Connectivity controls on the late Miocene eastern Mediterranean fish fauna

2016 ◽  
Vol 106 (3) ◽  
pp. 1147-1159 ◽  
Author(s):  
Konstantina Agiadi ◽  
Assimina Antonarakou ◽  
George Kontakiotis ◽  
Nefeli Kafousia ◽  
Pierre Moissette ◽  
...  
2015 ◽  
Vol 275 (1) ◽  
pp. 47-81 ◽  
Author(s):  
Dimitra Mantzouka ◽  
Zlatko Kvaček ◽  
Vasilis Teodoridis ◽  
Torsten Utescher ◽  
Nicolaos Tsaparas ◽  
...  

Author(s):  
Assimina Antonarakou ◽  
George Kontakiotis ◽  
Charalampos Vasilatos ◽  
Eva Besiou ◽  
Stergios Zarkogiannis ◽  
...  

The Holocene ◽  
2020 ◽  
Vol 30 (10) ◽  
pp. 1438-1450
Author(s):  
Konstantina Agiadi ◽  
Paolo G Albano

The eastern Mediterranean marine ecosystem is undergoing massive modification due to biological invasions, overfishing, habitat deterioration, and climate warming. Our ability to quantify these changes is severely hindered by the lack of an appropriate baseline; most ecological datasets date back a few decades only and show already strong signatures of impact. Surficial death assemblages (DAs) offer an alternative data source that provides baseline information on community structure and composition. In this study, we reconstruct the marine fish fauna of the southern shallow Israeli shelf before the opening of the Suez Canal based on fish otoliths. We quantify the age of the otolith DAs by radiocarbon dating, and describe its taxonomic composition, geographic affinity, and trophic structure. Additionally, we test by radiocarbon dating the hypothesis that Bregmaceros, a presumed Lessepsian invader with continuous presence in the Mediterranean throughout the late Cenozoic, is a relict species. The otolith DA dates back to the mid-Holocene because 75% of the dated otoliths of the native species are older than the opening of the Suez Canal in 1869, suggesting that the DA is a proper baseline for quantifying modern impacts. Consistently, 97% of the otoliths and 88% of the species we collected belong to native Mediterranean species. The native anchovy Engraulis encrasicolus dominates the DAs, although gobiids are the most diverse group (14 species, 28%). The DAs show similar trophic structure to present-day pristine Mediterranean coastal fish assemblages. Two non-indigenous species are recorded here for the first time in the Mediterranean Sea, Amblygobius albimaculatus and Callogobius sp., highlighting the importance of DAs for detecting non-indigenous species. Finally, Bregmaceros otoliths are modern, not supporting the previous hypothesis that the taxon is a Pleistocene relict.


2021 ◽  
Author(s):  
Evangelia Besiou ◽  
George Kontakiotis ◽  
Assimina Antonarakou ◽  
Andreas Mulch ◽  
Iuliana Vasiliev

<p>The Late Miocene has been considered one of the most climatically stable periods of the Cenozoic, time span characterized by minor long-term cooling and ice growth. Especially, the Tortonian-Messinian Transition is recognized as a priority for paleoenvironmental reconstruction and climate modelling due to the significant paleoenvironmental changes preceding the Messinian Salinity Crisis (MSC; 5.97-5.33 Ma). Here, we present stable oxygen (δ<sup>18</sup>O) and carbon (δ<sup>13</sup>C) isotopes measured on benthic and planktonic foraminifera from Potamida section (Crete Island, eastern Mediterranean). The δ<sup>18</sup>O results indicate a decoupling between the surface and the bottom water column starting before the Tortonian-Messinian boundary. The difference between planktonic and benthic oxygen isotope signals (Δδ<sup>18</sup>O) further provides an estimate of the degree of water column stratification during that time. The δ<sup>13</sup>C data indicate a generally trend towards lighter values as an excellent illustration of the Late Miocene Carbon Isotope Shift (LMCIS; 7.6-6.6 Ma) due to progressive restriction of the Mediterranean basin, with the exception of the 7.38-7.26 Ma time interval where significantly heavier δ<sup>13</sup>C values are documented in both records. Such changes in carbon cycle seem to be most pronounced in the planktonic foraminiferal record (surface waters) through a 6-cycle development indicative of a cyclic productivity pattern during the latest Tortonian. The entire record is substantiated by sea surface temperature (SST) estimates based on TEX<sub>86</sub> biomarker based proxy. The reconstructed SST record shows that a warm phase characterized the late Tortonian sea surface (~27⁰C), time followed by a strong, steady cooling starting with earliest Messinian, when the SSTs dropped to values as low as 20⁰C. The outcome of the combined stable isotope and biomarker based SST data hint to increased salinity in the surface waters already before the Messinian, while at the Tortonian-Messinian Transition, the conditions in the surface waters changed towards cooler (~24⁰C) and normal salinity conditions.</p>


2014 ◽  
Vol 635 ◽  
pp. 59-79 ◽  
Author(s):  
A.E. Aksu ◽  
J. Hall ◽  
C. Yaltırak ◽  
E. Çınar ◽  
M. Küçük ◽  
...  

2020 ◽  
Vol 100 (3) ◽  
pp. 773-792 ◽  
Author(s):  
Konstantina Agiadi ◽  
Christina Giamali ◽  
Angela Girone ◽  
Pierre Moissette ◽  
Efterpi Koskeridou ◽  
...  

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