It has become a highly polluted environment with marked anthropogenic inputs during the last millennium. a B.P., possibly during a distinct pluvial period, as shown by coarse siliciclastic sediments deposited on the flanks. The estuary was influenced by large fluvial inputs between 5,600 and 1,000 cal. was most likely caused by Mediterranean water outflow into the Black Sea through the Istanbul Strait. a B.P., with suboxic/dysoxic bottom-water conditions. Normal marine salinities prevailed at ca. It subsequently became gradually influenced by marine waters, and was a brackish-water environment until 9,500 cal. Chronostratigraphic and paleontological analyses of the infill sequence indicate that the GHE was a fluvial channel prior to 13,500 cal. The sedimentary infill of the GHE is 15–46 m thick, deposited unconformably above the turbiditic sandstones of the Carboniferous Trakya Formation. The historical Golden Horn Estuary (GHE), near the confluence of the Istanbul Strait (Bosphorus) and the Sea of Marmara in the European part of Istanbul, has been used as a natural harbor since 330 a.d. This cluster is further subdivided into three subclusters that reflect brackish surface flow (influenced by low salinity, higher temperature), pycnocline (rising salinity, falling temperature) and infra-littoral to circa-littoral transitional environments (higher oxygen from the Mediterranean countercurrent and the subsurface chlorophyll maximum), respectively.
Cluster C (15–50m) is characterized by neritic species typical of the infra-littoral environment. Cluster B (140–350m) is characterized by deep-infaunal dysoxic and suboxic species indicative of circa-littoral and upper epibathyal environments and strongly related to low dissolved oxygen values and increased water depth. Cluster A (55–130 m) is characterized by species typical of muddy substrates in the circa-littoral zone and related to declining dissolved oxygen values. Environmental parameters collected at each sampling station allowed the correlation between foraminiferal clusters and watermass characteristics, such as water depth, temperature, salinity and dissolved oxygen concentrations. Q-mode cluster and canonical correspondence analyses performed on the foraminiferal species abundance data revealed three clusters.
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