2015
DOI: 10.1016/j.jsames.2015.02.005
|View full text |Cite
|
Sign up to set email alerts
|

Insights into Pleistocene palaeoenvironments and biostratigraphy in southern Buenos Aires province (Argentina) from continental deposits

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
7
0

Year Published

2017
2017
2021
2021

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 7 publications
(7 citation statements)
references
References 27 publications
0
7
0
Order By: Relevance
“…The FA1 emerges in the basal sector (sometimes also at medium sector) of the cliffs that extend almost continuously from Centinela del Mar to Mar del Sur localities (Cenizo, 2011, p. 30; see also Cenizo and Tassara, 2013, p. 21). In addition, the FA1 has been recognized (in similar facies succession, although not equal) in the Chocorí stream area as “Lower Interval” by Beilinson et al (2015). The FA1 is characterized by a predominance of fluvial-alluvial depositional events of great homogeneity and amplitude, with the development of massive carbonate banks and “grid-like” carbonate infiltrations as main post-depositional facies, especially on its upper contact.…”
Section: Systematic Paleontologymentioning
confidence: 94%
See 1 more Smart Citation
“…The FA1 emerges in the basal sector (sometimes also at medium sector) of the cliffs that extend almost continuously from Centinela del Mar to Mar del Sur localities (Cenizo, 2011, p. 30; see also Cenizo and Tassara, 2013, p. 21). In addition, the FA1 has been recognized (in similar facies succession, although not equal) in the Chocorí stream area as “Lower Interval” by Beilinson et al (2015). The FA1 is characterized by a predominance of fluvial-alluvial depositional events of great homogeneity and amplitude, with the development of massive carbonate banks and “grid-like” carbonate infiltrations as main post-depositional facies, especially on its upper contact.…”
Section: Systematic Paleontologymentioning
confidence: 94%
“…The FA1 is characterized by a predominance of fluvial-alluvial depositional events of great homogeneity and amplitude, with the development of massive carbonate banks and “grid-like” carbonate infiltrations as main post-depositional facies, especially on its upper contact. The greater consolidation of its sediments, as well as the tabular appearance and the large horizontal extension of its deposits with respect to the overlying facies, are some of the main features that allow a rapid identification of FA1 in the field (Cenizo, 2011; Beilinson et al, 2015). Such facies association has been correlated with the Middle Allomember of the Punta San Andrés Alloformation described by Zárate (1989), ~40 km NE of the type locality (Cenizo, 2011; Beilinson et al, 2015).…”
Section: Systematic Paleontologymentioning
confidence: 99%
“…This biostratigraphical scheme has therefore become a standard with which other South America sequences are now routinely compared (e.g. Lopes et al, 2010;Tonni et al, 2009;Beilinson et al, 2015).…”
Section: Hereabouts 63 North and South Americamentioning
confidence: 99%
“…Both Lf G and Lf I are grouped into the Facies Association 2 (FA2, [36]). It was tentatively correlated with the unit Upper Allomember of the Punta San Andrés Alloformation [36], located about 50 km NE of the Centinela del Mar [39,40]. These units are well exposed and extend all over the cliff surface of Centinela del Mar to the NE and SW [36,40].…”
Section: Methodsmentioning
confidence: 85%