identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
0390879F3842FFB42DB7FC0EE37AFA2D.text	0390879F3842FFB42DB7FC0EE37AFA2D.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Actinastrea d'Orbigny 1849	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Actinastrea d’Orbigny, 1849</p>
            <p> Type species.  Actinastrea goldfussi d’Orbigny, 1850 a, 1850b , Maastrichtian of Te Netherlands (Maastricht). </p>
            <p>Diagnosis. Corallum colonial, often massive to subcolumnar, cerioid, cerio-plocoid. Budding extracalicular and extracalicular-marginal. Corallites small and prismatic in outline, often directly united by their walls. Columella styliform or short-lamellar. No intercalicinal coenosteum. Synapticular structures present peripherally. Paliform structures occasionally present. Endothecal dissepiments thin, sometimes arranged forming an innercorallite ring which is complete or incomplete. Septa compact, generally non-confluent, radially or bilaterally arranged, beaded marginally, and composed of a series of simple trabeculae, varying in diameter (up to 150 µm). Septal flanks covered by spiniform granulae. Wall septothecal to septoparathecal, with occasionally occurring pores (lacunes).</p>
            <p> Actinastrea pseudominima (Koby, 1897)</p>
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	https://treatment.plazi.org/id/0390879F3842FFB42DB7FC0EE37AFA2D	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3842FFB42DBDFDA5E37BFC96.text	0390879F3842FFB42DBDFDA5E37BFC96.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Actinastreidae Alloiteau 1952	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Actinastreidae Alloiteau, 1952</p>
            <p> Remarks. In some recent publications (e.g., Garberoglio, et al., 2020; Löser, 2012), material was grouped with the family  Actinastreidae that showed characteristics of families such as  Columastreidae ,  Cladophylliidae , and others (e.g., Baron-Szabo, 2014, p. 20; and discussion in Baron-Szabo, 2021b under  Cladophyllia crenata ). Terefore, a combination of the family concepts by Alloiteau (1954) and Baron-Szabo (2014) is followed. </p>
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	https://treatment.plazi.org/id/0390879F3842FFB42DBDFDA5E37BFC96	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3845FFB32DBDFD22E079FB10.text	0390879F3845FFB32DBDFD22E079FB10.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Complexastrea d'Orbigny 1850	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Complexastrea d’Orbigny, 1850b</p>
            <p>  Type species.  Complexastrea subburgundiae d’Orbigny, 1850b ,  Jurassic (‘Corallien’) of France  . </p>
            <p>Diagnosis. Colonial, often massive to subhemispherical, subbranching to subflabellate during various stages of astogeny, present or absent. Polyp integration astreoid, plocoid to cerio-plocoid; submeandroid to thamnasterioid integration during various stages of astogeny present or absent. Budding intracalicular and extracalicular. Costosepta compact, non-confluent to confluent, granulated and carinate laterally. Teir axial ends can be rhopaloid. Columella absent or formed by weakly parietal structures. No pali. Synapticulae absent. Intertrabecular distance ranging between 200 and 1300 µm. Endothecal dissepiments pass from one corallite to the next, they are vesicular, cellular, or tabuloid. Wall absent or paraseptothecal.</p>
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	https://treatment.plazi.org/id/0390879F3845FFB32DBDFD22E079FB10	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3845FFB12DBDFB62E325F951.text	0390879F3845FFB12DBDFB62E325F951.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Complexastrea zolleriana (Quenstedt 1879)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Complexastrea zolleriana (Quenstedt, 1879)</p>
            <p>Figs. 7B–F</p>
            <p> *1879  Coenotheca zolleriana : Quenstedt, p. 609, Pl. 165 figs. 36-43. </p>
            <p> (v)1996  Complexastrea zolleriana (Quenstedt) : Lathuilière, p. 597, Pl. 72, Fig. 1 –18, Pl. 73, Fig. 1 –13, Pl. 74, Fig. 1–4, Pl. 75, Fig. 1–7, Text-Figs. 5–6, 8–11 [older synonyms cited therein]. </p>
            <p> pars(v)2003  Montlivaltia decipiens (Goldfuss 1826) : Pandey &amp; Fürsich, p. 42–43, Pl. 10, Fig. 7–10, [?Pl. 8, Fig. 6]. </p>
            <p> (v)2003  Latiphyllia cf. confluens (Quenstedt, 1843) : Pandey &amp; Fürsich, p. 44–46, Pl. 11, Fig. 1. </p>
            <p> (v)2003  Coenotheca zolleriana Quenstedt, 1881 : Pandey &amp; Fürsich, p. 46–48, Pl. 11, Fig. 2–6. </p>
            <p>Dimensions. Great diameter of corallites: 10–30 mm; in areas of intense budding around 8 mm; septa/corallite: up to around 100, in corallites in areas of intense budding around 20; septa/mm: 3–9/5; distance of corallite centers: 5–21 mm; septal thickness ranges between 100 and 1300 µm.</p>
            <p> Description. Individual specimens are in various transgeneric stages including (1) cerio-plocoid to astreoid corallites in subflabellate arrangement (resembling  Latiphyllia ); (2) small submassive clumps consisting of a few polyps in subplocoid to submeandroid-thamnasterioid arrangement (resembling  Coenotheca ); and (3) tall corallum with subplocoid corallites (resembling Tecosmilia); costosepta straight to very wavy; endothecal dissepiments numerous, large vesicular peripherally, cellular to vesicular in central areas of corallum. </p>
            <p>  Type locality of species.  Middle Jurassic (“Brauner Jura gamma”) of Germany (Hohenzollern)  . </p>
            <p>Distribution. Middle Jurassic of France, Germany, and Iran, lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper).</p>
            <p>Material. NMSG Coll. PK–02.10.20a, 20b (= 02.10.21a), and 20c; –02.10.21c; –02.10.25a-II; –02.10.27c-A. –02.10.27c-B; –02.10.27d; –02.10.36;?–02.10.38.</p>
            <p> Remarks. Based on a population study including Middle Jurassic thecosmiliid corals, Lathuilière (1996) established a morphogenesis framework for the genus  Complexastrea using individuals that, with regard to the dimensions of their skeletal elements, correspond to the species  zolleriana . He came to the conclusion that during various stages of astogeny forms of the genus  Complexastrea show morphological overlaps with several other thecosmiliid genera such as  Coenotheca ,  Latiphyllia ,  Montlivaltia , and Tecosmilia. As a result, specimens that might show close resemblance to one of these genera are grouped with  Complexastrea . While this approach has not been accepted by some authors (e.g., Pandey &amp; Fürsich, 2003), it is followed here based on the fact that the genus  Complexastrea shows features that clearly distinguishes it from the genera with which it shows morphological convergence during different stages of astogeny. In having both extracalicular budding in addition to intracalicular multiplication and a paraseptothecal wall,  Complexastrea differs from genera such as  Latiphyllia and Tecosmilia (=characterized by intracalicular multiplication and the lack of septothecal thickenings). In its early (“solitary”) stage,  Complexastrea closely resembles the solitary genus  Montlivaltia but shows features such as (1) cerio-plocoid shapes and often paraseptothecal developments in the peripheral areas; (2) a rather flat to cupolate corallum; and (3) the presence of budding spots (“generator septa” and “linking septa” sensu Lathuilière [1996, Text-Fig. 10A ‒ B]) from which new corallites develop, closely corresponding to the situation in other genera such as the cunnolitid genus  Aspidastraea which can be misinterpreted for the solitary genus  Cunnolites in its early stages of astogeny (Baron-Szabo, 2003). In contrast to the “  Montlivaltia ”- stage of  Complexastrea , the genus  Montlivaltia is variably conical (rarely subdiscoidal-patellate in certain environments), and lacks both septothecal thickenings and budding spots. Te genus  Coenotheca very closely corresponds to the juvenile stage of  Complexastrea and is, therefore, considered to be a junior synonym of  Complexastrea . </p>
            <p>(See figure on next page.)</p>
            <p> Fig. 8 A  Placophyllia cf. dianthus (Goldfuss, 1826) , NMSG Coll. PK 02.10.26a; calicular view, polished surface; scale bar: 2.5 mm. B  Placophyllia cf. dianthus (Goldfuss, 1826) , NMSG Coll. PK 02.10.26a;calicular view, thin section; scale bar: 2.5 mm. C  Placophyllia cf. dianthus (Goldfuss,1826) , NMSG Coll. PK 02.10.27a; calicular view, polished surface; scale bar: 2.5 mm. D  Placophyllia cf. florosa Eliášová,1976b , NMSG Coll. PK 02.10.28a;calicular view, polished surface;scale bar: 3 mm. E  Placophyllia cf. florosa Eliášová,1976b , NMSG Coll.PK 02.10.31a;calicular view, thin section; scale bar: 2.5 mm. </p>
            <p> F  Dermosmilia sp. , NMSG Coll.PK 02.10.32a;calicular view, thin section; scale bar: 3.5 mm. G  Fungiastraea lamellosa (de Fromentel,1857) , NMSG </p>
            <p> Coll. PK 02.10.16b; upper surface of colony, calicular view; scale bar: 4 mm. H  Fungiastraea lamellosa (de Fromentel, 1857) , NMSG Coll. PK 02.10.28h; calicular view, thin section; scale bar: 2 mm. I  Actinaraea tenuis Morycowa,1971 , NMSG Coll. PK 02.10.30e; calicular view of colony, thin section; </p>
            <p> scale bar: 2 mm. J  Actinaraea tenuis Morycowa, 1971 , NMSG Coll. PK 02.10.28e; calicular and longitudinal view of colony, polished surface; scale bar: 3.5 mm. K  Latiastrea mucronata Sikharulidze, 1979 , NMSG Coll. PK 02.10. 22 g; calicular view of colony, polished surface; scale bar: 3 mm. L  Latiastrea mucronata Sikharulidze,1979 , NMSG Coll. PK 02.10. 22 g; close-up of Fig. M, scale bar: 1 mm. M  Latiastrea mucronata Sikharulidze,1979 , NMSG Coll. </p>
            <p>PK 02.10. 22 g; calicular view, thin section; scale bar: 2 mm</p>
            <p> Individual specimens from the Vitznau Marl correspond to different morphotypes of the species  C. zolleriana . Te specimen NMSG Coll. PK-02.10.20a resembles the “  Latiphyllia ” variation as shown in Lathuilière (1996, Pl. 72, Figs. 8 and 15, and Text-Fig. 10A–B); the specimens NMSG Coll. PK-02.10.20c, 02.10.25a-II, and 02.10.36 show close affinities to the “  Coenotheca ” morphotype as shown in Lathuilière (1996, Pl. 72, Figs. 7 and 10); the specimen NMSG Coll. PK-02.10.20b (= 02.10.21a) resembles the “ Tecosmilia ” variation as shown in Lathuilière (1996, Pl. 72, Fig. 5); the specimen NMSG Coll. PK-02.10.21c corresponds to a mix of transgeneric stages including variation of “  Complexastrea –  Coenotheca –Tecosmilia ” as shown in Lathuilière (1996, Pl. 73, Fig. 5–8); and the specimens NMSG Coll. PK-02.10.27c-A and B, and –02.10.27d show close affinities to early stages of astogeny of  Complexastrea , corresponding to a mix of “  Coenotheca –  Montlivaltia ” morphotypes as shown in Lathuilière (1996, Pl. 72, Figs. 3 and 6). </p>
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	https://treatment.plazi.org/id/0390879F3845FFB12DBDFB62E325F951	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3847FFB12D87F920E51DFE96.text	0390879F3847FFB12D87F920E51DFE96.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Montlivaltia Lamouroux 1821	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Montlivaltia Lamouroux, 1821</p>
            <p>  Type species.  Montlivaltia caryophyllata Lamouroux, 1821 ,  Middle Jurassic (Upper Bathonian) of Calvados  . </p>
            <p>Diagnosis. Solitary, trochoid to subcylindrical, or turbinate, rarely (subdiscoidal-) patellate. Costosepta compact, thin to thick, exsert, in general numerous and crowded. Columella absent. Intertrabecular distance ranging between 200 and 1300 µm. Endothecal dissepiments abundant, vesicular. Epitheca sensu lato membraniform or absent.</p>
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	https://treatment.plazi.org/id/0390879F3847FFB12D87F920E51DFE96	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3847FFB12E07FEE5E2B3F85C.text	0390879F3847FFB12E07FEE5E2B3F85C.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Montlivaltia truncata (Defrance 1817)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Montlivaltia truncata (Defrance, 1817)</p>
            <p>Figs. 7G–J</p>
            <p> *1817  Caryophyllia truncata : Defrance, vol. 7, p. 198. v1954  Montlivaltia truncata (Defrance) 1817 : Geyer, 1954, p. 174 [older synonyms cited therein]. </p>
            <p> (v)1977  Montlivaltia truncata Defrance, 1817 : Beauvais, in Beauvais &amp; M’Rabet, p. 109, Pl. 1, Fig. 3a–b, Pl. 2, Fig. 2 [older synonyms cited therein]. </p>
            <p> (v)1977  Montlivaltia sioufensis nov. sp. : Beauvais, in Beauvais &amp; M’Rabet, p. 112, Pl. 3, Fig. 1. </p>
            <p> (v)1994  Montlivaltia xizangensis Liao et Xia : Liao &amp; Xia, p. 158, Pl. 43, Figs. 9 –14 and 20–23. </p>
            <p> v2018  Montlivaltia truncata (Defrance, 1817) : Baron-Szabo, p. 38–39, Pl. 2, Figs. I–J [older synonyms cited therein]. </p>
            <p>Dimensions. Corallite diameter at top of corallum (d x D): 12 × 18 mm (estimated); d/D = 0.67; diameter at basal part of corallum (d x D): 10 × 12 mm (estimated); d/D = 0.83; septa at top of corallum; probably 96; septa at basal part: around 40; septa/mm (peripheral area of corallite): 7–10/5; height of corallum: at least 35 mm.</p>
            <p>Description. Incomplete solitary, turbinate, corallum; septa straight, regularly alternate in length and thickness, probably developed in 5 complete cycles in 6 systems at top of corallum; endothecal dissepiments numerous, long, mainly vesicular; membraniform epitheca sensu lato present.</p>
            <p>  Type locality of species.  Upper Jurassic of France  . </p>
            <p>Distribution. Upper Jurassic of France, Germany, and Switzerland, upper Oxfordian of Azerbaijan and Georgia (in Caucasus), upper Oxfordian–lower Tithonian of Russia, Kimmeridgian of Portugal, Berriasian of central Tibet, upper Berriasian of northern Tunisia and northeastern Switzerland (upper Őhrli Formation), lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper).</p>
            <p>Material. NMSG Coll. PK–02.10.25a (= 02.10.22d).</p>
            <p> Remarks. Because the specimen is incomplete the full range of its dimensions of skeletal elements can only be estimated. Te dimensions found in the Swiss material closely correspond to the ones of  M. truncata . </p>
            <p> Te species  M. truncata was recently discussed and revised (Baron-Szabo, 2018). For further synonyms of the species  M. truncata , see Paleobiology Database (paleo biodb.org). </p>
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	https://treatment.plazi.org/id/0390879F3847FFB12E07FEE5E2B3F85C	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3846FFB02DBDFC85E073F9B1.text	0390879F3846FFB02DBDFC85E073F9B1.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Placophyllia dianthus (Goldfuss 1826)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Placophyllia cf. dianthus (Goldfuss, 1826)</p>
            <p>Figs. 8A–C</p>
            <p> v*1826  Lithodendron dianthus : Goldfuss, p. 45, Pl. 3, Fig. 8. </p>
            <p> v1876  Placophyllia? rugosa Beck. : Becker, p. 140, Pl. 38, Fig. 9a–b (older synonyms cited therein). </p>
            <p> 1985  Placophyllia dianthus (Goldfuss, 1826) : Rosendahl, p. 49, Pl. 1, Fig. 10. </p>
            <p> 1989  Placophyllia cf. dianthus (Goldfuss) : Beauvais, p. 295. </p>
            <p> 1990  Placophyllia rugosa Becker, 1876 : Eliášová, p. 121, pl. 2, Fig. 1. </p>
            <p> v1991  Placophyllia dianthus (Goldfuss, 1826) : Lauxmann, p. 155, Text–Fig. 15. </p>
            <p> v1997  Placophyllia rugosa Becker, 1876 :  Turnšek , p. 153, Figs. 153A–F. </p>
            <p> 2003  Placophyllia dianthus (Goldfuss, 1826) : Kołodziej, p. 213, Fig. 27 [older synonyms cited therein]. </p>
            <p> 2005  Placophyllia cf. dianthus (Goldfuss, 1826) : Morycowa &amp; Mišik, 2005, p. 420, Fig. 3.5. </p>
            <p> 2008  Placophyllia rugosa Becker, 1876 : Roniewicz, p. 104, Figs. 6E–F. </p>
            <p> v2018  Placophyllia dianthus (Goldfuss, 1826) : Baron-Szabo, p. 48, Pl. 5, Fig. A–B, D–E [older synonyms cited therein]. </p>
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	https://treatment.plazi.org/id/0390879F3846FFB02DBDFC85E073F9B1	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3846FFB02E07FB01E5E7FABC.text	0390879F3846FFB02E07FB01E5E7FABC.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Placophyllia florosa Eliasova 1976	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Placophyllia cf. florosa Eliášová, 1976b</p>
            <p>Figs. 8D–E</p>
            <p> v*1976b  Placophyllia florosa n. sp: Eliášová, p. 339, Pl. 3, Figs. 1–2. </p>
            <p> 2018  Placophyllia cf. florosa Eliášová, 1976 : Ricci, et al., 2018, p. 451–453, Pl. 7, Fig. 1a–1c. </p>
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	https://treatment.plazi.org/id/0390879F3846FFB02E07FB01E5E7FABC	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3846FFB02DBDFF65E3C5FD36.text	0390879F3846FFB02DBDFF65E3C5FD36.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Placophylliidae Eliasova 1990	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Placophylliidae Eliášová, 1990 Genus  Placophyllia d’Orbigny, 1849</p>
            <p>  Type species.  Lithodendron dianthus Goldfuss, 1827 ,  Upper Jurassic of Germany (Giengen)  . </p>
            <p>Diagnosis. Colonial, mainly phaceloid, can be subdendroid or fasciculate with plocoid to cerioid polyp outlines in younger colonies. Budding extracalicular and intracalicular-marginal. Costosepta compact, septal flanks covered by small granules. Distal edge of septa smooth. In closely packed corallites costae may be subconfluent. Columella lamellar. Synapticulae and pali absent. Intertrabecular distance ranging between 40 and 130 µm in septa. Corallite wall parathecal, irregular. Septothecal thickenings present or absent. Endothecal dissepiments vesicular in peripheral corallite areas and subtabulate in axial corallite areas. Epithecal sensu lato wall folded.</p>
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	https://treatment.plazi.org/id/0390879F3846FFB02DBDFF65E3C5FD36	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3849FFBF2DBDFD9CE040FA5E.text	0390879F3849FFBF2DBDFD9CE040FA5E.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Dermosmiliidae Koby 1887	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Dermosmiliidae Koby, 1887 Genus  Dermosmilia Koby, 1884</p>
            <p> Type species.  Dermosmilia crassa Dacqué, 1933 , Upper Jurassic (Rauracian) of Switzerland (subsequent designation Dacqué, 1933). </p>
            <p>Diagnosis. Colonial, dendroid, phaceloid, fasciculate, subflabellate. Corallites nearly circular to subflabellate in outline. Budding intracalicular, di- to polystomodaeal, complete. Corallites united only basally. Costosepta generally compact to subcompact, sometimes irregularly perforated, straight or irregularly wavy, laterally granulated. Anastomosis present or absent. When present, septa may be arranged during various stages of ontogeny in a pattern resembling the kinds seen in micrabaciid or dendrophylliid genera (similar to Pourtalès plan). Columella spongy-papillose or formed by fusion of trabecular prolongations of axial ends of septa. Synapticulae present. Intertrabecular distance ranging between 80 and 300 µm. Endothecal dissepiments thin, vesicular to subtabulate. Wall parathecal to parasynapticulothecal, often secondarily thickened.</p>
            <p> Remarks. Te above given diagnosis for  Dermosmilia is based on both the study of material from Caquerelle and Sante-Ursanne strata from various localities of the Koby collections housed at the museums in Basel and Bern, and the information provided by Koby (1884, p. 194–195, Pl. 50, Figs. 1–6). </p>
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	https://treatment.plazi.org/id/0390879F3849FFBF2DBDFD9CE040FA5E	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3849FFBF2E07FF65E451FCB1.text	0390879F3849FFBF2E07FF65E451FCB1.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Haplaraeidae Vaughan & Wells 1943	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Haplaraeidae Vaughan &amp; Wells, 1943 Genus  Actinaraea d’Orbigny, 1849</p>
            <p>  Type species.  Agaricia granulata Münster , in  Goldfuss , 1829, Upper Jurassic of Germany (Nattheim)  . </p>
            <p>Diagnosis. Colonial, massive, folios, thamnasterioid, including ploco- to cerio-thamnasterioid. Budding intracalicular (-marginal). Corallites embedded in a coenosteum that is generally porous to reticulate. Costosepta few in number with irregular perforations, septal flanks granular. No paliform structures. Columella generally feebly developed, parietal, lamellar, substyliform. Synapticulae present. Intertrabecular distance ranging between 80 and 180 µm. Endothecal dissepiments thin, tabulate. Wall absent or incomplete synapticulothecal.</p>
            <p> Subgenus.  Camptodocis Dietrich, 1926 (Type species.  C. brancai Dietrich, 1926 , Barremian–lower Aptian of Tanzania): Having the characteristics of  Actinaraea but calices are not independent from perithecal colony tissue (similar as in  Actinacis ), corallites therefore with variably ploco- to cerio-thamnasterioid integration types. </p>
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	https://treatment.plazi.org/id/0390879F3849FFBF2E07FF65E451FCB1	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3849FFBE2E07FC05E336FC96.text	0390879F3849FFBE2E07FC05E336FC96.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Actinaraea tenuis Morycowa 1971	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Actinaraea tenuis Morycowa, 1971</p>
            <p>Figs. 8I–J</p>
            <p> (v)*1971  Actinaraea tenuis n. sp. : Morycowa, p. 128– 130, Pl. 35, Fig. 1a–d, Pl. 36, 1a–c, Text-Fig. 37. </p>
            <p> 1980  Actinaraea tenuis Morycowa, 1971 : Kuzmicheva, p. 106–107, Pl. 39, Fig. 4a–b. </p>
            <p> non1984  Actinaraea sp. aff.  A. tenuis Morycowa, 1971 : Scott, p. 344, Pl. 2, Figs. 12–13. </p>
            <p> 1992  Actinaraea cf.  A. tenuis Morycowa, 1971 :  Turnšek , 1992, p. 164, Fig. 2. </p>
            <p> v1996  Actinaraea tenuis Morycowa, 1971 : Wilmsen, 1996, p. 361, Pl. 4, Fig. 3. </p>
            <p> 1996  Actinaraea tenuis Morycowa, 1971 : Császár &amp;  Turnšek , p. 430, Fig. 7 (6). </p>
            <p> v1997  Actinaraea tenuis Morycowa, 1971 : Baron-Szabo, p. 79, Pl. 12, Fig. 1–2 [older synonyms cited therein]. </p>
            <p> 2003  Actinaraea tenuis Morycowa, 1971 :  Turnšek , et al., p. 179, Figs. 12A–B. </p>
            <p> v2014  Actinaraea tenuis Morycowa, 1971 : Baron-Szabo, p. 53, Pl. 58, Fig. 3 Pl. 59, Fig. 1–2. </p>
            <p> v2021b  Actinaraea tenuis Morycowa, 1971 : Baron-Szabo, p. 54, Pl. 8, Fig. A. </p>
            <p>Dimensions. Corallite diameter: 1–1.7 mm; distance of corallite centers: 2.3–4.5 mm; septa/corallite: up to around 24; septa/mm: 6–8/2; synapticulae (longitudinal view)/mm: 3–4/1.</p>
            <p>Description. Submassive to foliose, thamnasterioid colony; corallites subdistinct to indistinct, regularly disposed over the colony; septa confluent to subconfluent; 6–8 septa reach corallite center; columella substyliform or made of a small number of thin, twisted segments.</p>
            <p>  Type locality of species.  Lower Aptian of Romania (Valea Izvorul Alb)  . </p>
            <p>Distribution. Lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Valanginian of Hungary, Hauterivian of Georgia (in Caucasus), Barremian–lower Aptian of Serbia, Barremian–Aptian of Slovenia, upper Barremian–lower Aptian of western Austria (Schrattenkalk Formation, Vorarlberg), lower Aptian of Romania and southern Germany (Upper Schrattenkalk, Bavaria), middle Albian of the USA (New Mexico), lower Cenomanian of Spain, lower Coniacian of Austria (Gosau Group at Brandenberg).</p>
            <p>Material. NMSG Coll. PK–02.10.14b; –?02.10.16a; –02.10.23e (= 02.10.29e); –02.10.26c; –02.10.26c-1; –02.10.28e; –02.10.30e; –02.10.37a.</p>
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	https://treatment.plazi.org/id/0390879F3849FFBE2E07FC05E336FC96	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3848FFBE2DBDF980E51CFB71.text	0390879F3848FFBE2DBDF980E51CFB71.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Fungiastraea lamellosa (de Fromentel 1857)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Fungiastraea lamellosa (de Fromentel, 1857)</p>
            <p>Figs. 8G–H</p>
            <p> v*1857 Tamnastraea  lamellosa : de Fromentel, p. 61. v1887 Centastraea  lamellosa : de Fromentel, 1887, p. 617, Pl. 187, Fig. 1–1c. </p>
            <p> 1914 Centastraea  lamellosa : de Fromentel: Felix, 1914, p. 55. </p>
            <p> non1998  Fungiastraea lamellosa (de Fromentel, 1857) : Löser, p. 180. </p>
            <p> non2001  Dimorphastrea cf. lamellosa (de Fromentel, 1857) : Löser, p. 46. </p>
            <p>Dimensions. Diameter of corallites (monocentric): 2–3 mm, in areas of intense budding around 1.5 mm; distance of corallite centers: 2–4 mm; septa/corallite: 18–24 + s, in corallites in areas of intense budding around 12; septa/mm: 5–8/2.</p>
            <p>Description. Tamnasterioid-submeandroid colony; corallites irregularly disposed or arranged in short-meandroid series; septa subequal in thickness; up to 6 septa reach corallite center; columella made of a small number of papillae or twisted segments.</p>
            <p>  Type locality of species.  Lower Hauterivian of France (Yonne)  . </p>
            <p>Distribution. Lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), lower Hauterivian of France (Yonne).</p>
            <p>Material. NMSG Coll. PK–02.10.16b; –02.10.28h.</p>
            <p> Remarks. In having larger dimensions of skeletal elements (corallite diameter: 2.5– 4 mm; septa/corallite: 25–30; septa/mm: 8/2), the material from the lower Cenomanian of Germany provisionally assigned to  lamellosa in Löser (1998) differs from de Fromentel’s species. In forming a dimorphastreid corallum and having smaller dimensions of skeletal elements (septa/ corallite: 16–20 (24); septa/mm: 5–6/2), the material from the lower Hauterivian of France provisionally assigned to the species  lamellosa in Löser (2001) differs from de Fromentel’s species. Te Swiss material corresponds well to the syntype of the species  F. lamellosa (MNHN.F.M03558). </p>
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	https://treatment.plazi.org/id/0390879F3848FFBE2DBDF980E51CFB71	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3848FFBE2E07FB40E490F8D3.text	0390879F3848FFBE2E07FB40E490F8D3.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Latiastrea Beauvais 1964	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Latiastrea Beauvais, 1964</p>
            <p>  Type species.  Latiastrea foulassensis Beauvais, 1964 ,  Upper Jurassic (Kimmeridgian) of France (Valfin-les-Saint-Claude)  . </p>
            <p>Diagnosis. Colonial, massive, cerioid to meandroid. Budding intracalicular. Corallites prismatic, elongate, monocentric, or temporarily dicentric (to?polycentric) during budding processes, or arranged in meandroid series. Costosepta non-confluent to subconfluent, with rare perforations on axial ends of septa. Anastomosis present. Rudimentary young septa alternate with old ones. Septal flanks are ornamented with large, spiniform granulae. Pennulae present. Distal margins covered with small, regularly developed rounded denticles. Synapticulae present. Columella parietal-spongy, sometimes forming elongate segments. Intertrabecular distance ranging between 100 to around 200 µm. Endothecal dissepiments thin, vesicular. Wall synapticulothecal and septothecal.</p>
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	https://treatment.plazi.org/id/0390879F3848FFBE2E07FB40E490F8D3	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3848FFBE2DBDFC40E3CEFA30.text	0390879F3848FFBE2DBDFC40E3CEFA30.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Latomeandridae Alloiteau 1952	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Latomeandridae Alloiteau, 1952 Genus  Fungiastraea Alloiteau, 1952</p>
            <p>  Type species.  Fungiastraea laganum Alloiteau, 1952 ,  Upper Turonian of France (Uchaux, Vaucluse)  . </p>
            <p>Diagnosis. Colonial, massive, thamnasterioid to submeandroid. Budding intracalicular, occasionally extracalicular. Corallite centers distinct. Septa compact to subcompact, confluent, moderately granulated and pennulated laterally. Sub- to non-confluent septa sparse, occurring in areas of extracalicular budding. Columella spongy, papillose, or variably shaped when columellar trabeculae fuse. Paliform structures absent. Synapticulae present. Intertrabecular distance ranging between 90 to around 350 µm. Endothecal dissepiments thin, vesicular to subtabulate. No wall between corallites but parasynapticulothecal developments circumscribing some parts of corallites sometimes present.</p>
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	https://treatment.plazi.org/id/0390879F3848FFBE2DBDFC40E3CEFA30	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3848FFBD2E07F8A0E006FB30.text	0390879F3848FFBD2E07F8A0E006FB30.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Latiastrea mucronata Sikharulidze 1979	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Latiastrea mucronata Sikharulidze, 1979</p>
            <p>Figs. 8K–M.</p>
            <p> (v)*1979  Latiastraea mucronata Sikh. ,  sp. nov. : Sikharulidze, p. 37, Pl. 3, Fig. 4–4a, Pl. 23, Pl. 24, Fig. 1a–b. </p>
            <p> 1996  Latiastraea mucronata Sikharulidze, 1979 : Császár &amp;  Turnšek , p. 434, Fig. 26. </p>
            <p> v1999  Latiastraea mucronata Sikharulidze, 1979 : Baron-Szabo &amp; González-León, p. 490, Fig. 6e. </p>
            <p> (v)2002  Latiastrea mucronata Sikharulidze, 1979 : Morycowa &amp; Marcopoulou-Diacantoni, p. 53, Figs. 34F, G. </p>
            <p> v2003  Latiastraea mucronata Sikharulidze, 1979 : Baron-Szabo &amp; González-León, p. 220, Fig. 9D, F. </p>
            <p> v2018  Latiastrea mucronata Sikharulidze, 1979 : Baron-Szabo, p. 66, Pl. 9, Fig. A. </p>
            <p>Dimensions of skeletal elements. Diameter of corallite (monocentric): 2–4 mm; distance of corallite centers: 2–4.5 mm; septa/corallite (monocentric): up to around 30; septa/mm: 7–8/2.</p>
            <p>Description. Massive, cerioid colony; septa are subequal in thickness, irregularly alternate in length; columella often made of elongate segments.</p>
            <p>  Type locality of species.  Albian of Georgia (in Caucasus)  . </p>
            <p>Distribution. Upper Berriasian (upper Őhrli Formation [= Oerfla Formation]) of western Austria, lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Valanginian of Hungary, upper Aptian–lower Albian of Mexico, Albian of Georgia (in Caucasus) and Greece.</p>
            <p>Material. NMSG Coll. PK–02.10.22e (= 02.10.30a); –02.10.22g.</p>
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	https://treatment.plazi.org/id/0390879F3848FFBD2E07F8A0E006FB30	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384BFFBD2DBDFA82E423FE16.text	0390879F384BFFBD2DBDFA82E423FE16.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Tamnoseris de Fromentel 1861	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Tamnoseris de Fromentel, 1861</p>
            <p>  Type species.  Tamnoseris incrustans de Fromentel, 1861 ,  Middle Jurassic of France (Chaumont, Saint Claude, French Jura)  . </p>
            <p>Diagnosis. Colonial, massive, hemispherical, cerio-thamnasterioid, corallites arranged in short-meandroid series present or absent. Budding extracalicular-marginal. Costosepta confluent, irregularly perforated, granulate and probably pennulate laterally. Anastomosis frequently present. Columella parietal-papillose. Synapticulae numerous. Endothecal dissepiments vesicular, thin. Intertrabecular distance ranging between 120 and ca. 240 µm. Wall synapticulothecal, incomplete.</p>
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	https://treatment.plazi.org/id/0390879F384BFFBD2DBDFA82E423FE16	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384BFFBB2E07FE65E003FE76.text	0390879F384BFFBB2E07FE65E003FE76.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Tamnoseris carpathica Morycowa 1971	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Tamnoseris cf. carpathica Morycowa, 1971</p>
            <p>Figs. 9A–B</p>
            <p> v*1971?  Tamnoseris carpathica n. sp. : Morycowa, p. 106–108, Pl. 28, Fig. 1a–e. </p>
            <p> nonv1981  Tamnoseris carpathica Morycowa, 1971 :  Turnšek , in  Turnšek &amp; Mihajlović, p. 29, Pl. 31, Fig. 4–5. </p>
            <p> 1988  Tamnoseris carpathica Morycowa, 1971 : Kuzmicheva &amp; Aliev, 1988 p. 169, Pl. 5, Fig. 4a–b. </p>
            <p> 2006  Tamnoseris carpathica Morycowa, 1971 : Morycowa &amp; Decrouez, p. 810–812, Pl. 9, Figs. 5–7. [older synonyms cited therein] </p>
            <p> 2021b  Tamnoseris carpathica Morycowa, 1971 : Baron-Szabo, Appendix Tables 2–5, and 7–12. </p>
            <p>Dimensions. Diameter of corallites: 2–4.5 mm, in areas of intense budding around 1.5 mm; distance of corallite centers: 2.5– 5 mm, in areas of intense budding the distance is around 1.5 mm; septa/corallite: 20 to around 32, in corallites in areas of intense budding 12; septa/mm: 6–7/2.</p>
            <p>Description. Fragment of a massive, cerio-thamnasterioid colony; corallites isolated or arranged in short-meandroid series; septa subequal in thickness; up to around 12 septa reach corallite center.</p>
            <p>  Type locality of species.  Lower Aptian of Romania (Valea Izvorul Alb)  . </p>
            <p>Distribution. Lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Barremian of Azerbaijan, lower Aptian of Romania (Valea Izvorul Alb) and Switzerland (Upper Schrattenkalk of Hergiswil).</p>
            <p>(See figure on next page.)</p>
            <p> Fig. 9 A  Thamnoseris cf. carpathica Morycowa, 1971 , NMSG Coll. PK 02.10.37b; calicular view of colony, polished surface; scale bar: 2 mm. B  Thamnoseris cf. carpathica Morycowa, 1971 , NMSG Coll. PK 02.10.37b;oblique longitudinal view of colony, polished surface; scale bar: 1 mm. C  Adelocoenia parvistella Alloiteau, 1961 , NMSG Coll. PK 02.10.29d (= 23d); calicular view of colony, thin section; scale bar: 2 mm. D  Adelocoenia parvistella Alloiteau, 1961 , NMSG Coll. PK 02.10.29d (= 23d); close-up of Fig. C; scale bar: 1 mm. E  Adelocoenia parvistella Alloiteau, 1961 , NMSG Coll. </p>
            <p> PK 02.10.23d (=29d); upper surface of colony, calicular view,partially polished;scale bar: 2 mm. F  Pleurophyllia? tobleri (Koby, 1896) , NMSG Coll. </p>
            <p> PK 02.10.15;calicular view of corallum, polished surface; scale bar: 1 mm. G  Pleurophyllia? tobleri (Koby, 1896) , NMSG Coll. PK 02.10.20d; calicular view of corallum,upper surface;scale bar: 1 mm. H  Cyathophora claudiensis Étallon, 1859 , NMSG Coll. PK 02.10.22a; calicular view of colony, thin section;scale bar: 4 mm. I  Cyathophora claudiensis Étallon, 1859 , NMSG Coll. PK 02.10.22a; upper surface of colony, calicular view; scale bar: 10 mm. </p>
            <p> J  Cyathophora claudiensis Étallon, 1859 , NMSG Coll. PK 02.10.29b (= 23b); calicular view of colony, thin section;scale bar: 3 mm. K Stylophyllid indet., NMSG Coll. PK 02.10.14c (=13) longitudinal view of corallum, oblique, polished surface; green arrows indicate septa; orange arrow indicates corallite wall; scale bar: 4 mm. L  Stylophyllopsis silingensis (Liao, 1982) , NMSG Coll. PK 02.10.35l;calicular view of colony, thin section; scale bar: 2 mm </p>
            <p>Material. NMSG Coll. PK–02.10.37b.</p>
            <p> Remarks. Te material described as  Tamnoseris carpathica from the Barremian–lower Aptian of eastern Serbia (  Turnšek &amp; Mihajlović, 1981) has just recently been transferred to the genus  Talamocaeniopsis , grouping it with the species  T. stricta (Milne Edwards &amp; Haime) (see Baron-Szabo, 2021b). Because the Swiss material represents only a fragment of a colony, the total dimensions of the skeletal elements cannot be determined. Te skeletal features observed correspond to the species  T. carpathica . </p>
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	https://treatment.plazi.org/id/0390879F384BFFBB2E07FE65E003FE76	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384DFFBB2DBDFE62E385FB51.text	0390879F384DFFBB2DBDFE62E385FB51.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Adelocoenia d'Orbigny 1849	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Adelocoenia d’Orbigny, 1849</p>
            <p> Type species. Astrea  
castellum 
Michelin, 1844 ,  Upper Jurassic of France (neotype designation Lathuilière, et al., 2020). </p>
            <p> Diagnosis.   Colonial, massive to subhemispherical, small knobby, plocoid corallum. Septa compact, free, bicuneiform, costate, non-confluent, often straight, unequal in length, arranged mainly radially; bilateral arrangement might occur as a result of elongation of both calices and calicular fossae. Septal ornamentation very weak or smooth when covered by thickening deposits.  Secondary trabecular axes irregularly emerge from the mid-septal plan toward the septal faces.  Pali and synapticulae absent.  Endotheca made of tabulae or tabuloid dissepiments, rarely vesicular.  Peritheca made of vesicular dissepiments.  Columella absent but a clear central subcircular fossa present (in neotype of type species, in one out of 32 corallites, however, structures are present which may or may not correspond to a columella). Intertrabecular distance up to around 100 µm. Wall parathecal, developed in continuity with thickening deposits of septa  . </p>
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	https://treatment.plazi.org/id/0390879F384DFFBB2DBDFE62E385FB51	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384DFFBA2DBDFB22E385FE76.text	0390879F384DFFBA2DBDFB22E385FE76.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Adelocoenia parvistella Alloiteau 1961	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Adelocoenia parvistella Alloiteau, 1961</p>
            <p>Figs. 9C–E</p>
            <p> v*1961  Adelocoenia parvistella : Alloiteau, p. 289, pl. 9 fig. 5; pl. 10 fig. 9. </p>
            <p> v1972  Pseudocoenia slovenica n. sp. :  Turnšek , 1972: p. 20 and 83, Pl. 4, Fig. 1–2, Pl. 5, Figs. 1–4. </p>
            <p> 1976  Pseudocoenia slovenica Turnšek, 1973 : Roniewicz, p. 48, pl. 5 fig. 5. </p>
            <p> 1981  Pseudocoenia slovenica Turnšek, 1972 : Eliášová, 1981 p. 125, pl. 8 figs. 3–4. </p>
            <p> 1985  Pseudocoenia slovenica Turnšek : Rosendahl, p. 34, pl. 3 fig. 2. </p>
            <p> 1990  Pseudocoenia slovenica Turnšek, 1972 Errenst , p. 168, pl. 3 fig. 1. </p>
            <p> v1997  Pseudocoenia slovenica Turnšek, 1972 :  Turnšek , p. 171, Figs. A–F. </p>
            <p> 2001  Pseudocoenia cf. slovenica Turnšek, 1972 : Laternser, 2001 p. 162. </p>
            <p> 2002  Pseudocoenia slovenica Turnšek, 1972 Kashiwagi , et al., 2002 p. 10, fig. 5.2. </p>
            <p> pars?2003  Pseudocoenia slovenica Turnšek, 1972 : Pandey &amp; Fürsich, p. 27, pl. 5 fig. 5; pl. 6 fig. 1–6. </p>
            <p> non2003  Pseudocoenia cf. slovenica Turnšek, 1972 : Pandey &amp; Fürsich, p. 27, pl. 4 fig. 4. </p>
            <p> 2015  Pseudocoenia slovenica Turnšek : Kołodziej, 2015, p. 182. </p>
            <p> v2020  Adelocoenia parvistella Alloiteau, 1961 : Lathuilière, et al., p. 381–382, Figs. 15–16 [older synonyms cited therein] </p>
            <p>Dimensions. Diameter of corallites: 1–1.8 mm; in areas of intense budding the diameter is around 0.8 mm; distance of corallite centers: 1.2– 2 mm, in areas of intense budding the distance is around 0.8 mm; septa/corallite: 12 (6s1 + 6s2); costae/corallite: 12 and higher.</p>
            <p>Description. Small massive to knobby colony; corallites circular to subcircular in outline, regularly disposed over the colony; costosepta developed in 2 complete cycles in 6 systems, regularly alternating in length and thickness; number of costae is equal to or slightly larger than number of septa; columella absent but in a small number of corallites trabecular extensions of axial ends of septa reach corallite center where they might fuse, forming a pseudo-columella.</p>
            <p>  Type locality of species.  Upper Jurassic (Tithonian) of Spain (La Querola)  . </p>
            <p>Distribution. Upper Jurassic of Armenia and Japan, Oxfordian of Germany and France, upper Oxfordian of Romania, Oxfordian–Kimmeridgian of Slovenia, lower Kimmeridgian of Romania, Kimmeridgian–Tithonian of Spain, Tithonian of Portugal, Tithonian–lower Berriasian of the Czech Republic and Poland, lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; new material this paper).</p>
            <p>Material. NMSG Coll. PK–02.10.20f; –02.10.23d (= 02.10.29d); –02.10.27b; –02.10.28c and 28d; –02.10.29f; –02.10.30d; –02.10.32b.</p>
            <p> Remarks. In  Adelocoenia parvistella , auriculae are present which clearly distinguishes it from genera such as  Cyathophora (including its junior synonym  Cryptocoenia ). Tis represents an important fact, since Alloiteau (1958) also erected a species  Cryptocoenia parvistella , using material from the Cretaceous of Madagascar (MNHN.F.M05039; and thin sections). Because the latter is here considered to belong to  Cyathophora , the species is not a junior homonym. </p>
            <p> Some of the specimens from the Jurassic of Iran assigned to this species  A. slovenic a by Pandey and Fürsich (2003, p. 27), are considered as  Solenocoenia (such as material shown on their pl. 6, Fig. 5). In addition, it should be noted that these authors place within  A. slovenica material having dimensions that significantly differ from  A. slovenica (e.g., specimen SNSB-BSPG 1999 VIII 874: corallite diameter: 1.5–2.3 mm; and specimen SNSB-BSPG 1999 VIII 1085: corallite diameter: 1.5–2.6 mm). Te consequence of such a wide grouping would be a much wider stratigraphic range for this species. </p>
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	https://treatment.plazi.org/id/0390879F384DFFBA2DBDFB22E385FE76	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384CFFBA2E68FD80E59FFB93.text	0390879F384CFFBA2E68FD80E59FFB93.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Cyathophoridae Vaughan & Wells 1943	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Cyathophoridae Vaughan &amp; Wells, 1943 Genus  Cyathophora Michelin, 1843</p>
            <p> Type species.  Cyathophora richardi Michelin, 1843 , Upper Jurassic of France (lectotype designation Zaman &amp; Lathuilière, 2014). </p>
            <p>Diagnosis. Colonial, massive, columnar, hemispherical, knobby, plocoid, cerio-plocoid to cerioid in areas of closely spaced corallites. Budding extracalicular. Corallites circular to subpolygonal in outline, separated by a narrow costate peritheca. Costosepta compact, generally non-confluent to subconfluent, occasionally confluent, radially arranged. Sizes of septa range from very short (less of a quarter of the lumen size) to half the lumen size, in which case septa reach the axial region where they sometimes fuse. Axial ends of S1 are vertically discontinuous. No columella. No synapticulae. No pali. Endothecal and exothecal dissepiments tabulate, well-developed. Wall parathecal and septothecal.</p>
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	https://treatment.plazi.org/id/0390879F384CFFBA2E68FD80E59FFB93	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384CFFBA2DBDFE62E34BFCF1.text	0390879F384CFFBA2DBDFE62E34BFCF1.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Pleurophyllia De Fromentel 1856	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Pleurophyllia De Fromentel, 1856</p>
            <p>  Type species.  Pleurophyllia trichotoma De Fromentel, 1856 ,  Upper Jurassic of France (Mantoche)  . </p>
            <p>Diagnosis. Colonial, phaceloid. Budding intracalicinal. Septa compact, smooth laterally, arranged bilaterally. One major septum extends to the axial region of the corallite. Septal cycles indistinct. Costae and columella absent. Intertrabecular distance ranging between 90 and ca. 160 µm. Endothecal dissepiments thin. Multilamellate epithecal sensu lato wall possibly present.</p>
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	https://treatment.plazi.org/id/0390879F384CFFBA2DBDFE62E34BFCF1	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384CFFBA2DBDFCC2E038FB13.text	0390879F384CFFBA2DBDFCC2E038FB13.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Pleurophyllia tobleri (Koby 1896)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Pleurophyllia? tobleri (Koby, 1896)</p>
            <p>Figs. 9F–G</p>
            <p> parsv*1896  Cladophyllia Tobleri, Koby, 1896 : Koby, p. 42, Pl. 7, Fig. 5 (non Fig. 4–4a) </p>
            <p> 2008  Pleurophyllia aff. cara Eliášová, 1975 : Roniewicz, p. 97, Fig. 3B. </p>
            <p> v2014  Pleurophyllia tobleri (Koby, 1896) : Baron-Szabo, p. 82, Text–Fig. 21. </p>
            <p> v2018  Pleurophyllia tobleri (Koby, 1896) : Baron-Szabo, p. 81, Pl. 12, Figs. C–D [older synonyms cited therein]. </p>
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	https://treatment.plazi.org/id/0390879F384CFFBA2DBDFCC2E038FB13	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384CFFB92E07FBE3E3A7FD30.text	0390879F384CFFB92E07FBE3E3A7FD30.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Cyathophora claudiensis Etallon 1859	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Cyathophora claudiensis Étallon, 1859</p>
            <p>Figs. 9H–J</p>
            <p> *1859  Cyathophora claudiensis : Étallon, p. 479. </p>
            <p> 1897  Cyathophora claudiensis Ét. : Ogilvie, p. 176, Pl. 16, Figs. 11–12. </p>
            <p> v1954  Cyathophora claudiensis Étallon, 1859 : Geyer, 1954 p. 137, Pl. 9, Fig. 12. </p>
            <p> 1970  Amphiphora serannensis nov. sp. : Alloiteau &amp; Bernier, 1970 p. 926–927, Pl. 28, Figs. 1–3. </p>
            <p> 1976  Cyathophora claudiensis Étallon, 1859 : Roniewicz, p. 44–45, Pl. 4, Fig. 1–b [older synonyms cited therein]. </p>
            <p>(See figure on next page.)</p>
            <p> Fig. 10 A  Heterocoenia inflexa (Eichwald, 1865 –69), NMSG Coll.PK 02.10.31d; calicular view of colony, polished surface; scale bar: 1.25 mm. </p>
            <p> B  Heterocoenia inflexa (Eichwald,1865 –69), NMSG Coll. PK 02.10.31d; upper surface of colony, calicular and oblique views; scale bar: 8 mm. C  Aplosmilia semisulcata (Michelin, 1843) , NMSG Coll. PK 02.10.29h; calicular view of branch, polished surface; scale bar: 3.5 mm. D  Aplosmilia semisulcata (Michelin, 1843) , NMSG Coll. PK 02.10.29h; calicular view of branch, thin section; scale bar: 3 mm. E  Aplosmilia semisulcata (Michelin,</p>
            <p> 1843), NMSG Coll. PK 02.10.29h; calicular view of corallites in advanced budding stage, polished surface; scale bar: 3 mm. F  Stylophyllopsis silingensis (Liao, 1982) , NMSG Coll. PK 02.10.25b;calicular view of branch, slightly oblique, polished surface; scale bar: 2 mm. G  Stylophyllopsis silingensis (Liao, 1982) , NMSG Coll. PK 02.10.29c (= 23c); calicular view of branch, slightly oblique, polished surface;scale bar: 2 mm. H  Stylophyllopsis silingensis (Liao, 1982) , NMSG Coll. PK 02.10.35l;close-up of Pl. 3, Fig. L; scale bar: 6 mm. I  Axosmilia villersensis (Koby,1898) , NMSG Coll. PK 02.10.10; calicular view of corallum, thin section; younger cycle septa are preserved in only some parts of the corallum; scale bar: 3 mm. J  Stylophyllopsis silingensis (Liao,1982) , NMSG Coll. PK 02.10.35h; calicular view of juvenile corallite,thin section; scale bar: 1 mm </p>
            <p> 1982  Cyathophora claudiensis Étallon, 1859 : Bendukidze, 1982 p. 7, Pl. 1, Fig. 5. </p>
            <p> nonv1991  Cyathophora claudiensis Étallon, 1859 : Lauxmann, p. 114–115. </p>
            <p> (v)2008  Cyathophora sp. 1 : Roniewicz, p. 128, Figs. 16A–D. </p>
            <p> 2015  Cyathophora claudiensis : Kołodziej, 2015 p. 183. </p>
            <p>Dimensions. Great diameter of corallites: 4.5– 7 mm, in areas of intense budding around 3.5 mm; distance of corallite centers: 6–9 mm, in areas of intense budding the distance is around 4 mm; septa/corallite: 6 + 6 + 12.</p>
            <p>Description. Massive to subhemispherical, plocoid to cerio-plocoid colony; corallites are circular to elongate in outline; costosepta are very short and spine-like, developed in two to three complete cycles in 6 systems.</p>
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	https://treatment.plazi.org/id/0390879F384CFFB92E07FBE3E3A7FD30	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384FFFB92DBDF93EE2A4FD56.text	0390879F384FFFB92DBDF93EE2A4FD56.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Stylophyllopsis Frech 1890	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Stylophyllopsis Frech, 1890</p>
            <p> Type species.  Stylophyllopsis polyactis Frech, 1890 , Upper Triassic of Austria (Rhaetian, Zlambach Beds) (lectotype designation Roniewicz, 1989). </p>
            <p>Diagnosis. Solitary and phaceloid. Budding intracalicular. Septal spines long, connected by stereome, resulting in subcompact septal blades that have large pores. Additional stereome layers might fuse the septal spines and cover endothecal dissepiments. In the septal spines axial rods or lamellae are present. Axial ends of septa dissociate, forming septal spines. Distal edge of septa coarsely denticulate. Columella formed by isolated septal spines. Endothecal dissepiments vesicular to subtabulate; large and vesicular in peripheral area of corallite. Peripheral, large-vesicular dissepimentarium irregularly present. Microstructure made of bundles of fiber. Epitheca sensu lato present.</p>
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	https://treatment.plazi.org/id/0390879F384FFFB92DBDF93EE2A4FD56	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F384FFF872E07FD25E333FE56.text	0390879F384FFF872E07FD25E333FE56.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Stylophyllopsis silingensis (Liao 1982)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Stylophyllopsis silingensis (Liao, 1982)</p>
            <p>Fig. 9L, Figs. 10F–H, J</p>
            <p> *1982  Donacosmilia silingensis Liao (sp. nov.): Liao, p. 166, Pl. 14, Figs. 1–2. </p>
            <p> 1994  Donacosmilia silingensis Liao : Liao &amp; Xia, p. 78, Pl. 8, Figs. 5–6. </p>
            <p>Dimensions. Great diameter of corallites: 6–11 mm; small diameter of corallites: 5–7 mm; septa/corallite: 32 to around 46.</p>
            <p>Description. Phaceloid colony; corallites subcircular to elongate in outline; septa generally straight, arranged bilaterally in 4 to 5 size orders, irregularly alternating in length and thickness; up to around 20 septa reach corallite center; columella weakly developed.</p>
            <p>  Type locality of species.  Hauterivian of Tibet (Xainza County; Toiba Formation)  . </p>
            <p>Distribution. Lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Hauterivian of Tibet.</p>
            <p>Material. NMSG Coll. PK–02.10.23c (= 02.10.29c); –02.10.25b; –02.10.35c (= 02.10.35f and 35f-II); –02.10.35d (= 02.10.35g); –02.10.35e (= 02.10.35h); –02.10.35l.</p>
            <p> Remarks. Study of the lectotype of the type species of  Stylophyllopsis Frech (  S. polyactis [SNSB-BSPG-AS- XII-53]) in 2020 by one of the authors (RBS) revealed that, in addition to previously reported skeletal features, it also shows a peripheral, large-vesicular dissepimentarium in some places. </p>
            <p> In having (1) septa made of spines that are connected or dissociated; (2) large and vesicular dissepiments in the peripheral area of the corallite; (3) an epithecal sensu lato wall; (4) axial ends of septa that dissociate, forming septal spines; (5) a columella formed by isolated septal spines; and (6) lamellae that occur in some of the septal spines, the material described as  Donacosmilia silingensis from the Hauterivian of Tibet closely corresponds to the genus  Stylophyllopsis . Te Swiss specimens show very close resemblance to the Tibetan type material as presented in Liao (1982) and Liao and Xia (1994). </p>
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	https://treatment.plazi.org/id/0390879F384FFF872E07FD25E333FE56	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3871FF872E07FE05E470F973.text	0390879F3871FF872E07FE05E470F973.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Heterocoenia inflexa	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Heterocoenia inflexa (Eichwald, 1865 –69) </p>
            <p>Figs. 10A–B</p>
            <p> *1865–69  Stereopsammia inflexa m.: Eichwald, vol. 2, p. 164, Pl. 11, Fig. 2a–b. </p>
            <p> 1888  Latusastraea provincialis, d’Orb. sp.: Solomko, Geyer 1954 p. 76–77. </p>
            <p> 1907  Latusastraea? inflexa Eichw. : Karakash, p. 262. 2002  Latusastraea exigua Fromentel, 1862 : Kuzmicheva, p. 126, Pl. 8, Fig. 3. </p>
            <p> v2018  Heterocoenia cf. inflexa (Eichwald, 1865 –69): Baron-Szabo, p. 84, Pl. 12, Fig. G. </p>
            <p> v2021 b  Heterocoenia inflexa (Eichwald, 1865 –69): Baron-Szabo, p. 77, Pl. 13, Fig. F. </p>
            <p>Dimensions of skeletal elements. Great diameter of corallites: 1–1.8 mm, up to around 3 mm when wall exceptionally thick (around 0.5 mm or larger); great diameter of corallites (lumen): 0.8–1.8 mm; septa/corallite: 1–12; distance of corallite centers: 1.2– 3 mm, in areas of intense budding around 1 mm.</p>
            <p>Description. Small submassive to subramose colony; corallites plocoid to cerio-plocoid, cerioid when crowded, oval to irregularly shaped in outline, regularly disposed over the colony; septa arranged bilaterally; in some corallites, septal arrangement in 3 systems present; one major septum present; remaining septa highly irregularly developed including very thin and half the length of major septum, or very short, spine-like; axial end of major septum rhopaloid or cuneiform; costae short and thin, up to twice the number of septa.</p>
            <p>  Type locality of species.  Valanginian–lower Hauterivian of Ukraine  . </p>
            <p>Distribution. Upper Berriasian (upper Őhrli Formation [= Oerfla Formation]) of western Austria, lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Valanginian–lower Hauterivian of Ukraine, upper Barremian–lower Aptian of western Austria (Schrattenkalk Formation, Vorarlberg), lower Aptian of southern Germany (Upper Schrattenkalk, Bavaria).</p>
            <p>Material. NMSG Coll. PK–2.10.31d (= 2.10.32b).</p>
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	https://treatment.plazi.org/id/0390879F3871FF872E07FE05E470F973	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3871FF872DBDFBA1E2F1FEB6.text	0390879F3871FF872DBDFBA1E2F1FEB6.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Heterocoeniidae Oppenheim 1930	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Family  Heterocoeniidae Oppenheim, 1930 Genus  Heterocoenia Milne Edwards &amp; Haime, 1848b</p>
            <p>  Type species.  Lithodendron exiguum Michelin, 1847 ,  Santonian of France  . </p>
            <p>Diagnosis. Colonial massive, hemispherical, foliose, encrusting, ramose, plocoid, cerio-plocoid, (sub-) fasciculate; subphaceloid to reptoid when developments of coenosteum reduced. Budding extracalicular, extracalicular-marginal, and by septal division often dividing the corallite in three new ones (“trinity-arrangement” sensu Baron-Szabo, 2014). Corallites circular to elongate or irregularly polygonal in outline. Tey are directly united by their walls, or separated by extensive vesicular to dense coenosteum, or loosely connected by fragments of exotheca in form of traverses. Septa compact, arranged in various symmetries (e.g., trimerally, hexamerally, bilaterally, indistinct). One main septum, with remaining septa sometimes reduced to rudimentary spines. Costate zone present, weakly developed, or absent. Colony surface granulated or smooth. Columella, synapticulae, and paliform structures absent. Intertrabecular distance ranging between 60 and 120 µm in septa. Endothecal dissepiments thin, mainly tabulate to subtabulate, vesicular (often in peripheral and thecal areas). Exothecal dissepiments large vesicular. Wall often thick, possibly septothecal and paraseptothecal. Corallite wall tends to become more flaky, “bubbly” (cf. sclerenchymal deposits sensu Kołodziej, 1995, p. 4), and disintegrated during the process of budding.</p>
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	https://treatment.plazi.org/id/0390879F3871FF872DBDFBA1E2F1FEB6	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3871FF862E07F961E3B6FD96.text	0390879F3871FF862E07F961E3B6FD96.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Aplosmilia d'Orbigny 1849	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Aplosmilia d’Orbigny, 1849</p>
            <p>  Type species.  Lobophyllia semisulcata Michelin, 1843 ,  Jurassic of France (Verdun)  . </p>
            <p>Diagnosis. Colonial, phaceloid. Corallites cylindrical to elliptical in outline. Budding intracalicular and? extracalicular. Septa compact, radially or bilaterally arranged, smooth distally. Lateral flanks of septa covered by sharp granulae. Flabelliform auriculae present. Lonsdaleoid and apophysal septa present or absent. Columella lamellar. Wall septoparathecal and parathecal. Pali and synapticulae absent. Intertrabecular distance ranging between 90 to around 250 µm. Endothecal dissepiments vesicular, mainly occurring in the vicinity of the wall, sometimes forming a stereozone. Tectura present or absent.</p>
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	https://treatment.plazi.org/id/0390879F3871FF862E07F961E3B6FD96	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3870FF862DBDFDE5E083F8B3.text	0390879F3870FF862DBDFDE5E083F8B3.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Aplosmilia semisulcata (Michelin 1843)	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Aplosmilia semisulcata (Michelin, 1843)</p>
            <p>Figs. 10C–E</p>
            <p> v*1843  Lobophyllia semisulcata . N.: Michelin, p. 89, Pl. 17, Fig. 8. </p>
            <p> v1850  Aplosmilia semisulcata (Michelin, 1843) : d’Orbigny, vol. 2, p. 37. </p>
            <p> v1880  Aplosmilia semisulcata, Michelin , sp.: Koby, p. 50–51, Pl. 8, Figs. 3–4a, Pl. 14, Figs. 1–2a. </p>
            <p> v1976  Aplosmilia semisulcata (Michelin, 1843) : Roniewicz, p. 82–83, Pl. 20, Figs. 3a–d. </p>
            <p> 1985  Aplosmilia semisulcata (Michelin, 1843) : Geyer &amp; Rosendahl, p. 167, Pl. 2, Fig. 7. </p>
            <p> 1991  Aplosmilia semisulcata (Michelin, 1843) : Errenst, p. 3–4, Pl. 13, Fig. 2a–b. [older synonyms cited therein] </p>
            <p> 1991  Aplosmilia semisulcata (Michelin, 1843) : Lebanidze, 1991 p. 38–39, Pl. 14, Figs. 3a–b, Text-Fig. 8a–b. </p>
            <p> 2003  Aplosmilia cf. semisulcata Michelin, 1843 : Pandey &amp; Fürsich, p. 116–118, Pl. 16 Figs. 7–9. </p>
            <p>Dimensions. Great diameter of corallites: 7–12 mm; small diameter of corallites: 6.5– 8 mm; in areas of intense budding around 2 mm; septa/corallite: 24 to around 40, in corallites in areas of intense budding around 16; septa/ mm: 2–3/2.</p>
            <p>Description. Branches of a phaceloid colony; corallites subcircular to elongate in outline; septa developed in 3 to 4 size orders, regularly alternating in length and thickness; lamellar columella preserved deeper in corallum.</p>
            <p>  Type locality of species.  Jurassic of France (Verdun)  . </p>
            <p>Distribution. Jurassic of France, Bathonian–middle Callovian of Iran, Oxfordian of Montenegro, upper Oxfordian of Turkmenistan, upper Oxfordian–Kimmeridgian of Georgia (in Caucasus), lower Kimmeridgian of Portugal and Spain, Tithonian–lower Berriasian of the Czech Republic, upper Berriasian of southern Spain (Andalusia), lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper).</p>
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	https://treatment.plazi.org/id/0390879F3870FF862DBDFDE5E083F8B3	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3870FF862E07FE60E41FFC33.text	0390879F3870FF862E07FE60E41FFC33.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Axosmilia Milne Edwards & Haime 1848	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Genus  Axosmilia Milne Edwards &amp; Haime, 1848a</p>
            <p>  Type species.  Caryophyllia extinctorium Michelin, 1841 ,  Middle Jurassic (Bajocian) of France (Calvados)  . </p>
            <p>Diagnosis. Solitary, attached by small base or free. Corallite variably conical, elliptical in outline. Costosepta compact, generally free and straight, arranged bilaterally, regularly developed in cycles, granulated laterally. One first cycle septum often fused to columella. Columella lamellar. Distal margin of septa weakly ornamented, showing a zigzag pattern, especially visible in thin septa. Endothecal dissepiments vesicular. Paliform structures and synapticulae absent. Intertrabecular distance ranging between 150 to around 500 µm. Wall made of stereozone and enlarged costae that are fused to each other. Microstructure characterized by mid-septal zigzag line. Epithecal s.l. wall folded.</p>
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	https://treatment.plazi.org/id/0390879F3870FF862E07FE60E41FFC33	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3870FF862E07FB83E48CF9BD.text	0390879F3870FF862E07FB83E48CF9BD.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Axosmilia villersensis (Koby 1898) Refers	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Axosmilia villersensis (Koby, 1898)</p>
            <p>Fig. 10I</p>
            <p> *1898  Pleurosmilia villersensis, Koby, 1897 : Koby, p. 89–90, Pl. 22, Figs. 2–7. </p>
            <p> non1936  Pleurosmilia villersensis Koby : Alloiteau, p. 507, Pl. 36, Figs. 1–3. </p>
            <p> 1981  Axosmilia villersensis (Koby, 1898) :  Turnšek in  Turnšek &amp; Mihajlović, p. 22, Pl. 20, Figs. 1–6. </p>
            <p> 1992  Axosmilia villersensis (Koby, 1898) :  Turnšek , p. 164, Fig. 2. </p>
            <p> nonv1993  Axosmilia villersensis (Koby, 1898) : Baron-Szabo, p. 160–161, Pl. 4, Fig. 4. </p>
            <p> v1996  Axosmilia villersensis (Koby, 1898) : Baron-Szabo &amp; Steuber, p. 16–17, Pl. 5, Fig. 6. </p>
            <p> 2021  Miscellosmilia sp. : Löser, et al., p. 34, Figs. 41.1 ‒ 2. </p>
            <p>Dimensions. Diameter of corallite (d/D): 18 × 20 mm;</p>
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	https://treatment.plazi.org/id/0390879F3870FF862E07FB83E48CF9BD	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
0390879F3879FF8C2D8FFE3DE586F8B2.text	0390879F3879FF8C2D8FFE3DE586F8B2.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Microphyllia bachmayeri Geyer 1955	<html xmlns:mods="http://www.loc.gov/mods/v3">
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            <p> Microphyllia bachmayeri Geyer, 1955 b Refers to material assigned to  Microphyllia cf. bachmayeri</p>
            <p>[meandroid]</p>
            <p> Microphyllia undans Étallon, 1858</p>
            <p>[meandroid]</p>
            <p> Starostinia giseldonensis (Starostina &amp; Originally described as  Ironella Starostina &amp; Krasnov, 1970 , which is a junior Krasnov, in Krasnov &amp; Starostina, homonym of  Ironella Cobb, 1920 (Nematoda).  Starostinia Doweld, 2014 , is 1970). [astreoid, plocoid] used as the replacement taxon </p>
            <p> [7.1] (refers to locality 7 in Fig. 6) Valanginian; Hungary (Mecsek Mountains); Császár &amp;  Turnšek (1996) </p>
            <p> Taxon [corallite integration] Remarks  Actinaraea tenuis Morycowa, 1971 Species also found in the Vitznau Marl (see text) [thamnasterioid]  Adelocoenia sp. 1 [plocoid] Refers to material originally described as  Paretallonia bendukidzeae Sikharulidze , but seems to be more closely related to  Adelocoenia (see discussion in Baron-Szabo, 2021b) </p>
            <p> Ahrdorffia ornata (Morycowa, 1971) Originally assigned to  Mesomorpha Pratz, 1882 –1883, which is a junior [thamnasterioid-submeandroid] homonym of  Mesomorpha Hodgson, 1841 (a bird);  Ahrdorffia Trauth is used as the replacement taxon </p>
            <p> Baryhelia (Paronastraea) sp. 1 [plocoid to In having heterocoeniid thecal and septal microstructure, apophysal cerio-plocoid] developments, and the type of intracalicular-marginal budding characteristic of the heterocoeniids s.l. (including the “paronastraeids”), the material described as  Confusaforma sp. closely corresponds to  Baryhelia (Paronastraea)</p>
            <p> Columnocoenia ksiazkiewiczi Morycowa, 1964 [plocoid]  Cyathophora regularis de Fromentel, Refers to material described as  Adelocoenia biedai ; genus  Adelocoenia was 1884 [plocoid] recently revised (Lathuilière, et al., 2020)  Dendraraea mammelonata (  Turnšek , in Refers to material described as  Thamnaraea mammelonata ; genus  Turnšek &amp; Mihajlovic ˊ, 1981)  Thamnaraea is considered to be a junior synonym of  Dendraraea (also see [thamnasterioid] discussion in Lathuilière &amp; Gill, 1998)  Dimorphastrea explanata de Fromentel, In having latomeandrid corallites that are equal in size (around 6 mm) and in 1857 [thamnasterioid-circumoral] circumoral arrangement, the material described as  Dimorphastraeopsis patellaris closely corresponds to  Dimorphastrea explanata (transferred herein) </p>
            <p> Diplocoenia lobata (Étallon, 1859) Refers to material described as  Diplocoenia decaseptata Kuzmicheva, 1966 . [cerioid] Based on the description and illustration by Kuzmicheva (1967, p. 53–54, Pl. 2, Fig. 7), the species  D. decaseptata more closely corresponds to </p>
            <p> Columnocoeni   a (see below). The Hungarian material, however, shows features characteristic of  Diplocoenia , corresponding to the syntype MNHN  .F.M03057 </p>
            <p> of  D. lobata</p>
            <p> Ellipsocoenia haimei (de Fromentel, Refers to material described as  Thamnasteria meandra but seems to be a rather 1857) [plocoid to cerio-plocoid] plocoid form (not thamnasterioid) with pennular developments, thus closely corresponding to  Ellipsocoenia ; dimensions of skeletal elements are in the range of the species  haimei (see Baron-Szabo, 2021b) </p>
            <p> Enallhelia sp. 1 [dendroid-sympodial] Refers to material described as  Enallhelia sp. Epistreptophyllum sp. [none; solitary; conical]  Eugyra pusilla Koby, 1896 [meandroid]  Heliocoenia rarauensis Morycowa, 1971 [plocoid] </p>
            <p>Table 6 (continued) [8.2] (refers to locality 8 in Fig. 6)</p>
            <p> Valanginian; Bulgaria (  Lyubasha Mountain ; Slivnitsa Formation); Roniewicz (2008) </p>
            <p> Taxon [corallite integration] Remarks  Bilaterocoenia sp. [plocoid]  Calamophylliopsis compacta (Koby, 1884) [branching]  Calamophylliopsis cf. stockesi (M E &amp; Haime, 1851) [branching]  Cladophyllia clemencia de Fromentel, 1857 [branching]  Cladophyllia cf. dichotoma (Goldfuss, 1826) Refers to material described as  Cladophyllia skuviensis ; because it [phaceloid] has a larger number of septa and smaller corallite diameters (some corallites shown on Fig. 6A of Roniewicz, 2008, seem to be smaller than 2 mm), it seems to be more closely related to  C. dichotoma Columnaphyllia sp. [branching]  Comoseris jireceki Toula, 1889 [thamnasterioid to Refers to material described as  Comoseris cf. bargyensis meandroid]  Cyathophora bangoinensis Liao &amp; Xia, 1985 Refers to material described as  Pseudocoenia aff. baltovensis but [plocoid] shows characteristics typical of  Cyathophora (sensu Zaman &amp; </p>
            <p> Lathuilière, 2014) and dimensions of skeletal elements corresponding to  C. bangoinensis Cyathophora hexalobata Kuzmicheva, 1972 Refers to material described as  Cyathophora sp. 2 and  Cyathophora [plocoid] sp. 3, having dimensions of skeletal elements falling into the range of  C. hexalobata (see Kuzmicheva, 2002, p. 163–164, Pl. 23, Fig. 1; </p>
            <p> corallite diameter: 5.5–8.5 mm; s: 6+6+S3; diss/mm: 10–14/10)  Cyathophora claudiensis Étallon, 1859 [plocoid] Refers to material described as  Cyathophora sp. 1 (see text)  Dendraraea sp. [thamnasterioid] Refers to material described as “  Thamnarea " sp.; according to </p>
            <p> Lathuilière &amp; Gill (1998),  Thamnarea represents a junior synonym of  Dendraraea Dermoseris delgadoi Koby, 1905 [branching]  Dermoseris sp. [branching] Refers to material described as  Dermoseris sp. 2 Dimorphastrea excavata d’Orbigny, 1850b Refers to material described as  Dimorphastrea cf. dubia (see [thamnasterioid-circumoral] Roniewicz, 2008, Fig. 14D) but shows dimensions of skeletal elements which differ from the ones given (Roniewicz, 2008, p. 126) </p>
            <p> (corallite diameter and number of septa are often smaller than covered by the range given; therefore, transferred to  D. excavata ; see </p>
            <p> Baron-Szabo, 2018)  Dimorphastrea cf. heteromorpha (Quenstedt, 1857) [thamnasterioid-circumoral]  Dimorphocoenia ? sp. [thamnasterioid- circumoral to submeandroid]  Enallhelia sp. 2 [dendroid-sympodial] Refers to material described as  Enallhelia sp. Epistreptum cf. communeformae Ron., 2008 [none; solitary; conical]  Haplaraea aff. elegans Milaschewitsch, 1876 [none; solitary; conical]  Heliocoenia sp. 2 [plocoid]  Latiphyllia cf. suevica (Quenstedt, 1857) [phaceloid]  Latomeandra juettneri Eliášová, 1990 [phaceloid-subdendroid]  Latomeandra obliqua Roniewicz, 2008 [phaceloid-subdendroid]  Latomeandra ramosa (Koby, 1884) [phaceloid-subdendroid]  Latomeandra sp. [phaceloid-subdendroid] Refers to material described as  Latomeandra sp. 1 Lyubasha gracilis Roniewicz, 2008 [astreoid]  Microphyllia densecostata Sikharulidze, 1979 [meandroid] Table 6 (continued) [8.3] (refers to locality 8 in Fig. 6) </p>
            <p> Valanginian; Bulgaria (  Lyubasha Mountain ; Slivnitsa Formation); Roniewicz (2008) </p>
            <p> Taxon [corallite integration] Remarks  Microphyllia elevata Roniewicz, 2008 [meandroid]  Microsolena agariciformis Étallon, 1859 [thamnasterioid]  Microsolena aff. exigua Koby, 1887 [thamnasterioid]  Microsolena tuberosa (Michelin, 1843) [thamnasterioid]  Misistella cf. carpathica Eliášová, 1976 [dendroid-phaceloid]  Mitrodendron sp. 1 [dendroid]  Mitrodendron sp. 2 [dendroid]  Montlivaltia sp. 2 [none; solitary; conical] Refers to material described as  Montlivaltia sp. Ogilvinella elegans (Eliášová, 1973) [plocoid]  Ovalastrea sp. [plocoid]  Periseris lorioli (de From) [thamnasterioid-meandroid)] Refers to material described as  Periseris sp. A Placophyllia cf. blastemon Eliášová, 1976 [phaceloid]  Pleurophyllia tobleri (Koby, 1896) [phaceloid- Refers to material assigned to  Pleurophyllia aff. cara ; recently subfasciculate] transferred to  P. tobleri (see Baron-Szabo, 2018; and text)  Pleurostylina corallina de Fromentel, 1861 [cerioid] Refers to material described as  Latusastrea sp. but is a rather cerioid colony having 1) inner corallites embedded in a dissepimentarium; 2) showing intracalicular budding; 3) </p>
            <p>having corallite diameters of around 5 mm; and 4) around 30</p>
            <p> septa, thus closely corresponding to  Pleurostylina corallina Preverastraea cretacea (Roniewicz, 2008) [cerioid (- Refers to the type material (holotype NMNHS F-30251) subastreoid)] assigned to  Oedalmiopsis cretacea but, in contrast to the original description, is most likely a rhipidogyrid form that has a rather cerioid (-subastreoid) (not thamnasterioid) corallum corresponding to the genus  Preversastraea Protoseris sp. [thamnasterioid, mono- to multiserial]  Pruvostastraea crassisepta (Sikharulidze, 1979) [meandroid]  Psammogyra hykeli (Eliášová, 1973) [meandroid] In having long meandroid series, both the type specimen from the Tithonian of the Czech Republic and the material described as  Placogyra hykeli more closely correspond to the genus  Psammogyra Rhipidogyra minima Koby, 1880 [flabelliform] Refers to material described as  Rhipidogyra cf. minima Rhipidogyra sp. [flabelliform]  Siderastreites lyalintsensis Ron., 2008 [cerioid (- submeandroid)]  Solenocoenia sexradiata (Goldfuss, 1829) [plocoid]?  Somalica sp. [cerioid-subthamnasterioid] Refers to material (NMNHS F-30252) assigned to </p>
            <p> Oedalmiopsis cretacea but, in slight contrast to the original description, is a rhipidogyrid form with cerioid to subthamnasterioid corallites which seems to have pruvostastraeid wall structures, thus corresponding to the genus  Somalica Stylosmilia corallina Koby, 1881 [phaceloid-dendroid]  Stylosmilia octonaria Roniewicz, 1976 [phaceloid-dendroid]  Stylosmilia sp. [phaceloid]  Synastrea bellula d’Orbigny, 1850a [thamnasterioid (- In having septa ranging between 40–50 (in areas of intense submeandroid)] budding around 28 [see Roniewicz, 2008, Fig. 12L]) and a distance of corallite centers of 4–7 mm, the material described as  Synastrea microsolenoides very closely corresponds to the lectotype MNHN.F.R08338 of  Synastrea bellula Thecosmilia dichotoma Koby, 1884 [dendroid-phaceloid] Refers to material described as  Thecosmilia pinguis ; recently transferred to  Th. dichotoma (Baron-Szabo, 2018)</p>
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	https://treatment.plazi.org/id/0390879F3879FF8C2D8FFE3DE586F8B2	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	Baron-Szabo, Rosemarie Christine;Tschanz, Karl;KÜrsteiner, Peter	Baron-Szabo, Rosemarie Christine, Tschanz, Karl, KÜrsteiner, Peter (2022): Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages. Swiss Journal of Palaeontology (3) 141 (1): 1-61, DOI: 10.1186/s13358-021-00238-8, URL: https://doi.org/10.1186/s13358-021-00238-8
