Carbon–isotope stratigraphy and ammonite faunal turnover for the Middle Jurassic in the Southern Iberian palaeomargin

O’Dogherty, Luis; Sandoval, José; Bartolini, Annachiara; Bruchez, Sébastien; Bill, Markus; Guex, Jean

doi:10.1016/j.palaeo.2006.01.018

Cited by 80 publications

(61 citation statements)

References 29 publications

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“…O'Dogherty et al (2006), exploring ammonoid taxonomic fluctuations within the southern Iberian paleomargin, claim that trends during ecologically stable periods also show the development of more complex ornamentation. In another example, Navarro et al (2005) report that the trend toward more compressed forms of shell occur during the initial colonization of the Arctic Basin by the Cardioceratidae at the end of the Bajocian.…”

Section: A Review Of Macroevolutionary Patterns and Evolutionary Trenmentioning

confidence: 99%

Evolutionary Trends within Jurassic Ammonoids

Neige

Rouget²

2015

Topics in Geobiology

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Section: A Review Of Macroevolutionary Patterns and Evolutionary Trenmentioning

confidence: 99%

Evolutionary Trends within Jurassic Ammonoids

Neige

Rouget²

2015

Topics in Geobiology

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“…Occurrence.-Dimorphinites is known from Europe, northern Africa and southern Transcaucasus: England (Buckman, 1923;Donovan et al, 1981), France (d 'Orbigny, 1845;Rioult, 1994aRioult, , 1994bRioult, , 1994c, Algeria (Roman, 1930), northern Italy (Sturani, 1964a(Sturani, , 1964bClari et al, 1984), Sicily (Wendt, 1964;Pavia et al, 2002;Galacz, 2008), Alps (Krystyn, 1972), Hungary (Galacz, 1980), Betic Basin (Sandoval, 1983(Sandoval, , 1990Sandoval et al, 2001;O'Dogherty et al, 2006), Iberian Basin (Fernandez-Lopez, 1985, Transcaucasus (Rostovtsev, 1985), Atlas (Enay et al, 1987), Carpathian (Wierzbowski et al, 1999;Schlö gl et al, 2005), Tunisia (Soussi et al, 2000), Portugal (Fernandez-Lopez et al, 2006, 2009a and Germany (Dietze and Bernt, 2009). …”

Section: Systematic Paleontologymentioning

confidence: 99%

“…7a-e). Rioult et al, 1997;Mangold and Rioult, 1997;Hillebrandt, 2001;Callomon, 2003;O'Dogherty et al, 2006;Riccardi, 2008;Fernandez-Lopez et al, 2009b). Province, or subprovinces, and the Eastern Pacific Subrealm (Westermann and Riccardi, 1980;Westermann, 1981Westermann, , 1993Westermann, , 2000Westermann, , 2001Riccardi et al, 1990aRiccardi et al, , 1990bRiccardi et al, , 1992Riccardi et al, , 1994Riccardi and Westermann, 1991a, 1991bHillebrandt et al, 1992aHillebrandt et al, , 1992bFernandez-Lopez et al, 1994, 2009bGrö schke andHillebrandt, 1993, 1994;Hillebrandt, 2001;Grö schke, 1996;Page, 2008;Riccardi, 2008).…”

Section: Systematic Paleontologymentioning

confidence: 99%

Dimorphinites(Ammonoidea, Jurassic, upper Bajocian) in the precordillera of northern Chile

Fernández-López

Diaz

2011

J. Paleontol.

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A new upper Bajocian ammonite assemblage containing the morphoceratidsDimorphinites dimorphus(d'Orbigny) andVigoriceras defrancei(d'Orbigny) is reported from the circum-Pacific area. These ammonites were found at the top of the Torcazas Formation, in the Quebrada San Pedro area, Precordillera of northern Chile. Taphonomic, systematic, and paleobiogeographic data confirm these dimorphs were part of indigenous populations within the Tarapaca Basin, belonging to the same demic biospecies:Dimorphinites defrancei(d'Orbigny). The West Tethyan and East-Pacific distribution ofD. defranceicorroborates the availability of the migratory seaway, the so-called Hispanic Corridor, between the western Tethys and the eastern Pacific Ocean during the upper Bajocian Parkinsoni Zone. The discovery of this upper BajocianDimorphinitesassemblage provides a new biochronostratigraphic horizon in the Tarapaca Basin and an interoceanic correlation point for the latest Bajocian.

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“…The requirement of suitability for magnetostratigraphy and geochronometry, however, can be in directly satisfIed by reference to the Bathonian magnetostrati graphic scale of Steiner et al (1987;O'Dogherty et al 2006) as defmed in the Subbetic Cordillera.…”

Section: Gamma-ray Spectrometrymentioning

confidence: 99%

Formal proposal for the Bathonian GSSP (Middle Jurassic) in the Ravin du Bès Section (Bas-Auran, SE France)

Fernández-López

Pavia²,

Erba

et al. 2009

Swiss J. Geosci.

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The Bathonian Global Stratotype Section and Point (GSSP) is proposed at the base of limestone bed RB071 (bed 23 in Sturani 1967) in the Ravin du Bes Section (43057' 38" N, 6° IS' 55" E), Bas-Auran area, "Alpes de Haute Provence" French department. The Ravin du BesSectioll , as formal candidate GSSP for the base of the Bathonian Stage, satisfies most of the requirements recommended by the International Commission on Stratigraphy: 1) The ex posure extends over 13 m in thickness. At the Bajocian-Bathonian transition, no vertical (bio-, ichno-or tap ho-) facies changes, condensation, stratigraphic gaps or hiatuses have been recorded. Structural complexity, synsedimentary and tectonic disturbances, or important alterations by metamorphism are not relevant constraints. 2) There is a well-preserved, abundant and diverse fos sil record across the boundary interval, with key markers (ammonites and IntroductionThe present paper corresponds to part of the scientifIc dossier recently prepared by several specialists and sent to all mem bers of the Bathonian Working Group (International Subcom mission on Jurassic Stratigraphy, November 2007), in order to achieve the formal ballot on the selection and proposal of the Global Stratotype Section and Point (hereafter GSSP The Bathonian Working Group (BtWG) was established in 1984, during the 1st International Symposium on Jurassic Stratigraphy in Erlangen, in order to improve the geologic data relative to the Bajocian/Bathonian boundary. The Bas-Auran section was first proposed as stratotype in a presentation to the Luxembourg II (1967) Colloquium by Torren� but not pub lished until 1974lished until (Morton 1974Torrens 1974a Torrens , b, 1987 Torrens , 2002 fig. 8; pI. 19, fIgS. 1-2) are the index species, respectively, of the Bathonian basal zone and subzone. The Zigzag Zone was distinguished from the underlying Parkinsoni Zone by Oppel (1857Oppel ( . p. 579. 1862. and later assigned to the "Bath-Gruppe·· (Oppel 1865. p. 309) in a discussion of the section at "Mon tagne de Crussol" in the Ardeche (France). The Convergens Subzone was mentioned by Maubeuge (1950, p. 4), based on the "Convergens horizon" that was used in letters by Arkell (1951-59. p.10; 1956. p. 62). The Bajocian/Bathonian bound ary established between the Parkinsoni and Zigzag zones was recommended at the two congresses denominated "Colloque du Jurassique" held in Luxembourg in 1962(Rioult 1964 Tor rens 1965) and 1967(Torrens 1974a. The localities of Bath (England) and the "Montagne de Crussol" (France), however, have been considered quite unsuitable for a typological defini tion of the Bathonian Stage, because they are condensed sec tions with discontinuous and lenticular beds (Torrens 1974a(Torrens , b, 2002Page 1996b). After the publication of Sturani (1967) (Sturani 1967). The Parvum Sub zone has been proposed by Mangold (1990) to denote the first Bathonian subzone of the Zigzag Zone in the Sub-Mediter ranean Province, equivalent to the Convergens Sub zone of the Northwest European Province...

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Carbon–isotope stratigraphy and ammonite faunal turnover for the Middle Jurassic in the Southern Iberian palaeomargin

Cited by 80 publications

References 29 publications

Evolutionary Trends within Jurassic Ammonoids

Evolutionary Trends within Jurassic Ammonoids

Dimorphinites(Ammonoidea, Jurassic, upper Bajocian) in the precordillera of northern Chile

Formal proposal for the Bathonian GSSP (Middle Jurassic) in the Ravin du Bès Section (Bas-Auran, SE France)

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