Goniopora imperatoris Vaughan, 1919
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publication ID |
11755334 |
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persistent identifier |
https://treatment.plazi.org/id/D24287AB-FF57-8EBB-7DFF-700F6813FB56 |
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treatment provided by |
Felipe |
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scientific name |
Goniopora imperatoris Vaughan, 1919 |
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Goniopora imperatoris Vaughan, 1919 View in CoL
Pl. 12; figs 3, 4
v1873 Actinacis rollei, Reuss : Duncan, p. 561.
v*1919 Goniopora imperatoris: Vaughan , p. 493, pl. 142, figs 3, 3a.
1929 Goniopora casacadensis Vaughan, 1919 : Coryell & Ohlsen, p. 222, pl. 40, fig. 5.
1929 Goniopora imperatoris Vaughan, 1919 : Coryell & Ohlsen, p. 224, pl. 41, fig. 2.
1929 Goniopora portoricensis Vaughan, 1919 : Coryell & Ohlsen, p. 225, pl. 41, fig. 5.
1929 Goniopora regularis (Duncan), 1863 : Coryell & Ohlsen, p. 226, pl. 42, figs 1–1a.
1974 Goniopora regularis (Duncan) : Frost & Langenheim, p. 234, pl. 80, figs 4–7.
1979 Goniopora regularis: Frost & Weiss , p. 1113ff, fig. 8.
v1986 Goniopora imperatoris Vaughan : Foster, p. 85, pl. 35, figs 3–7, pl. 36, figs 1–7, pl. 37, figs 1–4, text-figs 2– 3, 6, 8, 11, 13, 14 (older synonyms cited therein).
v1988 Goniopora elegans ( Leymerie, 1846) : Drobne et al., p. 188, pl. 34, figs 1–3.
v1989 Goniopora imperatoris: Budd et al. , p. 267ff.
1992 Goniopora sp. , cf. G. vaughani Nomland, 1916 View in CoL : Squires & Demetrion, p. 19, figs 33–35.
v1994 Goniopora imperatoris: Budd et al. View in CoL , pp. 952, 957, 965, 974.
2002 Goniopora antiqua, Reig Oriol 1997 : Löser et al, p. 322.
v2000 Goniopora imperatoris Vaughan, 1919 View in CoL : Baron-Szabo, p. 118, pl. 9, fig. 3.
v2002 Goniopora imperatoris Vaughan, 1919 : Baron-Szabo, p. 127, pl. 89, figs 2–3.
Dimensions. d=1.8–2.8 mm, juveniles are as small as 1.4 mm; c-c=1.8– 4 mm; s=20–29.
Description. Ramose or massive, with calices that are rounded or polygonal in outline; septa subcompact, thin, equal in thickness, and have delicate granulations laterally; septal arrangement is bilaterally; one set, consisting of about 6 septa, extends to center of corallite, where the septa might dissociate to form pali or trabecular prolongations, which join with the columella ; about 6 septa, forming the second set, reach three quarters the length of the oldest ones; youngest septa are nearly equal with the septa of the preceding set; pali or paliform lobes irregularly occur axial to septa of every set; columella spongy or made of thin, twisted segments; wall synapticulothecal, incomplete.
Type locality of species. Middle Miocene of Panama (La Boca Formation) .
Distribution. Upper Santonian-Lower Campanian of northern Spain, Middle-Upper Maastrichtian of the UAE / Oman border region, Maastrichtian of Jamaica (new material), Danian of Italy and Slovenia (Dolenja vas), Middle Eocene of St. Bartholomew and Mexico (Bateque Formation), Upper Oligocene of Puerto Rico, Mexico (La Quinta Formation), and Antigua ( Antigua Formation), Lower Miocene of Anguilla ( Anguilla Formation) and?Georgia (Chattahoochee Formation), Lower-Middle Miocene of Florida (Tampa Formation, Panama (Emperador Limestone), and Anguilla ( Anguilla Formation), Middle Miocene of Panama (La Boca Formation) and Puerto Rico (Ponce Formation), Neogene of the Dominican Republic, Middle-Upper Pliocene of Jamaica (Bowden Formation) and Florida (Pinecrest Sandstone).
New Material. Maastrichtian of Jamaica, NMNH, Coates coll., sample nos.: 304b (=Jerusalem Mountain Inlier); 354a; 482; 490e; 506; 507; (=Ducketts Land Settlement); 570c; 570h; 570L (=probably Cambridge area); J-71-14d4 (=Road Sunderland Black); J-71-34p; J-71-40 (=Rio Minho).
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.
