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Operculina ammonoides

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Journal Article
Published: 01 April 1983
Journal of Foraminiferal Research (1983) 13 (2): 122–128.
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<span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span> .  A  equatorial and  B  axial views of chamber lumin...
Published: 01 January 2013
Figure 4 Operculina ammonoides . A equatorial and B axial views of chamber lumina, C axial view of chamber lumina covered by the test (note alar prolongations reaching the umbonal area), D chamber volume, E cubic root of chamber volume, F septal distance, G chamber width, H
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<span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span> . Residuals and standardized residuals (in %) for lin...
Published: 01 January 2013
Figure 5 Operculina ammonoides . Residuals and standardized residuals (in %) for linearized chamber volume ( A , B ), septal distance ( C , D ), chamber width ( E , F ), and chamber height ( G , H ).
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Axial section parameters measured in  <span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span>  (shown) and ot...
Published: 01 April 2012
Figure 1 Axial section parameters measured in Operculina ammonoides (shown) and other species (see Table 1 ). Chamber lumen area (in gray) and center of gravity (x) for each half whorl must be obtained by image analysis. Circles represent identical area of each half-volution lumen
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Scanning micrographs of operculinid foraminifera. 1.  <span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span>...
Published: 01 January 2004
TEXT-FIGURE 2 Scanning micrographs of operculinid foraminifera. 1. Operculina ammonoides (Gronovius), Sesoko Transect, sample Sesoko-11/1, 40m depth; 2. Operculina elegans Cushman, Minna Jima Transect, 40m depth; 3. Operculina complanata (Defrance), Sesoko Transect, sample Sesoko-4, 60m
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<span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span> ; relation between test diameter and test thickness f...
Published: 01 January 2004
TEXT-FIGURE 4 Operculina ammonoides ; relation between test diameter and test thickness for different samples. Regression by power function: broken line – using the average of species ( a k ) as the integrative constant, full line – using the average over all species ( a ) as the integrative
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Correlation between characters in the species  <span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span>  with ...
Published: 01 January 2004
TABLE 10 Correlation between characters in the species Operculina ammonoides with strong depth dependence of some characters, and Planostegina operculinoides with no depth dependence. Comparison of correlation matrices based on Pearson’s correlation coefficient with partial correlation
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Competition between  <span class="search-highlight">Operculina</span> <span class="search-highlight">ammonoides</span> – O. complanata,  and between  P...
Published: 01 January 2004
F igure 16. Competition between Operculina ammonoides – O. complanata, and between Planostegina longisepta–P. operculinoides at the northern transect of Sesoko Island.
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Differentiation between  <span class="search-highlight">Operculina</span> elegans  (empty dots) and  <span class="search-highlight">Operculina</span> a...
Published: 01 January 2004
TEXT-FIGURE 3 Differentiation between Operculina elegans (empty dots) and Operculina ammonoides (full dots) according to the relation between test diameter and thickness from two stations of the Sesoko transect; fit by power regression: Operculina ammonoides – full line, Operculina
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1–3  <span class="search-highlight">Operculina</span> discoidalis  (d’Orbigny), lateral and axial views, specimen...
Published: 01 January 2000
and others, 1999 ). 7–9 Operculina ammonoides (Gronovius), semiinvolute form, lateral and axial views, specimens from 19 m in the lagoon NE of Sesoko Island. 10–12 Operculina ammonoides (Gronovius), evolute form with strong sculptures, specimens from 30 m depth south of Amakusa Island (Fig. 1 ). All
Journal Article
Published: 01 October 2003
Journal of Foraminiferal Research (2003) 33 (4): 277–284.
... characterized by septate chambers ( Heterostegina depressa, Planostegina operculinoides , and Cycloclypeus carpenteri ) either group with species lacking septate chambers ( Operculina ammonoides, Nummulites venosus ) or branch separately. This suggests that chamber subdivisions developed several times...
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Journal Article
Journal: PALAIOS
Published: 01 May 2017
PALAIOS (2017) 32 (5): 321–329.
... are Operculina ammonoides , Heterostegina depressa , and Palaeonummulites venosus and fossil taxa used are Nummulites perforatus , N. fabianii , and N. tavertetensis (only A forms were used in this study). Our results seem to differentiate the hydrodynamic behavior of shells collected from banks from those...
FIGURES | View All (5)
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Micro-CT graphs of  Palaeonummulites venosus  (upper row) and  <span class="search-highlight">Operculina</span> a...
Published: 01 April 2012
Figure 3 Micro-CT graphs of Palaeonummulites venosus (upper row) and Operculina ammonoides (lower row). a micrograph showing all chambers; b equatorial section; c axial section cutting the final chamber; d areas of shell lumina in axial section.
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1–6  <span class="search-highlight">Operculina</span> discoidalis  (d’Orbigny).  1, 3, 5  photomicrographs.  2, 4...
Published: 01 January 2000
PLATE 2 1–6 Operculina discoidalis (d’Orbigny). 1, 3, 5 photomicrographs. 2, 4, 6 X-ray micrographs, specimens from 19 m in the lagoon NE of Sesoko Island ( Hohenegger and others, 1999 ). 7–12 Operculina ammonoides (Gronovius). 7, 9, 11 photomicrographs. 8, 10, 12 X-ray micrographs
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—Composition of average and typical samples of main classes of sediments in...
Published: 01 March 1959
Fig. 17. —Composition of average and typical samples of main classes of sediments in facies belts from active-water areas. Station numbers refer to Figure 2 . 1= Amphistegina madagascariensis 2= Amphistegina lessonii 3 = Marginopora vertebralis 4 = Operculina ammonoides
Journal Article
Published: 01 January 2004
Micropaleontology (2004) 50 (2): 149–177.
...TEXT-FIGURE 2 Scanning micrographs of operculinid foraminifera. 1. Operculina ammonoides (Gronovius), Sesoko Transect, sample Sesoko-11/1, 40m depth; 2. Operculina elegans Cushman, Minna Jima Transect, 40m depth; 3. Operculina complanata (Defrance), Sesoko Transect, sample Sesoko-4, 60m...
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Journal Article
Published: 01 April 2012
Journal of Foraminiferal Research (2012) 42 (2): 134–142.
...Figure 1 Axial section parameters measured in Operculina ammonoides (shown) and other species (see Table 1 ). Chamber lumen area (in gray) and center of gravity (x) for each half whorl must be obtained by image analysis. Circles represent identical area of each half-volution lumen...
FIGURES | View All (5)
Journal Article
Published: 01 January 2000
Journal of Foraminiferal Research (2000) 30 (1): 3–28.
... and others, 1999 ). 7–9 Operculina ammonoides (Gronovius), semiinvolute form, lateral and axial views, specimens from 19 m in the lagoon NE of Sesoko Island. 10–12 Operculina ammonoides (Gronovius), evolute form with strong sculptures, specimens from 30 m depth south of Amakusa Island (Fig. 1 ). All...
FIGURES | View All (12)
Journal Article
Published: 01 January 2004
Journal of Foraminiferal Research (2004) 34 (1): 9–33.
...F igure 16. Competition between Operculina ammonoides – O. complanata, and between Planostegina longisepta–P. operculinoides at the northern transect of Sesoko Island. ...
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(A) Planktic foraminifera mounted on double-sided carbon tape prior to inse...
Published: 22 October 2024
+ ], 10× natural 135 Ba/ 138 Ba, driving seawater and therefore test Mg/Ca to lower values) in the laboratory versus chambers precipitated prior to collection of the specimens ( Operculina ammonoides data from Hauzer et al., 2018 ). Each data point represents the mean of an analysis of an individual