Foraminiferal record of environmental changes: Messinian of the Los Yesos area (Sorbas Basin, SE Spain)

Goubert, Évelyne; Néraudeau, Didier; Rouchy, Jean-Marie; Lacour, Denis

doi:10.1016/s0031-0182(01)00386-8

Cited by 42 publications

(26 citation statements)

References 42 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…and CornØe et al (2002), however, proposed that the T3 deposits were coeval with both the Yesares and Sorbas Members, and that the Roger et al (2000) and CornØe et al(2002), Sorbas ages from Krijgsman et al (2001) gypsum developed in relatively deep basins. This proposal is in accordance with paleontological studies indicating rather deep marine environment in the uppermost part of the Abad Member, just under the gypsum Baggley 2000), and those concerning the marly interbeds in the Yesares gypsum, which indicate the deep part of the inner shelf with photophilic seagrass and the upper part of the outer shelf with sciaphilic seagrass (Saint Goubert et al 2001;Lacour et al 2002;NØraudeau et al 2002). Geochemical results by Rosell et al (1998) also suggest a rather deep depositional environment for the lowest gypsum beds.…”

Section: Alboran Seasupporting

confidence: 86%

Correlations and sequence stratigraphic model for Messinian carbonate platforms of the western and central Mediterranean

Cornée¹,

Martin²,

Conesa³

et al. 2004

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

Distance correlations of Late Tortonian-Messinian littoral carbonate complexes are proposed from the study of eight platforms in the western and central Mediterranean. Correlations are based on the identification of two major biological sedimentary cycles and of two index surfaces. Surface A is a maximum flooding surface during cycle 1 at around 6.7 Ma. Surface B is a regional marine planation surface at around 5.95 Ma, at the base of cycle 2 (Terminal Carbonate Complex). A general sedimentary model is proposed for the 7-5.6-Ma time-span. The boundary between cycles 1 and 2 is coincident with the onset of the Messinian Salinity Crisis, and appears to be related to major environmental-paleooceanographic changes in the Mediterranean, rather than to a major sea-level drop or to climatic change.

show abstract

Section: Alboran Seasupporting

confidence: 86%

Correlations and sequence stratigraphic model for Messinian carbonate platforms of the western and central Mediterranean

Cornée¹,

Martin²,

Conesa³

et al. 2004

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

show abstract

“…Krijgsman et al, 2001). Also benthic fossils are extremely rare (apart from few exceptions such as the Sorbas basin, where normal marine assemblages have been reported; Saint Martin et al, 2000;Goubert et al, 2001), thus reflecting diffuse anoxic bottom conditions related to a stratified water column (e.g. Sinninghe Damsté et al, 1995;Manzi et al, 2007).…”

Section: Accepted M Manuscriptmentioning

confidence: 99%

Flocculent layers and bacterial mats in the mudstone interbeds of the Primary Lower Gypsum unit (Tertiary Piedmont basin, NW Italy): Archives of palaeoenvironmental changes during the Messinian salinity crisis

et al. 2014

View full text Add to dashboard Cite

Terms of use:Open Access (Article begins on next page) Anyone can freely access the full text of works made available as "Open Access". Works made available under a Creative Commons license can be used according to the terms and conditions of said license. Use of all other works requires consent of the right holder (author or publisher) if not exempted from copyright protection by the applicable law. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Availability: This is the author's manuscript A C C E P T E D M A N U S C R I P T ACCEPTED MANUSCRIPT

show abstract

“…Broken, poorly preserved, pyritized and transported (abraided) specimens were categorized for each species (Table 4). Identifications were based on various taxonomic references (Redois, 1996;Murray, 2003;Perez-Belmonte, 2008) and interpretations of assemblages (Table 5) were carried out using ecological data (Fatela, 1995;Goubert, 1997;Perez-Belmonte, 2008) or morphofunction method for the sparsely documented species (Severin, 1983;Bernhard, 1986;Duleba et al, 1999;Goubert et al, 2001).…”

Section: Foraminiferal Content Analysismentioning

confidence: 99%

The paleo-Etel River incised valley on the Southern Brittany inner shelf (Atlantic coast, France): Preservation of Holocene transgression within the remnant of a middle Pleistocene incision?

Estournès¹,

Menier²,

Guillocheau³

et al. 2012

Marine Geology

View full text Add to dashboard Cite

Foraminiferal record of environmental changes: Messinian of the Los Yesos area (Sorbas Basin, SE Spain)

Cited by 42 publications

References 42 publications

Correlations and sequence stratigraphic model for Messinian carbonate platforms of the western and central Mediterranean

Correlations and sequence stratigraphic model for Messinian carbonate platforms of the western and central Mediterranean

Flocculent layers and bacterial mats in the mudstone interbeds of the Primary Lower Gypsum unit (Tertiary Piedmont basin, NW Italy): Archives of palaeoenvironmental changes during the Messinian salinity crisis

The paleo-Etel River incised valley on the Southern Brittany inner shelf (Atlantic coast, France): Preservation of Holocene transgression within the remnant of a middle Pleistocene incision?

Contact Info

Product

Resources

About