An Archaeogenomic Investigation of Consanguinity During the Neolithic Transition

2019-03-01
Taskent, Recep O.
Sumer, Arev P.
Koptekin, Dilek
Ozkan, Mustafa
Ceballos, Francisco C.
Gokcumen, Omer
Somel, Mehmet

Suggestions

An archival study of extended X-ray emission from classical and recurrent novae
Balman, Şölen (2005-01-21)
I discuss morphology and spectrum of the first resolved and detected classical nova shell in the X-rays - the remnant of GK Persei (1901). The existence of such a nebulosity brings about the possibility of other nova remnants emitting X-rays. I calculate that the X-ray luminosity should be about 10(26) - 10(33) ergs s(-1) on the onset of cooling for nova remnants. I have done an archival search on 250 classical and recurrent nova candidates using Chandra, XMM-Newton, ROSAT and ASCA databases. There is no si...
An Interpretation of the Basement Structure and Formation of the Black Sea Based on Deep Seismic Data and Gravity Modelling
Kaymakcı, Nuretdin (null; 2015-12-09)
It is widely accepted that the Black Sea consists of two separate back arc basins which opened at different times during the Cretaceous driven by northward subduction of the Neo-Tethys Ocean. The paucity of well data, complex geometries and seismic imaging challenges mean that questions remain regarding the basement architecture though most authors accept that, at least in part, both these basins are floored by oceanic crust, even though there a no magnetic stripes. Interpretation of deep, long offset SPAN ...
An evaluation of zooarchaeological finds in Turkey from Late Antiquity to Seljuk times
Pişkin, Evangelia (2018-09-02)
An Archaemotric study on the Iron age plant samples from Patnos(Ağrı).
Özdemir, Kameray; Department of Archaeometry (1999)
An approach to paleoclimatic conditions for Devonian (upper Lochkovian and middle Givetian) ironstone formation, NW Anatolian carbonate platform
Yılmaz, İsmail Ömer; Göncüoğlu, Mehmet Cemal (2015-01-01)
Lower-middle Devonian iron-bearing successions were studied along 2 measured stratigraphic sections in the Camdag region of NW Anatolia. Ironstones in the upper part of the Findikli Formation in Kabalakdere are characterized by alternating red and green mudstones and sandstones at the bottom, followed by a series of dolomite, dolomitic limestone with oolitic ironstones, and chamositic mudstones at the top. Conodonts from these carbonates indicate the delta-pesavis zones of the late Lochkovian. The 12-to 45-...
Citation Formats
R. O. Taskent et al., “An Archaeogenomic Investigation of Consanguinity During the Neolithic Transition,” 2019, vol. 168, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/54946.