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4 results for “Lophopodella”
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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