A high-resolution study of planktonic foraminifera during the Holocene at the Tilos-Symi sea basin in the SE Aegean Sea

High-resolution data for planktonic foraminifera and their groups of ecological interest, including Herbivores and Carnivores, combined with benthic foraminifera and a great variety of biogeochemical indices from the SE Aegean sediment core ST5, contribute to a detailed study concerning major and mi...

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Bibliographic Details
Published in:Holocene (Sevenoaks) 2023-11, Vol.33 (11), p.1317-1332
Main Authors: Kozanoglou, Caterina, Triantaphyllou, Maria V, Geraga, Maria, Rousakis, Grigoris, Papatheodorou, George, Arabas, Agnieszka, Dimiza, Margarita D, Gogou, Alexandra
Format: Article
Language:English
Subjects:
Anoxia
Anoxic sediments
Benthos
Carnivores
Deposition
Environmental changes
Foraminifera
Freshwater
Herbivores
High resolution
Holocene
Hypoxia
Inland water environment
Ocean basins
Oxygenation
Preconditioning
Sapropels
Seawater
Sediment
Water circulation
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Summary:High-resolution data for planktonic foraminifera and their groups of ecological interest, including Herbivores and Carnivores, combined with benthic foraminifera and a great variety of biogeochemical indices from the SE Aegean sediment core ST5, contribute to a detailed study concerning major and minor climatic episodes during Holocene. The ST5 sediment record, retrieved from the Tilos-Symi marine basin, evidences the impact of the nearby land, the local climate, and the Rhodes Gyre imprint on the eastern Mediterranean water circulation. Pronounced environmental changes are detected during a preconditioning period of ~400 years before the onset of sapropel S1 deposition and during the deposition phases S1a (10.0–8.4 ka BP) and S1b (8.0–6.1 ka BP). Major freshwater influx episodes (10.5 ka BP, 9.2–8.9 ka BP, 7.4 ka BP, 4.5–4.3 ka BP, and few additional during the Late-Holocene) are revealed, prominent oxygen deficiency time intervals (including a distinct brief anoxic period) as well as several drier, cooler and warmer climatic events. Herbivore planktonic foraminifera alternate their dominance with the Carnivores at the preconditioning period before the S1 onset and at the Late-Holocene (2.0–1.5 ka BP) when conditions of good seawater circulation, oxygenation, and productivity alternate with stratified low oxygenation waters and high freshwater influx from the land.
ISSN:0959-6836
1477-0911
DOI:10.1177/09596836231185831