Late Quaternary subsidence records from the Datça graben and Cnidus ancient city (SW Turkey): sea-level changes versus tectonics

Abstract

The Datça graben in southwestern Anatolia is a WNW-trending seismically active depression, with tectonic activity since Pliocene time. This tectonic activity is controlled by normal faults, which have effected ancient settlements. The Cnidus city (old and modern) –an ancient mercantile centre during the Hellenistic, Roman and Byzantine periods– is one of the places that has recorded this activity. The ancient harbour walls of Cnidus, lying 2.2-4.0m below sea level, contain important traces about sea-level changes and tectonics over the past 2.6kyr. Palaeostress analysis along boundary faults in the Datça graben yields an almost N–S oriented pure tensional regime, compatible with earthquake focal mechanism solutions located around the Datça Peninsula. Additionally, an almost E−W trending surface rupture related to a historical earthquake in modern Cnidus, which shows normal fault characteristics, gives further support to the ongoing extension along the Kızlan, Karaköy and Cnidus fault zones. Previous studies on late Quaternary sea-level changes around the Datça Peninsula suggest that 2.6kyr ago sea level was 1.0-1.25m lower than today. From the present-day depth of the Old Cnidus harbour remains and regional sea-level records, it can be inferred that tectonics has played a significant role. Our calculations show that the Datça graben is subsiding at rates of 0.36-0.46mm/yr in the central part and 1.05-1.15mm/yr in the southern part. These values match those found in other areas around the Datça Peninsula.

Holocene Relative Sea-Level Changes Along the Southern Coast of Bodrum Peninsula, SW Anatolia

“…While this rate is 0.5-0.6 mm/yr at Miletus, Ilıca, Kazıkbağlar and Mavişehir, in Ephesus, it increases up to 2.7 mm/yr (Pavlopoulos et al, 2012). The subsided areas on the Aegean coast of Turkey are Datça Peninsula (Anzidei et al, 2011;Özsayın et al, 2021) and Gemile Island in Fethiye. In the coastal part where the ancient city of Knidos is situated to the west of Datça Peninsula, immediately south of the Bodrum Peninsula, a subsidence rate of 0.73 mm/yr is reported (Anzidei et al, 2011), the eastern part, including the town of Datça, these rates were found to vary between 0.36 and 1.15 mm/yr (Özsayın, 2021).…”