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223 results for “Caspian Sea”
Fig. 12 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 12 Scanning electron micrographs of selected Ponto-Caspian origin ostracod species identified from the İzmit Gulf drilling cores. a-b. Camptocypria acronasuta; a right valve, internal view, b right valve, 201/104 m; c. Candona neglecta; right valve, 204/9.3 m; d. Candona parallela pannonica; left valve, 204/9.3 m; e-f. Candona schweyeri; e left valve, 204/34 m, f right valve, internal view, 204/18 m; g-h. Cryptocyprideis bogatschovi; g left valve, h right valve, 204/43 m; i-j. Euxinocythere bacuana; i left valve, 203/95 m, j right valve, 206/63 m; k-l. Euxinocythere bosqueti; k right valve, 204/36 m, l right valve, 203/143.5 m; m-n. Euxinocythere ex gr. bosqueti; m left valve, 203/143.5 m; n left valve; o-p. Euxinocythere relicta; o left valve, p right valve, 201/74 m, 10 m; q-r. Hemicytherura bulgarica; q left valve, male 208/14 m, r right valve, female, 201/1 m.
Fig. 8 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 8 Scanning electron micrographs of selected benthic foraminiferal species identified from the İzmit Gulf drilling cores. a. Planodiscorbis sp., 205/1.5 m: a1, spiral view; a2, umbilical view. b. Planorbulina mediterranensis, 201/1 m. c. Polymorphina sp., 206/41 m. d. Porosononion subgranosus, 207/31 m. e. Pseudotriloculina lecalvezae, 207/1 m. f. Pyrgo elongata, 201/1 m. g. Quinqueloculina berthelotiana, 208/1 m. k. Quinqueloculina laevigata, 208/9 m. i. Quinqueloculina laevigata, 208/2 m. j. Quinqueloculina parvula, 208/5 m: j1, side view; j2, apertural edge view. k. Quinqueloculina seminula, 201/1 m: k1, side view; k2, apertural edge view. l. Rectuvigerina phlegeri, 205/1.5 m. m. Reusella spinulosa, 201/1 m. n. Rosalina bradyi, 208/5 m: n1, spiral view; n2, umbilical view. o. Rosalina globularis, 208/1 m. p. Sahulia conica, 201/1 m. q. Sigmoilina costata, 208/5 m.
Fig. 13 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 13 Scanning electron micrographs of selected Ponto-Caspian origin ostracod species identified from the İzmit Gulf drilling cores. a-b. Loxocaspia lepida; a left valve, b right valve, 204/9.3 m; c-d. Loxoconcha immodulata; c left valve, male, d left valve, female, 204/9.3 m; e. Loxoconcha sp.; left valve, 206/63 m; f-h. Loxocorniculina djaffarovi; f left valve, 207/22.75 m, g dorsal view, 207/22.75 m, h left valve, 206/8 m; i. Trapezicandona sp.; right valve, 201/108 m; j-k. Tyrrhenoythere amnicola donetziensis; j right valve, k left valve, 204/9.3 m; l-n. Xestoleberis chanakovi; l right valve, 203/143.5 m; m right valve, internal view, 203/147 m; n left valve, internal view, 203/147 m.
Fig. 4 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 4 Scanning electron micrographs of selected benthic foraminiferal species identified from the İzmit Gulf drilling cores. a. Adelosina carinatastriata, 208/5 m. b. Adelosina mediterranensis, 201/1 m. c. Ammonia compacta, 207/31 m: c1, spiral view; c2, umbilical view. d. Ammonia compacta, 208/1 m: d1, spiral view; d2, peripheral view; d3, umbilical view. e. Ammonia parkinsoniana, 206/37.5 m: e1, spiral view; e2, umbilical view. f. Ammonia parkinsoniana, 208/1 m: f1, spiral view; f2, peripheral view; f3, umbilical view. g. Ammonia tepida, 208/5 m: g1, spiral view; g2, umbilical view. h. Amphicoryna scalaris, 206/4.5 m. i. Astrononion stelligerum, 205/1.5 m.
Fig. 11 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 11 Scanning electron micrographs of selected Ponto-Caspian origin ostracod species identified from the İzmit Gulf drilling cores. a-b. Amnicythere bendovanica; a right valve, 204/9.3 m, b left valve, 204/13 m; c-d. Amnicythere hilda; c right valve, d left valve, 204/56 m; e. Amnicythere longa; right valve, 204/9.3 m; f-g. Amnicythere olivia; f right valve, g left valve, 204/34 m; h-i. Amnicythere pediformis; h left valve, i right valve, 204/13 m; j-k. Amnicythere quinquetuberculata; j left valve, k right valve, 206/63 m; l-m. Amnicythere striatacostata; l right valve, 204/34 m; m left valve, 204/18 m; n-o. Bacunella dorsoarcuata; n right valve, o left valve 204/43 m.
Fig. 3 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 3 Lithological features and sand distributions of collected sediment samples a. Dilovası, b. Hersek Burnu. The lower intervals of drillings 10MB-204 (120-80 m), 10MB-205 (117.2-40 m), 10MB-206 (122-80 m), 10MB-207 (120.9-50 m) and 10MB-208 (200- 40 m) are not shown due to absence of sample.
Fig. 2 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 2 Growth curve used in determination of ED for sample 10MB-201 74 m by using regenerative procedure.
Fig. 14 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 14 Scanning electron micrographs of selected Mediterranean origin ostracod species identified from the İzmit Gulf drilling cores. a. Acanthocythereis hystrix; right valve, 205/1.5 m; b-c. Aurila convexa; b left valve, 205/1.5 m, c right valve, 208/5 m; d. Aurila interpretis; left valve, 205/1.5 m; e. Bosquetina carinella; left valve, 206/33 m; f. Bythocythere minima; left valve, 201/1 m; g-h. Callistocythere intricatoides; g left valve, h right valve, 206/37.5 m; i-j. Callistocythere pallida; i right valve, j left valve, 208/5 m; k-l. Carinocythereis carinata; k right valve, l left valve, 206/37.5 m; m. Carinocythereis rhombica; right valve, 206/4.5 m; n. Costa edwardsii; left valve, 206/37.5 m.
Fig. 7 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 7 Scanning electron micrographs of selected benthic foraminiferal species identified from the İzmit Gulf drilling cores. a. Favulina hexagona, 206/37.5 m. b. Fissurina staphyllearia, 206/37.5 m. c. Fursenkoina complanata, 206/14 m. d. Gavelinopsis praegeri, 206/37.5 m: d1, spiral view; d2, umbilical view. e. Globobulimina affinis, 201/1 m. f. Globocassidulina subglobosa, 201/1 m. g. Haynesina depressula, 206/33 m. h. Haynesina sp., 208/1 m. i. Hyalinea balthica, 206/33 m. j. Miliolinella subrotunda, 208/5 m. k. Miliolinella subrotunda, 208/9 m. l. Neoconorbina terquemi, 208/5 m: l1, spiral view; l2, umbilical view. m. Nonion subturgidum, 206/41 m: m1, side view; m2, apertural edge view. n. Nonionoides turgidus, 208/33 m: n1, spiral view; n2, peripheral view; n3, umbilical view.
Fig. 5 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 5 Scanning electron micrographs of selected benthic foraminiferal species identified from the İzmit Gulf drilling cores. a. Asterigerinata mamilla, 206/37.5 m: a1, spiral view; a2, peripheral view; a3, umbilical view. b. Aubignyna perlucida, 208/37.5 m: b1, spiral view; b2, umbilical view. c. Aubignyna perlucida, 207/31 m: c1, spiral view; c2, peripheral view; c3, umbilical view. d. Biloculinella labiata, 204/13 m. e. Bolivina alata, 207/22 m. f. Bolivina dilatata, 206/37.5 m. g. Bolivina dilatata, 208/18 m. h. Bolivina ordinaria, 207/22.75 m. i. Bolivina ordinaria, 206/8 m: i1, side view; i2, apertural edge view. j. Bolivina pseudoplicata, 206/37.5 m. k. Bolivina spathulata, 206/37.5 m. l. Bolivina striatula, 206/14 m. m. Bolivina striatula, 208/25 m. n. Bulimina aculeata, 208/33 m. o. Bulimina elongata, 208/18 m. p. Bulimina marginata, 207/18 m. q. Bulimina marginata, 207/22.75 m.
Fig. 10 in Ponto-Caspian And Mediterranean Faunal And Floral Records Of Upper Pleistocene-Holocene Sediments From The İzmit Gulf (Marmara Sea, Turkey)
Fig. 10 Total Benthic Foraminifera (TBF) and Species Number (SN) in drillings a. Dilovası and b. Hersek Burnu. TBF indicates numbers of specimens per 10 g dry sediment. The lower intervals of drillings 10MB-204 (120-80 m), 10MB-205 (117.2-40 m), 10MB- 206 (122-80 m), 10MB-207 (120.9-50 m) and 10MB-208 (200-40 m) are not shown due to absence of sample.
Figure 1. A in Online database "See The Sea" for the Caspian Sea
Figure 1. A satellite view (true color) of the Caspian Sea on 22 August 2019 from MODIS-Terra (©NASA, 2019).
Figure 6 in Main Pattern of the Caspian Sea Surface Oil Pollution Revealed by Satellite Data
Figure 6. Examples of the manifestations of oil slicks from natural seeps on the seafloor in the Sefid Rud Cap area in satellite images. Parts of SAR-C Sentinel-1A images: a) February 16, 2015, 14:36 UTC; b) August 9, 2016, 14:36 UTC; c) October 27, 2017, 14:36 UTC. Parts of MSI Sentinel-2A images (color composites of 4, 3 and 2 spectral channels): d) September 14, 2015, 07:39 UTC; e) May 28, 2016, 07:29 UTC; f) June 25, 2019, 07:38 UTC.
Figure 7 in Main Pattern of the Caspian Sea Surface Oil Pollution Revealed by Satellite Data
Figure 7. Consolidated maps of oil slicks due to natural seepages on the seafloor revealed from SAR imagery: a) in the Cheleken area; b) in the Sefid Rud Cape area.
Figure 4 in Main Pattern of the Caspian Sea Surface Oil Pollution Revealed by Satellite Data
Figure 4. Statistics on the frequency of detection of oil patches in the "Oil Rocks" oil producing area in SAR images in dependence on near-surface winds.
Figure 4 in Histopathological observations in Neogobius bathybius (Actinopterygii: Gobiidae) infected by Dichelyne minutus (Nematoda: Cucullanidae) in the Caspian Sea, Iran
Figure 4. Cross-section of parasitized fish intestinal epithelium: a) hyperplastic epithelium cells (arrowheads); b) congested blood vessels, veins (arrows); c and d) nodule-like structures via intense hyperplastic submucosal tissue, resulted in deeper folds and e) focal necrosis (star) and thickened muscular layer (2-headed arrow); f) increased number of goblet cells (arrows). M = mucous, s = submucosa, and mus = musculature.
Figure 1 in Histopathological observations in Neogobius bathybius (Actinopterygii: Gobiidae) infected by Dichelyne minutus (Nematoda: Cucullanidae) in the Caspian Sea, Iran
Figure 1. Anterior part of Dichelyne minutus: a) large pseudobuccal capsule; b) posterior end of esophagus; c) anterior ventral cecum; d) nerve ring.
Figure 8 in Assessment of the accuracy of determining the Caspian Sea surface temperature by Landsat-5, -7 satellites based on the measurements of drifters
Figure 8. The relationship between the temperature of the sea surface layer obtained from drifters and SST according to Landsat-5, -7 Level-2 data: (a) measurements that have a time difference of no more than two hours with the flight of the satellite; (b) all measurements on the day of the satellite flyby.
Figure 4 in Assessment of the accuracy of determining the Caspian Sea surface temperature by Landsat-5, -7 satellites based on the measurements of drifters
Figure 4. An example of the absence in the archives of images over the central part of the Caspian Sea (flight track N 166 of the Landsat-7 satellite on 22 July 2008.
Figure 2 in Assessment of the accuracy of determining the Caspian Sea surface temperature by Landsat-5, -7 satellites based on the measurements of drifters
Figure 2. Drifter tracks in the Caspian Sea: (a) from 4 October 2006 to 20 February 2007, and (b) from 19 July 2008 to 10 October 2008.
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