2019
DOI: 10.1007/s10347-019-0569-0
|View full text |Cite
|
Sign up to set email alerts
|

Larger foraminifera and strontium isotope stratigraphy of middle Campanian shallow-water lagoonal facies of the Pyrenean Basin (NE Spain)

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2020
2020
2025
2025

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 9 publications
(3 citation statements)
references
References 47 publications
0
3
0
Order By: Relevance
“…It is thus affirmed that during the Campanian a biogeographic connection, represented by foraminifers and Demospongiae, was established between the Tibetan and Mediterranean areas. The confidence in the age assignment is provided by a direct correlation with the European fauna, which stratigraphic age is calibrated by means of Strontium Isotope (e.g., STEUBER et al, 2005;FRIJIA et al, 2015;VILLALONGA et al, 2019). However, we cannot exclude the presence of a biogeographic effect, likely due to faunal dispersal, which may slightly affect such age-correlation.…”
Section: Comparison Of the Aksai Chin Fauna With Other Neotethys Faunasmentioning
confidence: 89%
“…It is thus affirmed that during the Campanian a biogeographic connection, represented by foraminifers and Demospongiae, was established between the Tibetan and Mediterranean areas. The confidence in the age assignment is provided by a direct correlation with the European fauna, which stratigraphic age is calibrated by means of Strontium Isotope (e.g., STEUBER et al, 2005;FRIJIA et al, 2015;VILLALONGA et al, 2019). However, we cannot exclude the presence of a biogeographic effect, likely due to faunal dispersal, which may slightly affect such age-correlation.…”
Section: Comparison Of the Aksai Chin Fauna With Other Neotethys Faunasmentioning
confidence: 89%
“…Although a more detailed study is required, preliminary interpretations suggest that the sedimentological sequence at Cal Torrades may represent one of the last transgressive pulses, before the regressive sequence represented by the Upper Cretaceous Gresos d' Areny Formation 29 in the Southern Pyrenees. The benthonic macroforaminifera assemblage recovered in the strata immediately above to the Perles Formation suggests a bathymetric depth between 20 and 80 m [34][35][36] . This interpretation concurs with the absence of high-energy sedimentary structures at the outcrop, suggesting that the depositional environment would be, at least, under the storm-affectation level.…”
Section: Geological Settingmentioning
confidence: 99%
“…Thereby, it is most likely that the sedimentological sequence at the Cal Torrades locality was established in a marine mid-ramp environment, as well as its lateral equivalent formations (e.g. Terradets Formation; see 32,35 ).…”
Section: Geological Settingmentioning
confidence: 99%