Aretz et al_2011.pdf - ORBi - Université de Liège
Aretz et al_2011.pdf - ORBi - Université de Liège
Aretz et al_2011.pdf - ORBi - Université de Liège
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Kölner Forum Geol. P<strong>al</strong>äont., 19 (2011)<br />
M. ARETZ, S. DELCULÉE, J. DENAYER & E. POTY (Eds.)<br />
Abstracts, 11th Symposium on Fossil Cnidaria and Sponges, <strong>Liège</strong>, August 19-29, 2011<br />
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Katian in units P/7 and P/13. Only few cor<strong>al</strong> colonies were observed from the Silurian part of the sequence<br />
(P/16). REED (1912) <strong>de</strong>scribed Streptelasma sp. aff. S. corniculum, Streptelasma sp. or Zaphrentis sp.,<br />
Streptelasma? sp., Heliolites <strong>de</strong>pauperata, Heliolites? sp., Lyopora? sp., Propora him<strong>al</strong>aica, C<strong>al</strong>apoecia? sp.,<br />
Protaraea kanaurensis, Favosites spitiensis, H<strong>al</strong>ysites catenularia var. kanaurensis, H<strong>al</strong>ysites w<strong>al</strong>lichi, H<strong>al</strong>ysites sp.<br />
and listed the species of Plasmoporella from the Takche Member. Among them, the species, except for<br />
Streptelasma? sp., Heliolites <strong>de</strong>pauperata, Lyopora? sp. and Plasmoporella sp., were ones that REED (1912)<br />
<strong>de</strong>scribed from HAYDEN’S Horizon 6 as the Silurian species. According to REED (1912), (?)Llandoverian<br />
strata (Mikkim Member) yiel<strong>de</strong>d Favosites sp. cf. F. forbesi?, Favosites sp. cf. F. niagarensis?, Lindstroemia sp.<br />
and C<strong>al</strong>ostylis dravidiana.<br />
Based on the present study of cor<strong>al</strong> materi<strong>al</strong> collected from the type section we can confirm occurrences<br />
of following tabulate and rugose cor<strong>al</strong>s: Favosites spitiensis, Favosites sp., Plasmoporella sp., H<strong>al</strong>ysites w<strong>al</strong>lichi,<br />
H<strong>al</strong>ysites? sp., Protaraea? sp., Proheliotidae? gen. <strong>et</strong> sp. ind<strong>et</strong>., C<strong>al</strong>ostylis? sp., Streptelasma sp.,<br />
Streptelasmatidae gen. <strong>et</strong> sp. ind<strong>et</strong>. Of them, Favosites sp. and Plasmoporella sp. occurred in the unit P/13.<br />
Streptelasma sp., Streptelasmatidae gen. <strong>et</strong> sp. ind<strong>et</strong>. and H<strong>al</strong>ysites? sp. were found in the units P/8, 10 and<br />
16, respectively. Others were collected in the well weathered rubble just below the section that <strong>de</strong>rived<br />
from the Takche Member.<br />
170<br />
This is a contribution to IGCP 591.<br />
BHARGAVA, O.N. & BASSI, U.K. (1986): Silurian reef<strong>al</strong> buildups, Spiti-Kinnaur, Himach<strong>al</strong> Him<strong>al</strong>aya, India. - Facies, 15:<br />
35-52.<br />
BHARGAVA, O.N. & BASSI, U.K. (1998): Geology of Spiti-Kinnauer Himach<strong>al</strong> Him<strong>al</strong>aya. - Memoir Geoloigic<strong>al</strong> Survey<br />
India, 124: 1-210.<br />
FORTEY, R.A. & COCKS, L.R.M. (2005): Late Ordovician glob<strong>al</strong> warming – The Boda event. - Geology, 33 (5): 405-408.<br />
HAYDEN, H.H. (1904): The geology of Spiti with parts of Bashahr and Rupshu. - Memoir Geoloigic<strong>al</strong> Survey India, 36: 1-<br />
129.<br />
LOI, A., GHIENNE, J.F., DABARD, M.P., PARIS, F., BOTQUELEN, A., CHRIST, N., ELAOUAD-DEBBAJ, Z., GORINI, A., VIDAL, M.,<br />
VIDET, B. & DESTOMBES, J. (2010): The Late Ordovician glacio-eustatic record from a high-latitu<strong>de</strong> storm-dominated<br />
shelf succession: The Bou Ingarf section (Anti-Atlas, Southern Morocco). - P<strong>al</strong>aeogeography, P<strong>al</strong>aeoclimatology,<br />
P<strong>al</strong>aeoecology, 296: 332-358.<br />
REED, F. R. C. (1912): Ordovician and Silurian Fossils from Centr<strong>al</strong> Him<strong>al</strong>aya. - P<strong>al</strong>aeontologica Indica, Series 15, 7/2: 1-<br />
168.<br />
SHEEHAN, P. M. (2001): The Late Ordovician mass extinction. - Annu<strong>al</strong> Review of Earth and Plan<strong>et</strong>ary Sciences, 29: 331-<br />
364.<br />
SUTTNER, T. (2003): Die Pin Formation (Altp<strong>al</strong>äozoikum) von Muth, Spiti (Indischer Him<strong>al</strong>aya): Stratigraphie und<br />
Fazies. - Diploma thesis, University of Vienna, 1- 80.<br />
SUTTNER, T. J. (2007): The Upper Ordovician to Lower Silurian Pin Formation (Farka Muth, Pin V<strong>al</strong>ley, North India) – A<br />
form<strong>al</strong> discussion and re<strong>de</strong>finition of its controversi<strong>al</strong> type-section. - Acta P<strong>al</strong>aeontologica Sinica, 46: 460-465.<br />
SUTTNER, T. J. & ERNST, A. (2007): Upper Ordovician bryozoans of the Pin Formation (Spiti v<strong>al</strong>ley, northern India). -<br />
P<strong>al</strong>aeontology, 50 (6): 1485-1518.<br />
SUTTNER, T. J., LEHNERT, O., JOACHIMSKI, M. & BUGGISCH, W. (2007): Recognition of the Boda event in the Pin Formation<br />
of northern India based on new δ 13C and conodont data. - Acta P<strong>al</strong>aeontologica Sinica, 46: 466-470.<br />
WEBBY, B. D. (2002): Patterns of Ordovician reef <strong>de</strong>velopment. - In: KIESSLING, W., FLÜGEL, E. & GOLONKA, J. (EDS.),<br />
Phanerozoic Reef Patterns. SEPM Speci<strong>al</strong> Publication, 72: 129-179.