Dynamic Properties of Some Eastern Mediterranean Marine Sediments

2013 ◽  
Vol 36 (4) ◽  
pp. 20120128 ◽  
Author(s):  
Ronald Chaney
2019 ◽  
Vol 142 ◽  
pp. 206-215 ◽  
Author(s):  
R.A. González-Fuenzalida ◽  
R. Herráez-Hernández ◽  
J. Verdú-Andrés ◽  
A. Bouzas-Blanco ◽  
A. Seco-Torrecillas ◽  
...  

2008 ◽  
Vol 254 (3-4) ◽  
pp. 224-229 ◽  
Author(s):  
Juan C. Larrasoaña ◽  
Andrew P. Roberts ◽  
Eelco J. Rohling

1986 ◽  
pp. 501-510 ◽  
Author(s):  
A. M. Davis ◽  
J. D. Bennell

2016 ◽  
Vol 47 (1) ◽  
pp. 112 ◽  
Author(s):  
H. Drinia ◽  
A. Antonarakou ◽  
S. Mihalakopoulos ◽  
E. Tsiolakis

The main objective of this work is to investigate the climatic influence on the sedimentation during mid to late Pliocene in Cyprus island. For this reason, a section located in Pissouri sub-basin, southern Cyprus, was chosen to be studied. The section comprises a nearly uninterrupted succession of marine sediments, dominated by grey marls, which are cyclically alternating with yellowish silty marls. The identification of age diagnostic planktonic foraminifera suggests a mid to upper Pliocene age. The calculated faunal parameters document cyclic fluctuations consistent with shifts in such climate belts. A good age resolution of the cycles and an indication of sedimentation rate would be required in order to connect cyclicity to orbital perturbations.


2019 ◽  
Vol 20 (4) ◽  
pp. 736
Author(s):  
VERA N. DE RUIJTER ◽  
ANASTASIA MILOU ◽  
VALENTINA COSTA

Microplastics (MPs) are becoming ubiquitous in the marine environment and shallow marine sediments are one of the major sinks for MPs. In order to improve the knowledge about the environmental fate of MPs in the Aegean Sea shallow sediments, the occurrence and spatial distribution of MPs in Samos Island (Greece) was investigated for the first time, along a land-sea transect. The highest concentration of MPs was recorded at the Beach (37.2 ± 6.9 MPs/Kg DW), while the lowest concentration was recorded in the Intertidal zone (1.1 ± 0.9 MPs/Kg DW). In relation to the different shapes, Fragments and Pellets were more abundant on the Beach, while Fibers were more abundant in the Intertidal zone and barely any Sheets were found along the transect, suggesting a distribution probably governed not only by size but also morphology and perhaps chemical composition. A higher accumulation of particles was recorded in the first 10 cm of sediments, in comparison to the deepest 5 cm, indicating an increase of microplastics in the shallow marine sediments.


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