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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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Orbitolites tenuissimus, Carpenter MSS..
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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Loeblich, A. R., Tappan, H. N., 1987: Foraminiferal genera and their classification. Van Nostrand, Reinhold Co. New York 1728 pp. Plate 406, Figs. 1-6: U. Cretaceous (U. Cenomanian-L. Turonian); 1-6, Bi'na Formation, Galilee, Israel; 1, Horizontal section, x 75; 2, nearly equatorial section, megalospheric, x 75; 3, nearly axial section, x 75; 4, vertical section becoming tangential in central part and showing many apertural pores, x 75; 5, nearly equatorial section of megalospheric test in incident light, x 20; 6, nearly equatorial section of microspheric test, x 30 (from Hamaoui, 1964). courtesy of Michael Hesemann https://foraminifera.eu
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left - Syntype, IPC no. M/2696 (BMNH no. P 35785), equatorial section of ?microspheric form. right -Syntype, IPC no. M/2434 I (BMNH no. P 35786), oblique section through rectilinear stage.
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Holotype in equatorial-longitudinal section
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Holotype in oblique to near-equatorial section
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Archaias angulatus sensu Jones, R.W. 1994. The Challenger Foraminifera. Image source: Brady, H.B. (1884) Pl. 14