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Maastrichtian Planktic Foraminiferal Paleoecology within the Tanjero Formation, Sulaymaniyah City, Kurdistan Region, Northeastern Iraq

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F25%3A73633924" target="_blank" >RIV/61989592:15310/25:73633924 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://www.micropress.org/microaccess/stratigraphy/issue-422/article-2439" target="_blank" >https://www.micropress.org/microaccess/stratigraphy/issue-422/article-2439</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.29041/strat.22.4.03" target="_blank" >10.29041/strat.22.4.03</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Maastrichtian Planktic Foraminiferal Paleoecology within the Tanjero Formation, Sulaymaniyah City, Kurdistan Region, Northeastern Iraq

  • Popis výsledku v původním jazyce

    This study focuses on planktic foraminifera to interpret the paleoecology and paleogeography of the uppermost 20 m of the Tanjero Formation below the Cretaceous/Paleogene (K/Pg) boundary of the Kurdistan Region, northeastern Iraq. In the lower part of the studied section, which was deposited in deep water (more than 100 m), the planktic foraminifera species with double-keeled tests Abathomphalus, Marginotruncana, Globotruncana, Gansserina, and Rugotruncana (Morphotype 3), are predominant. The middle part of the section is characterized by abundant species from the Globotruncanella and Globotruncanita genera, which have a single-keeled test, representing deposition in intermediate water (50–100 m depth) (Morphotype 2). The upper part of the section is marked by an abundance of genera with a nonkeeled test, including Hedbergella, Heterohelix, Pseudoguembelina, Pseudotextularia, Guembelitria, Planoheterohelix, Rugoglobigerina, Globigerinelloids Plummerita, and Rugotruncana, which are indicators of shallower water (approximately 50 m depth) (Morphotype 1). The diverse planktic foraminifera genera in this section are typical of Tethyan provinces, suggesting a stable, mesotrophic environment. The planktic foraminiferal assemblage from the uppermost part of the formation suggests paleoceanographic conditions that favored opportunistic organisms. This is evidenced by the presence of the genus Pseudoguembelina, a successful surface and subsurface dweller in tropical and subtropical open oceans with warm and oligotrophic surface waters. The expansion of this strongly photosymbiotic genus is attributed to favorable palaeoecological conditions in the Late Cretaceous oceans. The results obtained imply the presence of a well-stratified water column, a tropical to subtropical climate, and deposition in the outer shelf to upper bathyal environments. These conditions account for the presence of well-preserved and highly diversified Maastrichtian foraminifer assemblages of the globotruncanid species, which include: Hedbergella, Praeglobotruncana, Marginotruncana, Globotruncana, Contusotruncan, Globotruncanita, Archaeoglobigerina, Rugoglobigerina, Rugotruncana, Globotruncanella, Gansserina, and Abathomphalus.

  • Název v anglickém jazyce

    Maastrichtian Planktic Foraminiferal Paleoecology within the Tanjero Formation, Sulaymaniyah City, Kurdistan Region, Northeastern Iraq

  • Popis výsledku anglicky

    This study focuses on planktic foraminifera to interpret the paleoecology and paleogeography of the uppermost 20 m of the Tanjero Formation below the Cretaceous/Paleogene (K/Pg) boundary of the Kurdistan Region, northeastern Iraq. In the lower part of the studied section, which was deposited in deep water (more than 100 m), the planktic foraminifera species with double-keeled tests Abathomphalus, Marginotruncana, Globotruncana, Gansserina, and Rugotruncana (Morphotype 3), are predominant. The middle part of the section is characterized by abundant species from the Globotruncanella and Globotruncanita genera, which have a single-keeled test, representing deposition in intermediate water (50–100 m depth) (Morphotype 2). The upper part of the section is marked by an abundance of genera with a nonkeeled test, including Hedbergella, Heterohelix, Pseudoguembelina, Pseudotextularia, Guembelitria, Planoheterohelix, Rugoglobigerina, Globigerinelloids Plummerita, and Rugotruncana, which are indicators of shallower water (approximately 50 m depth) (Morphotype 1). The diverse planktic foraminifera genera in this section are typical of Tethyan provinces, suggesting a stable, mesotrophic environment. The planktic foraminiferal assemblage from the uppermost part of the formation suggests paleoceanographic conditions that favored opportunistic organisms. This is evidenced by the presence of the genus Pseudoguembelina, a successful surface and subsurface dweller in tropical and subtropical open oceans with warm and oligotrophic surface waters. The expansion of this strongly photosymbiotic genus is attributed to favorable palaeoecological conditions in the Late Cretaceous oceans. The results obtained imply the presence of a well-stratified water column, a tropical to subtropical climate, and deposition in the outer shelf to upper bathyal environments. These conditions account for the presence of well-preserved and highly diversified Maastrichtian foraminifer assemblages of the globotruncanid species, which include: Hedbergella, Praeglobotruncana, Marginotruncana, Globotruncana, Contusotruncan, Globotruncanita, Archaeoglobigerina, Rugoglobigerina, Rugotruncana, Globotruncanella, Gansserina, and Abathomphalus.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10505 - Geology

Návaznosti výsledku

  • Projekt

  • Návaznosti

    N - Vyzkumna aktivita podporovana z neverejnych zdroju

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Stratigraphy

  • ISSN

    1547-139X

  • e-ISSN

    2331-656X

  • Svazek periodika

    22

  • Číslo periodika v rámci svazku

    4

  • Stát vydavatele periodika

    US - Spojené státy americké

  • Počet stran výsledku

    12

  • Strana od-do

    235-246

  • Kód UT WoS článku

    001678376000002

  • EID výsledku v databázi Scopus

    2-s2.0-105025933710