HARAMİ FORMASYONU’NUN ELAZIĞ GÜNEYBATISINDAKİ YÜZEYLEMESİNDE MICROCODIUM BULGUSU

Sibel Kayğılı; Ismaıl Mari; Semih Sis

doi:10.17780/ksujes.1722280

EN TR

MICROCODIUM FINDING IN THE HARAMİ FORMATION OUTCROP IN THE SOUTHWEST OF ELAZIĞ, EASTERN TÜRKİYE

Abstract

This study is based on Microcodium findings in two sections, named Mangan Tepe 1 and Mangan Tepe 2, measured in the Harami Formation outcrop at Mangan Tepe, approximately 12 km southwest of Elazığ. The aim is to reveal the age and depositional environment of the sequence by utilizing these findings and the accompanying fossil content. The origin of Microcodium is very controversial, but it was determined that the Microcodium in this study were not transported because they did not have a fragmented structure and were evaluated as the calcification product of plant root cells that developed in the early stage of soil formation during the rise of sediments deposited in the shallow marine environment above the water level. Microcodiums determined in this study were divided into two groups as Type 1 and Type 2. The presence of fossils such as Fissoelphidium operculiferum, Orbitoides sp., Lepidorbitoides sp., rotalidae, miliolidae, textularidae, algae, coral, and bivalve were determined in the sequence containing Microcodium, and according to the benthic foraminifera content, the Maastrichtian age assign to the sequence. It was concluded that the Microcodium-bearing Maastrichtian Harami Formation limestones were deposited in the inner and middle shelf of a shallow marine environment.

Keywords

HARAMİ FORMASYONU’NUN ELAZIĞ GÜNEYBATISINDAKİ YÜZEYLEMESİNDE MICROCODIUM BULGUSU

Öz

Bu çalışmada Elazığ’ın yaklaşık 12 km güneybatısındaki Mangan Tepe’de yüzeyleyen Harami Formasyonu’nda ölçülen Mangan Tepe 1 ve Mangan Tepe 2 isimli stratigrafik kesitlerdeki Microcodium bulguları esas alınmıştır. Bu bulgular ve beraberinde bulunan fosil içeriğinden yararlanarak istifin yaşı ve depolanma ortamının ortaya konulması, çalışmanın amacını oluşturur. Microcodium’ların kökeni çok tartışmalı olup bu çalışmadaki Microcodium’ların parçalı bir yapıya sahip olmamaları nedeniyle taşınmamış olduğu belirlenmiş ve sığ deniz ortamında depolanan sedimanların su üstü olması sırasındaki topraklaşmanın erken evresinde gelişen bitki kök hücrelerinin kalsifikasyon ürünü olarak değerlendirilmiştir. Bu çalışmada belirlenen Microcodium’lar Tip 1 ve Tip 2 olarak ikiye ayrılmıştır. Microcodium’ların yer aldığı istifte Fissoelphidium operculiferum, Orbitoides sp., Lepidorbitoides sp., rotalidae, miliolidae, textularidae, alg, mercan ve bivalv gibi fosillerinin varlığı belirlenmiş ve bentik foraminifer içeriğine göre istife Maastrihtiyen yaşı verilmiştir. Microcodium içeren Maastrihtiyen yaşlı Harami Formasyonu kireçtaşlarının sığ bir denizel ortamın iç ve orta şelf bölümünde depolandığı sonucuna varılmıştır.

Anahtar Kelimeler

Supporting Institution

Türkiye Bilimsel ve Teknolojik Araştırma Kurumu (TÜBİTAK) Bilim İnsanı Destek Programları (BİDEB)

Project Number

1919B012326856

Ethical Statement

Yazarlar bu çalışmanın araştırma ve yayın etiğine uygun olduğunu beyan eder.

Thanks

Projeye verdiği destek nedeniyle TÜBİTAK’a teşekkürlerimizi sunarız

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Details

Primary Language

Turkish

Subjects

General Geology

Journal Section

Research Article

Authors

Sibel Kayğılı ^*
0000-0002-7124-1501
Türkiye

Ismaıl Mari
0009-0007-4799-4187
Syria

Semih Sis
0009-0002-7274-882X
Türkiye

Publication Date

December 3, 2025

Submission Date

June 18, 2025

Acceptance Date

November 5, 2025

Published in Issue

Year 2025 Volume: 28 Number: 4

DOI

https://doi.org/10.17780/ksujes.1722280

IZ

https://izlik.org/JA73ZP39NU

Cite

RIS / Bibtex

APA

Kayğılı, S., Mari, I., & Sis, S. (2025). HARAMİ FORMASYONU’NUN ELAZIĞ GÜNEYBATISINDAKİ YÜZEYLEMESİNDE MICROCODIUM BULGUSU. Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi, 28(4), 1829-1842. https://doi.org/10.17780/ksujes.1722280