identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
7668E43BFFCBFFDFBD344E30FBFA166C.text	7668E43BFFCBFFDFBD344E30FBFA166C.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Nephrolepidina praemarginata (Douville 1908)	<html xmlns:mods="http://www.loc.gov/mods/v3">
    <body>
        <div>
            <p> Nephrolepidina praemarginata (Douvillé, 1908) (Fig. 5 D-G) </p>
            <p> Lepidocyclina praemarginata Douvillé, 1908: 91-92 , figs 1, 2, 4a. </p>
            <p> Nephrolepidina praemarginata – Douvillé 1924: 51-123, pl. 6, figs 4, 6. — Gomez Llueca 1929: 1-400, pl. 32, figs 4-10. — Flandrin 1935: 251-272, pl. 15, figs 14-18. — Poignant 1967: 197-211, pl. V, fig. 2. — Gedik 2014: 101, pl. 6, figs 1-14. </p>
            <p>REMARKS</p>
            <p>The identification is based only upon axial sections. The small test is inflated, lenticular with a central umbo, so that the shell is thicker towards the center. The diameter of the test ranges from 1.5 to 2.1 mm and the thickness from 0.6 to 0.9 mm. The large, central umbo consists of numerous small pustules (Fig. 5E, G). Lateral chambers are numerous at the surface of test and rosette shaped, and this feature forms a comb-like surface appearance (Fig. 5E). The embryo consists of subspherical small protoconch (diameter 0.25 mm) and reniform deuteroconch (diameter 0.22 mm). Secondary chambers are very small and their sizes are almost equal to each other. The equatorial chambers are subrectangular or rhombic in outline. There are 6-7 orders of lateral chambers in the center of the test.</p>
        </div>
    </body>
</html>
	https://treatment.plazi.org/id/7668E43BFFCBFFDFBD344E30FBFA166C	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		Plazi	Gedik, Fatma;Karadenizli, Levent	Gedik, Fatma, Karadenizli, Levent (2021): Oligocene larger benthic foraminifera and sedimentation of the Burdur Basin, SW Anatolia, Turkey. Geodiversitas 43 (13): 377-389, DOI: 10.5252/geodiversitas2021v43a13
7668E43BFFCBFFDFBEA84C52FDBB172E.text	7668E43BFFCBFFDFBEA84C52FDBB172E.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Nummulites fichteli Michelotti 1841	<html xmlns:mods="http://www.loc.gov/mods/v3">
    <body>
        <div>
            <p> Nummulites fichteli Michelotti, 1841</p>
            <p>(Fig. 4 A-J; 5C, J)</p>
            <p> Nummulites fichteli Michelotti, 1841: 296 , figs 7a, b. — Cole 1960: pl. 3, figs 9-18. — Schaub 1981: pl. 50, figs 5-18. — Sirel 2003: pl. II, figs 12-19. — Gedik 2008: pl. 1, figs 1-14, 22. </p>
            <p> Nummulites intermedius D’Archiac, Sirel &amp; Gündüz, 1976 : pl. I, figs 5-9. </p>
            <p>REMARKS</p>
            <p> This reticulate species belongs to the  N. fabianii lineage. This form has inflated lenticular shell with rounded periphery. The diameter of test ranges from 2 to 6.4 mm and the thickness from 0.5 to 1.8 mm. The test surface is covered with a reticulation that has rectangular or subrectangular mesh (Fig. 4A, C-E; Fig. 5C). The large microsphere (diameter 0.3 to 0.4 mm) is followed by the regular coiled whorls. </p>
        </div>
    </body>
</html>
	https://treatment.plazi.org/id/7668E43BFFCBFFDFBEA84C52FDBB172E	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		Plazi	Gedik, Fatma;Karadenizli, Levent	Gedik, Fatma, Karadenizli, Levent (2021): Oligocene larger benthic foraminifera and sedimentation of the Burdur Basin, SW Anatolia, Turkey. Geodiversitas 43 (13): 377-389, DOI: 10.5252/geodiversitas2021v43a13
7668E43BFFCBFFDFBEB64AF4FEE115AF.text	7668E43BFFCBFFDFBEB64AF4FEE115AF.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Operculina complanata (Defrance 1822)	<html xmlns:mods="http://www.loc.gov/mods/v3">
    <body>
        <div>
            <p> Operculina complanata (Defrance, 1822) (Fig. 5A, B) </p>
            <p> Lenticulites complanata Defrance, 1822: 453 . </p>
            <p> Operculina complanata – Souaya 1963: pl. 53, figs 1, 2. — Cherif 1980: pl. I, figs 4, 10; pl. II, figs 1, 5. — Abdelgany 2002: pl. II, figs 2-4. — Sirel 2003: pl. III, figs 1-9. — Gedik 2008: pl. 2, figs 6-10. </p>
            <p>REMARKS</p>
            <p>The test is thin, bilateral and symmetric. Its diameter ranges from 2.5 to 2.9 mm, and the thickness from 0.4 to 1.8 mm. The test is planispiral and evolute, with numerous narrow chambers in many rapidly expanding whorls, so that the height of the chambers may be five times the width of the chambers (Fig. 5A, B). The proloculus is spherical and small (90 µ diameter).</p>
        </div>
    </body>
</html>
	https://treatment.plazi.org/id/7668E43BFFCBFFDFBEB64AF4FEE115AF	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		Plazi	Gedik, Fatma;Karadenizli, Levent	Gedik, Fatma, Karadenizli, Levent (2021): Oligocene larger benthic foraminifera and sedimentation of the Burdur Basin, SW Anatolia, Turkey. Geodiversitas 43 (13): 377-389, DOI: 10.5252/geodiversitas2021v43a13
