Opinions and comments on the benthic foraminiferal assemblage observed around the mineral submarine spring in Kuşadası (Aydın, Turkey) mehmet baki yokes 1 , engin meric ‚ 2 , niyazi avs ‚ar 3 , i ‹pek barut 4 , seyfettin tas 4 , mustafa eryilmaz 5 , feyza dinc ‚er 6 and cu ¤ neyt bircan 7The aim of the study was to investigate the benthic foraminiferal fauna around the mineral water spring in Pamucak Cove, north-west Kuşadası (Aydın) and figure out the effects of the spring on the fauna. The spring was located 200 m off the coast at 12.4 m depth and its temperature was 19.68C. The study area was found to include a rich population of Red Sea originated Amphistegina lobifera, of which the distribution pattern is noteworthy. It is abundant in the centre of the spring and its close vicinity; its abundance decreases when getting away from the spring. It is more abundantly observed on the southern and western sides of the spring, whereas, it is outnumbered by Ammonia compacta and Elphidium crispum on the northern and eastern parts. The water currents around the spring were in north-south and north-west directions. The observed diverse diatom population around the spring constitutes the main food source and dispersal according to the currents may explain the reason for the abundance of the Amphistegina population on the southern and western sides of the study area. High abundances of A. lobifera have not yet been observed elsewhere in the Aegean Sea, although large populations of this species have been recorded on the south-west coasts of Turkey and in several stations on the south-east of Gokceada. Abundance of coloured individuals and Red Sea originated benthic species suggests the presence of special environmental as well as ecological conditions around the spring.