Surface sediment around the Jabuka Islet and the Jabuka Shoal: Evidence of Miocene tectonics in the Central Adriatic Sea

2015 ◽  
Vol 359 ◽  
pp. 120-133 ◽  
Author(s):  
Kristina Pikelj ◽  
Morana Hernitz-Kučenjak ◽  
Šimun Aščić ◽  
Mladen Juračić
2021 ◽  
Vol 9 (8) ◽  
pp. 841
Author(s):  
Neda Bošković ◽  
Danijela Joksimović ◽  
Milica Peković ◽  
Ana Perošević-Bajčeta ◽  
Oliver Bajt

Considering that microplastics are widespread in the marine environment, in this study we evaluated the presence, identify distribution, abundance, shape type, and color of microplastics in surface sediment along the Montenegrin coast, on the Adriatic Sea. These preliminary results provide the first published record of microplastics found in the surface sediment of this area and highlight the importance of microplastics as a component of marine debris. We documented the presence of microplastics at all sampling locations. The identification of polymer types was performed using Fourier-transform infrared (FTIR) spectroscopy, whereby the presence of three polymer types became evident: polypropylene (54.5%), polyethylene (9.7%), and acrylate copolymer (2.0%). Another 22.2% of particles were unidentified polymers, and the remaining 11.5% were non-synthetic materials. The most common shape type of microplastics was filaments (55.5%), followed by granules (26.3%), fragments (14.9%), and films (3.3%). The dominant colors of microplastics followed the order: blue > yellow > red > clear > black > green > blue-white > white. The average abundance of microplastics in all sampling locations was 609 pieces of microplastic/kg of dry sediment. Compared with other studies, the surface sediment of the Montenegrin coast is moderately to highly polluted with microplastics, depending on the examined location.


2016 ◽  
Vol 23 (12) ◽  
pp. 11777-11789 ◽  
Author(s):  
Bojan Tanaskovski ◽  
Mihajlo Jović ◽  
Ljiljana Miličić ◽  
Lato Pezo ◽  
Milica Mandić ◽  
...  

2003 ◽  
Vol 107 ◽  
pp. 879-882 ◽  
Author(s):  
S. Miserocchi ◽  
M. Frignani ◽  
L. Langone ◽  
S. Albertazzi

2014 ◽  
Vol 509 ◽  
pp. 193-202 ◽  
Author(s):  
P Kružić ◽  
L Lipej ◽  
B Mavrič ◽  
P Rodić

2017 ◽  
Vol 566 ◽  
pp. 31-48 ◽  
Author(s):  
A Santelli ◽  
I Cvitković ◽  
M Despalatović ◽  
G Fabi ◽  
F Grati ◽  
...  
Keyword(s):  

2010 ◽  
Vol 2 (1) ◽  
Author(s):  
Suhartati M. Natsir

Foraminifera are generally live in sea water with various sizes. These organisms consist of planktonic and benthic foraminifera. Geological activity on plutonic and volcanic with vomiting magma is transpiring on, and then affects sedimentation and foraminiferal abundance of Ambon Bay. The study was determined to study the abundance and distribution of foraminifera based on the sediment characteristic of Ambon Bay. Sample collected in 2007 of Ambon Bay showed that only 29 samples of 50 samples containing foraminifera. The collected sediments have 86 species of foraminifera, consisting 61 species of benthic foraminifera and 25 species of planktonic foraminifera. The dominant benthic foraminifera in the surface sediment of Ambon bay were Amphistegina lessonii, Ammoniabeccarii,Elphidium craticulatum,Operculina ammonoides and Quinqueloculina parkery. The planktonic foraminifera that were frequently collected from the bay were Globorotalia tumida, Globoquadrina pseudofoliata, Globigerinoides pseudofoliata, Globigerinoides cyclostomus dan Pulleniatina finalis. Generally, the species dwelled as abundant on substrate sand, whereas the areas within substrate mud have no foraminifera lie on them. Keywords: Foraminifera, Abundance, Sediment, Ambon Bay


1984 ◽  
Vol 19 (1) ◽  
pp. 27-36 ◽  
Author(s):  
Alena Mudroch

Abstract Surface sediment samples obtained at the offshore and nearshore area of Lake Erie were separated into eight different size fractions ranging from <2 µm to 250 µm. The concentration of major elements (Si, Al, Ca, Mg, K, Na, Fe, Mn and P), metals (Zn, Cu, Cr, Ni, V, Co and Pb) and organic matter was determined together with the mineralogical composition and morphology of the particles in each size fraction. The distribution of the metals in the offshore sediment was bimodal with the majority of the metals divided between the 63 to 250 um size fraction which also contained the highest concentration of organic matter (about 20%) and the <4 µm fraction containing up to 60% of clay minerals. However, the metals in the nearshore sediment were associated mainly with the clay minerals.


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