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Bajocian Solenopora

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Journal Article
Published: 01 January 1946
Bulletin de la Société Géologique de France (1946) S5-XVI (7-9): 491–496.
... are assigned to a new variety, lingonensis, of Solenopora jurassica. GeoRef, Copyright 2015, American Geosciences Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States 1946 algae Bajocian...
Journal Article
Published: 01 April 1997
Journal of the Geological Society (1997) 154 (2): 321–333.
... of America Memoirs 1957 67 599 640 Leeder M.R. Nami M. Sedimentary models for the non-marine Scalby Formation (Middle Jurassic) and evidence for late Bajocian/Bathonian uplift of the Yorkshire Basin Proceedings of the Yorkshire Geological Society 1979 42 461 482 Lloyd R.M...
Journal Article
Published: 01 April 1977
Journal of the Geological Society (1977) 133 (4): 363–373.
... ) either. The red alga Solenopora certainly occurs abundantly in both (and also in the Bathonian), but is believed to have been ancestral or related to the modern calcitic coralline algae which have many species in cool waters (the Dasycladaceae are aragonitic). In the Middle Jurassic, marine limestones...
Journal Article
Published: 01 February 2012
Italian Journal of Geosciences (2012) 131 (1): 3–18.
... of angular, decimetre-sized blocks of Calcare Massiccio hosted in a micritic matrix are present along the south-eastern paleoescarpment. These deposits rest on the Calcare e Marne a Posidonia (Lower Dogger) and are lateral to the lower portion of the Bajocian p.p-Kimmeridgian p.p. Calcari Diasprigni ( G...
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Journal Article
Published: 01 November 2009
Proceedings of the Yorkshire Geological Society (2009) 57 (3-4): 193–216.
... arachnoides, T. concinna (Goldfuss), Rhabdophyllia phillipsii, Stylina sp., and small algal structures ( Solenopora ). Wilson (1936) confused these beds with the Malton Oolite, mistakenly believing that micritic limestones full of rolled shell fragments were ooidal. Localities in the area...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2009
GeoArabia (2009) 14 (1): 147–210.
... Jurassic series that follow without any apparent break from the Lower Jurassic are well developed. They consist of bioclastic and oolitic limestones that have the following age ranges ( Figure 13 ) ( Lapparent et al., 1966 ; Montenat and Bassoullet, 1983 ): Bajocian: Rhynchonellids and ammonites...
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Journal Article
Journal: AAPG Bulletin
Published: 15 March 2020
AAPG Bulletin (2020) 104 (3): 565–593.
... are Favositida corals, although numerous other taxa have been identified as well: Catenipora , Vermiporella , Solenopora , and stromatoporoids at Lijiapo outcrop ( Bao et al., 2016 ); Lichenaria , Amsassia , and Syringoporella corals at Haoshihe outcrop, and Favistella and Quepora corals at Taoqu...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2002
DOI: 10.1144/GOSPP.11
EISBN: 9781862393912
... fairweather wave base to below storm wave base. Ammonites are more common, witnessing open marine conditions between late Sinemurian and early Bajocian times. All ammonite zones from this interval have been identified ( Suárez-Vega 1974 ; Fernández-López & Suárez-Vega 1979 ), from Obtusum to Sauzei zones...
Series: SEPM Special Publication
Published: 01 January 2002
DOI: 10.2110/pec.02.72.0465
EISBN: 9781565761940
..., and Yemen; 29, Karakorum; 30, Kachchh, India; 31, southern Tanzania and southwestern Madagascar. Map provided by Wolfgang Kiessling. Fig. 3.— Global distribution of Bajocian and Bathonian reefs, indicating probable current systems and dominant reef biota. 1, mountains; 2, land; 3, shelf; 4, deep...
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Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.442(12)
... in the Wallowa Mountains as “1000 to 3000 feet of limestone, limy shale, and interbedded volcanic rocks of Upper Triassic age.” CORRELATIONAL AND NOMENCLATURAL PROBLEMS By Middle Jurassic (Bajocian) time, coral and bivalve faunas from the Wallowa terrane show stronger links to the Western Interior Embayment...
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