Foraminiferal Responses to Sea Level Changes Across the Mid-Carboniferous Boundary in Central Taurides (Turkey)

• Autorzy: Atakul-Özdemir Ayşe , Altiner Demir , Özkan-Altıner Sevinç

Identyfikatory

DOI

10.29227/IM-2024-01-70

Warianty tytułu

PL

Reakcje foraminiferałów na zmiany poziomu morza na granicy środkowego karbonu w środkowych Taurydach (Turcja)

• Języki publikacji: EN

Abstrakty

EN

The response of benthic foraminiferal assemblages to relative sea-level changes during the mid-Carboniferous succession of the Yarıcak Formation in the Central Taurides is assessed with respect to sedimentary cyclicity and sequence stratigraphy by quantitative analysis. The data derived from the relative abundances of foraminifera have critical significance in the understanding of cyclic patterns and sea level changes in carbonate deposits. Calcareous foraminiferal groups including archaediscids, eostaffellids, irregularly coiled bilocular forms, unilocular forms, paleotextularids, biseriamminids, endothyrids, and pseudoendothyrids have been counted and analysed in this study. The mid-Carboniferous boundary succession predominantly covering uniform lithology of carbonates alternated with sandstone layers involves shallowing upward cycles used for the revealing of sea-level fluctuations. The relative abundances of these foraminiferal groups reveal a striking response to cyclicity with the reductions in the abundances towards the upper part of the cycles. Conversely, the abundances of pseudoendothyrids and endothyrids do not exhibit any considerable variations within the studied interval.

Słowa kluczowe

EN

foraminiferal responses; sea level; mid-carboniferous boundary; central taurides; Turkey

PL

reakcje otwornic; poziom morza; granica środkowego karbonu; Środkowe Taurydy; Turcja

• Wydawca: Polskie Towarzystwo Przeróbki Kopalin
• Czasopismo: Inżynieria Mineralna
• Rocznik: 2024
• Tom: Vol. 1, no. 1
• Strony: 615--620
• Opis fizyczny: Bibliogr. 20 poz., rys., wykr.

Twórcy

autor

Atakul-Özdemir Ayşe

• Department of Geophysical Engineering, Van Yüzüncü Yıl University, Van, Turkey

• https://orcid.org/0000-0003-0660-3139

autor

Altiner Demir

• Department of Geological Engineering, Middle East Technical University, Ankara, Turkey

autor

Özkan-Altıner Sevinç

• Department of Geological Engineering, Middle East Technical University, Ankara, Turkey

Bibliografia

• [1] Ferguson L 1962 The Paleoecology of a Lower Carboniferous Marine Transgression J Paleontol 36 1090–107.
• [2] Gallagher S J 1998 Controls on the distribution of calcareous Foraminifera in the Lower Carboniferous of Ireland Mar Micropaleontol 34 187–211.
• [3] Gallagher S J and Somerville I D 2003 Lower carboniferous (Late Viséan) platform development and cyclicity in southern Ireland: Foraminiferal biofacies and lithofacies evidence Rivista Italiana di Paleontologia e Stratigrafia 109.
• [4] Baranova D V. and Kabanov P B 2003 Facies distribution of fusulinoid genera in the myachkovian (Upper Carboniferous, Upper Moscovian) of Southern Moscow region Rivista Italiana di Paleontologia e Stratigrafia 109.
• [5] Nagy J, Finstad E K, Dypvik H and Bremer M G 2001 Response of Foraminiferal Facies to Transgressive-Regressive Cycles in the Callovian Of Northeast Scotland. The Journal of Foraminiferal Research 31.
• [6] Della Porta G, Villa E and Kenter J A M 2005 Facies distribution of Fusulinida in a BashkirianMoscovian (Pennsylvanian) carbonate platform top (Cantabrian Mountains, NW Spain) J Foraminifer Res 35
• [7] Scott D S and Medioli F S 1978 Vertical zonations of marsh foraminifera as accurate indicators of former sea-levels Nature 272.
• [8] Scott D B, Collins E S, Duggan J, Asioli A, Saito T and Hasegawa S 1996 Pacific rim marsh foraminiferal distributions: implications for sea-level studies J Coast Res 12.
• [9] Jennings A E, Nelson A R, Scott D B and Aravena J C 1995 Marsh foraminiferal assemblages in the Valdivia Estuary, south-central Chile, relative to vascular plants and sea level J Coast Res 11.
• [10] Jennings A E and Nelson A R 1992 Foraminiferal assemblage zones in Oregon tidal marshes - relation to marsh floral zones and sea level J Foraminifer Res 22
• [11] Murray J W 2014 Ecology and palaeoecology of benthic foraminifera
• [12] Patterson R T 1990 Intertidal benthic foraminiferal biofacies on the Fraser River Delta, British Columbia: modern distribution and paleoecological importance Micropaleontology 36
• [13] Goldhammer R K, Dunn P A and Hardie L A 1990 Depositional cycles, composite sea-level changes, cycle stacking patterns, and the hierarchy of stratigraphic forcing: Examples from Alpine Triassic platform carbonates Bulletin of the Geological Society of America 102
• [14] Yang W, Kominz M A and Major R P 1998 Distinguishing the roles of autogenic versus allogenic processes in cyclic sedimentation, Cisco Group (Virgilian and Wolfcampian), north-central Texas Bulletin of the Geological Society of America 110
• [15] Osleger D and Read J F 1991 Relation of eustacy to stacking patterns of meter-scale Carbonate cycles, late Cambrian, USA J Sediment Petrol 61 1225–52
• [16] Ozgul N 1984 Stratigraphy and tectonic evolution of the Central Taurides. Geology of the Taurus Belt. International symposium, 1983, Ankara
• [17] Özgül N 1976 Toroslar’m bazı temel jeoloji özellikleri (Some geological aspects of the Taunts orogenic belt, Turkey) Bulletin of the Geological Society of Turkey 19
• [18] Atakul A 2006 Lower-Middle Carboniferous boundary in Central Taurides, Turkey (Hadim Area): Paleontological and sequence stratigraphic approach (Ankara: Middle East Technical University)
• [19] Atakul-Özdemir A, Altiner D, Özkan-Altiner S and Yilmaz I Ö 2011 Foraminiferal biostratigraphy and sequence stratigraphy across the mid-Carboniferous boundary in the Central Taurides, Turkey Facies 57
• [20] Atakul-Özdemir A, Altiner D and Özkan-Altiner S 2012 Conodont distribution across the MidCarboniferous boundary,in the Central Taurides, Turkey Rivista Italiana di Paleontologia e Stratigrafia 118

Uwagi

Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki i promocja sportu (2025).