Carboniferous Calcareous Algae

Mamet, Bernard

doi:10.1007/978-3-642-52335-9_19

Cited by 70 publications

(70 citation statements)

References 34 publications

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“…It has long been recognized that several cyanobacteria, algae and algosponges are limited to the Mississippian and/or Pennsylvanian (e.g., Garwood 1914;Wood 1940Wood , 1942Wood , 1963Wood , 1964Johnson & Konishi 1956;Maslov 1956;Elliott 1968a;Petryk & Mamet 1972;Emberger 1976;Vachard & Cózar 2010) and the importance of some algae and algosponges at least as regional biostratigraphic markers has been clearly demonstrated (e.g., Mamet & Rudloff 1972;Vachard 1977a, b;Perret & Vachard 1977;Skompski 1981Skompski , 1986Skompski , 1987Mamet & Roux 1983;Skompski et al 1989;Mamet 1991Mamet , 1997Mamet , 2002Mamet , 2006Vachard & Berkhli 1992;Sebbar & Mamet 1996Sebbar 1998;Berkhli & Vachard 2001;Krainer & Vachard 2002;Cózar 2004Cózar , 2005Cózar & Somerville 2004, 2005aCózar et al 2008Cózar et al , 2009Pille 2008;Somerville 2008;Pille & Vachard 2011). Several genera first appear and diversify in the late Viséan and Serpukhovian;e.g., Ungdarella, Kulikia, Neoprincipia, Richella, Archae...…”

Section: Discussionmentioning

confidence: 99%

“…However, in recent years, several discoveries in the Serpukhovian have been mentioned Koninckopora in China (Mamet 1991, Groves et al 2012, SW Spain (Cózar 2005) and the Moroccan Meseta (Cózar et al 2008). In the Montagne Noire, different species of Koninckopora also exist in the early Serpukhovian (biozones F-H).…”

Section: Discussionmentioning

confidence: 99%

“…-It is also possible that our material belongs to Hikorocodium Endo, 1951 sensu lato; first described as a codiale as indicated by its name but then assigned to the ischyrospongia or hypercalcified sponges (Vachard 1976, Senowbari-Daryan & Rigby 2007, Mamet & Préat 2013 (Lemosquet & Poncet 1977, Poncet 1986, Sebbar & Lys 1989, Sebbar 1990, Sebbar & Mamet 1996; early Bashkirian of northern Spain (Vachard & Beckary 1991 Bassoullet et al, 1979 (pars;see Bassoullet et al 1979, Roux 1985, Chuvashov et al 1987, and Mamet 1991 Comparison. -The Anatoliporaceae differ from the true Dasycladales in the small central cavity, the numerous, oblique, aspondyl laterals.…”

Section: Stratum Typicum -Tarusian (Earliest Serpukhovian)mentioning

confidence: 99%

“…-Latest Viséan (Brigantian) to late Serpukhovian (Arnsbergian). Japan, Montagne Noire, Pyrenees, Spain, Belgium, ?Algeria, Alaska, and Alberta (Mamet 1991).…”

Section: Stratum Typicum -Tarusian (Earliest Serpukhovian)mentioning

confidence: 99%

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Late Viséan-early Serpukhovian cyanobacteria and algae from the Montagne Noire (France); taxonomy and biostratigraphy

Vachard¹,

Cózar²,

Aretz³

et al. 2016

Bull. Geosci.

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Section: Discussionmentioning

confidence: 99%

Section: Discussionmentioning

confidence: 99%

Section: Stratum Typicum -Tarusian (Earliest Serpukhovian)mentioning

confidence: 99%

“…-Latest Viséan (Brigantian) to late Serpukhovian (Arnsbergian). Japan, Montagne Noire, Pyrenees, Spain, Belgium, ?Algeria, Alaska, and Alberta (Mamet 1991).…”

Section: Stratum Typicum -Tarusian (Earliest Serpukhovian)mentioning

confidence: 99%

See 2 more Smart Citations

Late Viséan-early Serpukhovian cyanobacteria and algae from the Montagne Noire (France); taxonomy and biostratigraphy

Vachard¹,

Cózar²,

Aretz³

et al. 2016

Bull. Geosci.

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“…The alga is generally rare and seems commonly associated with a bioturbated, peloidal facies (Mamet et al, 1987;Warnke, 1997). Rectangulina is reported from other localities, e.g., the Tethys and the Canadian Arctic (Mamet, 1991). Nevertheless, buildups of Rectangulina have not previously been reported outside the Carnic Alps.…”

Section: Description-mentioning

confidence: 97%

Upper Carboniferous-Lower Permian Buildups of The Carnic Alps, Austria-Italy

Samankassou¹

Permo-Carboniferous Carbonate Platforms and Reefs

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A variety of buildup types occur in the upper Paleozoic Auernig and Rattendorf Groups, Carnic Alps, at the present-day Austrian-Italian border, including coral, diverse algal (Anthracoporella, Archaeolithophyllum, Rectangulina, and phylloid green), bryozoan, brachiopod, and sponge buildups. Thin mounds and banks have a diverse fossil association (e.g., Archaeolithophyllum-bryozoanbrachiopod mounds) and occur in siliciclastic-dominated intervals, as do coral buildups. Some of the biodiverse thin mounds occur in strata that were deposited in cooler water. However, the thickest mounds are nearly monospecific (e.g., Anthracoporella mounds) and grew in carbonate-dominated, warm-water environments.Most of the mounds considered in this paper, particularly algal mounds, grew in quiet-water environments below wave base but within the photic zone. Mound growth was variously stopped by siliciclastic input, e.g., auloporid coral mounds, sea-level rise, e.g., the drowning of Anthracoporella mounds of the Rattendorf Group, influence of cool water, e.g., algal mounds of the Auernig Group overlain by limestone of cool-water biotic association, or sea-level fall, e.g., phylloid algal mounds that were subsequently exposed subaerially. There is no indication of ecological succession during mound growth. Growth, dimensions, biotic association, and termination of mounds seem to have been controlled by extrinsic factors, mainly sea level and water temperature.Phylloid algal mounds are similar to those described from other late Paleozoic settings. Auloporid coral buildups, and Rectangulina and Anthracoporella algal buildups, however, have not previously been reported from other regions, although these fossils are described from several localities outside the Carnic Alps.Permo-Carboniferous Carbonate Platforms and Reefs SEPM Special Publication No. 78 and AAPG Memoir 83,

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Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago)

Davydov

2016

Tectonics

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A warm‐water fauna and flora from a Carboniferous limestone xenolith that was captured during penetration of deep intraplate Cenozoic basalts through a Paleozoic carbonate platform have been found on Zhokhov Island, New Siberian Archipelago (NSA). This limestone xenolith contains a very high taxonomic diversity of Moscovian (Middle Pennsylvanian) tropical foraminifera and calcareous algae. As this warm‐water biota never occurs north of the forbiddance line, i.e., 30–35°N/S, this fauna and algal flora constrain the paleogeography and interpretation of the paleotectonics in the region. Thus, the location of the most of the New Siberian Archipelago islands at that time must have been within tropics or subtropics. Analyses of the existing data on fusulinid distribution within the Arctic region indicate that Zhokhov and Wrangel Islands were still a part of Alaska‐Chukotka composite terrane as late as in the Artinskian. Both fusulinid and detrital zircon provenance data suggest that the Chukotka microplate, NSA, and Wrangel Island probably were close to Arctic Alaska until Triassic time. The fusulinids from the Mankomen Formation and other formations in Wrangelia show a strong affinity with the Uralo‐Franklinian province regions including the Sverdrup Basin, Spitsbergen, Barents Sea, and Timan‐Pechora and the northern‐central Urals rather than with northern Panthalassa.

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Carboniferous Calcareous Algae

Cited by 70 publications

References 34 publications

Late Viséan-early Serpukhovian cyanobacteria and algae from the Montagne Noire (France); taxonomy and biostratigraphy

Late Viséan-early Serpukhovian cyanobacteria and algae from the Montagne Noire (France); taxonomy and biostratigraphy

Upper Carboniferous-Lower Permian Buildups of The Carnic Alps, Austria-Italy

Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago)

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