-P9; WNT-R/62; WNT-R6A; WNT-S3; WNT-S4; WNT-Z705
    Type: Dataset
    Format: text/tab-separated-values, 235 data points
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  • 18
    Publication Date: 2023-08-28
    Keywords: Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; HRS1; Iron; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Shape; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 19
    Publication Date: 2023-08-28
    Keywords: 2P-36; Antimony; Barium; Calcium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Europium; Event label; Hafnium; HRS1; Iron; Lanthanum; Latitude of event; Longitude of event; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63; Samarium; Sample ID; Scandium; Shape; Sodium; Terbium; Thorium; Titanium; Uranium; Vanadium; X-ray microprobe; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 20
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    PANGAEA
    In:  Supplement to: Winterhalter, Boris (1966): Pohjanlahden ja Suomenlahden rauta-mangaani-saostumista. Summary: Iron-manganese concretions from the gulf of Bothnia and the gulf of Finland. Geoteknillisiä julkaisuja - Geotekniska meddelanden - Geotechnical publications, 69, 77 pp, https://tupa.gtk.fi/julkaisu/geoteknillinen/gt_s_069.pdf
    Publication Date: 2023-08-28
    Description: Iron-manganese concretions, closely related to lacustrine ores and deep sea manganese nodules, are presently forming in different parts of Gulfs of Bothnia and Finland. They can be divided according to physical form into three distinct groups: (1) round pea-shaped concretions, (2) ring-shaped concrections, and (3) flat sheets and crusts of concretionary material. A definite correlation was found to exist between the form i.e. type of concretions and their chemical composition (Mn/Fe ratio). Trace element concentrations were generally rather high, although not as high as in deep sea manganese nodules. X-ray and DTA was used to study the mineralogy and crystal structure of the concretions. Surface concentrations and geographical distribution of the concretions were estimated on the basis of samples, diving observations and echo-grams.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
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    Format: application/zip, 4 datasets
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  • 21
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    PANGAEA
    In:  Supplement to: Burns, Roger G; Fuerstenau, D W (1966): Electron-probe determination of inter-element relationships in manganese nodules. American Mineralogist, 51, 895-902, http://www.minsocam.org/ammin/AM51/AM51_895.pdf
    Publication Date: 2023-08-28
    Description: Manganese nodules have attracted considerable attention in recent years as a potential source of Mn, Fe, Co, Ni, Cu and other minor elements. These elements are enriched in manganese nodules relative to igneous rocks, sea-water, and deep-sea clays. The present paper describes methods by which element correlations may be determined with the electron-probe, and summarizes the results obtained by electron-beam scanning and specimen traversing. The results obtained in the present electron-probe investigation of manganese nodules may be summarized as follows: (l) The iron concentration fluctuates whereas the manganese concentration is relatively uniform throughout a manganese nodule, hbing slightly higher where iron is low. (2) There is a distinct correlation between Fe, Co, Ti, and Ca. (3) There is pronounced element coherence between Xi, Cu, Zn, and Mg, and between K and Ba. These elements are enriched with Mn and Al in regions of a nodule where the iron concentration is low. (4) The pronounced inter element relationships suggest that isomorphic substitution is an important factor controlling minor element distribution in manganese nodules. The ions Ni2+. Cu2+, Zn2+, Mg2+, K+ and Ba2+ substitute for Mn2+ in the "manganite" phases, Co(III) occurs with Fe(III) in hydrated iron oxide phases and Ti(IV) in delta-MnO2.
    Keywords: Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD16; Electron Probe Microanalysis (EPMA); Horizon; Iron; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Sample ID; Silicon; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 22
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    PANGAEA
    In:  National Institute of Oceanography, Wormely | Supplement to: National Institute of Oceanography, Wormley (1966): Discovery Cruise 11 Report, April-May 1966, Geology and geophysics in the N.E. Atlantic. National Institute of Oceanography, Wormley, Godalming, Surrey (hdl:10013/epic.47825.d003 pdf 634 kB), 16 pp, https://www.bodc.ac.uk/resources/inventories/cruise_inventory/reports/d11.pdf
    Publication Date: 2023-08-28
    Description: During Discovery Cruise 11, April-May 1966, eleven hauls were made on the crest and on the southern facing slope of Palmer Ridge in the Peake Deep area in order to fill out the information gained last year. Limestones were collected ranging in age from lowest Eocene through to Upper Tertiary, and several hauls successfully sampled the basement beneath these, producing weathered basalts, metamorphosed basalts and dolerites. In Peake Deep on the north slope of Palmer Ridge hard Eocene sediments were core sampled near the base of the slope but no cores could be got near the top.
    Keywords: Atlantic Ocean; D11; D5975; D5978; D5983; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 23
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1966): TRIPOD Expedition, November-December 1966, List of sediment cores and dredge hawls, R/V Argo. Scripps Institution of Oceanography, UC San Diego, unpublished, 7 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/tripod/tripod_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on the TRIPOD Expedition from November until December 1966 by the Scripps Institution of Oceanography from the R/V Argo. A total of 38 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Argo; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; East Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TRI-01D; TRI-02D; TRI-02PG; TRI-03D; TRI-04D; TRI-04P; TRI-05D; TRI-06D; TRI-06P; TRI-06PG; TRI-07G; TRI-07P; TRI-08G; TRI-08P; TRI-08PG; TRI-09D; TRI-09G; TRI-09P; TRI-09PG; TRI-10G; TRI-13G; TRI-14G; TRIP02AR; TRIP03AR; TRIPOD_2; TRIPOD_3; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 301 data points
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  • 24
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Chromium; Cobalt; Copper; Date/Time of event; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Lead; Longitude of event; Manganese oxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Spectrometric analysis; Strontium; Vanadium; WNT-2A; WNT-5; WNT-6; WNT-A31; WNT-A7; WNT-CIV-A; WNT-CIV-B; WNT-F12A; WNT-F23-C; WNT-F58A; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 130 data points
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  • 25
    Publication Date: 2023-08-28
    Keywords: Baltic Sea; Comment; Core; CORE; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DIVER; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sampling by diver; Sediment type; Shape; Size; Substrate type; Uniform resource locator/link to image; WNT-11A; WNT-12A; WNT-14/61; WNT-14RR4; WNT-15A; WNT-17/61; WNT-19/61; WNT-23/61; WNT-24; WNT-28B; WNT-2A; WNT-3; WNT-36; WNT-4; WNT-4/61; WNT-5; WNT-6; WNT-8; WNT-9/61; WNT-A10; WNT-A11; WNT-A12; WNT-A18; WNT-A19; WNT-A22; WNT-A23; WNT-A24B; WNT-A3; WNT-A31; WNT-A5; WNT-A6; WNT-A7; WNT-A8; WNT-A9; WNT-B5A; WNT-B6; WNT-BII; WNT-BIII; WNT-BIV; WNT-BV; WNT-BVI; WNT-CI; WNT-CIII; WNT-CIV-A; WNT-CIV-B; WNT-CV; WNT-F10; WNT-F10A; WNT-F12A; WNT-F19A; WNT-F23-B; WNT-F23-C; WNT-F23E; WNT-F58A; WNT-L100; WNT-L103; WNT-L110; WNT-L115; WNT-L154; WNT-L162; WNT-L19; WNT-L22; WNT-L24; WNT-L32; WNT-L34; WNT-L36; WNT-L37; WNT-L65-A; WNT-L65-B; WNT-L67; WNT-L68; WNT-L70; WNT-L71; WNT-L73; WNT-L83; WNT-L89; WNT-L91; WNT-L92; WNT-L95; WNT-N1; WNT-N2; WNT-N3; WNT-N4; WNT-P20; WNT-P4; WNT-P7A; WNT-P9; WNT-R/62; WNT-R6A; WNT-S2; WNT-S3; WNT-S4; WNT-To3; WNT-Z705
    Type: Dataset
    Format: text/tab-separated-values, 888 data points
    Location Call Number Expected Availability
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  • 26
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Dietrich, Günter; Düing, Walter; Grasshoff, Klaus; Koske, Peter H (1966): Physikalische und chemische Daten nach Beobachtungen des Forschungsschiffes Meteor im Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A2, 1-155
    Publication Date: 2024-02-03
    Description: The present volume gives the observed physical and chemical data obtained by R.V. "Meteor" in the Indian Ocean during cruise 1964/65. The tables are based on the computations made by the National Oceanographic Data Center (NODC) in Washington. In addition to the normally communicated data, the tables contain four chemical parameters: alkalinity, ammonia, fluoride, and calcium.
    Keywords: Biscaya; CTD/Rosette; CTD-RO; Eastern Arabian Sea; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_001; M1_005; M1_006; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD001; M1_CTD005; M1_CTD006; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Mediterranean Sea; Meteor (1964); Red Sea; Western Arabian Sea
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 27
    Publication Date: 2024-02-03
    Keywords: Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_005; M1_006; M1_CTD005; M1_CTD006; Mediterranean Sea; Meteor (1964); Nitrate; Oxygen; Oxygen, microelectrode, ex-situ; Phosphate; Salinity; Silicate; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
    Location Call Number Expected Availability
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  • 28
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; Calcium; Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Eastern Arabian Sea; Elevation of event; Event label; Fluoride; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Meteor (1964); Nitrate; Nitrite; Oxygen; Oxygen, microelectrode, ex-situ; pH; Phosphate; Phosphorus, total; Red Sea; Salinity; Silicate; Temperature, water; Turnover-thermometer; Western Arabian Sea
    Type: Dataset
    Format: text/tab-separated-values, 38537 data points
    Location Call Number Expected Availability
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  • 29
    Publication Date: 2024-02-03
    Keywords: Biscaya; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_001; M1_CTD001; Meteor (1964); Oxygen; Oxygen, microelectrode, ex-situ; Salinity; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 176 data points
    Location Call Number Expected Availability
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  • 30
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bonatti, Enrico; Joensuu, Oiva (1966): Deep-Sea Iron Deposit from the South Pacific. Science, 154(3749), 643-645, https://doi.org/10.1126/science.154.3749.643
    Publication Date: 2024-04-20
    Description: Along with specimens of manganese oxides and basalt, rocks containing more than 30 percent iron by weight and consisting mainly of poorly crystallized goethite have been dredged from the flanks of a seamount located on the East Pacific Rise. The Fe-Mn ratio varies widely among the various oxide rocks deposited at this locality and at another seamount in the same area. The deposit was probably formed by fractional precipitation of iron and manganese which had been introduced locally into the bottom water by hydrothermal solutions of volcanic origin, and by leaching from deep-sea basaltic lavas.
    Keywords: Aluminium oxide; AMPH-002D; AMPH01AR; AMPH01AR-002D; AMPHITRITE; Argo; Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Iron; Loss on drying; Magnesium oxide; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Potassium oxide; Sample ID; Silicon dioxide; Strontium
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
    Location Call Number Expected Availability
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  • 31
    facet.materialart.
    Unknown
    PANGAEA
    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2024-05-02
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; RC10; RC10-003RD; RC10-101; RC10-101C1; RC10-101C3; RC10-103C1; RC10-104C4; RC10-11; RC10-110; RC10-123; RC10-123C4; RC10-13; RC10-131; RC10-153; RC10-154; RC10-164; RC10-165; RC10-168; RC10-171; RC10-172; RC10-176; RC10-178; RC10-179; RC10-182; RC10-205; RC10-21C2; RC10-21C3; RC10-233; RC10-239; RC10-244; RC10-26C6; RC10-26C7; RC10-274; RC10-278; RC10-279; RC10-36C1; RC10-36C2; RC10-40C2; RC10-40C4; RC10-41C1; RC10-41C2; RC10-41C4; RC10-44C2; RC10-45C3; RC10-49C2; RC10-49C3; RC10-69C2; RC10-70C1; RC10-76; RC10-77; RC10-78; RC10-79; RC10-7C2; RC10-7C6; RC10-81; RC10-87C7; RC10-88; RC10-8C1; RC10-8C2; RC10-91; RC10-93; RC10-96C2; RC10-96C4; RC10-97C1; RC10-97C4; RC10-97C5; RC10-98C1; RC10-98C3; RC10-98C4; RC10-99C2; Robert Conrad; Sediment type; Size; Substrate type; Uniform resource locator/link to file; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1142 data points
    Location Call Number Expected Availability
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  • 32
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Cordes, Eilhard (1966): Aufbau und Bildungsbedingungen der Schwermineralseifen bei Skagen (Dänemark). Meyniana, 16, 1-35, https://doi.org/10.2312/meyniana.1966.16.1
    Publication Date: 2024-04-19
    Description: Aufbau und Ausdehnung der Schwermineral-Anreicherungen (Ilmenit, Granat, Amphibol) am Strand südlich Skagens wurden in langen Schürfgräben untersucht. Die Seifenlagen ziehen durchgehend vom Kliff-Fuß bis zur mittleren Meereshöhe hin und liegen meist diskordant auf der alten Strandschichtung. Ihre strandparallele Ausdehnung beträgt bis zu 100 m. Aufgebaut werden sie aus dünnen Schwermineral-Lamellen, die in kleinerem Umfang überall in den Strandablagerungen zu finden sind und hier das Gefüge nachzeichnen (Rippeln, Strandwallschichtung, Schichtstörungen). Die Seifenbildung geht in einem Gebiet mit verstärktem Küstenabtrag vor sich (Lee-Erosion südlich der Hafenmolen von Skagen). Dieses deutet darauf hin, daß die Schwerminerale bei Aufarbeitung bereits vorhandener Sedimente infolge ihres unterschiedlichen hydraulischen Verhaltens Zurückbleiben und schließlich angereichert werden. Die Korngrößenverteilung der Minerale in verschiedenen Sedimentproben zeigen, daß mit steigender Schwermineral-Anreicherung eine Kornverfeinerung und Zunahme der spezifisch schwersten Minerale (opake Erzminerale und Zirkon) auftritt. In ähnlicher Weise werden die Sortierungswerte besser. Die Aufbereitung des Sedimentes wird, in Anlehnung an v. ENGELHARDT (1939), mit einem doppelten Sortierungsvorgang durch die Wasserbewegung am Strand erklärt. Beim Absinken des Sandes nach dem Brecherschwall tritt eine Vorsortierung ein, die den Abtransport der leichteren und größeren Minerale im Sog begünstigt. Verbindungen zu Vorstellungen der Aufbereitungstechnik (Rundherdverfahren) und Hydrodynamik ('laminare Unterschicht') werden hergestellt. Die Dünensande Skagens sind infolge ihres hohen Schwermineralgehaltes und günstiger Äquivalentgrößen der einzelnen Minerale besonders bedeutsam für die Seifenbildung am Strand.
    Keywords: Europe, Denmark; HAND; Sampling by hand; Skagen1964
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 33
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Distance; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Opaque minerals; Sample ID; Sampling by hand; Skagen1964
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
    Location Call Number Expected Availability
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  • 34
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Epidote; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Minerals, other; Opaque minerals; Sample ID; Sampling by hand; Skagen1964; Sorting; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 300 data points
    Location Call Number Expected Availability
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  • 35
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
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  • 36
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
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  • 37
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
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  • 38
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: The paper traces the history of the Wild series of rectifiers, paying particular attention to the mechanical solutions of the Newton and Scheimpflug conditions.
    Type of Medium: Electronic Resource
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  • 39
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
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  • 40
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: The author explains one of the chief problems, the composition of a survey aircraft navigation system, facing Commission I of the International Society for Photogrammetry. The tasks to be accomplished by such a system are outlined, and some of the alternative equipment available to carry out the various aspects of this work are discussed.
    Type of Medium: Electronic Resource
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  • 41
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: It is well known that there exists a “danger cylinder” for space resection, analogous to the “danger circle” in the plane, on which the resection is unstable. This paper shows how the existence of this surface may be detected and draws attention to the way in which the instability differs from that in the plane.
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  • 42
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: An attempt is made to review the factors affecting the use of colour photography in photogrammetry and photo-interpretation. Examples of current practice and results of comparative tests are quoted, as well as the advantages and deficiencies of the various materials available.
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  • 43
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: During the summer of 1965, colour, false colour, infra-red and panchromatic photography was flown of the Breidamerkur Glacier area in south-east Iceland. Subsequent comparative interpretation studies of the film types have indicated that colour photography is superior for the interpretation of glacierized† areas. This is attributed to brightness qualities and a continuous colour tone range, which, in this instance, closely matched visual representation of ground objects.The false colour film, due to the striking tonal qualities of vegetation and moisture, is considered best for studies involving the delimitation of these features. Panchromatic film appears to be satisfactory for general interpretation work, particularly where the utmost in definition is called for. The infra-red film, because of the dark tones produced by gravels and the subsequent high contrasts between ice and gravel debris on the ice surface, is considered a poor choice for the interpretation of glacierized areas.
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  • 44
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
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  • 45
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
    Notes: This paper gives convenient formulae for numerical relative orientation for use with instruments in which the Y-parallax may be accurately measured.
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  • 46
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    The @photogrammetric record 5 (1966), S. 0 
    ISSN: 1477-9730
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying
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  • 47
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. In cultures of Trypanosoma conorhini the authors have detected “cyst-like bodies” (CLBs) that, in the initial phase, have the appearance of 2 or more overgrown crithidiae fused together; after disorganization of the internal structure of the parent flagellates and division of their organelles, new crithidiae are formed within the CLB. The wall of the CLB consists of an irregularly thick layer of cytoplasm surrounded by the periplast of the parent flagellates and a true cystic membrane is not evident. The daughter crithidiae eventually escape from the CLB leaving the periplast and other residues of the parent flagellates. It is suggested that this represents a method of reproduction entirely different from binary or multiple fission, that is probably common to other trypanosomes of the Section STERCORARIA, and that it may provide for genetic exchange even if it is not a true sexual process.
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  • 48
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. During conjugation of Kahlia the micronuclei divide 3 times before synkaryon formation and 2 times thereafter. The 1st division is heterotypic, as in other ciliates, in that it is characterized by the parachute stage. Following this stage, 24 to 26 bivalents and 4 to 8 univalents appear in the micronuclear area. When the bivalents move to organize the metaphase plate, the univalents lag behind and fail to reach the equatorial region at the same time. Due to this irregular behavior of the univalents there is no distinct metaphase in the first meiotic division. A few meiotic irregularities including the breakdown of the spindle apparatus have been observed. During the breakdown of the spindle apparatus the chromosomes fuse into irregular bodies which resemble the chromosome aggregates observed during the somatic divisions. Generally 1, and rarely more, of the products of the 1st division enter the 2nd division. The spindles of this division are oriented parallel to the long axis of the cell, and 1 of the daughter nuclei reaches the partition membrane separating the conjugants. This nucleus alone undergoes the 3rd division, resulting in the formation of gametic nuclei. Reciprocal exchange and fusion of the gametic nuclei result in the synkaryon formation. The synkaryon divides twice in rapid succession resulting in 4 daughter nuclei; 1 of them degenerates and 2 condense and become functional micronuclei. The chromosomes of the remaining daughter nucleus resemble in size and number the bivalents of the 1st meiotic division. They become polytenic and then reproduce to give rise to the polyploid macronucleus. The development of the macronucleus has been traced from a single diploid set of chromosomes and no evidence has been found for the formation of genetic “subnuclei.” During the early stages of the development of the macronuclear anlage, somatic pairing forces keep the homologs together, while in the later stages these forces cease to exert influence. While these changes are in progress the old macronucleus; breaks up into small irregular polymorphic bodies which are scattered throughout in the cytoplasm. The exconjugants usually encyst and the cysts are not favorable for detailed cytologic study.
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  • 49
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. In young first generation schizonts of E. bovis, the nuclei appeared to have a random distribution. In calves killed 8 days after inoculation some of the schizonts had the nuclei arranged in a single layer at the periphery, with a few infoldings of this layer into the interior. In further development, such ingrowths of the nuclear layer resulted in the formation of compartments of varying size. In schizonts of calves killed 12 days after inoculation spherical or ellipsoidal bodies (blastophores), about 5–20 μ in diameter with a single peripheral layer of nuclei were formed. Merozoites developed as radial outgrowths from the blastophores, leaving residual bodies of variable size, which later disappeared. The response of the host cell to the presence of the schizont was characterized by marked growth of both the nucleus and cytoplasm. The nucleolus became greatly enlarged, and the chromatin was distributed in relatively fine granules. In the host cell cytoplasm, 2 concentric layers were observed; the inner was more dense than the outer. After growth of the schizont was completed its host cell was stretched into a thin covering layer about 1 μ thick. In some schizonts, the host cell disintegrated, and the schizont was then invaded by eosinophils, macrophages and other cells, which eventually destroyed the merozoites.
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  • 50
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Blood smears from 133 Rio Grande wild turkeys Meleagridis gallopavo intermedia live-trapped in the Welder Wildlife Refuge in south Texas, were examined for blood parasites. All of the 63 immature turkeys and 63% of the 70 adult turkeys were infected with Haemoproteus meleagridis. The infections were light, half the cases having less than 5 infected cells per 10,000 red blood cells. Infection with H. meleagridis caused significant enlargement of the host RBC. Other parasites specifically searched for but not found were Leucocytozoon, Trypanosoma, Plasmodium and microfilariae.
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  • 51
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
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    Topics: Biology
    Notes: SYNOPSIS. The fine structure of the tomite stage of Hyalophysa chattoni was examined with particular attention to its kinetal apparatus.The pellicle, thick and dense compared with that of other ciliates, is formed of three layers. The inner layer is composed of short fibrils oriented perpendicular to the surface.The cytoplasm around the oral passage and beneath falciform field 8 is crowded with dense inclusion bodies of unknown function. Dorsal to the oral passage is the rosette, a disc-shaped organelle subdivided by septa in the form of incomplete radii about a central chamber containing a tuft of cilia. The septa are composed of 3 membranes enclosing a fine layer of cytoplasm. At their inner ends 20 mμ fibers run dorsally and ventrally. Dense clumps of fibrous material line the luminal surface of the septa.Rows of fusiform trichocysts parallel the kineties. The trichocysts are composed of a finely periodic, moderately electron-dense material surrounded by 20 mμ fibrils oriented along the long axis of the trichocyst. Between and below the kinetosomes and the rows of trichocysts are electron-dense vesicles 300 mμ in diameter and bounded by a loose membrane. The large “trichocysts,” the “gros trichocystes” of Chatton and Lwoff, whose appearance heralds the beginnings of trichocystogenesis, prove to be canaliculi opening to the surface.Four separate ciliary membrane systems—the oral ciliature (XYZ), falciform field 8, falciform field 9, and the ogival field—are located on the ventral surface of the tomite. Each differs from the others and from the somatic kineties in the fibrillar organization around its kinetosomes.In the somatic kineties the kinetodesmos is a dense, periodic fiber which is formed of stacks of up to 18 subfibers, each arising from the base of a kinetosome. The kinetosomes are short (300 mμ) and contain dense central granules. In some kineties, alternating between the kinetosomes, are elliptical kinetosome-like structures which do not bear cilia and perhaps provide a reservoir of kinetosomes for future growth of the kinety.
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  • 52
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    Topics: Biology
    Notes: SYNOPSIS. The life cycle of the true slime mold Physarum polycephalum includes 2 vegetative stages: the multinucleate coenocytic plasmodium and the uninucleate amoeba. A clone of amoebae established from a single spore does not normally yield plasmodia. Plasmodia are formed when amoebae from particular clones are mixed; thus plasmodium formation is said to be controlled by a ‘mating-type’ system.Previous work by the author with a sample of P. polycephalum derived from a single source revealed that 2 mating types were present and were determined by a pair of alleles at 1 locus. The present paper reveals the presence of 2 more mating types in a sample of P. polycephalum derived from a different source and provides evidence that these are determined by 2 alleles at the same locus as the other 2.Evidence for the presence of other inherited factors affecting plasmodium formation, the mode of action of these factors and possible explanations for the occurrence of plasmodia in single-spore cultures are also discussed.
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  • 53
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    Topics: Biology
    Notes: SYNOPSIS. Transection and regeneration of Blepharisma intermedium initiate complex macronuclear activity and micronuclear division. Reversible condensation of the macronucleus is achieved by contraction which involves primary and secondary coiling. Primary coiling, evident in vegetative cells, is enhanced by pronounced constriction of the macronuclear extremities during regeneration. Secondary coiling is restricted to the period of contraction and is initiated at the ends of the mauonucleus. Condensation terminates the coiling processes and gives rise to an amorphous structure. Re-elongation of the macronucleus is not followed immediately by coiling. Micronuclear division begins early in regeneration, but the peak of visible activity is not reached until the 3rd through 5th hours.
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  • 54
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    Topics: Biology
    Notes: SYNOPSIS. Lipids in aging cultures of Tetrakymena pyriformis were extracted at various times after inoculation, purified, and weighed or chromatographed on thin layers of silica gel. The total cellular lipid increased throughout logarithmic and early stationary phases but decreased sharply after 72 hr. The amount of one lipid class, probably the triglycerides, followed the same trends. It may be a cellular reserve.
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  • 55
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    Topics: Biology
    Notes: SYNOPSIS. Rearing of cockroaches without sporozoan parasites of the Malpighian tubules permitted the 1st experimental infections reported for these organisms as well as study of the intracellular early stages of infection. Infectivity tests show that the route of invasion is peroral rather than transovarian; that fresh spores obtained from either the Malpighian tubules or the hindgut are infective; that fresh spores held in aqueous suspension for 36 hr are not infective; that all ages and both sexes of cockroaches are susceptible, although older cockroaches are more readily infected experimentally; that a single peroral dose of a few hundred spores is sufficient to produce infection; that the earliest signs of progressive infection in the Malpighian tubules appear 15 days after ingestion of spores; and that the infection, spread mainly by schizogony, is well established by 23 days. Spores are acid-fast. The PAS-positive spore membrane is not dissolved by 20-min treatment with hot KOH, but tests for chitin were inconclusive. The life history of the parasite is described. “Encapsulation” of the parasite has been observed. Electron microscope studies, the first reported for the class Haplosporea, show similarities of the cytoplasmic structure of this haplosporidian with that of some members of the sporozoan class Telosporea, though no specialized structures were seen. Finding of intracellular stages together with failure of interspecific infection attempts suggest that the microorganism should be placed in the genus Nephridiophaga Ivanic, 1937 with the specific name blattellae Crawley, 1905.
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    Topics: Biology
    Notes: SYNOPSIS. A centrifugation procedure for removing Tetrahymena from mass cultures is described. This method offers the following advantages: (a) inexpensive apparatus, (b) the short period of time required for harvesting large numbers of cells, (c) lack of cellular damage, (d) the ability to obtain proven dilution with regard to the culture fluid, (e) nearly quantitative recovery of the cells, and (f) the ease of assembling and disassembling the apparatus for cleaning.
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  • 57
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    Topics: Biology
    Notes: SYNOPSIS. Monocercomonas molae from the hindgut of the sunfish Mola mola is described. The host was taken from southern California coastal waters in October, 1964. The body of the flagellate is 8.0 × 10.7 microns. A single basal granule complex gives rise to 4 flagella, one of which is recurrent. The axostyle is relatively stout, with argentophilic granules, and possesses a periaxostylar ring. The capitulum of the axostyle continues into the sickle-shaped pelta, and the parabasal body is rod-shaped or lobed and roughly triangular in cross-section.
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  • 58
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    Topics: Biology
    Notes: SYNOPSIS. The complete life history of a homothallic, dioecious strain of Volvox aureus was studied in axenic culture. Asexual reproduction occurs by repeated division of specialized reproductive cells (gonidia), inversion of the resultant mass of cells to form daughter colonies, and subsequent morphologic differentiation of new gonidia in these daughters. Male colonies lack gonidia; however, the posterior 2/3 of the cells in a colony function as male initials each of which enlarges, divides, and undergoes rudimentary inversion to form a packet of 32 biflagellate sperm. Evidence was presented for the homology of eggs and undivided gonidia. The penetration of young vegetative colonies by sperm and the subsequent formation of apparent zygotes in these colonies was described and figured. Zygote germination, including division and inversion of the germling, was described; the cytological nature of the zygote divisions was not determined.A substance, MIS, in filtrates of sexual cultures induced differentiation of male colonies; a bioassay for it was perfected. Bioassay colonies show a differential susceptibility to male induction by MIS which is a function of the particular stage of development; colonies 48 hr after release from parentals are optimally susceptible. MIS was reasonably stable to heat, non-dialyzable, and Sephadex gel filtration indicated a molecular weight 〉 200,000. MIS activity is destroyed by trypsin and pronase but is unaffected by chymotrypsin. MIS was successfully concentrated ∼37-fold by the Carbowax method. The patterns of differentiation in other species of Volvox are described and possibilities discussed for studies of cellular differentiation in the genus as a whole.
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  • 59
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    Topics: Biology
    Notes: SYNOPSIS. Haemogregarina faiyumensis n. sp., a parasite of toads, Bufo regularis, in Faiyuni Province, Egypt, U.A.R., is described. In a survey of 689 toads from various localities in Cairo, Giza and Faiyurn provinces, only 3 out of 13 toads from Kom O Shim near Faiyum were infected. This species, known only by blood forms (most probably gametocytes) of two different staining reactions, is 13-17 μ long and 4-5 μ wide, with an average of 15.5 × 4.5 μ. The nucleus is typically subcircular and 3-5 × 3–5 μ, with an average of 4.5 × 3.9 μ.
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  • 60
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    Topics: Biology
    Notes: SYNOPSIS. Haemogregarina boueti França, 1910, was found to be the commonest blood parasite in the common toad, Bufo regularis Reuss, in Egypt. The rate of infection was about 30% (of 689 toads examined).In properly fixed blood films, the parasites were almost exclusively intraerythrocytic. Most characteristic was the encapsulated “elongate” form averaging 22.3 by 6 μ with a more-or-less central nucleus and a pointed, slightly bent, posterior end. Infected red cells were conspicuously hypertrophied and their nuclei were markedly displaced and frequently broken into 2-4 parts.Young and growing blood forms as well as two types of hepatic schizonts are described for the first time.Schizonts of the first type develop in hepatic cells, are 28–30 μ in diameter and produce numerous elongate oval merozoites about 8 × 2.2 μ radially arranged around a residual body about 10 μ in diameter.Schizonts of the second type start their growth in erythrocytes but later complete their development as free bodies in the liver sinusoids. When mature, they are 32–35 μ in diameter and produce a larger number of thin merozoites about 8 × 1.5 μ, surrounding a larger residual body about 19 μ in diameter.
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  • 61
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    Topics: Biology
    Notes: SYNOPSIS. Haemogregarina pestanae França, 1910, is apparently rare in Egypt, having been found in 1 toad Bufo regularis Reuss out of 689 examined. Capsulated capped, young thin, and young and advanced broad forms were present in the peripheral blood. Schizogony occurred in the liver. Two types of schizonts were present—macroschizonts producing 150 or more elongate oval merozoites surrounding a large residual body, and microschizonts producing 60 or less banana-shaped merozoites often radiating from a small, eccentric residual body.Merozoites of the first type developed into a large broad form representing early schizonts of the second type. The latter developed into thin young intraerythrocytic forms and apparently later into encapsulated capped gametocytes. H. pestanae, H. aegyptia and H. tunisiensis all occur in toads (Bufo regularis for the first two, and B. mauritanicus for the third), and produce characteristic encapsulated looped gametocytes in peripheral blood. The capsules contain dark-staining material condensed into a single well-developed cap in H. aegyptia and 1 or 2 much smaller caps in H. pestanae; this material is scattered regularly around the parasite in H. tunisiensis. The capsule of H. pestanae is more or less cylindrical along most of its length, more slender and slightly shorter than the regularly oval capsule of H. tunisiensis or the spindle- or egg-shaped capsule of H. aegyptia.
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  • 62
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    Topics: Biology
    Notes: SYNOPSIS. Spathidium spathula irradiated with 0 to 55 kr of × rays showed one or more of the following kinds of behavior: (1) Death of an undivided cell (primary death); (2) death of a descendant of an irradiated cell (secondary death); (3) permanent injury including one or more of the following: low daily division rate, excessive macronuclear enlargement, total loss of micronuclei, cytostome replication, heavy pigmentation, and decreased motility; (4) temporary division retardation for 1 to 2 days followed by apparent complete recovery; and (5) no apparent injury. The first 3 kinds of behavior increased with increasing dosage from 15 to 25 to 55 kr. At 6 kr only the last 2 categories were observed. The LD50 for 8 days was 46 kr for both primary and secondary death, or 60 kr for primary death alone.Micronuclear number varied greatly following irradiation in lines showing either permanent or temporary injury. Two different responses occurred: (1) The micronuclear number averaged about twice the normal number of 20 with a large range (0 to 360) 1 day after exposure. The number gradually decreased during the next 2 days; (2) some cells lost all micronuclei following irradiation, the incidence increasing with dose. At 55 kr complete loss of micronuclei occurred in 96% of the surviving lines.
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    Topics: Biology
    Notes: SYNOPSIS. Exchange of cytoplasm in Tetrahymena pyriformis, syngen 1, has been demonstrated by growing cells of 1 mating type in medium supplemented with H3-uridine or H3-histidine, washing, mixing with cells of an unlabeled, starved mating type, sampling conjugants at different times, and preparing autoradiographs. It was found that cytoplasmic interchange begins soon after the mates unite, and has become extensive before the end of the 1st prezygotic prophase (micronuclear crescent stage). When the RNA in one mating type had been labeled with H3-uridine, the activity was distributed almost evenly between the mates by late stages of conjugation. These results are consistent with electron micrographs of this syngen showing small pores in the attachment region of the mates, and many free ribosomes in the cytoplasm (8,11). By contrast, when protein in one mating type had been labeled with H3-histidine, these cells at late conjugation remained about twice as active as their originally unlabeled mates, presumably because of the physical characteristics of some structures which incorporated the amino acid (for example, cilia and membranes of the cell surface; cytoplasmic bodies, such as mitochondria, larger than the pores). That the radioactivity in the originally unlabeled cells came from their mates and not from the environment is indicated by the continued presence of inactive non-conjugants after 1 and 2 days in the mating type mixtures. Other cells which did acquire small amounts of active cytoplasm probably had engaged in abortive conjugation, separating from labeled mates before forming and exchanging pronuclei.
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    Topics: Biology
    Notes: SYNOPSIS. A major difference in heme content was found between leishmanias and leptomonads of Leishmania donovani. When tested with a fluorescence method for heme, leishmanias gave a negative response whereas leptomonads fluoresced brightly. Studies on the terminal respiration of L. tarentolae leptomonads by absorption spectra assay and respiratory inhibitors indicated the presence of cytochromes. Lactic dehydrogenase could not be detected in the leptomonad stage nor could it be found in any other hemoflagellate culture form tested.
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    Topics: Biology
    Notes: SYNOPSIS. The fine structure of various stages in the life cycle of Theileria parva is described. The appearance of the parasites suggests that there may be a double macroschizogony cycle. Micromerozoites are produced by a process of budding off from the body, known in light microscopy preparations as the residual body.
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  • 66
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    Notes: SYNOPSIS. A pure strain of Eimeria debliecki (University of Illinois strain A) established from a single oocyst was used to determine the endogenous cycle. Young parasite-free pigs 2 weeks to 3 months old were used throughout the study.The endogenous cycle was found to take place in the small intestine where the parasites were located in the distal portion of the striated simple columnar epithelial cells of the villi. The first generation schizonts were found in only the jejunum (15% of small intestine). The second generation schizonts and gametes occurred in the jejunum and ileum (70% of small intestine), a slight posterior progression occurring with each stage. The entire cycle required 6.5 days.The schizogonous cycle comprised 2 generations. The first generation schizonts required 2.5 days to reach maturity, measured 8-12 μ, contained 16 merozoites measuring 12-15 μ and had a polar residual mass. The second generation schizonts required 2 days to reach maturity, measured 13-16 μ, contained 32 rotund merozoites measuring 6–8 μ, and had only a few granules of residual material.Gametogony took place in 1.5 days. The macrogametes measured 12-16 μ, and the microgametocytes measured 9-14 μ with microgametes measuring 5–6 μ.
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    Notes: SYNOPSIS. Trypanosomatid-free plants of the family Asclepiadaceae identified as Asclepias syriaca, A. curassavica, A. incarnata, Stephanotis floribunda, Seutera maritima, Amphistelma scoparia and plants of the family Euphorbiaceae identified as Euphorbia tirucalli, E. trigona, and Pedilanthus tithymaloides were exposed to the bite of the bug, Oncopeltus fasciatus, infected with Phytomonas elmassiani, a flagellate which occurs naturally in A. syriaca and O. fasciatus. Two weeks subsequent to exposure to laboratory-infected oncopeltids all the experimental Asclepiadaceae were infected. The mean length of the protozoa varied depending on the host plant. The flagellates in A. syriaca, A. curassavica, and A. incarnata were shorter than those in S. floribunda, S. maritima, and A. scoparia.None of the Euphorbiaceae became infected.
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  • 68
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    Notes: SYNOPSIS. The mechanism of Prymnesium parvum ichthyotoxicity was studied in immersed minnows (Gambusia affinis) in the presence of various synergists (especially polyamines and invert soaps) and under varying conditions of pH and salinity. The effect of immersion in toxin-synergist solution on permeability of gill tissues to trypan blue and to radioactive substances, e.g., I125 and radio-iodinated albumin, was established. Fish sensitivity to various toxic substances was increased after immersion for short periods in suitable toxinsynergist solutions. This sensitivity, as well as the increased permeability of gill tissue, was transient and disappeared when fish were stored in tap water for several hours after the toxin-synergist treatment. Good correlation was found between the conditions (synergist quality and concentration, pH, salinity) leading to P. parvum ichthyotoxicity and conditions instrumental in increased gill permeability and toxin sensitivity. The primary site of damage is concluded to be the gill membrane.
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  • 69
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    Notes: SYNOPSIS. Tetratrichomonas gallinarum was found in the blood of 3 chickens experimentally infected with Borrelia anserina. The blood infection was successfully reproduced in healthy chickens and was accompanied by evidence that the trichomonads multiplied in the blood, ingested red blood cells, and were themselves phagocytized by leucocytes. T. gallinarum was maintained in serial passage in chicken embryos as well as in the usual trichomonad culture media.
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  • 70
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    Notes: SYNOPSIS. Schwartz identified a protozoan, parasite of the marine fish Leiostomus xanthurus as a haplosporidian belonging to genus Ichthyosporidium Caullery and Mesnil, 1905. Now, a coiled polar filament in the spore of that organism has been clearly recognized in certain PAS preparations which were used in the original study. The parasite is, therefore, a microsporidian rather than a haplosporidian. The generic characters of this and other protozoans still in genus Ichthyosporidium need further study.
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  • 71
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    Notes: SYNOPSIS. Suspensions of whole, killed ciliates were diffused against rabbit antisera for the respective strains to observe cross precipitation. The strains fell into the following groups: I. GL, H, ChS, GP, Aq, L-I, L-II, L-2, and V1; II. W, L-3, Gl-R, and V2; III. PR and F; and IV. BF and Lava. T. vorax strains V1 and V2 each resembled certain T. pyriformis strains more closely than they resembled each other. The same grouping of strains emerged in comparing antigenic suspensions and in comparing antisera and was confirmed by comparing absorption properties of antigens from the different strains.
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  • 72
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  • 73
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    Notes: SYNOPSIS. Two hundred and fifty-nine specimens of the sea urchins Echinometra lucunter (201), Diadema antillarum (52), Tripneustes ventricosus (5) and Eucidaris tribuloides (1), collected on the littoral of the Federal District of Venezuela, were examined for intestinal ciliates.Iron hematoxylin and silver-impregnation staining technics permitted determination of eight of the nine ciliates found: Anophrys aglycus, A. elongata, Cohnilembus caeci, Biggaria bermudensis, B. echinometris, Cyclidium rhabdotectum, Metopus circumlabens and M. rotundus. An unidentified species of Euplotes was also found.
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  • 74
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    Notes: SYNOPSIS. The firm union of the shells of adult Gromia oviformis in plastogamous pairs is followed by gametogenesis and fertilization with the production of distinctive fusiform zygotes that undergo further transformation into amoebulae initially having hyaline radiate pseudopodia. The amoebulae emerge from the parental shells and probably initiate the asexual phase of the life cycle.
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  • 75
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    Notes: SYNOPSIS. The establishment of Eimeria acervulina sporozoites in the duodenal glands of Lieberkühn of the chicken is described. Sporozoites were found to enter the tips of the villi and pass into the lamina propria, or core, of the villus. Within the lamina propria, sporozoites were engulfed by macrophages and taken to the glandular epithelium.Data are presented which indicate that macrophages serve as a defense against infection as well as a mode of transportation.
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  • 76
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    Notes: SYNOPSIS. Electron microscope observations of a strain of Labyrinthula indicate that the spindle cells glide within a collapsible slime tube rather than on top of it. These slimeways are clearly extracellular, partly covered with membranes, and consist of an amorphous matrix encrusted with many small vesicular elements.
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  • 77
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    Notes: SYNOPSIS. Thirty-one stocks of a marine ciliate, Euplotes minuta Yocom, collected from different localities, can be grouped in seven mating types. True pairs are formed only in mixtures of stocks belonging to different mating types. No selfing pairs or intraclonal conjugation have ever been observed. Synclonal inheritance of mating types is the rule, although about 10% of pairs show clonal inheritance. The latter can be explained by assuming syncaryon formation through cytogamy or through caryogamy of pronuclei derived from different products of meiosis. Mating type determination is due to 7 alleles at the single locus mt. There is complete dominance among the 7 alleles which can be orderly seriated, as shown in Table 3, according to their dominance relationship. The 5 stocks, and only these 5, of mating type VII have the autogamy trait. The mortality rate in F1 and F2 is very low–a maximum of 10%; however, the F2'S obtained by autogamy from F1 progenies in which mating type VII is involved have a very high mortality rate. The two facts (high mortality rate in F2 and strict association of autogamy trait with mating type VII in natural populations) have been considered as evidences of a probable isolation mechanism existing between mating type VII and the other 6 mating types. Thus, the 7 mating types have been assigned to the same syngen only tentatively.
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  • 78
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    Notes: SYNOPSIS. Sporozoites of Lankesterella hylae were found in 12 of 13 green tree frogs (Hyla caerulea) from Gin Gin, Queensland. The intraerythrocytic sporozoites had two pale-staining vacuoles at the poles of the nucleus and frequently a dome-like protuberance on the concavity of the crescentic protozoon.Motility was observed in free but not intracellular sporozoites in fresh blood. Locomotion was of a gliding nature, though in addition parasites flexed and extended, and a peristaltic constriction passed backwards along the body of two. One parasite entered and emerged from a red cell, the erythrocyte playing a passive role.All stages of sporogony were observed in liver smears from a debilitated frog. In araldite sections of the small intestine of another frog, parasites were found in the vacuoles within unidentified cells in the lamina propria, thus suggesting that the parasite's point of entry is possibly the alimentary tract.
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  • 79
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    Notes: SYNOPSIS. Some of the serotypes in Paramecium caudatum are described in this paper. Immobilization antigens of P. caudatum have been obtained by extracting paramecia in a dilute salt solution containing 15% alcohol. Immobilization antigen F from stock 162 has been isolated and has a sedimentation coefficient of 9.3 Svedbergs, diffusion coefficient of 2.3 × 10-7 cm/sec, and molecular weight of approximately 340,000.
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  • 80
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    Notes: SYNOPSIS. Two species of Isospora are described from Chloris chloris with the additional hosts Passer domesticus and Fringilla coelebs. I. lacazei Labbé has spherical oocysts measuring 16.6 to 30.0 μ; the oocyst wall is colorless and smooth, consisting of a thick layer and, in the majority of oocysts, an inner thin membrane. Stages of the life cycle in the epithelial cells of the duodenum are described. The internal stages consist of first and late generation schizonts which produce merozoites without any residual body, spindle-shaped microgametes and macrogametes without obvious “plastic granules.” The oocysts of I. chloridis sp. n. have colorless, smooth surfaced walls of one thick layer. They are ellipsoidal, measuring 17.2-33.2 μ× 16.6-30.0 μ. The internal stages of this species infect the epithelial cells of the small intestine in the same region as I. lacazei. They produce 2 generations of schizonts, consisting of merozoites and a residuum; microgametes are comma-shaped and macrogametes have obvious “plastic granules.”
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  • 81
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    Notes: SYNOPSIS. Blood and tissue smears from 156 yellow-billed magpies showed infection with hematozoa in 154 (99%). Leucocytozoon berestneffi was found in 149 (96%), Haemoproteus picae in 40 (26%), Plasmodium relictum, in 32 (21%), Trypanosoma sp. in 3 (2%), and microfilariae in 42 (27%). Fifty-two birds were infected with two genera of parasites, 27 with 3, and 4 with 4. Leucocytozoon, Plasmodium and microfilariae showed a higher incidence in tissue than in blood smears.
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  • 82
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    Notes: SYNOPSIS. Monolayers of cells of coverslips were produced by culturing known numbers of trypsinized chick cells in growth medium (solution 199 plus 20% calf serum) at 37 C for 2 days. The fluid was then replaced with maintenance medium (solution 199 plus 5% calf serum) containing various known numbers of T. cruzi and the preparations were incubated at 33 C for 5 days; fresh maintenance medium was substituted on the 2nd or 3rd day. The inocula of parasites were obtained from T. cruzi-cell cultures, supplemented with 2% sterile NNN overlay, or from NNN cultures.The numbers of extracellular parasites, proportions of infected cells, and percentage distribution of infected cells relative to the number of intracellular leishmanial bodies were determined on days 2 or 3 and 5 of parasite cultivation in many experiments. Analyses of the data gave the following results. Extracellular parasites increased 2- to 14-fold during the first 2 or 3 days, depending upon the source and size of the inocula, and 10- to 20-fold during the last 2 or 3 days. Cell infection continued throughout incubation at daily rates of 1.4-4.5%; 8-22% of the cells became infected during the 5 days of incubation. Intracellular growth was reflected most clearly by increases in the proportion of cells having 〉10 leishmanial bodies. This increase was about 5% daily during the last 2 or 3 days of incubation.A useful test procedure for assessing the antiparasitic action and chick embryo cell toxicity of drugs is illustrated by data obtained with furazolidone and tris (p-aminophenyl)carbonium chloride.
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  • 83
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    Notes: SYNOPSIS. Tetrahymena pyriformis strains E, A-136 31C and IMT II survived freezing in 10% dimethylsulfoxide when the temperature was lowered to freezing at 4.5 C/min. Survival was then obtained for at least 128 days by lowering the temperature rapidly to 95°C. Of the 3 strains, T. pyriformis IMT II was most resistant to the effects of freezing. Its volume averaged about half that of either of the other strains and may have contributed to the differences in survival. In addition to differences among strains, a medium relatively low in the concentration of nutrients, a culture nearing peak population, and a rate of cooling of 4.5 C/min, all gave best survival. Paramecium aurelia regained motility after being frozen in 6 to 7.5% dimethylsulfoxide for as long as 7 days at either –27 or –196 C, but cultures were obtained only after storage for 20 min at –27 C. A concentration of 6 to 7.5% dimethyl-sulfoxide, cooling at 4.5 C/min, and culture media containing Aerobacter aerogenes or composed of a commercially available composition were all required for survival of P. aurelia.
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    Notes: SYNOPSIS. Cysts of Sarcocystis sp. are described from a dog. They are spherical to elongate, 110–250 μ in diameter, and contain numerous crescentic trophozoites measuring 4–5 × 1.5 μ. No septa were seen. This is the first report of Sarcocystis from a domestic carnivore.
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    Notes: SYNOPSIS. Cytoplasmic inclusions appear rapidly in Leishmania enriettii exposed to 37 C. The staining of these droplets with oil red O, their extraction in non-polar solvents, and their fine structure by electron microscopy establish their identity as lipid droplets. Fatty acid profiles of these organisms show alterations concomitant with the development of these inclusions. Oleic acid increases while linolenic acid is depressed in cells exposed to elevated temperature. A greater incorporation of exogenous radioactive stearic acid occurs, with depressed specific activities of linoleic and linolenic acids compared to values obtained with control organisms. The isolated lipids of L. enriettii have temperature-dependent changes consistent with a physical interpretation of events which occur with temperature inactivation. The temperature lability of fatty acid metabolism is discussed in terms of the synthesis and stability of cellular membranes and organelles.
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    Notes: SYNOPSIS. Total counts of Eimeria vilasi and E. wisconsinensis oocysts in 0.05 g fecal samples from the eastern chipmunk over a 2-year period indicated that the 2 species had respective occurrences of 100% and 11% and an actual abundance ratio of 35 to 1. In the red squirrel similar counts of E. tamiasciuri and E. toddi over a 3-year period indicated occurrences of 98% and 6% and an actual abundance ratio of 26 to 1, respectively. These results parallel a similar dichotomy in percent occurrence of 7 Eimeria in the sciurid genera Cynomys and Marmota.
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  • 88
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    Notes: SYNOPSIS. By means of precipitation with protamine sulfate, a soluble antigen (PS) was obtained from erythrocytes of horses with acute babesiosis due to Babesia caballi and B. equi. This antigen reacted in gel diffusion tests with sera from horses recovered from acute babesiosis. The PS antigen was found to be muco-protein, susceptible to destruction by trypsin and taka-diastase. Analysis of the antigen by paper electrophoresis revealed 2 components which were not present in similar preparations made from erythrocytes of Babesia-free horses.When the PS antigen was heated in boiling water for 30 minutes, a serologically inactive precipitate was formed; however, the supernate remained serologically active and was termed boiled PS (BPS) antigen. This antigen was polysaccharide in nature; its serologic activity was destroyed by taka-diastase.In gel diffusion tests with sera of recovered horses, the PS antigen formed 2 lines of precipitation which coalesced in a single line formed between these sera and the BPS antigen. Both PS and BPS antigens reacted with sera of horses recovered from acute babesiosis in the gel-diffusion test, but not with sera of dogs and rats recovered from acute infection with Babesia canis and Babesia rodhaini, respectively. The serologic specificity of these antigens suggests that they might have application in the serodiagnosis of inapparent Babesia infections of equine animals.
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    Notes: SYNOPSIS. Euglena gracilis (bacillaris variety, strain SM-L1, streptomycin-bleached) used the following amino adds (10−3 M) as sole nitrogen source for growth on a defined medium: glycine, alanine, valine, leucine, isoleucine, serine, threonine, and glutamic acid. Aspartic acid was used at 10−2 M. Glutamine and asparagine were used at 10−3 M and were better N sources than their parent dicarboxylic amino acids. Not used as sole N source for growth were phenylalanine, tyrosine, tryptophan, cysteine, cystine, methionine, proline, hydroxyproline, histidine, arginine, lysine, and taurine. Astasia longa (Jahn strain) was more restricted than Euglena and used only asparagine and glutamine as N sources for growth.
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    Notes: SYNOPSIS. Gigantomonas usually exists in the multinucleate stage. Hence, multiple fission is more common than binary fission. In its flagellate as well as its aflagellate state it is always an amoeboid cell which possesses from one to several large, clear pseudopodia. Fairly often in the multinucleate, as well as the uninucleate, stage no extranuclear organelles are present except large plain centrioles, two of which are always closely associated with each nucleus. During nuclear reproduction four centrioles, two old ones and two new ones, are always present with each nucleus. During all nuclear reproductions, regardless of the number of nuclei present, extranuclear organelles, such as flagella, axostyle, undulating membrane, and costa when present are discarded. If they are renewed, it is by the new centrioles at the same time that the old ones produce new central spindles, two always cooperating in the process. Thus, Gigantomonas, like other genera of the Devescovinidae, the family to which it belongs, never has for each nucleus present more than one set of extranuclear organelles, a characteristic which Devescovinidae and Lophomonadidae have in common. It is the only genus of Devescovinidae without a parabasal body.Owing to the liquidness of the cytoplasm, the central spindle, which becomes very long indeed, often extends beyond the cytoplasm and thus pushes the nucleus fastened to this end of it completely out of the cell. Mainly because of this situation, multinucleate forms with an odd number of nuclei occur often; otherwise the nuclear numbers would be 2, 4, 8, 16, 32, etc., because, no matter how many nuclei are present, they all reproduce simultaneously or nearly so.An unusual situation occurs in which Gigantomonas ingests and digests a small species of Holomastigotoides, while several hundred individuals of the latter become attached to and destroy Gigantomonas.
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    Notes: SYNOPSIS. A new species of coccidium is described: Eimeria urosauris n. sp., in the gall bladder of the lizard Urosaurus graciosus Hollowell, from the Mojave Desert in California. The oocyst of E. urosauris is smooth, bilaminar, nearly cylindrical, with long borders only slightly convex, ends rounded and very nearly hemispherical. It is usually 32 × 20 μ, and its length/width ratio is 1.6. It contains 4 ellipsoid sporocysts, each 10.5 × 9 μ, for which 1/w is 1.17. Each sporocyst contains 2 tapered bent sporozoites with rounded ends, 11 μ long, 4 μ in diameter at the larger end, and 1.5 μ in diameter at the smaller end. Each sporocyst also contains a central granular sporocyst residuum 3.5 μ in diameter. The oocyst lacks a micropyle and oocyst residuum, and there is no Stieda body on the sporocyst. Sporulation time is 6–10 hr. Endogenous development, with reinfection by liberated sporozoites, occurs in the epithelial lining of the gall bladder. E. urosauris is compared to other morphologically similar lacertilian eimerias with which it might be confused.
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    Notes: SYNOPSIS. In rats infected with T. lewisi, 2 morphologically distinct forms of the trypanosome occur. By means of the immunodiffusion technic several antigenic differences between the 2 forms were observed. The time course in the antigenic and morphologic changes is somewhat different. The antigenic change from young to adult forms is gradual. It starts 12 days after infection and is complete in 14 days, 3 to 5 days after the morphologic appearance of the trypanosomes is that of adult forms. In addition, there appear to be 2 separate stages of young forms when they are analyzed for antigenic composition.
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  • 93
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    Notes: SYNOPSIS. Nucleic acid hybridisation involving DNA samples was used to study relationships between various protozoa. The most hybridisation or nucleic acid homology was always in the homologous reaction between 2 DNA samples from the same source. It was concluded that all the protozoa tested have nucleotide sequences or genes in common with Paramecium aurelia. The ciliates could be placed in a sequence of decreasing homology relative to Paramecium: Tetrahymena, Colpidium, Stentor, Didinium, Dileptus, Blepharisma. Actinosphaerium had fewer sequences than any of the ciliates and the flagellate Euglena had the fewest sequences in common. The bacterium Aerobacter had none. Similar relationships were inferred from competitive hybridisation experiments; these relationships were also in general mirrored by morphologic relationships and overall G + C base compositions which ranged from 46% for Euglena to 32% for P. aurelia. These experiments, it is hoped, will contribute to studies on origins of the metazoa.
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    Notes: SYNOPSIS. Nicotinamide adenine dinucleotide phosphate (NADP) and nicotinamide adenine dinucleotide (NAD) linked isocitrate dehydrogenase and NADP linked alcohol dehydrogenase have been detected in Euglena gracilis var. bacillaris.The NADP isocitrate dehydrogenase showed half-maximal activity at a concentration of 3 × 10−5 M DL-isocitrate, but did not follow simple Michaelis-Menten kinetics with respect to substrate concentration. The optimal NADP concentration was about 0.06 mM, and activity fell off sharply on either side of this optimum. Fresh preparations of the enzyme migrated as single bands in disc electrophoresis, but two enzymatically active bands were present after frozen storage.The NAD isocitrate dehydrogenase followed Michaelis-Menten kinetics with respect to substrate. In crude extracts, no requirement for adenosine monophosphate, adenosine diphosphate, or sulfhydryl compounds could be found.NADP alcohol dehydrogenase activity could be found with either ethanol or propanol as substrate. Low concentrations of coenzyme A were moderately inhibitory.In tris(hydroxymethyl) aminomethane buffer (tris buffer), Euglena extracts reduced NAD slowly in the absence of exogenous substrate. In the absence of tris, no such reduction occurred. A similar phenomenon was observed with NADP.
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    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Hepatocystis has been found extremely common in a number of species of Formosan mammals, notably the large leafnosed bat (Hipposideros armiger terasensis), the Formosan macaque (Macaca cyclopis), and various subspecies of the red-bellied tree squirrel (Callosciurus erythraeus). Less often infected were the long-winged bat (Miniopterus schreibersii) and the Formosan giant flying squirrel (Petaurista grandis). The species occurring in H. a. terasensis is believed to be new, and is named Hepatocystis hipposideri. It causes considerable enlargement (but not other changes) of the host cell, is often amoeboid, and usually has numerous fine pigment granules.
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  • 96
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Tracer technic has proved to be an excellent tool in the study of predator-prey relationships among the foraminifera. More than fifty axenic species of protists including diatoms, dinoflagellates, chlorophytes, chrysophytes, cyanophytes, bacteria and yeasts were tested as potential food for Allogromia sp (NF), A. laticollaris, Am. monia beccarii, Quinqueloculina spp, Rosalina floridana, Anomalina sp, Elphidium sp, Spiroloculina hyalina, Globigerina bulloides, and Globorotalia truncatulinoides. Although many types of potential food are present in the environment, foraminifera select only certain organisms. The yeasts, cyanophytes, dinoflagellates, chrysophytes and most bacteria tested were not eaten. Selected species of diatoms, chlorophytes and bacteria were eaten in large quantity. Three additional factors affect feeding: the “age” of the food organism, the “age” of the foraminifer or its position in the life cycle, and the concentration of the food. Feeding by foraminifera on most food is erratic below a concentration of 103 organisms and is approximately directly proportional to concentration within a range of 103-106 organisms per 10 ml experimental tube. A natural bloom of Protelphidium tisburyensis was analyzed. A high concentration of 6 species of diatoms characterized the community. A “bloom”-feeder hypothesis for foraminiferal nutrition is presented.
    Type of Medium: Electronic Resource
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  • 97
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. The reorganization in resting cysts which produce a single emerging individual was followed in 5 species of Colpodidae forming a possible evolutionary series with increasing numbers of kineties. Stomatogenesis in Colpoda maupasi and C. inflata was studied for the first time; that in C. steinii, C. cucullus and Tillina magna was reinvestigated with new observations. In all, the oral primordium is double and originates from segments of certain somatic kineties, constant for each species. The larger mouthparts in the larger ciliates are produced from a correspondingly greater number of kineties. Morphogenetic and evolutionary implications of this series of observations are discussed.
    Type of Medium: Electronic Resource
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  • 98
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. When large batches of Paramecium (more than 100,000 cells) are centrifuged in conventional centrifuges, extensive lysis occurs, typically lowering recovery to around 30%. An easily constructed centrifuge with a cylindrical plastic head operated at low accelerations permits centrifugation of large batches of Paramecium with about 90% recovery, even after exhaustive washing. Operation requires only a few minutes, and the system is easily cleaned. The inexpensive heads can be instantly interchanged, and cultures can even be centrifuged in their original low form glass culture vessels. This system, which should be applicable to any large fragile cells, permits timed experiments that are usually impossible because of the need for exhaustive washing or concentration from large initial volumes.
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  • 99
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Defined media for Leptomonas collosoma, L. mirabilis, and L. sp. from Dysdercus are described. In addition to factors required by Crithidia spp., including a source of Crithidia factor, all 3 organisms require glycine. Leptomonas collosoma and L. sp. from Dysdercus require choline. All trypanosomatids thus far studied require calcium pantothenate but L. collosoma has an especially large requirement. Leptomonas mirabilis but not L. sp. from Dysdercus can synthesize methionine from homocysteine thiolactone during growth. Homocysteine thiolactone is toxic to L. sp. from Dysdercus. Methionine plus vitamin B12 partly annul homocysteine thiolactone toxicity but only if glycine is also present.
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  • 100
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 13 (1966), S. 0 
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SYNOPSIS. Glauconema trihymene n. g., n. sp., a marine hymenostome ciliate, is described from the Virginia coast. Morphologic studies were made on specimens treated with the Chatton-Lwoff silver impregnation technic and on animals observed with the phase microscope. Particular attention is given to the buccal ciliature and its importance to generic assignment in the order Hymenostomatida.
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