The occurrence and role of microencruster frameworks in Late Jurassic to Early Cretaceous platform margin deposits of the Northern Calcareous Alps (Austria)

Schlagintweit, Félix; Gawlick, Hans‐Jürgen

doi:10.1007/s10347-007-0131-3

Cited by 42 publications

(57 citation statements)

References 66 publications

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“…This could be taken as evidence that most of the Mateiaş Limestone developed in shelf margin and slope environments. Similar microfacies were documented by Schlagintweit and Gawlick (2008) for Upper Jurassic forereef slope environments on the margins of Neothetyan platforms.…”

Section: Discussionsupporting

confidence: 83%

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

Bucur¹,

Beles²,

Săsăran³

et al. 2010

Studia UBB, Geologia

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ABSTRACT. The Mateiaş Limestone is a lithostratigraphic unit in the Braşov Series, a component of the eastern part of the Getic Nappes' cover (the Getic carbonate platform). Four main facies and their associated microfacies are identified in the Mateiaş Limestone in the Hulei-Mateiaş-Măgura area. A Kimmeridgian (possibly also Early Tithonian) age is assigned to the Mateiaş Limestone, based on the microfossil association identified in thin sections. The regional setting, as well as sedimentological and micropaleontological features, indicates deposition of these limestones in shelf margin and slope environments. The succession in the area studied corresponds to the lower-mid part of the carbonate succession developed in the more internal part of the eastern sector of the Getic carbonate platform (e.g. Piatra Craiului Mountains).

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Section: Discussionsupporting

confidence: 83%

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

Bucur¹,

Beles²,

Săsăran³

et al. 2010

Studia UBB, Geologia

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“…Oncoid distribution is from Védrine et al (2007). Published distribution refers to Darga & Schlagintweit (1991), Schlagintweit & Ebli (1999), Sasaran et al (2000), Velić et al (2002), Gawlick et al (2003) and Flügel (2004).…”

Section: Discussionmentioning

confidence: 99%

“…Several authors found this foraminifer preferentially in high-energy facies from the internal platform to the slope, commonly associated with Protopeneroplis sp., Trocholina sp., Pseudocyclammina sp., Andersenolina sp., Nautiloculina sp., Lenticulina sp., Valvulina sp. and miliolids (Darga & Schlagintweit, 1991;Sasaran et al, 2000;Schlagintweit & Ebli, 1999;Velić et al, 2002;Gawlick et al, 2003). Recently, Flügel (2004) and Velić et al (2002) described Mohlerina basiliensis as characteristic of upper slope facies.…”

Section: Taxonomy the Benthic Foraminifer Mohlerina Basiliensismentioning

confidence: 99%

Co-occurrence of the foraminifer <i>Mohlerina basiliensis</i> with <i>Bacinella–Lithocodium</i> oncoids: palaeoenvironmental and palaeoecological implications (Late Oxfordian, Swiss Jura)

Védrine¹

2008

J. Micropalaeontol.

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-The stratigraphical and spatial distribution of the foraminifer Mohlerina basiliensis and Bacinella-Lithocodium oncoids was studied in the lagoonal deposits of the oncoid-rich Hauptmumienbank Member from the Swiss Jura Mountains (Late Oxfordian, NW Switzerland). Mohlerina basiliensis has a double-layered wall structure (thick outer hyaline-radial calcite layer with a lamellar structure and thin inner microgranular calcite layer) and is preferentially found in low-energy facies and associated with normal-marine bioclasts and Bacinella-Lithocodium oncoids. The distribution of Mohlerina basiliensis is relatively patchy. The 'distal' platform facies present a higher abundance and a more extensive stratigraphic occurrence of this foraminifer. The timing of the ecological evolution is given by the sequence-and cyclostratigraphic framework and illustrates the stepwise flooding of the platform. Bacinella-Lithocodium oncoids have diameters of a few millimetres to several centimetres and are composed of an alternation of Bacinella-Lithocodium meshwork and thin micritic laminae. They are found preferentially in low-energy facies (bioclastic wackestones) of open lagoons. The distribution of Bacinella-Lithocodium oncoids through time and space is also patchy; however, they appear more abundantly in 'distal' platform facies. This study reveals the co-occurrence of Mohlerina basiliensis and Bacinella-Lithocodium oncoids and thus suggests similar environmental conditions.

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“…Crescentiella represents symbiosis between nubecularid foraminifers and cyanophyceans (e.g., Senowbari-Daryan et al 2008;Pleş et al 2013). Commonly, the individual specimens in life position are connected with cyanophycean crusts, forming a kind of colony, which builds micro-constructions (e.g., Schlagintweit and Gawlick 2008;Krajewski 2008;SenowbariDaryan et al 2008). Such an association is common in a mid-ramp setting (e.g., Leinfelder et al 1996).…”

Section: Ft 2: Microbial-crescentiella Limestonementioning

confidence: 99%

Late Jurassic facies architecture of the Złoczew Graben: implications for evolution of the tectonic-controlled northern peri-Tethyan shelf (Upper Oxfordian–Lower Kimmeridgian, Poland)

Krajewski

Olchowy

Felisiak

2015

Facies

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The occurrence and role of microencruster frameworks in Late Jurassic to Early Cretaceous platform margin deposits of the Northern Calcareous Alps (Austria)

Cited by 42 publications

References 66 publications

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

Co-occurrence of the foraminifer <i>Mohlerina basiliensis</i> with <i>Bacinella–Lithocodium</i> oncoids: palaeoenvironmental and palaeoecological implications (Late Oxfordian, Swiss Jura)

Late Jurassic facies architecture of the Złoczew Graben: implications for evolution of the tectonic-controlled northern peri-Tethyan shelf (Upper Oxfordian–Lower Kimmeridgian, Poland)

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The occurrence and role of microencruster frameworks in Late Jurassic to Early Cretaceous platform margin deposits of the Northern Calcareous Alps (Austria)

Cited by 42 publications

References 66 publications

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

New data on facies development and micropaleontology of the eastern margin of the Getic Carbonate Platform (South Carpathians, Romania): case study of Mateiaş Limestone

Co-occurrence of the foraminifer &lt;i&gt;Mohlerina basiliensis&lt;/i&gt; with &lt;i&gt;Bacinella–Lithocodium&lt;/i&gt; oncoids: palaeoenvironmental and palaeoecological implications (Late Oxfordian, Swiss Jura)

Late Jurassic facies architecture of the Złoczew Graben: implications for evolution of the tectonic-controlled northern peri-Tethyan shelf (Upper Oxfordian–Lower Kimmeridgian, Poland)

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Co-occurrence of the foraminifer <i>Mohlerina basiliensis</i> with <i>Bacinella–Lithocodium</i> oncoids: palaeoenvironmental and palaeoecological implications (Late Oxfordian, Swiss Jura)