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    A new look at the rock art on the island of Gokceada, northeast Aegean
    (Archaeological Publ, 2023) Erdogu, Burcin; Yucel, Nejat; Gurcal, Erkan; Demir, Kerem; Izlier, Nazli Ilgin
    [Anstract Not Available]
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    SPECIAL BUILDINGS AT NEOLITHIC GIRMELER, NEAR TLOS IN SOUTH-WEST ANATOLIA
    (Wiley, 2025) Erdogu, Burcin; Korkut, Taner; Takaoglu, Turan; Yucel, Nejat; Usanmaz, Uygar Ozan; Derici, Yasin Cemre
    Special buildings, or communal buildings, were ubiquitous in most Neolithic settlements in the Levant, Upper Mesopotamia, and Anatolia. Recently, remains of three special buildings with terrazzo floors dating to the early seventh millennium BC representing the Initial Neolithic period in west Anatolian chronology were unearthed in the basal layers of the mound located in front of the Girmeler cave in south-west Anatolia. The terrazzo floors in these three special buildings feature traces of red-painted linear and geometric decorations, while one also contains human burials. These special buildings may enhance our understanding of the symbolic and ritual behaviours of the Neolithic communities living on the south-west fringes of Anatolia. They may have been gathering places for ritual activities that helped create social memories and define group identities, as well as strengthen intra- and inter-societal relations among Neolithic groups. It is argued that the location of these special buildings adjacent to a natural hot spring before a cave with an impressive fa & ccedil;ade may have been one of the factors that eventually led Neolithic groups to form a gathering pattern here.
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    SPELEOTHEMS OF CATALHOYUK, TURKEY
    (Univ Agean, Dept Mediterranean Stud, 2013) Erdogu, Burcin; Uysal, I. Tonguc; Ozbek, Onur; Ulusoy, Ulku
    Speleothem samples such as flowstone, stalagmite and stalactites are one of the important finds at Catalhoyuk, which they have been carried hundreds of kilometers from its source. The Catalhoyuk Speleothem Project have been initiated with the aim of investigating Catalhoyuk's speleothems and identifying their provenance. In order to achieve this, speleothem samples at Catalhoyuk have been recognized and documented, and caves around Catalhoyuk have been investigated. Later, both selected Catalhoyuk speleothem and cave samples of flowstone, stalagmite and stalactites have been analysed by ICP-MS to recognize similar trace elements. In addition, the ages of samples have been obtained by U-Th method to find similarities between the Catalhoyuk samples and speleothem deposits from surrounding caves. The comparative results have been used to identify the sources of Catalhoyuk's speleothems.