250 Bin Yıl Uzunluğundaki Van Gölü Çökelleri’nin Spektral Özellikleri: Milankoviç Döngüleri ve Onların Harmonikleri

Yıl 2017, Cilt: 60 Sayı: 4 - Türkiye'de Kuvaterner Araştırmaları, 471 - 488, 29.12.2017

Z. Bora Ön , M. Sinan Özeren Sena Akçer Ön M. Namık Çağatay

https://doi.org/10.25288/tjb.360604

Öz

Dünya’nın
en büyük sodalı gölü olan Van Gölü, Doğu Anadolu Yüksek Platosu’nda yer
almaktadır. ICDP projesi olan PALEOVAN kapsamında, Van Gölü’nden son 250 bin
yılı ve 90 bin yılı temsil eden iki karot alınmıştır. Bu çalışmada, astronomik
ve solar döngülerin etkileri ile oluştuğu düşünülen, iklimin yarı periyodik
davranışını sınamak amacıyla Van Gölü çökelleri jeokimya verileri Lomb-Scargle
Periodogramı (LSP) spektral yöntemi ile analiz edilmiştir. Elde edilen
sonuçlar, Doğu Akdeniz LC21 çökel karotu ve Soreq ile Sofular Mağaraları
speleotem duraylı izotop verileri LSP sonuçlarıyla karışılaştırılmıştır. Analizler
Milankoviç döngülerini, harmoniklerini, Holosen Bond döngülerini ve
Hallstadtzeit güneş döngüsünü vermiştir. Ancak, GÖ 11,5-75 bin yılları arasında
1500 yıllık bir döngü gözlenmemiştir.

Anahtar Kelimeler

Doğu Akdeniz, Holosen Bond döngüleri, Lomb-Scargle periyodogramı, paleoiklim, güneş döngüleri

Spectral Features of 250 kyr Long Lake Van Sediments: Milankovitch Cycles and Their Harmonics

Öz

Lake Van, which is the largest soda lake of the earth, lies in the Eastern Anatolian High Plateau. Two different composite cores, that span the last 250 kyr and 90 kyr, were drilled in Lake Van within the framework of PALEOVAN project (ICDP). In order to test the theories of quasi-periodic behavior of climate, generated by astronomical and solar forces, this study investigates the cycles in Lake Van sediment geochemistry data by the Lomb-Scargle Periodogram (LSP) spectral method. The results are correlated with the Eastern Mediterranean LC21 sediment core, Soreq and Sofular Cave speleothem stable isotope data with LSP results. The analyses show the presence of the Milankovitch cycles, harmonics of the Milankovitch cycles, Holocene Bond cycles and the Hallstadtzeit solar cycle. However, the results do not give a 1500 year cycle for 11.5-75 kyr BP interval.

Anahtar Kelimeler

Eastern Mediterranean, Holocene Bond cycles, Lomb-Scargle periodogram, paleoclimate, solar cycles

Kaynakça

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