Comparison of the structures of hybrid κ-/β-carrageenans extracted from Furcellaria lumbricalis and Tichocarpus crinitus

2012 ◽  
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pp. 31-36 ◽  
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Anna Barabanova ◽  
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Irina Yermak ◽  
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Author(s):  
Rando Tuvikene ◽  
Kalle Truus ◽  
Marju Robal ◽  
Olga Volobujeva ◽  
Enn Mellikov ◽  
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2020 ◽  
Vol 52 ◽  
pp. 102058
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Mihkel Saluri ◽  
Margit Kaldmäe ◽  
Mihkel Rospu ◽  
Hannes Sirkel ◽  
Tiina Paalme ◽  
...  

1990 ◽  
Vol 206 (2) ◽  
pp. 367-372 ◽  
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Svein H. Knutsen ◽  
David E. Myslabodski ◽  
Hans Grasdalen

2015 ◽  
Vol 28 (1) ◽  
pp. 545-553 ◽  
Author(s):  
Alexandra A. Kalitnik ◽  
Stanislav D. Anastyuk ◽  
Ekaterina V. Sokolova ◽  
Anna O. Kravchenko ◽  
Eleonora I. Khasina ◽  
...  

Author(s):  
Irina Chubarenko ◽  
Irina Chubarenko ◽  
Margarita Bagaeva ◽  
Margarita Bagaeva

The problem of microplastic pollution is of increasing concern. Behaviour of microplastic particles (0.5 mm < L < 5mm in the largest dimension) in marine environment is difficult to predict, and no field observations are available up to now. Baltic amber (succinite), with its density of about 1.05-1.09 g/cm3, fits the range of densities of slightly negatively buoyant plastics: polyamide, polystyrene, acrylic, etc. Baltic citizens have observed amber migrations for centuries, and the collected information may shed some light onto general features of microplastic particles behaviour. Events of “amber washing-out” at the sea shore of the Sambian peninsula (Kaliningrad oblast, Russia) typically take place in autumn-winter time. Experience of divers indicates that amber is washed out from the depths as deep as 15 m. Massive presence in amber-containing debris of the red algae Furcellaria lumbricalis, dominating in the sea at depths of 6-15 m, proves this fact. From oceanographic viewpoint, important for the “amber washing-out” are: strong and long-lasting storm, phase of wind decrease or direction change, developed long surface waves, shore exposure to wind. Analysis of characteristic wave lengths after long storms, dimensions of their surf zone, and changes in underwater bottom profile is carried out. Conclusion is that slightly negatively buoyant microplastic particles should migrate for a long time between beaches and underwater slopes until they are broken into small enough pieces that can be transported by currents to deeper area and deposited out of reach of stormy waves.


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