Kızılırmak Nehrinin Denizel İzotop Katı 6 Sırasındaki İklim Değişimlerine Tepkisi

Uğur Doğan; Çetin Şenkul; Suzan Altıparmak

doi:10.46453/jader.788712

EN TR

The response of Kızılırmak River to Climate Change During Marine Isotope Stage 6

Abstract

This study was carried out on the Cappadocia section of the Kızılırmak River valley. In this area, 15 terrace staircases, referred to as T1 to T15, were identified. This study aimed to illustrate river response to climate changes during the formation of T13 (+15-20 m) terrace. Three samples, taken from the lower part of this terrace deposit, were dated to 148 ± 8, 154 ± 8 and 159 ± 8 ka BP with pIRIR290 method. In a previous study, the same terrace deposit was dated to 160 ± 30 ka BP 36Cl cosmogenic nuclide method. Our data show that the main valley incision phase before accumulation of the T13 terrace deposits occurred during Marine Isotope Stage (MIS) 7 and 6 (warm to cold) climate transition. Our results suggest that the T13 terrace deposits accumulated during the early part of MIS 6. It could further be proposed that lower part of the terrace deposits have developed at the early part of the MIS 6 (betwen 180 and 165 ka BP) because of the presence of a paleosol in the old floodplain deposits at T13, which characterizes a warm dry climate. The incision process of the deposits of T13 terrace appears to have started at the end of a warm period of the MIS 6 and formation of the terrace staircase was completed during the full glacial part of MIS 6.

Keywords

Kızılırmak River , Cappadocia , River Terrace , Marine Isotope Stage 6 , Climate Changes , River Response

Kızılırmak Nehrinin Denizel İzotop Katı 6 Sırasındaki İklim Değişimlerine Tepkisi

Öz

Bu çalışma Kızılırmak vadisinin Kapadokya yöresinde, Gülşehir-Tuzköy arasında kalan kesiminde yapılmıştır. Bu sahada T1’den (en yaşlı) T15’e (en genç) kadar numaralandırılmış 15 seki basamağı bulunmaktadır. Bu çalışmanın amacı, T13 sekisine (+15-20 m) ait üç lokasyonda Denizel İzotop Katı (DİK) 6 sırasında Kızılırmak Nehri’nin küresel iklim değişimlerine karşı tepkisini saptamaktır. Sekinin taban depolarından alınmış olan kum örnekleri pIRIR290 yöntemiyle 148 ±8, 154 ± 8 ve 159 ± 8 bin yıl (by) öncesine tarihlendirilmiştir. Önceki bir çalışmadaysa seki deposu kozmojenik izotop yöntemiyle 160±30 by öncesine tarihlendirilmiştir. Elde ettiğimiz veriler T13 teras depdepolarının birikimi öncesindeki ana vadi kazılmasının DİK 7 ve 6 (sıcak–soğuk) iklim geçişinde olduğunu göstemektedir. Veriler, T13 seki depolarının DİK 6’nın ilk evresinde biriktiğini ortaya koymaktadır. Ayrıca, T13 sekisinin ilk taşkınovası deposunda sıcak iklimi karakterize eden paleosolerin varlığı, seki deposunun alt kısmının olasılıkla DİK 6'nın erken evresinde (günümüzden önce 180 ile 165 bin yıl arasında) oluştuğunu gösterir. T13 sekisi depolarının yarılması ise DİK 6’nın sıcak periyodunun sonunda başlamış ve DİK 6’nın tam glasyal periyodunda tamamlanmıştır.

Anahtar Kelimeler

Kızılırmak Nehri , Kapadokya , Akarsu Sekisi , Denizel İzotop Katı 6 , İklim Değişimi , Akarsu Tepkisi

Kaynakça

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Ayrıntılar

Birincil Dil

Türkçe

Konular

Fiziksel Coğrafya ve Çevre Jeolojisi

Bölüm

Araştırma Makalesi

Yazarlar

Uğur Doğan ^*
0000-0002-1300-3484
Türkiye

Çetin Şenkul
Türkiye

Suzan Altıparmak
0000-0002-4449-0895
Türkiye

Yayımlanma Tarihi

15 Ekim 2020

Gönderilme Tarihi

1 Eylül 2020

Kabul Tarihi

18 Eylül 2020

Yayımlandığı Sayı

Yıl 2020 Sayı: 5

DOI

https://doi.org/10.46453/jader.788712

IZ

https://izlik.org/JA54EA46YU

APA

Doğan, U., Şenkul, Ç., & Altıparmak, S. (2020). Kızılırmak Nehrinin Denizel İzotop Katı 6 Sırasındaki İklim Değişimlerine Tepkisi. Jeomorfolojik Araştırmalar Dergisi, 5, 48-63. https://doi.org/10.46453/jader.788712

Cited By

Kirmir Çayı’nın İklim ve Tektonik Kontrollü Sekileri, İç Anadolu - Türkiye

Jeomorfolojik Araştırmalar Dergisi

https://doi.org/10.46453/jader.1332862

Jeomorfolojik Araştırmalar Dergisi ( JADER ) - Journal of Geomorphological Researches

TR Dizin - DOAJ - Crossref - Google Scholar tarafından taranmaktadır.

Jeomorfoloji Derneği - Turkish Society for Geomorphology

www.jd.org.tr

The response of Kızılırmak River to Climate Change During Marine Isotope Stage 6

Abstract

Keywords

Kızılırmak Nehrinin Denizel İzotop Katı 6 Sırasındaki İklim Değişimlerine Tepkisi

Öz

Anahtar Kelimeler

Kaynakça

Ayrıntılar

Birincil Dil

Konular

Bölüm

Yazarlar

Yayımlanma Tarihi

Gönderilme Tarihi

Kabul Tarihi

Yayımlandığı Sayı

DOI

IZ

Kaynak Göster

Cited By

Kirmir Çayı’nın İklim ve Tektonik Kontrollü Sekileri, İç Anadolu - Türkiye