Los Olcostephaninae Haug, 1910 (Ammonoidea) valanginianos de la cuenca andina de Chañarcillo del Cretácico Inferior del Norte de Chile.

Mourgues, Francisco Amaro; Bulot, Luc G.; Frau, Camille

doi:10.5027/andgeov42n2-a04

Cited by 10 publications

(1 citation statement)

References 27 publications

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“…Analogously, in the Chañarcillo Basin (northern Chile), the beds with Paraspiticeras and Sabaudiella from the lower part of the Upper Nantoco Member were correlated by Mourgues (2007) with the P. mortilleti and P. picteti ASzs. These beds are followed by the subtidal to supratidal deposits of the uppermost Nantoco Formation evincing an important regression phase in the basin.…”

Section: Correlationmentioning

confidence: 86%

The Global Boundary Stratotype Section and Point (GSSP) of the Barremian Stage at Río Argos (Caravaca, SE Spain)

Company,

Aguado,

Baudin

et al. 2024

Episodes

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Barremian Stage is defined at the base of bed 171 of the Río Argos section, near Caravaca (SE Spain) and correlated by the first appearance of the ammonite species Taveraidiscus hugii. This event falls within the NC5C calcareous nannofossil Subzone, the Lilliputianella semielongata planktonic foraminiferal Zone, and the Dorothia ouachensis benthic foraminiferal Zone. It roughly coincides with the beginning of a slightly negative trend interval in the δ 13 C curve. Indirect calibration to the magnetostratigraphic scale suggests that the boundary falls in the lowermost part of polarity chron M3r. According to the astrochronological analysis, a time interval of 0.74 myr separates the beginning of the late Hauterivian Faraoni Episode from the base of the Barremian, which is dated at 125.77 MA.

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Section: Correlationmentioning

confidence: 86%