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12 results for “statoblasts”
Fig. 5 in Bryozoan statoblasts from lake sediments in Madagascar, including two new species
Fig. 5. Floatoblasts of Plumatella kisalensis Wood, 2018. a. Paired valves, dorsal on left, ventral on right. b. SEM image of one end of ventral valve showing tuberculation. c. One end of ventral valve showing toothed margin. Scale bars: a = 100 µm; b–c = 50 µm.
Fig. 4 in Bryozoan statoblasts from lake sediments in Madagascar, including two new species
Fig. 4. Floatoblasts of Plumatella sofiae sp. nov. a. Paired floatoblast valves, dorsal on left, ventral on right. b. One end of ventral valve showing toothed margin. c. SEM of a portion of the ventral valve showing tuberculation. Scale bars: a = 100 µm; b–c = 50 µm.
Fig. 3 in Bryozoan statoblasts from lake sediments in Madagascar, including two new species
Fig. 3. Floatoblasts related to Plumatella tsimiheta sp. nov. a. Unpaired valves, dorsal on left with arrows showing annulus encroachment over the capsule, image of ventral valve (right) electronically composed to show two planes in focus. b. SEM micrograph showing floatoblast surface details on dorsal (left) and ventral (right) valves. c. SEM view of a portion of floatoblast in P. patagonica Wiebach, 1974 showing similar tuberculation. Scale bars: a–b = 100 µm; c = 50 µm.
FIGURE 4. Plumatella bombayensis. Statoblasts from ZEV 3804 in Phylactolaemate bryozoans at the Zoological Survey of India and a taxonomic key to Indian Phylactolaemata
FIGURE 4. Plumatella bombayensis. Statoblasts from ZEV 3804, Zoological Gardens, Kolkata. (a) Floatoblast dorsal valve showing small, unmarked fenestra; (b) Floatoblast ventral valve showing pronounced fenestra reticulation; (c) Sessoblast showing reticulation in which each cell bears a single tubercle; (d) Partial enlargement of previous image. Scale bars for a–c = 100 µm, scale bar for d = 20 µm.
FIGURE 5. Plumatella longigemmis. Statoblasts from specimen P47 in Phylactolaemate bryozoans at the Zoological Survey of India and a taxonomic key to Indian Phylactolaemata
FIGURE 5. Plumatella longigemmis. Statoblasts from specimen P47 labeled Plumatella longigemmis (syntype), now recognized as Hyalinella lendenfeldi. (a) Floatoblast valves with dorsal valve on the left; (b) SEM image showing the floatoblast dorsal side in greater detail. Scale bars = 100 µm.
FIGURE 3. Statoblasts from specimen P92 in Phylactolaemate bryozoans at the Zoological Survey of India and a taxonomic key to Indian Phylactolaemata
FIGURE 3. Statoblasts from specimen P92 labeled Plumatella bigemmis (Holotype), now identified as Plumatella fungosa. a) Floatoblast valves with dorsal valve above, ventral valve below; b) Scanning electron micrograph of floatoblast ventral valve with inset showing tubercles on the annulus; c) Scanning electron micrograph of sessoblast with inset showing tubercles on annulus. All scale bars = 100 µm.
Fig. 1 in Bryozoan statoblasts from lake sediments in Madagascar, including two new species
Fig. 1. Map (left) showing the location of Lake Sofia within Madagascar, in relation to the capital city of Antananarivo, and (right) showing the location of the SOF3 core within Lake Sofia.
Fig. 2. A in Bryozoan statoblasts from lake sediments in Madagascar, including two new species
Fig. 2. A stratigraphic graph displaying the total number of plumatellid bryozoan statoblast valves found in the SOF3 wide diameter core from Lake Sofia, Madagascar. Each bar represents the number of valves found in 30 cm3 of sediment.
Figures 5-8 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figures 5-8 - Lophopodella capensis statoblasts and organic detritus, including charcoal at right, from the sieved sediment subsample from25–26 cm stratigraphic depth, dated to 220–230 yr BP (5). A well preserved statoblast observed at 41–42 cm, dated to 670–711 (6). Pleistocene-aged statoblast from 480–481 cm, dated to 15600–15700 (7). Same specimen as Fig. 6 showing the split layers of the polar spine and recurved hooks (8).
Figure 1 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figure 1 - Location of the study site in Africa (A) and within Kenya (B). The location of the coring site (black circle) within Enapuiyapui (C). The red line represents a fire break cutline.
Figure 4 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figure 4 - BACON version 2.2 R program language script age-depth model for the Enapuiyapui stratigraphy using MCMC random walks (greyscale shading) through the probable radiocarbon dates (1σ age probability distributions represented in blue) that were calibrated using the IntCal13 curve (Table 1; Blaauw and Christenson 2011; Reimer et al. 2013; R Development Core Team 2015). The final model used the weighted average of the random walk densities (red line) and 95% CI (dotted grey lines) and parameter settings are shown at the top right (red font). Ages reported as calibrated year BP (before present, 1950 CE). ITRAX optical core face photographs and magnetic susceptibility profile (grey line) at bottom left that shows the 484–0 cm section of the 537 cm core. Zones were defined using a regime shift index of the magnetic susceptibility values (Rodionov 2004). Lophopodella capensis presence data are represented by red '+' symbols on the magnetic susceptibility profile. Abbreviations are AHP: African Humid Period, H: Holocene, Ps: Pleistocene.
Figures 2-3 from: Courtney Mustaphi CJ, Githumbi EN, Shotter LR, Rucina SM, Marchant R (2016) Subfossil statoblasts of Lophopodella capensis (Sollas, 1908) (Bryozoa, Phylactolaemata, Lophopodidae) in the Upper Pleistocene and Holocene sediments of a montane wetland, Eastern Mau Forest, Kenya. African Invertebrates 57(1): 39-52. https://doi.org/10.3897/afrinvertebr.57.8191
Figures 2-3 - An wide angle aerial oblique photograph of Enapuiyapui wetland from the northwest facing southeast (2). Coring the center of the Cyperaceae-Poaceae wetland, April 2014 (3).
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