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AN EXAMPLE TO THE CHANGE OF EARTH SHAPE: EVIDENCE OF TETHYS SEA IN DİYARBAKIR

Yıl 2018, Cilt: 4 Sayı: 1, 36 - 44, 04.06.2018
https://doi.org/10.23884/mejs.2018.4.1.05

Öz

The change of earth shape over time is expressed as
Geological Evolution. The German meteorologist Alfred Wegener (1880-1930)
describes the geological evolution of the Continental Drift Theory, which means
that terrestrial parts of the earth and large water bodies change over time.
According to the Continental Drift Theory, during the Mesozoic Era, the large
earth continent Pangaea was divided into two gigantic continents (Laurasia and
Gondwana), forming the Tethys Sea. The Tethys Sea was connected to the present
Indian Ocean through the Atlantic Ocean and the Mediterranean Sea. A large part
of Anatolia, especially in Southeastern Anatolia, was covered with the sea for
a long time. Today's both Mediterranean and Black Sea is considered as a
remnant of Tethys Sea. These seas were also subjected to some other important
changes. In the studies carried out within the province of Diyarbakır, the
biological evidences of the Tethys Sea were found in invertebrate fossils. The
marine form of fossils belonging to Echinodermata and Bivalvia phyla are
frequently encountered in the Southeastern Anatolia Region. They were collected
from the Diyarbakır province and photographed. The fossil specimens are of
great importance in terms of understanding the geological changes (Geological
evolution) that the region has undergone over time.

Kaynakça

  • References
  • [1] Demirsoy, A., Basic Rules of Life. General Biology and General Zoology. Vol: 1, Section 1. 19th Edition, Meteksan Inc. Ankara, p 770, 2005.
  • [2] Sakınç, M. (2011). http://www.yaziyaz.net/Evrim/konular/54-inorganik-evrim/161-dunyanin-evrimi-jeolojik-ve-biyolojik-evrim-icice.html
  • [3] Robetson, A. H. F., and Dixon, J. E., Introduction: aspects of the geological evolution of the Eastern Mediterranean. Geological Society, London, Special Publications, (1984), 17, pp. 1-74.
  • [4] İnan, N., Important Invertebrate Fossils of Turkey, TUBITAK, Popular Science Books, No: 287, p 138, 2008.
  • [5] Demirsoy, A., General Zoogeography and Turkey Zoogeography ̎ Animal Geography ̎, 5th Edition, Meteksan, Ankara, p 1005, 2008.
  • [6] Salman, S. Invertebrate Biology. Palme Publishing, Ankara, p 501, 2006.
  • [7] Demirsoy, A., Inheritance and Evolution. 14th Edition, Meteksan. Ankara, p 946, 2008.
Yıl 2018, Cilt: 4 Sayı: 1, 36 - 44, 04.06.2018
https://doi.org/10.23884/mejs.2018.4.1.05

Öz

Kaynakça

  • References
  • [1] Demirsoy, A., Basic Rules of Life. General Biology and General Zoology. Vol: 1, Section 1. 19th Edition, Meteksan Inc. Ankara, p 770, 2005.
  • [2] Sakınç, M. (2011). http://www.yaziyaz.net/Evrim/konular/54-inorganik-evrim/161-dunyanin-evrimi-jeolojik-ve-biyolojik-evrim-icice.html
  • [3] Robetson, A. H. F., and Dixon, J. E., Introduction: aspects of the geological evolution of the Eastern Mediterranean. Geological Society, London, Special Publications, (1984), 17, pp. 1-74.
  • [4] İnan, N., Important Invertebrate Fossils of Turkey, TUBITAK, Popular Science Books, No: 287, p 138, 2008.
  • [5] Demirsoy, A., General Zoogeography and Turkey Zoogeography ̎ Animal Geography ̎, 5th Edition, Meteksan, Ankara, p 1005, 2008.
  • [6] Salman, S. Invertebrate Biology. Palme Publishing, Ankara, p 501, 2006.
  • [7] Demirsoy, A., Inheritance and Evolution. 14th Edition, Meteksan. Ankara, p 946, 2008.
Toplam 8 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Yapısal Biyoloji
Bölüm Makale
Yazarlar

İhsan Ekin

Rıdvan Şeşen

Yayımlanma Tarihi 4 Haziran 2018
Gönderilme Tarihi 19 Aralık 2017
Kabul Tarihi 3 Mayıs 2018
Yayımlandığı Sayı Yıl 2018 Cilt: 4 Sayı: 1

Kaynak Göster

IEEE İ. Ekin ve R. Şeşen, “AN EXAMPLE TO THE CHANGE OF EARTH SHAPE: EVIDENCE OF TETHYS SEA IN DİYARBAKIR”, MEJS, c. 4, sy. 1, ss. 36–44, 2018, doi: 10.23884/mejs.2018.4.1.05.

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This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License

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