western anatolia
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2022 ◽  
Vol 276 ◽  
pp. 107293
Author(s):  
Nicholas L. Riddick ◽  
Joseph I. Boyce ◽  
Gillian M. Krezoski ◽  
Vasıf Şahoğlu ◽  
Hayat Erkanal ◽  
...  
Keyword(s):  

2021 ◽  
Vol 24 ◽  
Author(s):  
Mieszek Jagiełło

The following paper deals with the mythological story about Apollo’s fight against a she-snake at Pytho, where he eventually builds a sanctuary – the Delphic Oracle. First, it is attempted to decipher the terms Pytho, Delphi and Omphalos. A symbolism revolving around an underlying theme of birth is considered. Then, the stories about Apollo and about Kadmos, as well as a motif in Pherecydes’ theogony, and the Anatolian Illuyanka Myth are being presented as subjects of a comparative analysis. This leads to the proposal that all four narratives have a common origin in Western Anatolia or Pre-Greek Hellas.


Phytotaxa ◽  
2021 ◽  
Vol 528 (3) ◽  
pp. 180-190
Author(s):  
HASAN YILDIRIM ◽  
MEHMET ÇİÇEK ◽  
KENAN AKBAŞ ◽  
ERKAN ŞEKER

Scutellaria topcuoglui (Lamiaceae) from Muğla Province (south-western Anatolia) is described as a new species to science. The new species is morphologically similar to S. glaphyrostachys, but differs from it by several morphological characters, such as the presence of glandular hairs in stems, leaves, bracts, calyx and corolla, scutellum length, corolla length, coloration, and indumentum, mericarp length, coloration, and sculpture, pollen shape, and habitat preference. Diagnostic characters, a comprehensive description, photographs, and a distribution map are provided.


2021 ◽  
Vol 64 (6) ◽  
pp. GM661
Author(s):  
Mualla Cengiz ◽  
Savaş Karabulut ◽  
Ferhat Özçep ◽  
Burak Semih Çabuk ◽  
Friedrich Heller

The eastern Aegean region has undergone north dipping subduction in the Oligocene, continental collision and then Miocene-Pliocene extension, which is associated with widespread Miocene volcanism. The aim of this study is to assess the possibility of block rotations due to stress variations in the Dikili (İzmir) province, Western Anatolia, based on paleomagnetic data obtained from 35 independent sites in addition to results from 19 sites in earlier studies. The lower Miocene Yuntdağ volcanic rocks were emplaced in three different structural blocks, the Dikili, Zeytindağ and Bergama blocks. Clockwise rotation is found in the Dikili and Zeytindağ blocks that varies from R (± DR) = 12.5° (± 7.4°) in the west to R (± DR) = 35.6°± (13.2°) in the east, respectively. In contrast, a counterclockwise rotation of R (± DR) =-38.1° (± 6.4°) resulted in the Bergama block, in the north of the Dikili and Zeytindağ blocks. A scissor-like basin evolution is suggested during the opening of the Bakırçay graben which led to counterclockwise rotation of the Bergama block and clockwise rotation of the Dikili and Zeytindağ blocks after lower Miocene to present. The rotation pattern derived from results of this study demonstrates that localized small scale deformation due to basin evolution besides regional affects must be considered as part of the deformation matrix in this area.


2021 ◽  
pp. 1-23
Author(s):  
Ergün Laflı ◽  
Werner Seibt ◽  
Doğukan Çağlayan

This article presents 19 lead seals from the Museum of Bergama (ancient Pergamon), dating from the early eighth to the early twelfth century. We offer a descriptive catalogue of these Middle and Late Byzantine seals preserved in a western Turkish museum. The owners of these seals were primarily ecclesiastical, legal or military dignitaries who were probably active in Pergamon, in southwestern Mysia, Aeolis or Lydia. The catalogue is followed by an appendix on a Byzantine magical amulet.


2021 ◽  
Vol 71 ◽  
pp. 813-834
Author(s):  
Marika Asztalos ◽  
Dinçer Ayaz ◽  
Yusuf Bayrakcı ◽  
Murat Afsar ◽  
Cemal Varol Tok ◽  
...  

Using two mitochondrial DNA fragments and 13 microsatellite loci, we examined the phylogeographic structure and taxonomy of two codistributed snake species (Natrix natrix, N. tessellata) in their eastern distribution area, with a focus on Turkey. We found evidence for frequent interspecific hybridization, previously thought to be extremely rare, and for backcrosses. This underscores that closely related sympatric species should be studied together because otherwise the signal of hybridization will be missed. Furthermore, the phylogeographic patterns of the two species show many parallels, suggestive of a shared biogeographic history. In general, the phylogeographies follow the paradigm of southern richness to northern purity, but the dice snake has some additional lineages in the south and east in regions where grass snakes do not occur. For both species, the Balkan Peninsula and the Caucasus region served as glacial refugia, with several mitochondrial lineages occurring in close proximity. Our results show that the mitochondrial divergences in both species match nuclear genomic differentiation. Yet, in the former glacial refugia of grass snakes there are fewer nuclear clusters than mitochondrial lineages, suggesting that Holocene range expansions transformed the glacial hotspots in melting pots where only the mitochondrial lineages persisted, bearing witness of former diversity. On the other hand, the deep mitochondrial divergences in N. tessellata across its entire range indicate that more than one species could be involved, even though lacking microsatellite data outside of Turkey prevent firm conclusions. On the contrary, our microsatellite and mitochondrial data corroborate that N. megalocephala is invalid and not differentiated from sympatric populations of N. natrix. For Cypriot grass snakes, our analyses yielded conflicting results. A critical assessment of the available evidence suggests that N. natrix is a genetically impoverished recent invader on Cyprus and taxonomically not distinct from a subspecies also occurring in western Anatolia and the southern Balkans. Based on combined mitochondrial and nuclear genomic evidence we propose that for grass snakes the following subspecies should be recognized in our study region: (1) Natrix natrix vulgaris Laurenti, 1768, southeastern Central Europe and northern Balkans; (2) Natrix natrix moreoticus (Bedriaga, 1882), southern Balkans, western Anatolia, and Cyprus; and (3) Natrix natrix scutata (Pallas, 1771), eastern Anatolia, Caucasus region, Iran, northeastern distribution range (from eastern Poland and Finland to Kazakhstan and the Lake Baikal region). Thus, Natrix natrix cypriaca (Hecht, 1930) becomes a junior synonym of N. n. moreoticus and Natrix natrix persa (Pallas, 1814) becomes a junior synonym of N. n. scutata. Due to insufficient material, we could not resolve the status of Natrix natrix syriaca (Hecht, 1930) from the Gulf of İskenderun, southeastern Turkey.


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