Key Environmental Factors Controlling Planktonic Foraminiferal and Pteropod Community’s Response to Late Quaternary Hydroclimate Changes in the South Aegean Sea (Eastern Mediterranean)

• Published in: Journal of Marine Science and Engineering
• Main Authors: Christina Giamali, George Kontakiotis, Efterpi Koskeridou, Chryssanthi Ioakim, Assimina Antonarakou
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2020
• Subjects: paleoceanographic evolution; planktonic foraminifera; pteropods; stable isotopes; sea surface temperature (SST); stratification; Naval architecture. Shipbuilding. Marine engineering; VM1-989; Oceanography; GC1-1581; Planktonic foraminifera
• Online Access: https://doi.org/10.3390/jmse8090709; https://doaj.org/article/476fd972198344bc8861d8449b62e5a2

A multidisciplinary study was conducted in order to investigate the environmental factors affecting the planktonic foraminiferal and pteropod communities of the south Aegean Sea. Aspects of the Late Quaternary paleoceanographic evolution were revealed by means of quantitative analyses of planktonic foraminiferal and pteropod assemblages (including multivariate statistical approach; principal component analysis (PCA)), the oxygen (δ 18 O) and carbon (δ 13 C) isotopic composition of planktonic foraminifera and related paleoceanographic (planktonic paleoclimatic curve (PPC), productivity (E-index), stratification (S-index), seasonality) indices, extracted by the gravity core KIM-2A derived from the submarine area between Kimolos and Sifnos islands. Focusing on the last ~21 calibrated thousands of years before present (ka BP), cold and eutrophicated conditions were identified during the Late Glacial period (21.1–15.7 ka BP) and were followed by warmer and wetter conditions during the deglaciation phase. The beginning of the Holocene was marked by a climatic amelioration and increased seasonality. The more pronounced environmental changes were identified during the deposition of the sapropel sublayers S1a (9.4–7.7 ka BP) and S1b (6.9–6.4 ka BP), with extremely warm and stratified conditions. Pteropod fauna during the sapropel deposition were recorded for the first time in the south Aegean Sea, suggesting arid conditions towards the end of S1a. Besides sea surface temperature (SST), which shows the highest explanatory power for the distribution of the analyzed fauna, water column stratification, primary productivity, and seasonality also control their communities during the Late Quaternary.